A Model-Based Climatology of Low-Level Jets in the Weddell Sea Region of the Antarctic

Low-level jets (LLJs) are climatological features in polar regions. It is well known that katabatic winds over the slopes of the Antarctic ice sheet are associated with strong LLJs. Barrier winds occurring, e.g., along the Antarctic Peninsula may also show LLJ structures. A few observational studies...

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Published in:Atmosphere
Main Authors: Günther Heinemann, Rolf Zentek
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12121635
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spelling ftmdpi:oai:mdpi.com:/2073-4433/12/12/1635/ 2023-08-20T04:02:24+02:00 A Model-Based Climatology of Low-Level Jets in the Weddell Sea Region of the Antarctic Günther Heinemann Rolf Zentek agris 2021-12-07 application/pdf https://doi.org/10.3390/atmos12121635 EN eng Multidisciplinary Digital Publishing Institute Atmospheric Techniques, Instruments, and Modeling https://dx.doi.org/10.3390/atmos12121635 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 12; Pages: 1635 Antarctic stable boundary layer low-level jets inversion katabatic winds Text 2021 ftmdpi https://doi.org/10.3390/atmos12121635 2023-08-01T03:28:42Z Low-level jets (LLJs) are climatological features in polar regions. It is well known that katabatic winds over the slopes of the Antarctic ice sheet are associated with strong LLJs. Barrier winds occurring, e.g., along the Antarctic Peninsula may also show LLJ structures. A few observational studies show that LLJs occur over sea ice regions. We present a model-based climatology of the wind field, of low-level inversions and of LLJs in the Weddell Sea region of the Antarctic for the period 2002–2016. The sensitivity of the LLJ detection on the selection of the wind speed maximum is investigated. The common criterion of an anomaly of at least 2 m/s is extended to a relative criterion of wind speed decrease above and below the LLJ. The frequencies of LLJs are sensitive to the choice of the relative criterion, i.e., if the value for the relative decrease exceeds 15%. The LLJs are evaluated with respect to the frequency distributions of height, speed, directional shear and stability for different regions. LLJs are most frequent in the katabatic wind regime over the ice sheet and in barrier wind regions. During winter, katabatic LLJs occur with frequencies of more than 70% in many areas. Katabatic LLJs show a narrow range of heights (mostly below 200 m) and speeds (typically 10–20 m/s), while LLJs over the sea ice cover a broad range of speeds and heights. LLJs are associated with surface inversions or low-level lifted inversions. LLJs in the katabatic wind and barrier wind regions can last several days during winter. The duration of LLJs is sensitive to the LLJ definition criteria. We propose to use only the absolute criterion for model studies. Text Antarc* Antarctic Antarctic Peninsula Ice Sheet Sea ice Weddell Sea MDPI Open Access Publishing Antarctic Antarctic Peninsula The Antarctic Weddell Weddell Sea Atmosphere 12 12 1635
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Antarctic
stable boundary layer
low-level jets
inversion
katabatic winds
spellingShingle Antarctic
stable boundary layer
low-level jets
inversion
katabatic winds
Günther Heinemann
Rolf Zentek
A Model-Based Climatology of Low-Level Jets in the Weddell Sea Region of the Antarctic
topic_facet Antarctic
stable boundary layer
low-level jets
inversion
katabatic winds
description Low-level jets (LLJs) are climatological features in polar regions. It is well known that katabatic winds over the slopes of the Antarctic ice sheet are associated with strong LLJs. Barrier winds occurring, e.g., along the Antarctic Peninsula may also show LLJ structures. A few observational studies show that LLJs occur over sea ice regions. We present a model-based climatology of the wind field, of low-level inversions and of LLJs in the Weddell Sea region of the Antarctic for the period 2002–2016. The sensitivity of the LLJ detection on the selection of the wind speed maximum is investigated. The common criterion of an anomaly of at least 2 m/s is extended to a relative criterion of wind speed decrease above and below the LLJ. The frequencies of LLJs are sensitive to the choice of the relative criterion, i.e., if the value for the relative decrease exceeds 15%. The LLJs are evaluated with respect to the frequency distributions of height, speed, directional shear and stability for different regions. LLJs are most frequent in the katabatic wind regime over the ice sheet and in barrier wind regions. During winter, katabatic LLJs occur with frequencies of more than 70% in many areas. Katabatic LLJs show a narrow range of heights (mostly below 200 m) and speeds (typically 10–20 m/s), while LLJs over the sea ice cover a broad range of speeds and heights. LLJs are associated with surface inversions or low-level lifted inversions. LLJs in the katabatic wind and barrier wind regions can last several days during winter. The duration of LLJs is sensitive to the LLJ definition criteria. We propose to use only the absolute criterion for model studies.
format Text
author Günther Heinemann
Rolf Zentek
author_facet Günther Heinemann
Rolf Zentek
author_sort Günther Heinemann
title A Model-Based Climatology of Low-Level Jets in the Weddell Sea Region of the Antarctic
title_short A Model-Based Climatology of Low-Level Jets in the Weddell Sea Region of the Antarctic
title_full A Model-Based Climatology of Low-Level Jets in the Weddell Sea Region of the Antarctic
title_fullStr A Model-Based Climatology of Low-Level Jets in the Weddell Sea Region of the Antarctic
title_full_unstemmed A Model-Based Climatology of Low-Level Jets in the Weddell Sea Region of the Antarctic
title_sort model-based climatology of low-level jets in the weddell sea region of the antarctic
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/atmos12121635
op_coverage agris
geographic Antarctic
Antarctic Peninsula
The Antarctic
Weddell
Weddell Sea
geographic_facet Antarctic
Antarctic Peninsula
The Antarctic
Weddell
Weddell Sea
genre Antarc*
Antarctic
Antarctic Peninsula
Ice Sheet
Sea ice
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Ice Sheet
Sea ice
Weddell Sea
op_source Atmosphere; Volume 12; Issue 12; Pages: 1635
op_relation Atmospheric Techniques, Instruments, and Modeling
https://dx.doi.org/10.3390/atmos12121635
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos12121635
container_title Atmosphere
container_volume 12
container_issue 12
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