Scipediacontent at 11:33, 15 May 2017

2017-05-15T11:33:59Z

Scipediacontent: Scipediacontent moved page Draft Content 635019552 to Mao Liao 2016a

2017-05-15T09:32:54Z

Scipediacontent moved page Draft Content 635019552 to Mao Liao 2016a

Scipediacontent: Created page with "==Abstract== We quantified the impacts of variations in meteorological parameters and emissions on decadal, interannual, and seasonal variations of atmospheric black carbon (..."

2017-05-15T09:28:59Z

Created page with "==Abstract== We quantified the impacts of variations in meteorological parameters and emissions on decadal, interannual, and seasonal variations of atmospheric black carbon (..."

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 {| style="text-align: center; margin:auto;"
 |-
-| <math>APDM=100\mbox{%}\times MAD/\left(\frac{1}{n}{\sum }_{i=1}^nM_i\right)\quad \mbox{,}</math>
+| <math>APDM=100%\times MAD/\left(\frac{1}{n}{\sum }_{i=1}^nM_i\right)\quad \mbox{,}</math>
 |}
 | style="width: 5px;text-align: right;white-space: nowrap;" | ( 3)
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 Following the process analyses, [[#bib23|Mao et al. (2016)]]  pointed out that wind is the major meteorological factor to influence the interannual variations of surface BC. The interannual variations of surface concentrations of BC due to biomass burning emissions are largest in the nonmonsoon season, as the APDM values of surface BC concentrations due to changes in anthropogenic alone (VEMISAN) is only 85% of those due to variations in both anthropogenic and biomass burning emissions (VEMIS). The influences of non-China emissions on BC are also largest in the nonmonsoon season.
 ===3.3. Direct radiative forcing of BC===

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Mao Liao 2016a - Revision history

Scipediacontent at 11:33, 15 May 2017

Scipediacontent: Scipediacontent moved page Draft Content 635019552 to Mao Liao 2016a

Scipediacontent: Created page with "==Abstract== We quantified the impacts of variations in meteorological parameters and emissions on decadal, interannual, and seasonal variations of atmospheric black carbon (..."