An Innovative Approach to Improve Assessment of Climate Model Clouds: Scientists show the latest Community Atmospheric Model (CAM5) significantly improves cloud simulations
ESMD
J. E. Kay
2012-08
Exposing Global Cloud Biases in the Community Atmosphere Model (CAM) Using Satellite Observations and Their Corresponding Instrument Simulators
RGMA
J. E. Kay
2012-08
Pollution Weakens Monsoon's Might: Local, Global Emissions Suppress South Asian Summer Rainfall
ESMD
Dilip Ganguly
2012-07
Bytes for Bits: Researchers Develop a New, Efficient Aerosol Module for Climate Models
ESMD
Xiahong Liu
2012-05
Evaluating Aerosol-Cloud Interaction: Scientists Show Climate Model Reasonably Simulates The Relationship Between Aerosol And Cloud Droplet Size
ESMD
Chuanfeng Zhao
2012-04
Simplified Metrics for the Identification of the Madden-Julian Oscillation in Models
RGMA
Kenneth R. Sperber
Lawrence Livermore National Laboratory (LLNL)
2012-04
Desert Dust Intensifies Summer Rainfall in U.S. Southwest
ESMD
Chun Zhao
2012-04
Can Data Mining Help Constrain Climate Sensitivity?
RGMA
2012-03
The Future of Clean Air: Century-Scale Scenarios Connect Clean Air with Prosperity
MSD
Steven J Smith
2011-09
Atmospheric River Landfall-Latitude Changes in Future Climate Simulations
RGMA
Christine Shields
National Center for Atmospheric Research (NCAR)
Variability in the Sensitivity among Model Simulations of Permafrost and Carbon Dynamics in the Permafrost Region between 1960 and 2009
RGMA
David Lawrence
National Center for Atmospheric Research (NCAR)
The Land Use Model Intercomparison Project (LUMIP) Contribution to CMIP6: Rationale and experimental design
RGMA
David Lawrence
National Center for Atmospheric Research (NCAR)
Exploring an Ensemble-Based Approach to Atmospheric Climate Modeling and Testing at Scale
ESMD
Salil Mahajan
Oak Ridge National Laboratory (ORNL)
Exploration of Turbulent Heat Fluxes and Wind Stress Curl in WRF and ERA-Interim during Wintertime Mesoscale Wind Events Around Southeastern Greenland
RGMA
John Cassano
University of Colorado - Boulder
The Climatological Distribution of Extreme Arctic Winds and Implications for Ocean and Sea Ice Processes
RGMA
John Cassano
University of Colorado - Boulder
The Interaction of the SST Trend and La Nina in Austral Spring 2010
RGMA
Julie Arblaster
University of Monash
The Impact of the Southern Annular Mode on Future Changes in Southern Hemisphere
RGMA
Julie Arblaster
University of Monash
Simulated Differences in 21st Century Aridity due to Different Scenarios of GHG and Aerosols
RGMA
Andrew Gettelman
National Center for Atmospheric Research (NCAR)
The Effects of Volcanic Eruptions on Climate Prediction Skill
RGMA
Gerald Meehl
National Center for Atmospheric Research (NCAR)
Understanding the Varied Influence of the Mid-Latitude Jet on Clouds and Cloud-Radiative Effects in Observations and Global Climate Models
RGMA
Brian Medeiros
National Center for Atmospheric Research (NCAR)
The Global Methane Budget 2000 - 2012
RGMA
William J. Riley
Lawrence Berkeley National Laboratory (LBNL)
Discrete Conservation Properties for Shallow Water Flows using Mixed Mimetic Spectral Elements
ESMD
David Lee
Los Alamos National Laboratory (LANL)
Tracer Transport within an Unstructured Grid Ocean Model using Characteristic Discontinuous Galerkin Advection
ESMD
David Lee
Los Alamos National Laboratory (LANL)
CAUSES: On the Role of Surface Energy Budget Errors to the Warm Surface Air Temperature Error Over the Central United States
RGMA
Hsi-Yen Ma
Lawrence Livermore National Laboratory (LLNL)
Interdecadal Connection between Arctic Temperature and Summer Precipitation over the Yangtze River Valley in the CMIP5 Historical Simulations
RGMA
K Balaguru
Marine Low Cloud Cover is Likely to Decrease in the 21st Century
RGMA
On Increasing Global Temperatures: 75 Years After Callendar
RGMA
How Well Does ERA-Interim Reanalysis Replicate Trends in Extremes of Surface Temperature Across Europe
RGMA
Updated High-resolution Monthly Grids of Monthly Climatic Observations: The CRU TS 3.10 Data Set
RGMA
Independent Confirmation of Global Land Warming Without the Use of Station Temperatures
RGMA