Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation
The seasonal change in the development of Aleutian low pressure systems from early fall to early winter is analyzed using a combination of meteorological reanalysis fields, satellite sea surface temperature (SST) data, and satellite wind data. The time period of the study is September–December 2002,...
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ftuniveastangl:oai:ueaeprints.uea.ac.uk:26855 2023-05-15T13:14:52+02:00 Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation Pickart, Robert S. Moore, G. W. K. MacDonald, Alison M. Renfrew, Ian A. Walsh, John E. Kessler, William S. 2009 application/pdf https://ueaeprints.uea.ac.uk/id/eprint/26855/ https://ueaeprints.uea.ac.uk/id/eprint/26855/1/pickart_etal_aleutian_low_impact_JPO_2009.pdf https://doi.org/10.1175/2008JPO3891.1 en eng https://ueaeprints.uea.ac.uk/id/eprint/26855/1/pickart_etal_aleutian_low_impact_JPO_2009.pdf Pickart, Robert S., Moore, G. W. K., MacDonald, Alison M., Renfrew, Ian A., Walsh, John E. and Kessler, William S. (2009) Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation. Journal of Physical Oceanography, 39. pp. 1317-1339. doi:10.1175/2008JPO3891.1 Article PeerReviewed 2009 ftuniveastangl https://doi.org/10.1175/2008JPO3891.1 2023-03-23T23:31:37Z The seasonal change in the development of Aleutian low pressure systems from early fall to early winter is analyzed using a combination of meteorological reanalysis fields, satellite sea surface temperature (SST) data, and satellite wind data. The time period of the study is September–December 2002, although results are shown to be representative of the long-term climatology. Characteristics of the storms were documented as they progressed across the North Pacific, including their path, central pressure, deepening rate, and speed of translation. Clear patterns emerged. Storms tended to deepen in two distinct geographical locations—the Gulf of Alaska in early fall and the western North Pacific in late fall. In the Gulf of Alaska, a quasi-permanent “notch” in the SST distribution is argued to be of significance. The signature of the notch is imprinted in the atmosphere, resulting in a region of enhanced cyclonic potential vorticity in the lower troposphere that is conducive for storm development. Later in the season, as winter approaches and the Sea of Okhotsk becomes partially ice covered and cold, the air emanating from the Asian continent leads to enhanced baroclinicity in the region south of Kamchatka. This corresponds to enhanced storm cyclogenesis in that region. Consequently, there is a seasonal westward migration of the dominant lobe of the Aleutian low. The impact of the wind stress curl pattern resulting from these two regions of storm development on the oceanic circulation is investigated using historical hydrography. It is argued that the seasonal bimodal input of cyclonic vorticity from the wind may be partly responsible for the two distinct North Pacific subarctic gyres. Article in Journal/Newspaper aleutian low Kamchatka Subarctic Alaska University of East Anglia: UEA Digital Repository Curl ENVELOPE(-63.071,-63.071,-70.797,-70.797) Gulf of Alaska Okhotsk Pacific Journal of Physical Oceanography 39 6 1317 1339 |
institution |
Open Polar |
collection |
University of East Anglia: UEA Digital Repository |
op_collection_id |
ftuniveastangl |
language |
English |
description |
The seasonal change in the development of Aleutian low pressure systems from early fall to early winter is analyzed using a combination of meteorological reanalysis fields, satellite sea surface temperature (SST) data, and satellite wind data. The time period of the study is September–December 2002, although results are shown to be representative of the long-term climatology. Characteristics of the storms were documented as they progressed across the North Pacific, including their path, central pressure, deepening rate, and speed of translation. Clear patterns emerged. Storms tended to deepen in two distinct geographical locations—the Gulf of Alaska in early fall and the western North Pacific in late fall. In the Gulf of Alaska, a quasi-permanent “notch” in the SST distribution is argued to be of significance. The signature of the notch is imprinted in the atmosphere, resulting in a region of enhanced cyclonic potential vorticity in the lower troposphere that is conducive for storm development. Later in the season, as winter approaches and the Sea of Okhotsk becomes partially ice covered and cold, the air emanating from the Asian continent leads to enhanced baroclinicity in the region south of Kamchatka. This corresponds to enhanced storm cyclogenesis in that region. Consequently, there is a seasonal westward migration of the dominant lobe of the Aleutian low. The impact of the wind stress curl pattern resulting from these two regions of storm development on the oceanic circulation is investigated using historical hydrography. It is argued that the seasonal bimodal input of cyclonic vorticity from the wind may be partly responsible for the two distinct North Pacific subarctic gyres. |
format |
Article in Journal/Newspaper |
author |
Pickart, Robert S. Moore, G. W. K. MacDonald, Alison M. Renfrew, Ian A. Walsh, John E. Kessler, William S. |
spellingShingle |
Pickart, Robert S. Moore, G. W. K. MacDonald, Alison M. Renfrew, Ian A. Walsh, John E. Kessler, William S. Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation |
author_facet |
Pickart, Robert S. Moore, G. W. K. MacDonald, Alison M. Renfrew, Ian A. Walsh, John E. Kessler, William S. |
author_sort |
Pickart, Robert S. |
title |
Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation |
title_short |
Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation |
title_full |
Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation |
title_fullStr |
Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation |
title_full_unstemmed |
Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation |
title_sort |
seasonal evolution of aleutian low pressure systems: implications for the north pacific subpolar circulation |
publishDate |
2009 |
url |
https://ueaeprints.uea.ac.uk/id/eprint/26855/ https://ueaeprints.uea.ac.uk/id/eprint/26855/1/pickart_etal_aleutian_low_impact_JPO_2009.pdf https://doi.org/10.1175/2008JPO3891.1 |
long_lat |
ENVELOPE(-63.071,-63.071,-70.797,-70.797) |
geographic |
Curl Gulf of Alaska Okhotsk Pacific |
geographic_facet |
Curl Gulf of Alaska Okhotsk Pacific |
genre |
aleutian low Kamchatka Subarctic Alaska |
genre_facet |
aleutian low Kamchatka Subarctic Alaska |
op_relation |
https://ueaeprints.uea.ac.uk/id/eprint/26855/1/pickart_etal_aleutian_low_impact_JPO_2009.pdf Pickart, Robert S., Moore, G. W. K., MacDonald, Alison M., Renfrew, Ian A., Walsh, John E. and Kessler, William S. (2009) Seasonal evolution of Aleutian low pressure systems: Implications for the North Pacific subpolar circulation. Journal of Physical Oceanography, 39. pp. 1317-1339. doi:10.1175/2008JPO3891.1 |
op_doi |
https://doi.org/10.1175/2008JPO3891.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
39 |
container_issue |
6 |
container_start_page |
1317 |
op_container_end_page |
1339 |
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1766265845235843072 |