Supported by the National Key Research and Development Program of China (2023YFC3010700);Second Tibetan Plateau Comprehensive Scientific Expedition and Research Program (2019QZKK0105);Science and Technology Development Fund of Chinese Academy of Meteorological Sciences (2023KJ027 and 2024KJ012)。
The Asian monsoon(AM) region is a well-known region with prevailing stratosphere–troposphere exchange(STE).However,how the STE across this region changes with the weakening AM remains unclear.Here,we particularly dia...
Supported by the National Natural Science Foundation of China(42088101);Guangdong Major Project of Basic and Applied Basic Research(2020B0301030004);Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies(2020B1212060025);Jiangsu Collaborative Innovation Center for Climate Change.
We investigate the relative importance of spring sea surface temperatures(SSTs)in different Indian Ocean(IO)domains,especially the northern and southern IO,for the development and intensity of the Asian summer monsoon...
Supported by the National Natural Science Foundation of China(41830969);the Second Tibetan Plateau Scientific Expedition and Research(STEP)Program(2019QZKK0105);National Natural Science Foundation of China(42005131);Basic Scientific Research and Operation Fund of the Chinese Academy of Meteorological Sciences(CAMS)(2021Z004);Science and Technology Development Fund of CAMS(2020KJ009 and 2020KJ012)。
Subseasonal to seasonal(S2S)variability represents the atmospheric disturbance on the 10–90-day timescale,which is an important bridge linking weather and climate.In 2015,China Meteorological Administration(CMA)liste...
Supported by the National Natural Science Foundation of China(41930972,41775055,51778617,and 42005141);Science and Technology Development Funds of the Chinese Academy of Meteorological Sciences(2020KJ019)。
Based on best-track,outgoing longwave radiation,sea surface temperature,and reanalysis data during 1979-2018,statistical and composite analyses were performed to investigate characteristics of the southwesterly water ...
Supported by the Special Strategic Project of Leading Science and Technology of Chinese Academy of Sciences(XDA20100304);National Natural Science Foundation of China(41790471)。
In the summers of 1998 and 1999, Chinese and Japanese scientists cooperatively conducted the first large-scale energy and water cycle experiment(WCRP/GEWEX/GAME/HUBEX: World Climate Research Program/Global Energy and ...
Supported by the National(Key)Basic Research and Development(973)Program of China(2011CB403406);Priority Academic Program Development(PAPD)of Jiangsu Higher Education Institutions
Seasonal variation features of aerosol optical depth (AOD) over East China and India in association with the Asian monsoon system are investigated, based on the latest AOD data derived from the Moderate Resolution I...
Supported jointly by the National Natural Science Foundation of China(41125017 and 41330423);National(Key) Basic Research and Development(973) Program of China(2010CB951904);Public Science and Technology Research Project Funds of Ocean(201105019-3)
An overview of Chinese contribution to Coupled Model Intercomparison Project-Phase 5 (CMIP5) is presented. The performances of five Chinese Climate/Earth System Models that participated in the CMIP5 pro ject are ass...
Supported by National Natural Science Foundation of China under Grant No.40675041.
The features of the temperate jet stream including its location, intensity, structure, seasonal evolution and the relationship with the Asian monsoon are examined by using NCEP/NCAR reanalysis data. It is indicated th...
Supported by NSF climate dynamics program (ATM06-47995);by IPRC,which is in part sponsored by FRCGC/JAMSTEC,NASA,and NOAA.
Development of monsoon climate prediction through integrated research efforts to improve our understanding of monsoon variability and predictability is a primary goal of the Asian Monsoon Years (200-2011) and Intern...
This work is supported by the Open Research Fund of Laboratory for Climate Studies of China Meteorological Administrationunder Grant Nos. CCSF2005-2-QH04 and LC2004C-04.
A better understanding of the long-term global carbon cycle required estimateof the changes in terrestrial carbon storage after the last glacial period. The results ofsimulation at mid-Holocene (MH) from PMIP (Paleocl...