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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Published in:Monthly Weather Review
Main Authors: Lamraoui, Fayçal, Booth, James F., Naud, Catherine M.
Language:unknown
Published: 2021
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1541866
https://www.osti.gov/biblio/1541866
https://doi.org/10.1175/mwr-d-17-0281.1
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spelling ftosti:oai:osti.gov:1541866 2023-07-30T04:05:20+02:00 WRF Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study Lamraoui, Fayçal Booth, James F. Naud, Catherine M. 2021-08-02 application/pdf http://www.osti.gov/servlets/purl/1541866 https://www.osti.gov/biblio/1541866 https://doi.org/10.1175/mwr-d-17-0281.1 unknown http://www.osti.gov/servlets/purl/1541866 https://www.osti.gov/biblio/1541866 https://doi.org/10.1175/mwr-d-17-0281.1 doi:10.1175/mwr-d-17-0281.1 54 ENVIRONMENTAL SCIENCES 2021 ftosti https://doi.org/10.1175/mwr-d-17-0281.1 2023-07-11T09:34:58Z 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-km 2 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 SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Monthly Weather Review 146 8 2417 2432
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Lamraoui, Fayçal
Booth, James F.
Naud, Catherine M.
WRF Hindcasts of Cold Front Passages over the ARM Eastern North Atlantic Site: A Sensitivity Study
topic_facet 54 ENVIRONMENTAL SCIENCES
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-km 2 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.
author Lamraoui, Fayçal
Booth, James F.
Naud, Catherine M.
author_facet Lamraoui, Fayçal
Booth, James F.
Naud, Catherine M.
author_sort Lamraoui, Fayçal
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 2021
url http://www.osti.gov/servlets/purl/1541866
https://www.osti.gov/biblio/1541866
https://doi.org/10.1175/mwr-d-17-0281.1
genre North Atlantic
genre_facet North Atlantic
op_relation http://www.osti.gov/servlets/purl/1541866
https://www.osti.gov/biblio/1541866
https://doi.org/10.1175/mwr-d-17-0281.1
doi:10.1175/mwr-d-17-0281.1
op_doi https://doi.org/10.1175/mwr-d-17-0281.1
container_title Monthly Weather Review
container_volume 146
container_issue 8
container_start_page 2417
op_container_end_page 2432
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