Yang Kai

发布时间:2020-09-10  字体大小T|T
       Kai Yang, PhD, Young Research Fellow, master supervisor. Research areas of Dr. Yang focus on the climate model, modeling and land-atmosphere interactions. He has conducted a series research works on the impacts of soil moisture anomalies related to freeze-thaw (FT) process and snow cover anomalies over Tibetan Plateau (TP) on general circulation in East Asia and response of atmosphere dynamic process to TP thermal forcing. He has also developed model parameterizations, incorporating a new water-heat transport scheme in CLM, and proposing new FT parameterizations to improve the simulation of soil moisture and temperature in clod region.
Area of Expertise
Land-atmosphere interaction, land surface process, model and modeling
Ph. D. in Meteorology (Jun. 2020), College of Atmospheric Sciences, Lanzhou University
M. S. in Meteorology (Jun. 2017), College of Atmospheric Sciences, Lanzhou University
B. S. in Atmospheric Sciences (Jun. 2014), College of Atmospheric Sciences, Lanzhou University
[1]Yang K., Wang C. (2019). Seasonal persistence of soil moisture anomalies related to freeze–thaw over the Tibetan Plateau and prediction signal of summer precipitation in eastern China. Climate Dynamics, 53, 2411-2424. https://doi.org/10.1007/s00382-019-04867-1
[2]Yang K., Wang C. (2019). Water storage effect of soil freeze-thaw process and its impacts on soil hydro-thermal regime variations. Agricultural and Forest Meteorology, 265, 280-294. https://doi.org/10.1016/j.agrformet.2018.11.011
[3]Yang K., Wang C., Li S. (2018). Improved simulation of Frozen-Thawing Process in Land Surface Model (CLM4.5). Journal of Geophysical Research: Atmospheres, 123, 238–258. https://doi.org/10.1029/2017JD028260
[4]Yang K., Wang C., Bao H. (2016). Contribution of soil moisture variability to summer precipitation in the Northern Hemisphere. Journal of Geophysical Research: Atmospheres, 121, 108-124. https://doi.org/10.1002/2016JD025644
[5]Wang C., Yang K. (2018). A new scheme for considering soil water‐heat transport coupling based on Community Land Model: Model description and preliminary validation. Journal of Advances in Modeling Earth Systems, 10, 927-950. https://doi.org/10.1002/2017MS001148
[6]Wang C., Yang K., Li Y., Wu D., and Bo Y. (2017). Impacts of Spatiotemporal Anomalies of Tibetan Plateau Snow Cover on Summer Precipitation in Eastern China. Journal of Climate, 30, 885-903. https://doi.org/10.1175/JCLI-D-16-0041.1
[7]Bao H., Yang K., Wang C. (2017). Characteristics of GLDAS soil-moisture data on the Tibet Plateau. Sciences in Cold and Arid Regions, 9, 127–141. doi: 10.3724/SP.J.1226.2017.00127.
[8]Wang C., Yang K., Zhang F. Impacts of Soil Freeze-Thaw Process and Snow Melting over Tibetan Plateau on Asian Summer Monsoon System: a Review and Perspective. Frontiers in Earth Science, 2020, 8, 133.
[9]Wang C., Wang Z., Kong Y., Zhang F., Yang K., Zhang T. (2019). Most of the Northern Hemisphere Permafrost Remains under Climate Change. Scientific Report, 9, 3295. https://doi.org/10.1038/s41598-019-39942-4
[10]Yang K., Hu T., Wang C. (2017). A numerical study on the relationship between the spring–winter snow cover anomalies over the northern and southern Tibetan Plateau and summer precipitation in East China. Chinese Journal of Atmospheric Sciences (in Chinese), 41 (2): 345–356.
[11]Li S., Yang K., Wang C. (2018). Bias characteristics of land surface model (CLM4.5) over Tibetan Plateau during soil freezing-thawing period and its causes. Journal of Glaciology and Geocryology (in Chinese), 40(2): 322–344.

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