This work was supported by the National Natural Science Foundation of China(Grant Nos.41405058 and 41861144015);the National Key R&D Program of China(2017YFA0603201).
Based on observational and reanalysis data,the relationships between the eastern Pacific(EP)and central Pacific(CP)types of El Niño−Southern Oscillation(ENSO)during the developing summer and the South Asian summer mon...
supported in part by the National Key Research and Development Program of China(Grant No.2017YFC1501601);the National Natural Science Foundation of China(Grant No.41875067)。
As a follow-up of a previously published article on the contribution of tropical waves,this study explores the evolution of the mid-tropospheric mesoscale cyclonic vortex(MV)during the formation of Typhoon Megi(2010)w...
supported by the National Key Research and Development Program of China (Grant No. 2018YFC1506402);the National Program on Global Change and Air–Sea Interaction (Grant Nos. GASI-IPOVAI-03 and GASIIPOVAI-06);the National Key Technology Research and Development Program of the Ministry of Science and Technology of China (Grant No. 2015BAC03B07)
A new method to quantify the predictability limit of ensemble forecasting is presented using the Kullback–Leibler(KL)divergence(also called the relative entropy), which provides a measure of the difference between th...
supported by the National Basic Research Program of China(Grant Nos.2013CB430203 and 2012CB417205);the National Key Research and Development Program of China(during the 13th Five-year Plan)(Grant No.2016YFA0601501);the China Meteorological Special Programs(Grant No.GYHY201306033)
The Afro-Asian summer monsoon is a zonally planetary-scale system, with a large-scale rainbelt covering Africa, South Asia and East Asia on interdecadal timescales both in the past century(1901-2014) and during the ...
jointly supported by the National Department Public Benefit Research Foundation(Grant No.GYHY201406003);the 973 Program(Grant Nos.2013CB956203 and 2012CB957803);the National Natural Science Foundation of China(Grant Nos.41490642,41475070 and 41305045);the Jiangsu Natural Science Foundation(Grant No.BK20151447)
A regional heavy precipitation event that occurred over Sichuan Province on 8-9 September 2015 is analyzed based on hourly observed precipitation data obtained from weather stations and NCEP FNL data. Two moist dynami...
Sponsored by the National (973) Program on Key Basic Research project entitled "Observation,Prediction and Analysis of Severe Convection of China" (Grant No. 2013CB430104);the National Natural Science Foundation of China (Grant No. 41575047)
Short squall lines that occurred over Lishui, southwestern Zhejiang Province, China, on 5 July 2012, were investigated using the WRF model based on 1°× 1° gridded NCEP Final Operational Global Analysis data. The re...
supported by the Key Program of the Chinese Academy of Sciences (KZZD-EW05);the National Basic Research Program of China (Grant No. 2013CB430105);the Beijing Natural Sciences Foundation (Grant No. 8142035);the National Natural Sciences Foundation of China (Grant No. 41575065)
The non-hydrostatic wave equation set in Cartesian coordinates is rearranged to gain insight into wave generation in a mesoscale severe convection system. The wave equation is characterized by a wave operator on the l...
supported by the National Natural Science Foundation of China (Grant Nos. 41175060 and 41375052);the Key Program of the Chinese Academy of Sciences (Grant No. KZZD-EW-05);the National Basic Research Program of China (Grant No. 2013CB430105);the State Key Laboratory of Severe Weather (LASW),Chinese Academy of Meteorological Sciences (Grant No. 2013LASW-A06)
NCEP-NCAR reanalysis data were used to analyze the characteristics and evolution mechanism of convective and symmetric instability before and during a heavy rainfall event that occurred in Beijing on 21 July 2012.Appr...
supported by the National Key Basic Research Project of China (Grant No. 2009CB 421404);the Chinese NSF key project (Grant Nos. 40930950 and 40730951);the Chinese NSF (Grant Nos. 40775031 and 40575021)
It is well known that the quasi-geostrophic (QG) omega equation with only two contributors respectively associated with vorticity advection (VA) and temperature advection is derived for midlatitude synoptic-scale ...
Both water vapor and heat processes play key roles in producing surface rainfall.While the water vapor effects of sea surface temperature and cloud radiative and microphysical processes on surface rainfall have been i...