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Skillful multiyear prediction of marine habitat shifts jointly constrained by ocean temperature and dissolved oxygen
Fast upper-level jet stream winds get faster under climate change
Sensitivity of data size vs. deep-learning model performance using GEFSv12  reforecast products for rainfall and temperatures over CONUS
Contribution of anthropogenic aerosols to persistent La Niña-like conditions in the early 21st century
Future water storage changes over the Mediterranean, Middle East, and North Africa in response to global warming and stratospheric aerosol intervention
Investigation of different ΣO/N2 variations observed by GOLD during a minor geomagnetic storm from 2 to 4 August 2021
Arctic heatwaves could significantly influence the isoprene emissions from shrubs
Measurements and modeling of the interhemispheric differences of atmospheric chlorinated very short-lived substances
Characterizing ice nucleating particles over the Southern Ocean using simultaneous aircraft and ship observations
Larger cloud liquid water enhances both aerosol indirect forcing and cloud radiative feedback in two Earth System Models
How does the Pinatubo eruption influence our understanding of long-term changes in ocean biogeochemistry?
Modeling the water systems of the Western US to support climate-resilient electricity system planning
Evaluating different geothermal heat-flow maps as basal boundary conditions during spin-up of the Greenland ice sheet
Community-driven marine archaeology: NOAA ocean exploration operations in the Pacific Basin 2024-2026
Validation of Aeolus L2B products over the tropical Atlantic using radiosondes
Water vapor measurements inside clouds and storms using a differential absorption radar
Last Glacial Maximum cooling induced positive moisture balance and maintained stable human populations in Australia
 Evaluating modelled tropospheric columns of CH 4 , CO, and O 3 in the Arctic using ground-based Fourier transform infrared (FTIR) measurements
Surface mass balance and climate of the Last Glacial Maximum Northern Hemisphere ice sheets: simulations with CESM2.1
The influence of terrain smoothing on simulated Convective Boundary-Layer depths in mountainous terrain

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