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		<title>Pantoja 2017b - Revision history</title>
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		<updated>2026-04-09T20:18:12Z</updated>
		<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70111&amp;oldid=prev</id>
		<title>Zarate: Zarate moved page Review Pantoja 2017b to Pantoja 2017b</title>
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				<updated>2017-11-22T15:34:25Z</updated>
		
		<summary type="html">&lt;p&gt;Zarate moved page &lt;a href=&quot;/public/Review_Pantoja_2017b&quot; class=&quot;mw-redirect&quot; title=&quot;Review Pantoja 2017b&quot;&gt;Review Pantoja 2017b&lt;/a&gt; to &lt;a href=&quot;/public/Pantoja_2017b&quot; title=&quot;Pantoja 2017b&quot;&gt;Pantoja 2017b&lt;/a&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 15:34, 22 November 2017&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan='2' style='text-align: center;' lang='en'&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
&lt;/td&gt;&lt;/tr&gt;&lt;/table&gt;</summary>
		<author><name>Zarate</name></author>	</entry>

	<entry>
		<id>https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70110&amp;oldid=prev</id>
		<title>Zarate at 15:33, 22 November 2017</title>
		<link rel="alternate" type="text/html" href="https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70110&amp;oldid=prev"/>
				<updated>2017-11-22T15:33:57Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;tr style='vertical-align: top;' lang='en'&gt;
				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 15:33, 22 November 2017&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l352&quot; &gt;Line 352:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 352:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[1] R. Álvarez, &amp;quot;Submarine topography and faulting in Bahía de Banderas, Mexico&amp;quot;. Geofísica Internacional, Vol. 46, Num. 2, pp. 93-116, (2007). &amp;lt;br /&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[1] R. Álvarez, &amp;quot;Submarine topography and faulting in Bahía de Banderas, Mexico&amp;quot;. Geofísica Internacional, Vol. 46, Num. 2, pp. 93-116, (2007). &amp;lt;br /&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[2] CNA-SEMARNAT, &amp;quot;Régimen de almacenamientos hasta 1999. Banco Nacional de Datos de Aguas Superficiales&amp;quot;. En CD-ROM, (1999). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[3] R. K. Cowen and S. Sponaugle, &amp;quot;Larval Dispersal and Marine Population Connectivity&amp;quot;. Annual Review of Marine Science. 1:443-466, (2002).&amp;#160; [4] Delft3DFLOW, &amp;quot;Simulation of multidimensional hydrodynamic flows and transport phenomena, including sediments&amp;quot;. User Manual, Deltares, The Netherlands. http://oss.deltares.nl/, (2011). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[5] C. A. González D, &amp;quot;La geomática aplicada del estudio de la dinámica superficial de detritos suspendidos en la Bahía de Banderas&amp;quot;. Tesis Maestría en Ciencias en Hidrometeorología. Guadalajara, Jalisco, México, (2017). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[6] AE. Filonov, &amp;quot;Internal tide and tsunami waves in the continental shelf of the Mexican western coast&amp;quot;. Oceanogr. East. Pacific. 1:31–45, (2000). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[7] AE, Filonov y KV. Konyaev,&amp;#160; &amp;quot;Nonlinear internal waves near Mexico’s central Pacific coast&amp;quot;. In: Velasco-Fuentes OU, Scheinbaum J, Ochoa J (eds.), Nonlinear Processes in Geophysical Fluid Dynamics. Kluwer Academic Publishers, Netherlands,&amp;#160; 377–386, (2003). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[8] J. P. Finley, &amp;quot;Tornado predictions. Amer. Meteor&amp;quot;. J., 1, 85-88, (1884). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[9] W. S. Kessler, &amp;quot;The circulation of the eastern tropical Pacific: A review. Progress in Oceanography&amp;quot;. 69(2-4):181–217., (2006).&amp;#160; [10] J. A. Kurczyn, E. Beier, M. F. Lavín,&amp;#160; y A. Chaigneau, &amp;quot;Mesoscale eddies in the northeastern Pacific tropical-subtropical transition zone: Statistical characterization from satellite altimetry&amp;quot;. Journal of Geophysical Research. 117(C10): C10021, (2012). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[11]&amp;#160; M. G. León, &amp;quot;Análisis comparativo de los patrones de conectividad genética de especies arrecifales del Pacífico mexicano&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CICESE, Ensenada, Baja California, México, (2015). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;&amp;#160; &lt;/del&gt;[12] S. G. Marinone, &amp;quot;On the three-dimensional numerical modeling of the deep circulation around Ángel de la Guarda Island in the Gulf of California&amp;quot;. Estuarine, Coastal and Shelf Science. 80:430–434, (2008). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[13] S. G. Marinone, &amp;quot;Seasonal Surface connectivity in the Gulf of California&amp;quot;. Estuarine Coastal and Shelf Science, 100:133-141., (2012). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[14] G. Martínez Flores, E. H. Nava Sánchez y O. Zaitsev, &amp;quot;Teledetección de plumas de material suspendido influenciadas por escorrentía en el Sur del Golfo de California&amp;quot;. CICIMAR Oceánides. 26(1): 1-8, (2011). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[15] S. Mitarai, D. A. Siegel, J. R. Watson, C. Dong&amp;#160; and J. C. McWilliams, &amp;quot;Quantifying connectivity in the coastal ocean with application to the Southern California Bight&amp;quot;. Journal Of Geophysical Research. 114(5):110-115, (2009). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;&amp;#160; &lt;/del&gt;[16] M. M. Nishimoto y&amp;#160; L. Washburn,&amp;#160; &amp;quot;Patterns of coastal eddy circulation and abundance of pelagic juvenile fish in the Santa Barbara Channel, California, USA&amp;quot;. Marine Ecology Progress Series, 241:183-199, (2002). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[17] D. A. Pantoja, &amp;quot;Modelación Numérica de la Circulación General del Cañón Submarino en Bahía de Banderas&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CISECE. Ensenada, Baja California, México., (2013). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;&amp;#160; &lt;/del&gt;[18] M. Peguero Icaza, L. Sánchez Velasco, M. F. Lavín,&amp;#160; y&amp;#160; S. G. Marinone,&amp;#160; &amp;quot;Larval fish assemblages, environment and circulation in a semienclosed sea (Gulf of California, México)&amp;quot;. Estuarine Coastal and Shelf Science. 79:277–288, (2008). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;&amp;#160; &lt;/del&gt;[19] L. Plata y A. Filonov, &amp;quot;Marea interna en la parte NorOeste de la Bahía de Banderas, México&amp;quot;. Ciencias Marinas. Universidad Autónoma de Baja California. Ensenada, México. 33(2):197-215, (2007). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[20] J. A. Proehl, D. R. Lynch, D. J. McGillicuddy y J. R. Ledwell, &amp;quot;Modeling turbulent dispersion on the North Flank of Georges Bank using Lagrangian particle methods&amp;quot;. Continental Shelf Research, 25:875–900, (2005). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[21] J. M. Rodriguez, S. Hernández León y E. D. Barton, &amp;quot;Mesoscale distribution of fish larvae in relation to an upwelling filament off Northwest Africa&amp;quot;. Deep Sea Research I, 46:1969–1984, (1999). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[22] J. M. Rodriguez, E. D. Barton, S. Hernández León y&amp;#160; J. Aristegui, &amp;quot;The influence of mesoscale physical processes on the larval fish community in the Canaries CTZ&amp;quot;, in summer. Progress in Oceanography, 62:171-188, (2004). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[23]&amp;#160; M. Santiago, &amp;quot;La conectividad tridimensional en el Golfo de California, a partir de un modelo numérico&amp;quot;. Tesis presentada en opción al grado de Maestro en Ciencias. Ensenada, Baja California, México, (2013). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[24] SECTUR, &amp;quot;Secretaria de Turismo&amp;quot;. Obtenido del sitio Web:&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[2] CNA-SEMARNAT, &amp;quot;Régimen de almacenamientos hasta 1999. Banco Nacional de Datos de Aguas Superficiales&amp;quot;. En CD-ROM, (1999). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[3] R. K. Cowen and S. Sponaugle, &amp;quot;Larval Dispersal and Marine Population Connectivity&amp;quot;. Annual Review of Marine Science. 1:443-466, (2002).&amp;#160; &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[4] Delft3DFLOW, &amp;quot;Simulation of multidimensional hydrodynamic flows and transport phenomena, including sediments&amp;quot;. User Manual, Deltares, The Netherlands. http://oss.deltares.nl/, (2011). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[5] C. A. González D, &amp;quot;La geomática aplicada del estudio de la dinámica superficial de detritos suspendidos en la Bahía de Banderas&amp;quot;. Tesis Maestría en Ciencias en Hidrometeorología. Guadalajara, Jalisco, México, (2017). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[6] AE. Filonov, &amp;quot;Internal tide and tsunami waves in the continental shelf of the Mexican western coast&amp;quot;. Oceanogr. East. Pacific. 1:31–45, (2000). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[7] AE, Filonov y KV. Konyaev,&amp;#160; &amp;quot;Nonlinear internal waves near Mexico’s central Pacific coast&amp;quot;. In: Velasco-Fuentes OU, Scheinbaum J, Ochoa J (eds.), Nonlinear Processes in Geophysical Fluid Dynamics. Kluwer Academic Publishers, Netherlands,&amp;#160; 377–386, (2003). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[8] J. P. Finley, &amp;quot;Tornado predictions. Amer. Meteor&amp;quot;. J., 1, 85-88, (1884). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[9] W. S. Kessler, &amp;quot;The circulation of the eastern tropical Pacific: A review. Progress in Oceanography&amp;quot;. 69(2-4):181–217., (2006).&amp;#160; [10] J. A. Kurczyn, E. Beier, M. F. Lavín,&amp;#160; y A. Chaigneau, &amp;quot;Mesoscale eddies in the northeastern Pacific tropical-subtropical transition zone: Statistical characterization from satellite altimetry&amp;quot;. Journal of Geophysical Research. 117(C10): C10021, (2012).&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[11]&amp;#160; M. G. León, &amp;quot;Análisis comparativo de los patrones de conectividad genética de especies arrecifales del Pacífico mexicano&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CICESE, Ensenada, Baja California, México, (2015). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; &amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[12] S. G. Marinone, &amp;quot;On the three-dimensional numerical modeling of the deep circulation around Ángel de la Guarda Island in the Gulf of California&amp;quot;. Estuarine, Coastal and Shelf Science. 80:430–434, (2008). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[13] S. G. Marinone, &amp;quot;Seasonal Surface connectivity in the Gulf of California&amp;quot;. Estuarine Coastal and Shelf Science, 100:133-141., (2012). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[14] G. Martínez Flores, E. H. Nava Sánchez y O. Zaitsev, &amp;quot;Teledetección de plumas de material suspendido influenciadas por escorrentía en el Sur del Golfo de California&amp;quot;. CICIMAR Oceánides. 26(1): 1-8, (2011). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[15] S. Mitarai, D. A. Siegel, J. R. Watson, C. Dong&amp;#160; and J. C. McWilliams, &amp;quot;Quantifying connectivity in the coastal ocean with application to the Southern California Bight&amp;quot;. Journal Of Geophysical Research. 114(5):110-115, (2009). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; &amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[16] M. M. Nishimoto y&amp;#160; L. Washburn,&amp;#160; &amp;quot;Patterns of coastal eddy circulation and abundance of pelagic juvenile fish in the Santa Barbara Channel, California, USA&amp;quot;. Marine Ecology Progress Series, 241:183-199, (2002). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[17] D. A. Pantoja, &amp;quot;Modelación Numérica de la Circulación General del Cañón Submarino en Bahía de Banderas&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CISECE. Ensenada, Baja California, México., (2013). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; &amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[18] M. Peguero Icaza, L. Sánchez Velasco, M. F. Lavín,&amp;#160; y&amp;#160; S. G. Marinone,&amp;#160; &amp;quot;Larval fish assemblages, environment and circulation in a semienclosed sea (Gulf of California, México)&amp;quot;. Estuarine Coastal and Shelf Science. 79:277–288, (2008). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; &amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[19] L. Plata y A. Filonov, &amp;quot;Marea interna en la parte NorOeste de la Bahía de Banderas, México&amp;quot;. Ciencias Marinas. Universidad Autónoma de Baja California. Ensenada, México. 33(2):197-215, (2007). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[20] J. A. Proehl, D. R. Lynch, D. J. McGillicuddy y J. R. Ledwell, &amp;quot;Modeling turbulent dispersion on the North Flank of Georges Bank using Lagrangian particle methods&amp;quot;. Continental Shelf Research, 25:875–900, (2005). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[21] J. M. Rodriguez, S. Hernández León y E. D. Barton, &amp;quot;Mesoscale distribution of fish larvae in relation to an upwelling filament off Northwest Africa&amp;quot;. Deep Sea Research I, 46:1969–1984, (1999). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[22] J. M. Rodriguez, E. D. Barton, S. Hernández León y&amp;#160; J. Aristegui, &amp;quot;The influence of mesoscale physical processes on the larval fish community in the Canaries CTZ&amp;quot;, in summer. Progress in Oceanography, 62:171-188, (2004). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[23]&amp;#160; M. Santiago, &amp;quot;La conectividad tridimensional en el Golfo de California, a partir de un modelo numérico&amp;quot;. Tesis presentada en opción al grado de Maestro en Ciencias. Ensenada, Baja California, México, (2013). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[24] SECTUR, &amp;quot;Secretaria de Turismo&amp;quot;. Obtenido del sitio Web:&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;www.sectur.gob.mx/work/models/sectur/Resource/&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;www.sectur.gob.mx/work/models/sectur/Resource/&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;5975/1/images/Agenda21.pdf, (2011).&amp;#160;  &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;5975/1/images/Agenda21.pdf, (2011).&amp;#160;  [25] D. Wilks, &amp;quot;Statistical Methods in the Atmospheric Sciences&amp;quot;, 2nd ed.; Academic Press: San Diego, CA, USA, p. 627, (2006).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[25] D. Wilks, &amp;quot;Statistical Methods in the Atmospheric Sciences&amp;quot;, 2nd ed.; Academic Press: San Diego, CA, USA, p. 627, (2006).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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		<author><name>Zarate</name></author>	</entry>

	<entry>
		<id>https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70109&amp;oldid=prev</id>
		<title>Zarate at 15:31, 22 November 2017</title>
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				<updated>2017-11-22T15:31:44Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
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				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 15:31, 22 November 2017&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l351&quot; &gt;Line 351:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 351:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Referencias==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Referencias==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[1] R. Álvarez, &amp;quot;Submarine topography and faulting in Bahía de Banderas, Mexico&amp;quot;. Geofísica Internacional, Vol. 46, Num. 2, pp. 93-116, (2007). &amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[1] R. Álvarez, &amp;quot;Submarine topography and faulting in Bahía de Banderas, Mexico&amp;quot;. Geofísica Internacional, Vol. 46, Num. 2, pp. 93-116, (2007). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br /&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[2] CNA-SEMARNAT, &amp;quot;Régimen de almacenamientos hasta 1999. Banco Nacional de Datos de Aguas Superficiales&amp;quot;. En CD-ROM, (1999).&amp;#160; [3] R. K. Cowen and S. Sponaugle, &amp;quot;Larval Dispersal and Marine Population Connectivity&amp;quot;. Annual Review of Marine Science. 1:443-466, (2002).&amp;#160; [4] Delft3DFLOW, &amp;quot;Simulation of multidimensional hydrodynamic flows and transport phenomena, including sediments&amp;quot;. User Manual, Deltares, The Netherlands. http://oss.deltares.nl/, (2011).&amp;#160; [5] C. A. González D, &amp;quot;La geomática aplicada del estudio de la dinámica superficial de detritos suspendidos en la Bahía de Banderas&amp;quot;. Tesis Maestría en Ciencias en Hidrometeorología. Guadalajara, Jalisco, México, (2017).&amp;#160; [6] AE. Filonov, &amp;quot;Internal tide and tsunami waves in the continental shelf of the Mexican western coast&amp;quot;. Oceanogr. East. Pacific. 1:31–45, (2000).&amp;#160; [7] AE, Filonov y KV. Konyaev,&amp;#160; &amp;quot;Nonlinear internal waves near Mexico’s central Pacific coast&amp;quot;. In: Velasco-Fuentes OU, Scheinbaum J, Ochoa J (eds.), Nonlinear Processes in Geophysical Fluid Dynamics. Kluwer Academic Publishers, Netherlands,&amp;#160; 377–386, (2003).&amp;#160; [8] J. P. Finley, &amp;quot;Tornado predictions. Amer. Meteor&amp;quot;. J., 1, 85-88, (1884).&amp;#160; [9] W. S. Kessler, &amp;quot;The circulation of the eastern tropical Pacific: A review. Progress in Oceanography&amp;quot;. 69(2-4):181–217., (2006).&amp;#160; [10] J. A. Kurczyn, E. Beier, M. F. Lavín,&amp;#160; y A. Chaigneau, &amp;quot;Mesoscale eddies in the northeastern Pacific tropical-subtropical transition zone: Statistical characterization from satellite altimetry&amp;quot;. Journal of Geophysical Research. 117(C10): C10021, (2012).&amp;#160; [11]&amp;#160; M. G. León, &amp;quot;Análisis comparativo de los patrones de conectividad genética de especies arrecifales del Pacífico mexicano&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CICESE, Ensenada, Baja California, México, (2015).&amp;#160;  [12] S. G. Marinone, &amp;quot;On the three-dimensional numerical modeling of the deep circulation around Ángel de la Guarda Island in the Gulf of California&amp;quot;. Estuarine, Coastal and Shelf Science. 80:430–434, (2008).&amp;#160; [13] S. G. Marinone, &amp;quot;Seasonal Surface connectivity in the Gulf of California&amp;quot;. Estuarine Coastal and Shelf Science, 100:133-141., (2012).&amp;#160; [14] G. Martínez Flores, E. H. Nava Sánchez y O. Zaitsev, &amp;quot;Teledetección de plumas de material suspendido influenciadas por escorrentía en el Sur del Golfo de California&amp;quot;. CICIMAR Oceánides. 26(1): 1-8, (2011).&amp;#160; [15] S. Mitarai, D. A. Siegel, J. R. Watson, C. Dong&amp;#160; and J. C. McWilliams, &amp;quot;Quantifying connectivity in the coastal ocean with application to the Southern California Bight&amp;quot;. Journal Of Geophysical Research. 114(5):110-115, (2009).&amp;#160;  [16] M. M. Nishimoto y&amp;#160; L. Washburn,&amp;#160; &amp;quot;Patterns of coastal eddy circulation and abundance of pelagic juvenile fish in the Santa Barbara Channel, California, USA&amp;quot;. Marine Ecology Progress Series, 241:183-199, (2002).&amp;#160; [17] D. A. Pantoja, &amp;quot;Modelación Numérica de la Circulación General del Cañón Submarino en Bahía de Banderas&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CISECE. Ensenada, Baja California, México., (2013).&amp;#160;  [18] M. Peguero Icaza, L. Sánchez Velasco, M. F. Lavín,&amp;#160; y&amp;#160; S. G. Marinone,&amp;#160; &amp;quot;Larval fish assemblages, environment and circulation in a semienclosed sea (Gulf of California, México)&amp;quot;. Estuarine Coastal and Shelf Science. 79:277–288, (2008).&amp;#160;  [19] L. Plata y A. Filonov, &amp;quot;Marea interna en la parte NorOeste de la Bahía de Banderas, México&amp;quot;. Ciencias Marinas. Universidad Autónoma de Baja California. Ensenada, México. 33(2):197-215, (2007).&amp;#160; [20] J. A. Proehl, D. R. Lynch, D. J. McGillicuddy y J. R. Ledwell, &amp;quot;Modeling turbulent dispersion on the North Flank of Georges Bank using Lagrangian particle methods&amp;quot;. Continental Shelf Research, 25:875–900, (2005).&amp;#160; [21] J. M. Rodriguez, S. Hernández León y E. D. Barton, &amp;quot;Mesoscale distribution of fish larvae in relation to an upwelling filament off Northwest Africa&amp;quot;. Deep Sea Research I, 46:1969–1984, (1999).&amp;#160; [22] J. M. Rodriguez, E. D. Barton, S. Hernández León y&amp;#160; J. Aristegui, &amp;quot;The influence of mesoscale physical processes on the larval fish community in the Canaries CTZ&amp;quot;, in summer. Progress in Oceanography, 62:171-188, (2004).&amp;#160; [23]&amp;#160; M. Santiago, &amp;quot;La conectividad tridimensional en el Golfo de California, a partir de un modelo numérico&amp;quot;. Tesis presentada en opción al grado de Maestro en Ciencias. Ensenada, Baja California, México, (2013).&amp;#160; [24] SECTUR, &amp;quot;Secretaria de Turismo&amp;quot;. Obtenido del sitio Web:&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[2] CNA-SEMARNAT, &amp;quot;Régimen de almacenamientos hasta 1999. Banco Nacional de Datos de Aguas Superficiales&amp;quot;. En CD-ROM, (1999).&amp;#160; [3] R. K. Cowen and S. Sponaugle, &amp;quot;Larval Dispersal and Marine Population Connectivity&amp;quot;. Annual Review of Marine Science. 1:443-466, (2002).&amp;#160; [4] Delft3DFLOW, &amp;quot;Simulation of multidimensional hydrodynamic flows and transport phenomena, including sediments&amp;quot;. User Manual, Deltares, The Netherlands. http://oss.deltares.nl/, (2011).&amp;#160; [5] C. A. González D, &amp;quot;La geomática aplicada del estudio de la dinámica superficial de detritos suspendidos en la Bahía de Banderas&amp;quot;. Tesis Maestría en Ciencias en Hidrometeorología. Guadalajara, Jalisco, México, (2017).&amp;#160; [6] AE. Filonov, &amp;quot;Internal tide and tsunami waves in the continental shelf of the Mexican western coast&amp;quot;. Oceanogr. East. Pacific. 1:31–45, (2000).&amp;#160; [7] AE, Filonov y KV. Konyaev,&amp;#160; &amp;quot;Nonlinear internal waves near Mexico’s central Pacific coast&amp;quot;. In: Velasco-Fuentes OU, Scheinbaum J, Ochoa J (eds.), Nonlinear Processes in Geophysical Fluid Dynamics. Kluwer Academic Publishers, Netherlands,&amp;#160; 377–386, (2003).&amp;#160; [8] J. P. Finley, &amp;quot;Tornado predictions. Amer. Meteor&amp;quot;. J., 1, 85-88, (1884).&amp;#160; [9] W. S. Kessler, &amp;quot;The circulation of the eastern tropical Pacific: A review. Progress in Oceanography&amp;quot;. 69(2-4):181–217., (2006).&amp;#160; [10] J. A. Kurczyn, E. Beier, M. F. Lavín,&amp;#160; y A. Chaigneau, &amp;quot;Mesoscale eddies in the northeastern Pacific tropical-subtropical transition zone: Statistical characterization from satellite altimetry&amp;quot;. Journal of Geophysical Research. 117(C10): C10021, (2012).&amp;#160; [11]&amp;#160; M. G. León, &amp;quot;Análisis comparativo de los patrones de conectividad genética de especies arrecifales del Pacífico mexicano&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CICESE, Ensenada, Baja California, México, (2015).&amp;#160;  [12] S. G. Marinone, &amp;quot;On the three-dimensional numerical modeling of the deep circulation around Ángel de la Guarda Island in the Gulf of California&amp;quot;. Estuarine, Coastal and Shelf Science. 80:430–434, (2008).&amp;#160; [13] S. G. Marinone, &amp;quot;Seasonal Surface connectivity in the Gulf of California&amp;quot;. Estuarine Coastal and Shelf Science, 100:133-141., (2012).&amp;#160; [14] G. Martínez Flores, E. H. Nava Sánchez y O. Zaitsev, &amp;quot;Teledetección de plumas de material suspendido influenciadas por escorrentía en el Sur del Golfo de California&amp;quot;. CICIMAR Oceánides. 26(1): 1-8, (2011).&amp;#160; [15] S. Mitarai, D. A. Siegel, J. R. Watson, C. Dong&amp;#160; and J. C. McWilliams, &amp;quot;Quantifying connectivity in the coastal ocean with application to the Southern California Bight&amp;quot;. Journal Of Geophysical Research. 114(5):110-115, (2009).&amp;#160;  [16] M. M. Nishimoto y&amp;#160; L. Washburn,&amp;#160; &amp;quot;Patterns of coastal eddy circulation and abundance of pelagic juvenile fish in the Santa Barbara Channel, California, USA&amp;quot;. Marine Ecology Progress Series, 241:183-199, (2002).&amp;#160; [17] D. A. Pantoja, &amp;quot;Modelación Numérica de la Circulación General del Cañón Submarino en Bahía de Banderas&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CISECE. Ensenada, Baja California, México., (2013).&amp;#160;  [18] M. Peguero Icaza, L. Sánchez Velasco, M. F. Lavín,&amp;#160; y&amp;#160; S. G. Marinone,&amp;#160; &amp;quot;Larval fish assemblages, environment and circulation in a semienclosed sea (Gulf of California, México)&amp;quot;. Estuarine Coastal and Shelf Science. 79:277–288, (2008).&amp;#160;  [19] L. Plata y A. Filonov, &amp;quot;Marea interna en la parte NorOeste de la Bahía de Banderas, México&amp;quot;. Ciencias Marinas. Universidad Autónoma de Baja California. Ensenada, México. 33(2):197-215, (2007).&amp;#160; [20] J. A. Proehl, D. R. Lynch, D. J. McGillicuddy y J. R. Ledwell, &amp;quot;Modeling turbulent dispersion on the North Flank of Georges Bank using Lagrangian particle methods&amp;quot;. Continental Shelf Research, 25:875–900, (2005).&amp;#160; [21] J. M. Rodriguez, S. Hernández León y E. D. Barton, &amp;quot;Mesoscale distribution of fish larvae in relation to an upwelling filament off Northwest Africa&amp;quot;. Deep Sea Research I, 46:1969–1984, (1999).&amp;#160; [22] J. M. Rodriguez, E. D. Barton, S. Hernández León y&amp;#160; J. Aristegui, &amp;quot;The influence of mesoscale physical processes on the larval fish community in the Canaries CTZ&amp;quot;, in summer. Progress in Oceanography, 62:171-188, (2004).&amp;#160; [23]&amp;#160; M. Santiago, &amp;quot;La conectividad tridimensional en el Golfo de California, a partir de un modelo numérico&amp;quot;. Tesis presentada en opción al grado de Maestro en Ciencias. Ensenada, Baja California, México, (2013).&amp;#160; [24] SECTUR, &amp;quot;Secretaria de Turismo&amp;quot;. Obtenido del sitio Web:&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Zarate</name></author>	</entry>

	<entry>
		<id>https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70108&amp;oldid=prev</id>
		<title>Zarate at 15:30, 22 November 2017</title>
		<link rel="alternate" type="text/html" href="https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70108&amp;oldid=prev"/>
				<updated>2017-11-22T15:30:23Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class='diff-marker' /&gt;
				&lt;col class='diff-content' /&gt;
				&lt;col class='diff-marker' /&gt;
				&lt;col class='diff-content' /&gt;
				&lt;tr style='vertical-align: top;' lang='en'&gt;
				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 15:30, 22 November 2017&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l352&quot; &gt;Line 352:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 352:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[1] R. Álvarez, &amp;quot;Submarine topography and faulting in Bahía de Banderas, Mexico&amp;quot;. Geofísica Internacional, Vol. 46, Num. 2, pp. 93-116, (2007). &amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[1] R. Álvarez, &amp;quot;Submarine topography and faulting in Bahía de Banderas, Mexico&amp;quot;. Geofísica Internacional, Vol. 46, Num. 2, pp. 93-116, (2007). &amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[2] CNA-SEMARNAT, &amp;quot;Régimen de almacenamientos hasta 1999. Banco Nacional de Datos de Aguas Superficiales&amp;quot;. En CD-ROM, (1999).&amp;#160; [3] R. K. Cowen and S. Sponaugle, &amp;quot;Larval Dispersal and Marine Population Connectivity&amp;quot;. Annual Review of Marine Science. 1:443-466, (2002).&amp;#160; [4] Delft3DFLOW, &amp;quot;Simulation of multidimensional hydrodynamic flows and transport phenomena, including sediments&amp;quot;. User Manual, Deltares, The Netherlands. http://oss.deltares.nl/, (2011).&amp;#160; [5] C. A. González D, &amp;quot;La geomática aplicada del estudio de la dinámica superficial de detritos suspendidos en la Bahía de Banderas&amp;quot;. Tesis Maestría en Ciencias en Hidrometeorología. Guadalajara, Jalisco, México, (2017).&amp;#160; [6] AE. Filonov, &amp;quot;Internal tide and tsunami waves in the continental shelf of the Mexican western coast&amp;quot;. Oceanogr. East. Pacific. 1:31–45, (2000).&amp;#160; [7] AE, Filonov y KV. Konyaev,&amp;#160; &amp;quot;Nonlinear internal waves near Mexico’s central Pacific coast&amp;quot;. In: Velasco-Fuentes OU, Scheinbaum J, Ochoa J (eds.), Nonlinear Processes in Geophysical Fluid Dynamics. Kluwer Academic Publishers, Netherlands,&amp;#160; 377–386, (2003).&amp;#160; [8] J. P. Finley, &amp;quot;Tornado predictions. Amer. Meteor&amp;quot;. J., 1, 85-88, (1884).&amp;#160; [9] W. S. Kessler, &amp;quot;The circulation of the eastern tropical Pacific: A review. Progress in Oceanography&amp;quot;. 69(2-4):181–217., (2006).&amp;#160; [10] J. A. Kurczyn, E. Beier, M. F. Lavín,&amp;#160; y A. Chaigneau, &amp;quot;Mesoscale eddies in the northeastern Pacific tropical-subtropical transition zone: Statistical characterization from satellite altimetry&amp;quot;. Journal of Geophysical Research. 117(C10): C10021, (2012).&amp;#160; [11]&amp;#160; M. G. León, &amp;quot;Análisis comparativo de los patrones de conectividad genética de especies arrecifales del Pacífico mexicano&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CICESE, Ensenada, Baja California, México, (2015).&amp;#160;  [12] S. G. Marinone, &amp;quot;On the three-dimensional numerical modeling of the deep circulation around Ángel de la Guarda Island in the Gulf of California&amp;quot;. Estuarine, Coastal and Shelf Science. 80:430–434, (2008).&amp;#160; [13] S. G. Marinone, &amp;quot;Seasonal Surface connectivity in the Gulf of California&amp;quot;. Estuarine Coastal and Shelf Science, 100:133-141., (2012).&amp;#160; [14] G. Martínez Flores, E. H. Nava Sánchez y O. Zaitsev, &amp;quot;Teledetección de plumas de material suspendido influenciadas por escorrentía en el Sur del Golfo de California&amp;quot;. CICIMAR Oceánides. 26(1): 1-8, (2011).&amp;#160; [15] S. Mitarai, D. A. Siegel, J. R. Watson, C. Dong&amp;#160; and J. C. McWilliams, &amp;quot;Quantifying connectivity in the coastal ocean with application to the Southern California Bight&amp;quot;. Journal Of Geophysical Research. 114(5):110-115, (2009).&amp;#160;  [16] M. M. Nishimoto y&amp;#160; L. Washburn,&amp;#160; &amp;quot;Patterns of coastal eddy circulation and abundance of pelagic juvenile fish in the Santa Barbara Channel, California, USA&amp;quot;. Marine Ecology Progress Series, 241:183-199, (2002).&amp;#160; [17] D. A. Pantoja, &amp;quot;Modelación Numérica de la Circulación General del Cañón Submarino en Bahía de Banderas&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CISECE. Ensenada, Baja California, México., (2013).&amp;#160;  [18] M. Peguero Icaza, L. Sánchez Velasco, M. F. Lavín,&amp;#160; y&amp;#160; S. G. Marinone,&amp;#160; &amp;quot;Larval fish assemblages, environment and circulation in a semienclosed sea (Gulf of California, México)&amp;quot;. Estuarine Coastal and Shelf Science. 79:277–288, (2008).&amp;#160;  [19] L. Plata y A. Filonov, &amp;quot;Marea interna en la parte NorOeste de la Bahía de Banderas, México&amp;quot;. Ciencias Marinas. Universidad Autónoma de Baja California. Ensenada, México. 33(2):197-215, (2007).&amp;#160; [20] J. A. Proehl, D. R. Lynch, D. J. McGillicuddy y J. R. Ledwell, &amp;quot;Modeling turbulent dispersion on the North Flank of Georges Bank using Lagrangian particle methods&amp;quot;. Continental Shelf Research, 25:875–900, (2005).&amp;#160; [21] J. M. Rodriguez, S. Hernández León y E. D. Barton, &amp;quot;Mesoscale distribution of fish larvae in relation to an upwelling filament off Northwest Africa&amp;quot;. Deep Sea Research I, 46:1969–1984, (1999).&amp;#160; [22] J. M. Rodriguez, E. D. Barton, S. Hernández León y&amp;#160; J. Aristegui, &amp;quot;The influence of mesoscale physical processes on the larval fish community in the Canaries CTZ&amp;quot;, in summer. Progress in Oceanography, 62:171-188, (2004).&amp;#160; [23]&amp;#160; M. Santiago, &amp;quot;La conectividad tridimensional en el Golfo de California, a partir de un modelo numérico&amp;quot;. Tesis presentada en opción al grado de Maestro en Ciencias. Ensenada, Baja California, México, (2013).&amp;#160; [24] SECTUR, &amp;quot;Secretaria de Turismo&amp;quot;. Obtenido del sitio Web:&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[2] CNA-SEMARNAT, &amp;quot;Régimen de almacenamientos hasta 1999. Banco Nacional de Datos de Aguas Superficiales&amp;quot;. En CD-ROM, (1999).&amp;#160; [3] R. K. Cowen and S. Sponaugle, &amp;quot;Larval Dispersal and Marine Population Connectivity&amp;quot;. Annual Review of Marine Science. 1:443-466, (2002).&amp;#160; [4] Delft3DFLOW, &amp;quot;Simulation of multidimensional hydrodynamic flows and transport phenomena, including sediments&amp;quot;. User Manual, Deltares, The Netherlands. http://oss.deltares.nl/, (2011).&amp;#160; [5] C. A. González D, &amp;quot;La geomática aplicada del estudio de la dinámica superficial de detritos suspendidos en la Bahía de Banderas&amp;quot;. Tesis Maestría en Ciencias en Hidrometeorología. Guadalajara, Jalisco, México, (2017).&amp;#160; [6] AE. Filonov, &amp;quot;Internal tide and tsunami waves in the continental shelf of the Mexican western coast&amp;quot;. Oceanogr. East. Pacific. 1:31–45, (2000).&amp;#160; [7] AE, Filonov y KV. Konyaev,&amp;#160; &amp;quot;Nonlinear internal waves near Mexico’s central Pacific coast&amp;quot;. In: Velasco-Fuentes OU, Scheinbaum J, Ochoa J (eds.), Nonlinear Processes in Geophysical Fluid Dynamics. Kluwer Academic Publishers, Netherlands,&amp;#160; 377–386, (2003).&amp;#160; [8] J. P. Finley, &amp;quot;Tornado predictions. Amer. Meteor&amp;quot;. J., 1, 85-88, (1884).&amp;#160; [9] W. S. Kessler, &amp;quot;The circulation of the eastern tropical Pacific: A review. Progress in Oceanography&amp;quot;. 69(2-4):181–217., (2006).&amp;#160; [10] J. A. Kurczyn, E. Beier, M. F. Lavín,&amp;#160; y A. Chaigneau, &amp;quot;Mesoscale eddies in the northeastern Pacific tropical-subtropical transition zone: Statistical characterization from satellite altimetry&amp;quot;. Journal of Geophysical Research. 117(C10): C10021, (2012).&amp;#160; [11]&amp;#160; M. G. León, &amp;quot;Análisis comparativo de los patrones de conectividad genética de especies arrecifales del Pacífico mexicano&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CICESE, Ensenada, Baja California, México, (2015).&amp;#160;  [12] S. G. Marinone, &amp;quot;On the three-dimensional numerical modeling of the deep circulation around Ángel de la Guarda Island in the Gulf of California&amp;quot;. Estuarine, Coastal and Shelf Science. 80:430–434, (2008).&amp;#160; [13] S. G. Marinone, &amp;quot;Seasonal Surface connectivity in the Gulf of California&amp;quot;. Estuarine Coastal and Shelf Science, 100:133-141., (2012).&amp;#160; [14] G. Martínez Flores, E. H. Nava Sánchez y O. Zaitsev, &amp;quot;Teledetección de plumas de material suspendido influenciadas por escorrentía en el Sur del Golfo de California&amp;quot;. CICIMAR Oceánides. 26(1): 1-8, (2011).&amp;#160; [15] S. Mitarai, D. A. Siegel, J. R. Watson, C. Dong&amp;#160; and J. C. McWilliams, &amp;quot;Quantifying connectivity in the coastal ocean with application to the Southern California Bight&amp;quot;. Journal Of Geophysical Research. 114(5):110-115, (2009).&amp;#160;  [16] M. M. Nishimoto y&amp;#160; L. Washburn,&amp;#160; &amp;quot;Patterns of coastal eddy circulation and abundance of pelagic juvenile fish in the Santa Barbara Channel, California, USA&amp;quot;. Marine Ecology Progress Series, 241:183-199, (2002).&amp;#160; [17] D. A. Pantoja, &amp;quot;Modelación Numérica de la Circulación General del Cañón Submarino en Bahía de Banderas&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CISECE. Ensenada, Baja California, México., (2013).&amp;#160;  [18] M. Peguero Icaza, L. Sánchez Velasco, M. F. Lavín,&amp;#160; y&amp;#160; S. G. Marinone,&amp;#160; &amp;quot;Larval fish assemblages, environment and circulation in a semienclosed sea (Gulf of California, México)&amp;quot;. Estuarine Coastal and Shelf Science. 79:277–288, (2008).&amp;#160;  [19] L. Plata y A. Filonov, &amp;quot;Marea interna en la parte NorOeste de la Bahía de Banderas, México&amp;quot;. Ciencias Marinas. Universidad Autónoma de Baja California. Ensenada, México. 33(2):197-215, (2007).&amp;#160; [20] J. A. Proehl, D. R. Lynch, D. J. McGillicuddy y J. R. Ledwell, &amp;quot;Modeling turbulent dispersion on the North Flank of Georges Bank using Lagrangian particle methods&amp;quot;. Continental Shelf Research, 25:875–900, (2005).&amp;#160; [21] J. M. Rodriguez, S. Hernández León y E. D. Barton, &amp;quot;Mesoscale distribution of fish larvae in relation to an upwelling filament off Northwest Africa&amp;quot;. Deep Sea Research I, 46:1969–1984, (1999).&amp;#160; [22] J. M. Rodriguez, E. D. Barton, S. Hernández León y&amp;#160; J. Aristegui, &amp;quot;The influence of mesoscale physical processes on the larval fish community in the Canaries CTZ&amp;quot;, in summer. Progress in Oceanography, 62:171-188, (2004).&amp;#160; [23]&amp;#160; M. Santiago, &amp;quot;La conectividad tridimensional en el Golfo de California, a partir de un modelo numérico&amp;quot;. Tesis presentada en opción al grado de Maestro en Ciencias. Ensenada, Baja California, México, (2013).&amp;#160; [24] SECTUR, &amp;quot;Secretaria de Turismo&amp;quot;. Obtenido del sitio Web:&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Zarate</name></author>	</entry>

	<entry>
		<id>https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70107&amp;oldid=prev</id>
		<title>Zarate at 15:29, 22 November 2017</title>
		<link rel="alternate" type="text/html" href="https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70107&amp;oldid=prev"/>
				<updated>2017-11-22T15:29:58Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class='diff-marker' /&gt;
				&lt;col class='diff-content' /&gt;
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				&lt;col class='diff-content' /&gt;
				&lt;tr style='vertical-align: top;' lang='en'&gt;
				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 15:29, 22 November 2017&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l351&quot; &gt;Line 351:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 351:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Referencias==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==Referencias==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[1] R. Álvarez, &amp;quot;Submarine topography and faulting in Bahía de Banderas, Mexico&amp;quot;. Geofísica Internacional, Vol. 46, Num. 2, pp. 93-116, (2007). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[2] CNA-SEMARNAT, &amp;quot;Régimen de almacenamientos hasta 1999. Banco Nacional de Datos de Aguas Superficiales&amp;quot;. En CD-ROM, (1999).&amp;#160; [3] R. K. Cowen and S. Sponaugle, &amp;quot;Larval Dispersal and Marine Population Connectivity&amp;quot;. Annual Review of Marine Science. 1:443-466, (2002).&amp;#160; [4] Delft3DFLOW, &amp;quot;Simulation of multidimensional hydrodynamic flows and transport phenomena, including sediments&amp;quot;. User Manual, Deltares, The Netherlands. http://oss.deltares.nl/, (2011).&amp;#160; [5] C. A. González D, &amp;quot;La geomática aplicada del estudio de la dinámica superficial de detritos suspendidos en la Bahía de Banderas&amp;quot;. Tesis Maestría en Ciencias en Hidrometeorología. Guadalajara, Jalisco, México, (2017).&amp;#160; [6] AE. Filonov, &amp;quot;Internal tide and tsunami waves in the continental shelf of the Mexican western coast&amp;quot;. Oceanogr. East. Pacific. 1:31–45, (2000).&amp;#160; [7] AE, Filonov y KV. Konyaev,&amp;#160; &amp;quot;Nonlinear internal waves near Mexico’s central Pacific coast&amp;quot;. In: Velasco-Fuentes OU, Scheinbaum J, Ochoa J (eds.), Nonlinear Processes in Geophysical Fluid Dynamics. Kluwer Academic Publishers, Netherlands,&amp;#160; 377–386, (2003).&amp;#160; [8] J. P. Finley, &amp;quot;Tornado predictions. Amer. Meteor&amp;quot;. J., 1, 85-88, (1884).&amp;#160; [9] W. S. Kessler, &amp;quot;The circulation of the eastern tropical Pacific: A review. Progress in Oceanography&amp;quot;. 69(2-4):181–217., (2006).&amp;#160; [10] J. A. Kurczyn, E. Beier, M. F. Lavín,&amp;#160; y A. Chaigneau, &amp;quot;Mesoscale eddies in the northeastern Pacific tropical-subtropical transition zone: Statistical characterization from satellite altimetry&amp;quot;. Journal of Geophysical Research. 117(C10): C10021, (2012).&amp;#160; [11]&amp;#160; M. G. León, &amp;quot;Análisis comparativo de los patrones de conectividad genética de especies arrecifales del Pacífico mexicano&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CICESE, Ensenada, Baja California, México, (2015).&amp;#160;  [12] S. G. Marinone, &amp;quot;On the three-dimensional numerical modeling of the deep circulation around Ángel de la Guarda Island in the Gulf of California&amp;quot;. Estuarine, Coastal and Shelf Science. 80:430–434, (2008).&amp;#160; [13] S. G. Marinone, &amp;quot;Seasonal Surface connectivity in the Gulf of California&amp;quot;. Estuarine Coastal and Shelf Science, 100:133-141., (2012).&amp;#160; [14] G. Martínez Flores, E. H. Nava Sánchez y O. Zaitsev, &amp;quot;Teledetección de plumas de material suspendido influenciadas por escorrentía en el Sur del Golfo de California&amp;quot;. CICIMAR Oceánides. 26(1): 1-8, (2011).&amp;#160; [15] S. Mitarai, D. A. Siegel, J. R. Watson, C. Dong&amp;#160; and J. C. McWilliams, &amp;quot;Quantifying connectivity in the coastal ocean with application to the Southern California Bight&amp;quot;. Journal Of Geophysical Research. 114(5):110-115, (2009).&amp;#160;  [16] M. M. Nishimoto y&amp;#160; L. Washburn,&amp;#160; &amp;quot;Patterns of coastal eddy circulation and abundance of pelagic juvenile fish in the Santa Barbara Channel, California, USA&amp;quot;. Marine Ecology Progress Series, 241:183-199, (2002).&amp;#160; [17] D. A. Pantoja, &amp;quot;Modelación Numérica de la Circulación General del Cañón Submarino en Bahía de Banderas&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CISECE. Ensenada, Baja California, México., (2013).&amp;#160;  [18] M. Peguero Icaza, L. Sánchez Velasco, M. F. Lavín,&amp;#160; y&amp;#160; S. G. Marinone,&amp;#160; &amp;quot;Larval fish assemblages, environment and circulation in a semienclosed sea (Gulf of California, México)&amp;quot;. Estuarine Coastal and Shelf Science. 79:277–288, (2008).&amp;#160;  [19] L. Plata y A. Filonov, &amp;quot;Marea interna en la parte NorOeste de la Bahía de Banderas, México&amp;quot;. Ciencias Marinas. Universidad Autónoma de Baja California. Ensenada, México. 33(2):197-215, (2007).&amp;#160; [20] J. A. Proehl, D. R. Lynch, D. J. McGillicuddy y J. R. Ledwell, &amp;quot;Modeling turbulent dispersion on the North Flank of Georges Bank using Lagrangian particle methods&amp;quot;. Continental Shelf Research, 25:875–900, (2005).&amp;#160; [21] J. M. Rodriguez, S. Hernández León y E. D. Barton, &amp;quot;Mesoscale distribution of fish larvae in relation to an upwelling filament off Northwest Africa&amp;quot;. Deep Sea Research I, 46:1969–1984, (1999).&amp;#160; [22] J. M. Rodriguez, E. D. Barton, S. Hernández León y&amp;#160; J. Aristegui, &amp;quot;The influence of mesoscale physical processes on the larval fish community in the Canaries CTZ&amp;quot;, in summer. Progress in Oceanography, 62:171-188, (2004).&amp;#160; [23]&amp;#160; M. Santiago, &amp;quot;La conectividad tridimensional en el Golfo de California, a partir de un modelo numérico&amp;quot;. Tesis presentada en opción al grado de Maestro en Ciencias. Ensenada, Baja California, México, (2013).&amp;#160; [24] SECTUR, &amp;quot;Secretaria de Turismo&amp;quot;. Obtenido del sitio Web:&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[1] R. Álvarez, &amp;quot;Submarine topography and faulting in Bahía de Banderas, Mexico&amp;quot;. Geofísica Internacional, Vol. 46, Num. 2, pp. 93-116, (2007). &amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[2] CNA-SEMARNAT, &amp;quot;Régimen de almacenamientos hasta 1999. Banco Nacional de Datos de Aguas Superficiales&amp;quot;. En CD-ROM, (1999).&amp;#160; [3] R. K. Cowen and S. Sponaugle, &amp;quot;Larval Dispersal and Marine Population Connectivity&amp;quot;. Annual Review of Marine Science. 1:443-466, (2002).&amp;#160; [4] Delft3DFLOW, &amp;quot;Simulation of multidimensional hydrodynamic flows and transport phenomena, including sediments&amp;quot;. User Manual, Deltares, The Netherlands. http://oss.deltares.nl/, (2011).&amp;#160; [5] C. A. González D, &amp;quot;La geomática aplicada del estudio de la dinámica superficial de detritos suspendidos en la Bahía de Banderas&amp;quot;. Tesis Maestría en Ciencias en Hidrometeorología. Guadalajara, Jalisco, México, (2017).&amp;#160; [6] AE. Filonov, &amp;quot;Internal tide and tsunami waves in the continental shelf of the Mexican western coast&amp;quot;. Oceanogr. East. Pacific. 1:31–45, (2000).&amp;#160; [7] AE, Filonov y KV. Konyaev,&amp;#160; &amp;quot;Nonlinear internal waves near Mexico’s central Pacific coast&amp;quot;. In: Velasco-Fuentes OU, Scheinbaum J, Ochoa J (eds.), Nonlinear Processes in Geophysical Fluid Dynamics. Kluwer Academic Publishers, Netherlands,&amp;#160; 377–386, (2003).&amp;#160; [8] J. P. Finley, &amp;quot;Tornado predictions. Amer. Meteor&amp;quot;. J., 1, 85-88, (1884).&amp;#160; [9] W. S. Kessler, &amp;quot;The circulation of the eastern tropical Pacific: A review. Progress in Oceanography&amp;quot;. 69(2-4):181–217., (2006).&amp;#160; [10] J. A. Kurczyn, E. Beier, M. F. Lavín,&amp;#160; y A. Chaigneau, &amp;quot;Mesoscale eddies in the northeastern Pacific tropical-subtropical transition zone: Statistical characterization from satellite altimetry&amp;quot;. Journal of Geophysical Research. 117(C10): C10021, (2012).&amp;#160; [11]&amp;#160; M. G. León, &amp;quot;Análisis comparativo de los patrones de conectividad genética de especies arrecifales del Pacífico mexicano&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CICESE, Ensenada, Baja California, México, (2015).&amp;#160;  [12] S. G. Marinone, &amp;quot;On the three-dimensional numerical modeling of the deep circulation around Ángel de la Guarda Island in the Gulf of California&amp;quot;. Estuarine, Coastal and Shelf Science. 80:430–434, (2008).&amp;#160; [13] S. G. Marinone, &amp;quot;Seasonal Surface connectivity in the Gulf of California&amp;quot;. Estuarine Coastal and Shelf Science, 100:133-141., (2012).&amp;#160; [14] G. Martínez Flores, E. H. Nava Sánchez y O. Zaitsev, &amp;quot;Teledetección de plumas de material suspendido influenciadas por escorrentía en el Sur del Golfo de California&amp;quot;. CICIMAR Oceánides. 26(1): 1-8, (2011).&amp;#160; [15] S. Mitarai, D. A. Siegel, J. R. Watson, C. Dong&amp;#160; and J. C. McWilliams, &amp;quot;Quantifying connectivity in the coastal ocean with application to the Southern California Bight&amp;quot;. Journal Of Geophysical Research. 114(5):110-115, (2009).&amp;#160;  [16] M. M. Nishimoto y&amp;#160; L. Washburn,&amp;#160; &amp;quot;Patterns of coastal eddy circulation and abundance of pelagic juvenile fish in the Santa Barbara Channel, California, USA&amp;quot;. Marine Ecology Progress Series, 241:183-199, (2002).&amp;#160; [17] D. A. Pantoja, &amp;quot;Modelación Numérica de la Circulación General del Cañón Submarino en Bahía de Banderas&amp;quot;. Tesis de doctorado en Ciencias en Oceanografía Física. CISECE. Ensenada, Baja California, México., (2013).&amp;#160;  [18] M. Peguero Icaza, L. Sánchez Velasco, M. F. Lavín,&amp;#160; y&amp;#160; S. G. Marinone,&amp;#160; &amp;quot;Larval fish assemblages, environment and circulation in a semienclosed sea (Gulf of California, México)&amp;quot;. Estuarine Coastal and Shelf Science. 79:277–288, (2008).&amp;#160;  [19] L. Plata y A. Filonov, &amp;quot;Marea interna en la parte NorOeste de la Bahía de Banderas, México&amp;quot;. Ciencias Marinas. Universidad Autónoma de Baja California. Ensenada, México. 33(2):197-215, (2007).&amp;#160; [20] J. A. Proehl, D. R. Lynch, D. J. McGillicuddy y J. R. Ledwell, &amp;quot;Modeling turbulent dispersion on the North Flank of Georges Bank using Lagrangian particle methods&amp;quot;. Continental Shelf Research, 25:875–900, (2005).&amp;#160; [21] J. M. Rodriguez, S. Hernández León y E. D. Barton, &amp;quot;Mesoscale distribution of fish larvae in relation to an upwelling filament off Northwest Africa&amp;quot;. Deep Sea Research I, 46:1969–1984, (1999).&amp;#160; [22] J. M. Rodriguez, E. D. Barton, S. Hernández León y&amp;#160; J. Aristegui, &amp;quot;The influence of mesoscale physical processes on the larval fish community in the Canaries CTZ&amp;quot;, in summer. Progress in Oceanography, 62:171-188, (2004).&amp;#160; [23]&amp;#160; M. Santiago, &amp;quot;La conectividad tridimensional en el Golfo de California, a partir de un modelo numérico&amp;quot;. Tesis presentada en opción al grado de Maestro en Ciencias. Ensenada, Baja California, México, (2013).&amp;#160; [24] SECTUR, &amp;quot;Secretaria de Turismo&amp;quot;. Obtenido del sitio Web:&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;www.sectur.gob.mx/work/models/sectur/Resource/&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;www.sectur.gob.mx/work/models/sectur/Resource/&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;5975/1/images/Agenda21.pdf, (2011).&amp;#160;  [25] D. Wilks, &amp;quot;Statistical Methods in the Atmospheric Sciences&amp;quot;, 2nd ed.; Academic Press: San Diego, CA, USA, p. 627, (2006).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;5975/1/images/Agenda21.pdf, (2011).&amp;#160;  [25] D. Wilks, &amp;quot;Statistical Methods in the Atmospheric Sciences&amp;quot;, 2nd ed.; Academic Press: San Diego, CA, USA, p. 627, (2006).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Zarate</name></author>	</entry>

	<entry>
		<id>https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70106&amp;oldid=prev</id>
		<title>Zarate at 15:29, 22 November 2017</title>
		<link rel="alternate" type="text/html" href="https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=70106&amp;oldid=prev"/>
				<updated>2017-11-22T15:29:21Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='2' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 15:29, 22 November 2017&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;CONECTIVIDAD Y DISPERSÍON DE PARTÍCULAS EN BAHÍA DE BANDERAS&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;MÉXICO&lt;/del&gt;==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;==&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Conectividad y dispersíon de partículas en Bahía de Banderas&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;México&lt;/ins&gt;==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Christian De la Torre, Diego Pantoja, Anatoliy Filonov &amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;'''Christian De la Torre, Diego Pantoja, Anatoliy Filonov &amp;#160;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Zarate</name></author>	</entry>

	<entry>
		<id>https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=69756&amp;oldid=prev</id>
		<title>Diegopantoja: Diegopantoja moved page Draft Pantoja 450669517 to Review Pantoja 2017b</title>
		<link rel="alternate" type="text/html" href="https://www.scipedia.com/wd/index.php?title=Pantoja_2017b&amp;diff=69756&amp;oldid=prev"/>
				<updated>2017-11-17T15:24:02Z</updated>
		
		<summary type="html">&lt;p&gt;Diegopantoja moved page &lt;a href=&quot;/public/Draft_Pantoja_450669517&quot; class=&quot;mw-redirect&quot; title=&quot;Draft Pantoja 450669517&quot;&gt;Draft Pantoja 450669517&lt;/a&gt; to &lt;a href=&quot;/public/Review_Pantoja_2017b&quot; class=&quot;mw-redirect&quot; title=&quot;Review Pantoja 2017b&quot;&gt;Review Pantoja 2017b&lt;/a&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;tr style='vertical-align: top;' lang='en'&gt;
				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan='1' style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 15:24, 17 November 2017&lt;/td&gt;
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		<author><name>Diegopantoja</name></author>	</entry>

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		<title>Diegopantoja: Created page with &quot;==CONECTIVIDAD Y DISPERSÍON DE PARTÍCULAS EN BAHÍA DE BANDERAS, MÉXICO==  '''Christian De la Torre, Diego Pantoja, Anatoliy Filonov   Posgrado de Hidrometeorología, Depar...&quot;</title>
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				<updated>2017-11-17T15:19:05Z</updated>
		
		<summary type="html">&lt;p&gt;Created page with &amp;quot;==CONECTIVIDAD Y DISPERSÍON DE PARTÍCULAS EN BAHÍA DE BANDERAS, MÉXICO==  &amp;#039;&amp;#039;&amp;#039;Christian De la Torre, Diego Pantoja, Anatoliy Filonov   Posgrado de Hidrometeorología, Depar...&amp;quot;&lt;/p&gt;
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		<author><name>Diegopantoja</name></author>	</entry>

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