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Research Highlights Topic: Modeling

Quantifying the contributions of surface forcing to sea level variability along the US Gulf Coast
Quantifying the contributions of surface forcing to sea level variability along the US Gulf Coast
What explains the interannual variability of O2 content and distribution in the tropical Pacific?
What explains the interannual variability of O2 content and distribution in the tropical Pacific?
Intrinsic biases in AGCM and OGCM
Tracing the origins of equatorial Pacific biases in a coupled climate model
Coupled air-sea simulations reveal the dynamics of surface wave growth and breaking-induced dissipation
Coupled air-sea simulations reveal the dynamics of surface wave growth and breaking-induced dissipation
How interfering waves drive the MJO
How interfering waves drive the MJO
Comparing projections of multiple fire weather indices across the contiguous United States
Comparing projections of multiple fire weather indices across the contiguous United States
high-resolution global climate simulation ensembles highlights major advances in representing mesoscale convective systems (MCSs)
New high-resolution climate simulation ensembles highlight the importance of mesoscale dynamics in shaping future extreme precipitation
Figure 1. The 35-year trends of winter-spring sea surface temperature, precipitation, and sea level pressure. a, observation of 1980-2014. Model-simulated 35-year trends for pre-industrial climate grouped and averaged for b, the strongest El Niño-like trends and c, the strongest  La Niña-like trends. Model-simulated 35-year trends for 1980-2014  grouped and averaged for the ensemble members d, with the strongest El Niño-like trends and e, with the strongest La Niña-like trends.
Drivers of the Southwestern US precipitation decline
Adapted from Figures 6 and 11 of Chen et al. (2025). See full paper for more details and complete captions.
Small SST warm anomalies in Tropical Atlantic locally increase trade cumulus formation
Trend in SST and subsurface temperature for observation and Large Ensemble (LE) simulations
Why tropical Pacific subsurface cooling doesn't surface in climate models
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