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A New Dynamical Downscaling Approach and Its Validation With 30...
IAP reveals the biases in simulation of the Indian Ocean basin ...
What Are Moisture Sources of the Torrential Rainfall in the Sic...
Precipitation over East Asia Simulated by NCAR CAM5 at Differen...
Tropical Indian Ocean Warming Intensifies Winter Precipitation ...
Two Major Circulation Structures Leading to Heavy Summer Rainfa...
What Caused the Decrease of Eurasian Snow at the Late 1980s?
How Do Groundwater Exploitation and Utilization Affect Land Sur...
Simulated heat sink in the Southern Ocean and its contribution ...
Global Warming Hiatus Explained by Natural Climate Variations
Observed diurnal cycle of summer precipitation over South Asia ...
How Does Land Use and Land Cover Change Affect Monsoon Asian Cl...
The Siberian high under global warming in CMIP5 models
IAP Scientists Identified Key Circulation Features of Northeast...
ENSO—East Asian Winter Monsoon Relationship Depends on the ENS...
Interannual climate variability of the past millennium from sim...
Systematic model biases and their origins are identified to imp...
Projected climate change against natural internal variability o...
IAP reveals the Indo-Pacific forcing of SCS precipitation varia...
How Do North Atlantic Oscillation and Euro-Atlantic Blocking Af...
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