Wrf Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study

The present study explores the ability of the Weather Research and Forecasting (WRF) Model to accurately reproduce the passage of extratropical cold fronts at the DOE ARM eastern North Atlantic (ENA) observation site on the Azores. An analysis of three case studies is performed in which the impact o...

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Main Authors: Lamraoui, Faycal, Booth, James F., Naud, Catherine M.
Format: Other/Unknown Material
Language:unknown
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/2060/20180005451
id ftnasantrs:oai:casi.ntrs.nasa.gov:20180005451
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:20180005451 2023-05-15T17:31:20+02:00 Wrf Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study Lamraoui, Faycal Booth, James F. Naud, Catherine M. Unclassified, Unlimited, Publicly available July 16,2018 application/pdf http://hdl.handle.net/2060/20180005451 unknown Document ID: 20180005451 http://hdl.handle.net/2060/20180005451 Copyright, Use by or on behalf of the U.S. Government permitted CASI Meteorology and Climatology GSFC-E-DAA-TN57716 Monthly Weather Review (ISSN 0027-0644) (e-ISSN 1520-0493); 146; 8; 2417–2432 2018 ftnasantrs 2019-11-02T23:47:15Z The present study explores the ability of the Weather Research and Forecasting (WRF) Model to accurately reproduce the passage of extratropical cold fronts at the DOE ARM eastern North Atlantic (ENA) observation site on the Azores. An analysis of three case studies is performed in which the impact of the WRF domain size, position of the model boundary relative to the ENA site, grid spacing, and spectral nudging conditions are explored. The results from these case studies indicate that model biases in the timing and duration of cold front passages change with the distance between the model domain boundary and the ENA site. For these three cases, if the western model boundary is farther than 1500 km from the site, the front becomes too meridional and fails to reach the site, making 1000 or 1500 km the optimal distances. In contrast, integrations with small distances (e.g., 500 km) between the site and domain boundaries have inadequate spatial spinup (i.e., the domain is too small for the model to properly stabilize). For all three cases, regardless of domain size, the model has biases in its upper-level circulation that impact the position and timing of the front. However, this issue is most serious for 4000-km2 domains and larger. For these domains, prolonged spectral nudging can correct cold front biases. As such, this analysis provides a framework to optimize the WRF Model configuration necessary for a realistic hindcast of a cold front passage at a fixed location centered in a domain as large as computationally possible. Other/Unknown Material North Atlantic NASA Technical Reports Server (NTRS)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic Meteorology and Climatology
spellingShingle Meteorology and Climatology
Lamraoui, Faycal
Booth, James F.
Naud, Catherine M.
Wrf Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study
topic_facet Meteorology and Climatology
description The present study explores the ability of the Weather Research and Forecasting (WRF) Model to accurately reproduce the passage of extratropical cold fronts at the DOE ARM eastern North Atlantic (ENA) observation site on the Azores. An analysis of three case studies is performed in which the impact of the WRF domain size, position of the model boundary relative to the ENA site, grid spacing, and spectral nudging conditions are explored. The results from these case studies indicate that model biases in the timing and duration of cold front passages change with the distance between the model domain boundary and the ENA site. For these three cases, if the western model boundary is farther than 1500 km from the site, the front becomes too meridional and fails to reach the site, making 1000 or 1500 km the optimal distances. In contrast, integrations with small distances (e.g., 500 km) between the site and domain boundaries have inadequate spatial spinup (i.e., the domain is too small for the model to properly stabilize). For all three cases, regardless of domain size, the model has biases in its upper-level circulation that impact the position and timing of the front. However, this issue is most serious for 4000-km2 domains and larger. For these domains, prolonged spectral nudging can correct cold front biases. As such, this analysis provides a framework to optimize the WRF Model configuration necessary for a realistic hindcast of a cold front passage at a fixed location centered in a domain as large as computationally possible.
format Other/Unknown Material
author Lamraoui, Faycal
Booth, James F.
Naud, Catherine M.
author_facet Lamraoui, Faycal
Booth, James F.
Naud, Catherine M.
author_sort Lamraoui, Faycal
title Wrf Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study
title_short Wrf Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study
title_full Wrf Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study
title_fullStr Wrf Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study
title_full_unstemmed Wrf Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study
title_sort wrf hindcasts of cold front passages over the arm eastern north atlantic site: a sensitivity study
publishDate 2018
url http://hdl.handle.net/2060/20180005451
op_coverage Unclassified, Unlimited, Publicly available
genre North Atlantic
genre_facet North Atlantic
op_source CASI
op_relation Document ID: 20180005451
http://hdl.handle.net/2060/20180005451
op_rights Copyright, Use by or on behalf of the U.S. Government permitted
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