Representation of Ethiopian Wet Spells in Global and Nested Models

Weather forecast and reanalysis models exhibit different performance in daily rainfall estimation over the Ethiopian highlands, 2000–2012, with ECMWF closer to observations than other models. Background is given to illustrate the Hadley circulation and easterly jets over Ethiopia, using sections on...

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Main Authors: Mark R. Jury, Sen Chiao
Format: Article
Language:English
Published: Wiley 2014-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2014/237374
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author Mark R. Jury
Sen Chiao
author_facet Mark R. Jury
Sen Chiao
author_sort Mark R. Jury
collection DOAJ
description Weather forecast and reanalysis models exhibit different performance in daily rainfall estimation over the Ethiopian highlands, 2000–2012, with ECMWF closer to observations than other models. Background is given to illustrate the Hadley circulation and easterly jets over Ethiopia, using sections on 37°E in July–August 2011. ECMWF reanalysis has a narrow band of rainfall >15 mm/day on 10°N, consistent with TRMM satellite estimates, associated with a steep gradient in meridional wind. MERRA and GFS models have a wider band of rainfall and weaker gradients in meridional winds. The contrasting background states influence a nested WRF model simulation of heavy rain in the upper Nile Valley on 29 July, 2011. The GFS (ECMWF) initialization yields stronger northerly (southerly) winds north (south) of Ethiopia, while aircraft observations are southerly at 850 mb and northerly at 700 mb. ECMWF produces heavy and widespread rainfall consistent with observations, with a potentially more realistic simulation of the Hadley circulation.
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spelling doaj-art-4a38259d170044bc8a7202e4947f3c482025-02-03T00:59:51ZengWileyAdvances in Meteorology1687-93091687-93172014-01-01201410.1155/2014/237374237374Representation of Ethiopian Wet Spells in Global and Nested ModelsMark R. Jury0Sen Chiao1University of Zululand, KwaDlangezwa, Richards Bay 3886, South AfricaDepartment of Meteorology and Climate Science, San José State University, San José, CA 95192, USAWeather forecast and reanalysis models exhibit different performance in daily rainfall estimation over the Ethiopian highlands, 2000–2012, with ECMWF closer to observations than other models. Background is given to illustrate the Hadley circulation and easterly jets over Ethiopia, using sections on 37°E in July–August 2011. ECMWF reanalysis has a narrow band of rainfall >15 mm/day on 10°N, consistent with TRMM satellite estimates, associated with a steep gradient in meridional wind. MERRA and GFS models have a wider band of rainfall and weaker gradients in meridional winds. The contrasting background states influence a nested WRF model simulation of heavy rain in the upper Nile Valley on 29 July, 2011. The GFS (ECMWF) initialization yields stronger northerly (southerly) winds north (south) of Ethiopia, while aircraft observations are southerly at 850 mb and northerly at 700 mb. ECMWF produces heavy and widespread rainfall consistent with observations, with a potentially more realistic simulation of the Hadley circulation.http://dx.doi.org/10.1155/2014/237374
spellingShingle Mark R. Jury
Sen Chiao
Representation of Ethiopian Wet Spells in Global and Nested Models
Advances in Meteorology
title Representation of Ethiopian Wet Spells in Global and Nested Models
title_full Representation of Ethiopian Wet Spells in Global and Nested Models
title_fullStr Representation of Ethiopian Wet Spells in Global and Nested Models
title_full_unstemmed Representation of Ethiopian Wet Spells in Global and Nested Models
title_short Representation of Ethiopian Wet Spells in Global and Nested Models
title_sort representation of ethiopian wet spells in global and nested models
url http://dx.doi.org/10.1155/2014/237374
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AT senchiao representationofethiopianwetspellsinglobalandnestedmodels