- A
- A new soil moisture initialization scheme
- Analyses of simulation Temperature
- Assessment of bias in simulation of monsoon climate of China Korea and Japan
- B - 2
- Bimodality of the EASWJ core in midsummer
- Bimodality of the SAH in the seasonal cycle
- Changes in climate extreme in associated with the mean state
- Changes in extreme and total precipitation
- Changes in temperature extremes and mean temperature
- Changes of surface dynamic parameters under two vegetation coverages
- Characteristics of the onset of Asian summer monsoon
- Circulation features of the strong DFC summers
- Climate effects of SAH on the regional climate
- Climate simulation of the last years
- Climatic features of atmospheric heat sourcesink over the TP
- Climatological distribution of the atmospheric heat sourcesink
- Climatological features of the winter snow Spatial pattern of snow depth over TP
- Cloudradiative forcing over East Asia
- Conclusions
- Conclusions and discussions
- Conclusions and some outstanding issues
- Data and methodology
- Data and model comparison of climate at ka BP
- Design of the simulation experiments
- Discussion - 2
- East Asian summer monsoon
- Effects of increasing greenhouse gases and aerosols on regional climate of East Asia
- Ensemble Methods
- ENSO and its global impacts
- Extreme precipitation
- Field observation at Lanzhou another Reference Site of CEOP program over Loess Plateau
- Forcing conditions - 2
- Frequency and intensity of precipitation
- Global aridity trend in the second half of the th century
- H P
- Hot and cold summer climate in China In Reaches of Yangtze and Huaihe Rivers
- Hot days and frost days
- Ice cores
- Impact of climate change on runoff
- Impact of climate warming on the crop diseases and insect pests
- Impact of global warming on crop yield
- Impact of humaninduced largescale land cover changes on the East Asian monsoon climate in RCM simulations
- Impacts of aerosols on East Asia monsoon climate
- Impacts of climate change on agriculture Impact of climate change on cropping system
- Impacts of pure ENSO events on Summer climate of China
- Impacts of pure IOD on the Summer climate of China
- Impacts on mean climate
- Impacts on the surface temperature variation
- In middle latitude of eastern China
- In Northeastern China
- In Poyang Lake Area
- In situ measured soil moisture in China Soil moisture measurement in China
- In the decaying phase of an ENSO event
- In the developing phase of an ENSO event
- In the Northeast China
- In the south of Eastern China
- In the southern part of southern China
- Indian Ocean variabilities especially the Indian Ocean dipole
- Influence of IOD on the East Asian summer monsoon
- Intensified field observation of water energy and CO fluxes over semiarid area of China
- Interdecadal atmospheric anomalies in East Asia
- Interdecadal change of ENSOs impact on the climate of China
- Interdecadal climate anomalies in China
- Interdecadal variability of Southern Oscillation and Walker Circulation and their relationships with Asian summer monsoon
- Interference of IOD in the Ensoeasm relation
- Introduction - 2 3 4 5 6
- Issues in the recent decades
- Lake sediments
- Land surface process
- Largescale characteristics of Asian summer monsoon onset
- Loess
- Maximum and minimum temperatures
- Mean climate and biases
- Mechanisms of vegetation effects on climate change
- Middle latitude of Eastern China
- Model and data comparison
- Model description - 2
- North of Eastern China
- Parameterization of radiation
- Pollen
- Precipitation
- Precipitation extremes
- Preface
- Project Design
- Projection of extreme events
- Projections of changes in precipitation Global climate modeling
- Ps E dt
- R x fc
- Reconstruction data
- References - 2 3 4
- Regional climate modeling - 2
- Relationship between SST in the North Pacific and Northeast Cold Vortex
- Results - 2
- Seasonal distribution
- Seasonal eastwest movement of the EASWJ and its association with the diabatic heating over the TP
- Seasonal eastwest movement of the EASWJ core
- Seasonal transition features
- Seasonal variation of SAH
- Sensible heat driven airpump SHAP over the TP
- Sensitive simulation of climate in LIA
- Simulation on the dynamicthermodynamic effect of the TP
- Simulation Results
- Sm Co CiHt CHt C log Ht
- Soil moisture and climatic interannual variability
- Soil moisture variations with depth
- South China Sea summer monsoon
- Springer
- SST features of the strong DFC summers
- Stalagmite
- Statistical downscaling - 2
- Statistical relationship between snow anomaly and precipitation
- Summary - 2
- Summary and discussions 3 4
- Summer
- T C
- Temperature extremes
- Temporal variation of atmospheric heat sourcesink
- Temporal variation of the paleomonsoon and drywet oscillation on earth orbital time scales
- The analysis on continuous effect of soil moisture anomaly
- The heavy rain simulation with remote sensing data retrieved soil moisture
- The importance of Asian Australian land bridge in the onset
- The influence of SHAP on seasonal variation and Asian monsoon
- The influence of SHAP on upper level circulation
- The ka BP climate simulations - 2
- The model and the experimental schemes
- The nature of the South Asia High and its climate effects
- The potential evapotranspiration
- The Scheme for Retrieving Soil Moisture SRSM
- The temporal variation characteristics of soil moisture
- The validation of retrieved soil moisture
- Total precipitation
- Tree rings Dendroclimatology
- Tropical cyclones
- Typhoons
- Understanding the ENSOChina climate relations before
- Warm nights and cool nights
- Winter - 2
- Z M O