Seasonal range test run with Global Eta Framework

Global Eta Framework (GEF) is a global atmospheric model developed in general curvilinear coordinates and capable of running on arbitrary rectangular quasi-uniform spherical grids, using stepwise (<q>Eta</q>) representation of the terrain. In this study, the model is run on a cubed-s...

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Main Authors: D. Latinović, S. C. Chou, M. Rančić
Format: Article
Language:English
Published: Copernicus Publications 2017-07-01
Series:Advances in Science and Research
Online Access:https://www.adv-sci-res.net/14/247/2017/asr-14-247-2017.pdf
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spelling doaj-be77cd6dd8b24a0787eb6ee6c7a448082020-11-24T21:44:55ZengCopernicus PublicationsAdvances in Science and Research1992-06281992-06362017-07-011424725110.5194/asr-14-247-2017Seasonal range test run with Global Eta FrameworkD. Latinović0S. C. Chou1M. Rančić2CPTEC/INPE, Cachoeira Paulista, 12630-000, SP, BrazilCPTEC/INPE, Cachoeira Paulista, 12630-000, SP, BrazilNCEP, College Park, 20740, MD, USAGlobal Eta Framework (GEF) is a global atmospheric model developed in general curvilinear coordinates and capable of running on arbitrary rectangular quasi-uniform spherical grids, using stepwise (<q>Eta</q>) representation of the terrain. In this study, the model is run on a cubed-sphere grid topology, in a version with uniform Jacobians (UJ), which provides <q>equal-area</q> grid cells, and a smooth transition of coordinate lines across the edges of the cubed-sphere. Within a project at the Brazilian Center for Weather Forecasts and Climate Studies (CPTEC), a nonhydrostatic version of this model is under development and will be applied for seasonal prediction studies. This note describes preliminary tests with the GEF on the UJ cubed-sphere in which model performance is evaluated in seasonal simulations at a horizontal resolution of approximately 25 km, running in the hydrostatic mode. Comparison of these simulations with the ERA-Interim reanalyses shows that the 850 hPa temperature is underestimated, while precipitation pattern is mostly underestimated in tropical continental regions and overestimated in tropical oceanic regions. Nevertheless, the model is still able to well capture the main seasonal climate characteristics. These results will be used as a control run in further tests with the nonhydrostatic version of the model.https://www.adv-sci-res.net/14/247/2017/asr-14-247-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. Latinović
S. C. Chou
M. Rančić
spellingShingle D. Latinović
S. C. Chou
M. Rančić
Seasonal range test run with Global Eta Framework
Advances in Science and Research
author_facet D. Latinović
S. C. Chou
M. Rančić
author_sort D. Latinović
title Seasonal range test run with Global Eta Framework
title_short Seasonal range test run with Global Eta Framework
title_full Seasonal range test run with Global Eta Framework
title_fullStr Seasonal range test run with Global Eta Framework
title_full_unstemmed Seasonal range test run with Global Eta Framework
title_sort seasonal range test run with global eta framework
publisher Copernicus Publications
series Advances in Science and Research
issn 1992-0628
1992-0636
publishDate 2017-07-01
description Global Eta Framework (GEF) is a global atmospheric model developed in general curvilinear coordinates and capable of running on arbitrary rectangular quasi-uniform spherical grids, using stepwise (<q>Eta</q>) representation of the terrain. In this study, the model is run on a cubed-sphere grid topology, in a version with uniform Jacobians (UJ), which provides <q>equal-area</q> grid cells, and a smooth transition of coordinate lines across the edges of the cubed-sphere. Within a project at the Brazilian Center for Weather Forecasts and Climate Studies (CPTEC), a nonhydrostatic version of this model is under development and will be applied for seasonal prediction studies. This note describes preliminary tests with the GEF on the UJ cubed-sphere in which model performance is evaluated in seasonal simulations at a horizontal resolution of approximately 25 km, running in the hydrostatic mode. Comparison of these simulations with the ERA-Interim reanalyses shows that the 850 hPa temperature is underestimated, while precipitation pattern is mostly underestimated in tropical continental regions and overestimated in tropical oceanic regions. Nevertheless, the model is still able to well capture the main seasonal climate characteristics. These results will be used as a control run in further tests with the nonhydrostatic version of the model.
url https://www.adv-sci-res.net/14/247/2017/asr-14-247-2017.pdf
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