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Supporting advancement in weather and water prediction in the Upper Colorado River Basin: The SPLASH campaign
Geochemical differences between alive, uncrusted and dead, crusted shells of Neogloboquadrina pachyderma: Implications for paleoreconstruction
Evaluating skill in predicting the Interdecadal Pacific Oscillation in initialized decadal climate prediction hindcasts in E3SMv1 and CESM1 using two different initialization methods and a small set of start years
Little change in apparent hydrological sensitivity at large CO2 forcing
Emission factors for crop residue and prescribed fires in the Eastern US during FIREX-AQ
The role of in-cloud wet removal in simulating aerosol vertical profiles and cloud radiative forcing
Sensitivity of burned area and fire radiative power predictions to containment efforts, fuel density, and fuel moisture using WRF-fire
Future dust concentration over the Middle East and North Africa region under global warming and stratospheric aerosol intervention scenarios
Projections of winter polynyas and their biophysical impacts in the Ross Sea Antarctica
 Inferring the photolysis rate of NO 2 in the stratosphere based on satellite observations
My rewarding life in science
Magnetohydrodynamic mode conversion in the solar corona: Insights from Fresnel-like models of waves at sharp interfaces
Diagnosing Hurricane Barry track errors and evaluating physics scalability in the UFS Short-Range Weather Application
Assimilation of the AMSU-A radiances using the CESM (v2.1.0) and the DART (v9.11.13)–RTTOV (v12.3)
Global health and climate effects of organic aerosols from different sources
The lack of a QBO-MJO connection in climate models with a nudged stratosphere
Climate base state influences on South Asian monsoon processes derived from analyses of E3SMv2 and CESM2
On the links between ice nucleation, cloud phase, and climate sensitivity in CESM2
The QBO-MJO connection: A possible role for the SST and ENSO
OH, HO2, and RO2 radical chemistry in a rural forest environment: Measurements, model comparisons, and evidence of a missing radical sink

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