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Can We Do Better at Teaching Mathematics to Undergraduate Atmospheric Science Students?
Accurate assessment of land–atmosphere coupling in climate models requires high-frequency data output
NSF NCAR C-130 during CAESAR
Interannual Variability of Winds in the Antarctic Mesosphere and Lower Thermosphere Over Rothera (67°S, 68°W) During 2005–2021 in Meteor Radar Observations and WACCM‐X
New model ensemble reveals how forcing uncertainty and model structure alter climate simulated across CMIP generations of the Community Earth System Model
A new process-based and scale-aware desert dust emission scheme for global climate models – Part II: Evaluation in the Community Earth System Model version 2 (CESM2)
Local Volume Solvers for Earth System Data Assimilation: Implementation in the Framework for Joint Effort for Data Assimilation Integration
Detecting the human fingerprint in the summer 2022 western–central European soil drought
Energy-conserving physics for nonhydrostatic dynamics in mass coordinate models
NSF NCAR C-130 ahead of CAESAR field campaign
NSF NCAR C-130 during preparations for CAESAR
Towards the definition of a solar forcing dataset for CMIP7
A bioenergy-focused versus a reforestation-focused mitigation pathway yields disparate carbon storage and climate responses
 Underestimation of multi-decadal global O 2 loss due to  an optimal interpolation method
Snow water equivalent retrieval over Idaho – Part 2: Using L-band UAVSAR repeat-pass interferometry
Observationally constrained analysis of sulfur cycle in the marine atmosphere with NASA ATom measurements and AeroCom model simulations
The utility of simulated ocean chlorophyll observations: a case study with the Chlorophyll Observation Simulator Package  (version 1) in CESMv2.2
Experimental Evidence on Four Policies to Increase Learning at Scale
FAIR Facilities and Instruments Workshop #1 Report: Exploring Persistent Identifier Needs, Barriers and Incentives
The Extraordinary March 2022 East Antarctica “Heat” Wave. Part II: Impacts on the Antarctic Ice Sheet

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