Cooperation and Exchange
Climatology of Tibetan Plateau Vortices and Connection to Up...
CSSP MESETA - Simulation of the East Asian Summer Monsoon wi...
Factors Determining ENSO Asymmetry
Development of Resilient Design through the Understanding of...
Adiabatic Motions in the Oceans & Extended Isopycnal Analysi...
Jet Streams, Vortices, and the Antarctic Ozone Hole
Dependency of Radiation and Clouds to the Horizontal Resolut...
Using High Resolution Global Modelling for Improved Understa...
Investigating the Role of the Oceans in West African Monsoon...
ENSO in the Holocene: energetics and link with SPCZ
Pacific Sea Level Rise Pattern and Global Surface Temperatur...
Regional Re-analysis Without Regional Data
High-resolution Climate Modeling: Getting New Insights about...
Cloud Microphysics and the Interaction between Forcing and F...
Clouds after Paris: Why we must and how we can improve clima...
Global-to-regional Simulations of Aerosols with O(10 km) Gri...
Cloud Microphysics and Climate: Use of Satellite Observation...
Climate Feedbacks by Tropical Low Clouds: constraints from o...
The Influences of Southeastern Pacific and Tropical North At...
Interhemispheric SST Gradient Trends in the Indian Ocean Pri...
Understanding Land-atmosphere Interactions and Their Respons...
On Sea Ice Predictability in the US Arctic Regional Seas
Climate Downscaling Using LMDZ Model
An Efficient and Parallelizable Numerical Method For Random ...
Impacts of Climate Change on Arctic Storms and the Loss of S...
The Crucial Role of the Sahara Greening in Suppressing ENSO ...
Disentangling Natural and Anthropogenic Controls on Terrestr...
Mechanisms for El Niño and La Niña Evolution A...
Global Warming Hiatus and the Curious Intensification of Tra...
Two faces of Arctic and Antarctic climate change and their l...
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