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Classification of warm-season precipitation in High-Resolution Rapid Refresh (HRRR) model forecasts over the contiguous United States
Perturbing parameters to understand cloud contributions to climate change
Satellite-based solar-induced fluorescence tracks seasonal and elevational patterns of photosynthesis in California’s Sierra Nevada mountains
Pliocene Model Intercomparison Project Phase 3 (PlioMIP3) – Science plan and experimental design
Evaluation of a stochastic mixing scheme in the deep convective gray zone using a tropical oceanic deep convection case study
Advancing South American water and climate science through multidecadal Convection-Permitting modeling
 Investigation of hydrostatic imbalance with field observations
Improvements in September Arctic sea ice predictions via assimilation of summer CryoSat-2 sea ice thickness observations
Surface ocean cooling in the Eocene North Atlantic coincides with declining atmospheric CO2
Greenhouse gas forcing and climate feedback signatures identified in hyperspectral infrared satellite observations
Comprehensive analysis of the NOAA National Water Model: A call for heterogeneous formulations and diagnostic model selection
 Tracking mesoscale convective systems in IMERG and regional variability of their properties in the tropics
Mesospheric water vapor from SABER as a tracer for the residual mean circulation during SSW events
Quantifying the contributions of aerosol - and snow-produced ClNO 2 through observations and 1D modeling
Sources of Formaldehyde in U.S. Oil and Gas Production Regions
Editorial to the Topical Collection: Solar and stellar dynamos: A new era
Two-dimensional inverse energy cascade in a laboratory surf zone for varying wave directional spread
Long-term annual and seasonal mass balance reconstruction and sensitivity analysis of Chhota Shigri Glacier in Western Himalaya
Observation-based sowing dates and cultivars significantly affect yield and irrigation for some crops in the Community Land Model (CLM5)
Recent multi-decadal Southern Ocean surface cooling unlikely caused by Southern Annular Mode trends

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