Results 221 to 230 of about 11,795 (298)
Rising flood risks in semiarid South Asia driven by changing intraseasonal oscillations under global warming. [PDF]
Xie J +6 more
europepmc +1 more source
Reversal of the ITCZ Shift During the Satellite Era
Abstract A southward shift of the Intertropical Convergence Zone (ITCZ) during the latter half of the 20th century has been primarily attributed to interhemispheric differences in anthropogenic aerosol forcing. However, in recent decades anthropogenic aerosol emissions have declined, particularly over Northern Hemisphere (NH).
S. Shrestha, B. J. Soden, H. He
wiley +1 more source
Widespread increase in frequency and duration of European wind droughts based on CMIP6 projections. [PDF]
Mostue IA +4 more
europepmc +1 more source
Interactive Climate Projection via Conditional Generative AI
Abstract Dynamical Earth System Models are extremely expensive, requiring ∼106 core‐hours for century‐scale simulations. This limits climate projections to only a few Shared Socioeconomic Pathways (SSPs) and leaves numerous policy trajectories unexplored.
Chengjie Sun +4 more
wiley +1 more source
Warming and vegetation greening drive recent surge in flash droughts. [PDF]
Li J +10 more
europepmc +1 more source
Abstract The northern Atlantic south of Greenland and Iceland is the only part of the world which has cooled significantly since the 19th Century both in the atmosphere and ocean. The oceanic cooling is widely assumed to be a result of reduced ocean heat transport into this region.
Stefan Rahmstorf +5 more
wiley +1 more source
Correction: The Ouranos CRCM5-CMIP6 ensemble: A dynamically downscaled ensemble of CMIP6 simulations over North America. [PDF]
Paquin D +7 more
europepmc +1 more source
SamudrACE: Fast and Accurate Coupled Climate Modeling With 3D Ocean and Atmosphere Emulators
Abstract Traditional numerical global climate models simulate the full Earth system by exchanging boundary conditions between separate simulators of the atmosphere, ocean, sea ice, land surface, and other geophysical processes. This paradigm allows for distributed development of individual components within a common framework, unified by a coupler that
James P. C. Duncan +17 more
wiley +1 more source

