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Geophysical Research Letters
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4.58
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51791
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#1Heidi M. Pickard (Harvard University)H-Index: 2
#2Alison S. Criscitiello (U of A: University of Alberta)H-Index: 7
Last. Cora J. Young (York University)H-Index: 23
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#1Guanglei Zhang (Monash University)H-Index: 2
#2Pathegama Gamage Ranjith (Monash University)H-Index: 42
Last. Beining ZhangH-Index: 1
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1 CitationsSource
#1H. L. F. Huybrighs (ESTEC: European Space Research and Technology Centre)
#2Elias Roussos (MPG: Max Planck Society)H-Index: 30
Last. Olivier Witasse (ESTEC: European Space Research and Technology Centre)H-Index: 27
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#1Kristopher B. Karnauskas (CIRES: Cooperative Institute for Research in Environmental Sciences)H-Index: 20
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#1Wenyuan Fan (FSU: Florida State University)H-Index: 11
#2Jeffrey J. McGuire (USGS: United States Geological Survey)
Last. Peter M. Shearer (SIO: Scripps Institution of Oceanography)H-Index: 66
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#1Xiaoqin Shi (MPG: Max Planck Society)
#2Guy P. Brasseur (PolyU: Hong Kong Polytechnic University)
Abstract During the COVID-19 outbreak that took place in early 2020, the economic activities in China were drastically reduced and accompanied by a strong reduction in the emission of primary air pollutants. On the basis of measurements made at the monitoring stations operated by the China National Environmental Monitoring Center, we quantify the reduction in surface PM2.5, NO2, CO and SO2 concentrations in northern China during the lockdown, which started on 23 January 2020. We find that, on th...
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#1Michael R. Gallagher (ESRL: Earth System Research Laboratory)H-Index: 1
#1Michael R. Gallagher (ESRL: Earth System Research Laboratory)
Last. Rodrigo Guzman (École Polytechnique)H-Index: 4
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#1Louis De Barros (CNRS: Centre national de la recherche scientifique)H-Index: 12
#2Frédéric Cappa (Institut Universitaire de France)H-Index: 30
Last. Pierre Dublanchet (ENSMP: Mines ParisTech)H-Index: 1
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#1Ishan S. Anjikar (AU: Auburn University)
#2Shelby Wales (AU: Auburn University)
Last. Lauren E. Beckingham (AU: Auburn University)H-Index: 5
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#1Chirag Dhara (IITM: Indian Institute of Tropical Meteorology)
Changes in the atmospheric composition alter the magnitude and partitioning between the downward propagating solar and atmospheric longwave radiative fluxes heating the Earth's surface. These changes are computed by radiative transfer codes in Global Climate Models, and measured with high precision at surface observation networks. Changes in radiative heating signify changes in the global surface temperature and hydrologic cycle. Here, we develop a conceptual framework using an Energy Balance Mo...
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