Guolin Feng
China Meteorological Administration
175 Papers
222 Citations
Guolin Feng is an academic researcher from China Meteorological Administration. The author has contributed to research in topics: Environmental science & Climatology. The author has an hindex of 15, co-authored 116 publications. Previous affiliations of Guolin Feng include Lanzhou University & Beijing Normal University.
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Papers
Linkages of unprecedented 2022 Yangtze River Valley heatwaves to Pakistan flood and triple-dip La Niña
Shankai Tang,Shaobo Qiao,Bin Wang,Meilin Liu,Taichen Feng,Jie Yang,Meng He,Dong Chen,Jianbo Cheng,Guolin Feng,Wen-Fei Dong +10 more
TL;DR: In this paper , the authors present convergent empirical and modelling evidence to show that the record-breaking Pakistan rainfall, along with the 2022 tripe-dip La Niña, produces anomalous high pressure over YRV, causing intense heatwaves.
Impacts of climate change on vegetation pattern: mathematical modelling and data analysis
TL;DR: In this article , the influence of climate change on vegetation growth in both time and space by dynamical modeling the interactions of meteorological elements and vegetation growth is analyzed. And the long-term evolution trend of vegetation growth under climate change in some typical regions based on data analysis is characterized.
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Evaporation variability under climate warming in five reanalyses and its association with pan evaporation over China
TL;DR: In this paper, an assessment of evapotranspiration variability under climate warming over China was made from five sets of reanalysis data sets [National Centers for Environmental Prediction-National Center for Atmospheric Research (NCEP-NCAR), NCEP Department of Energy (N CEP-DOE), Modern-Era Retrospective Analysis for Research and Applications (MERRA), Interim Reanalysis, and Japanese 55-year Reanalysis (JRA-55)].
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Impact of the December North Atlantic Oscillation on the following February East Asian trough
TL;DR: In this paper, it is shown that the circulation anomalies affected by the December NAO for December and for the following January are primarily confined to the Euro-Atlantic sector while they extend to East Asia during the following February, and this is related to anomalous wave trains originating from the southwestern Atlantic and spreading to the northeastern Atlantic, northern Europe, western Siberia, and East Asia.
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