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Dynamics of track deflection associated with the passage of a tropical cyclone over a mesoscale mountain
Comparing Statistics of Precipitation Variations during the American Monsoon in CESM1
Statistical characteristics of nighttime Medium-Scale Traveling Ionospheric Disturbances from 10-years of airglow observation by the machine learning method
Alfvénic thermospheric upwelling in a global geospace model
A high-resolution Asia-Pacific regional coupled prediction system with dynamically downscaling coupled data assimilation
Ensemble-based estimates of the predictability of wind-driven coastal ocean flow over topography
The path to CAM6: Coupled simulations with CAM5.4 and CAM5.5
Simulation of hurricane-ocean interaction for Hurricane Katrina: Coupling WRF with a 1-D ocean model
Coordination to understand and reduce global model biases by U.S. and Chinese institutions
Taking a multi-pronged approach to expand the reach of climate research results [poster]
Comparing machine learning-derived global estimates of soil respiration and its components with those from terrestrial ecosystem models
The use of the Community Earth System Model in human dimensions climate research and applications
Coupled air quality and boundary-layer meteorology in Western U.S. basins during winter: Design and rationale for a comprehensive study
Confronting the challenge of modeling cloud and precipitation microphysics
The positive North Atlantic oscillation with downstream blocking and Middle East snowstorms: The large-scale environment
A decomposition of feedback contributions to Polar warming amplification
An urban parameterization for a global climate model. Part II: Sensitivity to input parameters and the simulated urban heat island in offline simulations
Variability in the sensitivity among model simulations of permafrost and carbon dynamics in the permafrost region between 1960 and 2009
Evaluation of WRF model output for severe-weather forecasting from the 2008 NOAA Hazardous Weather Testbed Spring Experiment
The response of the Walker circulation to Last Glacial Maximum forcing: Implications for detection in proxies

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