High-latitude Climates
High-latitude climates in the northern hemisphere occupy the northern subarctic and arctic latitude zones and includes an ocean that is largely surrounded by land. The Arctic is a complex system that includes physical, biological, chemical, and climatological processes that have changed over time. The Arctic is warming much faster than the rest of the planet in a process now known as Arctic amplification. Arctic scientists are working to understand future changes to permafrost, atmospheric and soil chemistry, sea ice, cloud processes, and more.
Aerosol Regimes and Processes with SAIL Data
Creating a Sea-Level-Enabled E3SM
ESGF2: Earth System Grid Federation 2
FAntSSIE: Framework for Antarctic System Science in E3SM
HiLAT-RASM: High Latitude Application and Testing of Earth System Models - Regional Arctic System Model
InteRFACE: Interdisciplinary Research for Arctic Coastal Environments
NGEE Arctic: Next Generation Ecosystem Experiments - Arctic
RUBISCO: Reducing Uncertainties in Biogeochemical Interactions through Synthesis and Computation
Soil Carbon Response to Environmental Change