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Projecting Antarctica's contribution to future sea level rise from basal ice shelf melt using linear response functions of 16 ice sheet models (LARMIP-2)
The Community Climate System Model
Climates of the 20th and 21st centuries simluated by the NCAR Climate System Model
Improvements in typhoon forecasts with assimilated GPS occultation refractivity
High ice water content conditions associated with airborne temperature measurement anomalies near tropical convection [presentation]
HTAP2 multi-model estimates of premature human mortality due to intercontinental transport of air pollution and emission sectors
Detecting the permafrost carbon feedback: Talik formation and increased cold-season respiration as precursors to sink-to-source transitions
Harmonising the land-use flux estimates of global models and national inventories for 2000-2020
Ozone depletion and climate change: Impacts on UV radiation
Robust land-ocean contrasts in energy and water cycle feedbacks
Ionosphere Sounding for Pre-seismic Anomalies Identification (INSPIRE): Results of the Project and Perspectives for the Short-Term Earthquake Forecast
Synthetic Lyman-α emissions for the coronagraph aboard the ASO-S mission
An evaluation of ENSO asymmetry in the community climate system models: A view from the subsurface
Ozone depletion and climate change: Impacts on UV radiation
Variational assimilation of precipitable water using a nonhydrostatic mesoscale adjoint model. Part I: Moisture retrieval and sensitivity experiments
Phase characterization of cold sector southern ocean cloud tops: Results from SOCRATES
Dispersion of droplet size distributions in supercooled non‐precipitating stratocumulus from aircraft observations obtained during the Southern Ocean Cloud Radiation Aerosol Transport Experimental Study
The role of natural halogens in global tropospheric ozone chemistry and budget under different 21st century climate scenarios
Description and performance of a sectional aerosol microphysical model in the Community Earth System Model (CESM2)
Annual cycle in upper-ocean heat content and the global energy budget

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