- 08月29日
Study on the Structure of a Horizontal Shear Line over the Tibetan Plateau Based on CRA-Interim Datasets and Its Comparison with ERA-Interim Datasets
The CRA-Interim trial production of the global atmospheric reanalysis for 10 years from 2007 to 2016...
- 08月29日
DIURNAL VARIATION OF GLOBAL PRECIPITATION:AN ANALYSIS OF CMORPH DATA
In this study, the observed CMORPH precipitation data from 1998 to 2015 are used to analyze diurnal ...
- 08月28日
Resonance Effect in Interaction Between South Asian Summer Monsoon and ENSO During 1958-2018
The study has shown that the shear component of the vertical integrated kinetic energy(Ks)over the b...
- 08月28日
Synoptic Characteristics Related to Warm-Sector Torrential Rainfall Events in South China During the Annually First Rainy Season
Warm-sector torrential rainfall(WSTR)events that occur in the annually first rainy season in south C...
- 08月27日
Squall Line and Its Vertical Motion Under Different Moisture Profiles in Eastern China
The impacts of different moisture profiles on the structure and vertical motion of squall lines were...
- 08月27日
IMPACT OF VERTICAL RESOLUTION, MODEL TOP AND DATA ASSIMILATION ON WEATHER FORECASTING——A CASE STUDY
The impacts of stratospheric initial conditions and vertical resolution on the stratosphere by raisi...
- 08月26日
THE EFFECT OF MODEL HORIZONTAL RESOLUTION ON THE PRECIPITATION OF RAMMASUN
...
- 08月26日
A COMBINED VERIFICATION METHOD FOR PREDICTABILITY OF PERSISTENT HEAVY RAINFALL EVENTS OVER EAST ASIA BASED ON ENSEMBLE FORECAST
Persistent Heavy Rainfall(PHR)is the most influential extreme weather event in Asia in summer,and th...
- 08月25日
A COMPARISON AND EVALUATION OF TWO CENTENNIAL-SCALE SEA SURFACE TEMPERATURE DATASETS IN THE CHINA SEAS AND THEIR ADJACENT SEA AREAS
Two reconstructed sea surface temperature (SST)datasets (HadISST1 and COBE SST2)with centennial-scal...
- 08月25日
TESTING DRAG COEFFICIENT APPROACHES BY USING THE BUOY DATA COLLECTED IN MODERATE TO HIGH WIND UNDER FOLLOWING,CROSSING AND OPPOSING SWELL CONDITIONS
Hurricane intensity and track are strongly affected by air-sea interactions. Classified as following...