 |
Dipole Mode of the Precipitation Anomaly Over the Tibetan Plateau in Mid-Autumn Associated With Tropical Pacific-Indian Ocean Sea Surface Temperature Anomaly: Role of Convection Over the Northern Maritime Continent |
|
|
 |
Arctic autumn warming since 2002 dominated by changes in moisture modulated by multiple large-scale atmospheric circulations |
|
|
 |
Precursor effect of the Tibetan Plateau heating anomaly on the seasonal march of the East Asian summer monsoon precipitation |
|
|
 |
Connection between winter Arctic sea ice and west Tibetan Plateau snow depth through the NAO |
|
|
 |
Asymmetrical Response of the East Asian Summer Monsoon to the Quadrennial Oscillation of Global Sea Surface Temperature Associated With the Tibetan Plateau Thermal Feedback |
|
|
 |
Atmospheric Bridge Connecting the Barents Sea Ice and Snow Depth in the Mid-West Tibetan Plateau |
|
|
 |
Interdecadal summer warming of the Tibetan Plateau potentially regulated by a sea surface temperature anomaly in the Labrador Sea |
|
|
 |
Land–atmosphere–ocean coupling associated with the Tibetan Plateau and its climate impacts |
|
|
 |
The energy and water cycles under climate change |
|
|
 |
CASEarth Poles: Big Data for the Three Poles |
|
|