supported by the National Key R&D Program of China (Grant No. 2017YFC1501603);the China National Program on Key Basic Research Project (973 Program) (Grant No. 2013CB430103);the National Natural Science Foundation of China (Grants Nos. 41775054, 41375061 and 40705019)
The initiation processes of one of the initial convective cells near and on the east side of a dryline on 19 June 2002 during the IHOP 2002 field experiment in the central United States is analyzed in detail based on ...
Supported by the National Basic Research Program of China(973 Program)(Nos.2010CB428504,2012CB956002);the National Natural Science Foundation of China(Nos.40906005,41105059,41065005,GYHY201106017,GYHY201306027);the National Key Technology Research and Development Program(No.2009BAC51B01)
This paper attempts to analyze in detail the remote influence of the Indian Ocean Basin warming on the Northwest Pacific (NWP) during the year of decaying E1 Nifio. Observation data and the Fast Ocean- Atmosphere co...
Supported by the National Basic Research Program(973Program)(Nos.2007CB816001,2005CB422302,2005CB422307and2007CB411806);the National Natural Science Foundation of China(Nos.41030854,40776016,40906015,and40906016);the Major Project of National Natural Science Foundation of China(Nos.40490263,40976005);the Research Project of National Marine Data and Information Service(No.29106006C)
We investigated the Stokes drift-driven ocean currents and Stokes drift-induced wind energy input into the upper ocean using a two-way coupled wave-current modeling system that consists of the Princeton Ocean Model ge...
supported by the National Basic Research Program of China (973 Program) under Grant 2009CB421406;the National Key Technologies R & D Programof China under Grant 2009BAC51B02
In this paper,the dynamical evolutions of two types of Arctic Oscillation (AO),the stratospheric (S) and tropospheric (T) types,have been investigated on an intermediate time scale in terms of transient eddy feedback ...