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Diurnal cycle of precipitation over the tropics and central United States: Intercomparison of general circulation models
The polar field reversal process over five solar cycles
Brief communication: The Lahaina Fire disaster - how models can be used to understand and predict wildfires
Intensification and weakening of equatorial plasma bubble development observed by GOLD during different phases of a geomagnetic storm
Evaluation of multi-decadal UCLA-CFSv2 simulation and impact of interactive atmospheric-ocean feedback on global and regional variability
Detection of Superrefraction at the top of the Atmospheric Boundary Layer from COSMIC-2 Radio Occultations
Surface mass balance and climate of the Last Glacial Maximum Northern Hemisphere ice sheets: simulations with CESM2.1
Separating daily 1 km PM 2.5 inorganic chemical composition in China since 2000 via deep learning integrating ground, satellite, and model data
The African regional greenhouse gases budget (2010-2019)
Chemical data assimilation with aqueous chemistry in WRF‐Chem coupled with WRFDA (V4.4.1)
Explaining and predicting Earth system change: A world climate research programme call to action
Advancing solar magnetic field extrapolations through multiheight magnetic field measurements
Validation of Aeolus L2B products over the tropical Atlantic using radiosondes
Future water storage changes over the Mediterranean, Middle East, and North Africa in response to global warming and stratospheric aerosol intervention
Can models adequately reflect how long-term nitrogen enrichment alters the forest soil carbon cycle?
Improving Postdoctoral Training Programs through alumni perspectives and experiences: A study of NCAR’s Advanced Study Program
Anomalously large latent heat fluxes in low to moderate wind conditions within the eddy-rich zone of the Northwestern Pacific
Simulation of groundwater-flow dynamics in the U.S. Northern High Plains driven by multi-model estimates of surficial aquifer recharge
Applications of aerosondes in the Arctic
Assessment of the sensitivity to the thermal roughness length in Noah and Noah-MP land surface model using WRF in an arid region

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