Development of the GEOS-5 atmospheric general circulation model: evolution from MERRA to MERRA2

The Modern-Era Retrospective Analysis for Research and Applications-2 (MERRA2) version of the Goddard Earth Observing System-5 (GEOS-5) atmospheric general circulation model (AGCM) is currently in use in the NASA Global Modeling and Assimilation Office (GMAO) at a wide range of resolutions for a var...

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Main Authors: A. Molod, L. Takacs, M. Suarez, J. Bacmeister
Format: Article
Language:English
Published: Copernicus Publications 2015-05-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/8/1339/2015/gmd-8-1339-2015.pdf
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author A. Molod
L. Takacs
M. Suarez
J. Bacmeister
author_facet A. Molod
L. Takacs
M. Suarez
J. Bacmeister
author_sort A. Molod
collection DOAJ
description The Modern-Era Retrospective Analysis for Research and Applications-2 (MERRA2) version of the Goddard Earth Observing System-5 (GEOS-5) atmospheric general circulation model (AGCM) is currently in use in the NASA Global Modeling and Assimilation Office (GMAO) at a wide range of resolutions for a variety of applications. Details of the changes in parameterizations subsequent to the version in the original MERRA reanalysis are presented here. Results of a series of atmosphere-only sensitivity studies are shown to demonstrate changes in simulated climate associated with specific changes in physical parameterizations, and the impact of the newly implemented resolution-aware behavior on simulations at different resolutions is demonstrated. The GEOS-5 AGCM presented here is the model used as part of the GMAO MERRA2 reanalysis, global mesoscale simulations at 10 km resolution through 1.5 km resolution, the real-time numerical weather prediction system, and for atmosphere-only, coupled ocean-atmosphere and coupled atmosphere-chemistry simulations. <br><br> The seasonal mean climate of the MERRA2 version of the GEOS-5 AGCM represents a substantial improvement over the simulated climate of the MERRA version at all resolutions and for all applications. Fundamental improvements in simulated climate are associated with the increased re-evaporation of frozen precipitation and cloud condensate, resulting in a wetter atmosphere. Improvements in simulated climate are also shown to be attributable to changes in the background gravity wave drag, and to upgrades in the relationship between the ocean surface stress and the ocean roughness. The series of resolution-aware parameters related to the moist physics was shown to result in improvements at higher resolutions and result in AGCM simulations that exhibit seamless behavior across different resolutions and applications.
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spelling doaj.art-d2b2fe86a36143bb948a96499e6a4faa2022-12-22T01:25:23ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032015-05-01851339135610.5194/gmd-8-1339-2015Development of the GEOS-5 atmospheric general circulation model: evolution from MERRA to MERRA2A. Molod0L. Takacs1M. Suarez2J. Bacmeister3University of Maryland College Park, College Park, MD, USAScience Systems and Applications, Inc., Lanham, MD, USANASA Goddard Space Flight Center, Greenbelt, MD, USANational Center for Atmospheric Research, Boulder, CO, USAThe Modern-Era Retrospective Analysis for Research and Applications-2 (MERRA2) version of the Goddard Earth Observing System-5 (GEOS-5) atmospheric general circulation model (AGCM) is currently in use in the NASA Global Modeling and Assimilation Office (GMAO) at a wide range of resolutions for a variety of applications. Details of the changes in parameterizations subsequent to the version in the original MERRA reanalysis are presented here. Results of a series of atmosphere-only sensitivity studies are shown to demonstrate changes in simulated climate associated with specific changes in physical parameterizations, and the impact of the newly implemented resolution-aware behavior on simulations at different resolutions is demonstrated. The GEOS-5 AGCM presented here is the model used as part of the GMAO MERRA2 reanalysis, global mesoscale simulations at 10 km resolution through 1.5 km resolution, the real-time numerical weather prediction system, and for atmosphere-only, coupled ocean-atmosphere and coupled atmosphere-chemistry simulations. <br><br> The seasonal mean climate of the MERRA2 version of the GEOS-5 AGCM represents a substantial improvement over the simulated climate of the MERRA version at all resolutions and for all applications. Fundamental improvements in simulated climate are associated with the increased re-evaporation of frozen precipitation and cloud condensate, resulting in a wetter atmosphere. Improvements in simulated climate are also shown to be attributable to changes in the background gravity wave drag, and to upgrades in the relationship between the ocean surface stress and the ocean roughness. The series of resolution-aware parameters related to the moist physics was shown to result in improvements at higher resolutions and result in AGCM simulations that exhibit seamless behavior across different resolutions and applications.http://www.geosci-model-dev.net/8/1339/2015/gmd-8-1339-2015.pdf
spellingShingle A. Molod
L. Takacs
M. Suarez
J. Bacmeister
Development of the GEOS-5 atmospheric general circulation model: evolution from MERRA to MERRA2
Geoscientific Model Development
title Development of the GEOS-5 atmospheric general circulation model: evolution from MERRA to MERRA2
title_full Development of the GEOS-5 atmospheric general circulation model: evolution from MERRA to MERRA2
title_fullStr Development of the GEOS-5 atmospheric general circulation model: evolution from MERRA to MERRA2
title_full_unstemmed Development of the GEOS-5 atmospheric general circulation model: evolution from MERRA to MERRA2
title_short Development of the GEOS-5 atmospheric general circulation model: evolution from MERRA to MERRA2
title_sort development of the geos 5 atmospheric general circulation model evolution from merra to merra2
url http://www.geosci-model-dev.net/8/1339/2015/gmd-8-1339-2015.pdf
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