Impact of Arctic sea ice loss on tropical cyclone genesis frequency over the North Pacific

Anthropogenic global warming generally has been shown to cause the rapid loss of Arctic sea ice in recent decades. However, whether this rapid loss has exerted significant impact on recent changes in tropical cyclone (TC) activity over the North Pacific remains unknown. Here, we first extract the le...

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Main Authors: Zhan, R., Lan, H., Jiuwei, Z.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018324
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018324 2023-09-05T13:16:26+02:00 Impact of Arctic sea ice loss on tropical cyclone genesis frequency over the North Pacific Zhan, R. Lan, H. Jiuwei, Z. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018324 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2418 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018324 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-2418 2023-08-13T23:41:24Z Anthropogenic global warming generally has been shown to cause the rapid loss of Arctic sea ice in recent decades. However, whether this rapid loss has exerted significant impact on recent changes in tropical cyclone (TC) activity over the North Pacific remains unknown. Here, we first extract the leading mode of the rapid loss of Arctic sea ice concentration (SIC) averaged in July-October during 1950-2021, and then investigate the impact of this leading mode on long-term changes in TC genesis frequency over the western North Pacific (WNP) and the eastern North Pacific (ENP). Results show that the reduced SIC was favorable for more TC geneses over the whole ENP but led to fewer TC geneses over most of the WNP. Further analyses based on dynamical diagnosis and CMIP6 model data demonstrate that the rapid loss of Arctic SIC is responsible for local warming and weakened upper-tropospheric westerly over most of the Arctic. This triggers a teleconnection wave train over the upper troposphere from high to low latitudes, leading to the weakening of tropical easterly jet over the tropical western Pacific and the strengthening over the tropical eastern Pacific. The former dynamically contributes to decrease in mid-level upward motion and low-level vorticity, and eventually accounts for few TCs over the WNP. The opposite dynamical process is true for the ENP TCs. The finding not only has an important implication for future TC changes but also suggests a possible link between Arctic sea ice and tropical climate. Conference Object Arctic Global warming Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic Pacific
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Anthropogenic global warming generally has been shown to cause the rapid loss of Arctic sea ice in recent decades. However, whether this rapid loss has exerted significant impact on recent changes in tropical cyclone (TC) activity over the North Pacific remains unknown. Here, we first extract the leading mode of the rapid loss of Arctic sea ice concentration (SIC) averaged in July-October during 1950-2021, and then investigate the impact of this leading mode on long-term changes in TC genesis frequency over the western North Pacific (WNP) and the eastern North Pacific (ENP). Results show that the reduced SIC was favorable for more TC geneses over the whole ENP but led to fewer TC geneses over most of the WNP. Further analyses based on dynamical diagnosis and CMIP6 model data demonstrate that the rapid loss of Arctic SIC is responsible for local warming and weakened upper-tropospheric westerly over most of the Arctic. This triggers a teleconnection wave train over the upper troposphere from high to low latitudes, leading to the weakening of tropical easterly jet over the tropical western Pacific and the strengthening over the tropical eastern Pacific. The former dynamically contributes to decrease in mid-level upward motion and low-level vorticity, and eventually accounts for few TCs over the WNP. The opposite dynamical process is true for the ENP TCs. The finding not only has an important implication for future TC changes but also suggests a possible link between Arctic sea ice and tropical climate.
format Conference Object
author Zhan, R.
Lan, H.
Jiuwei, Z.
spellingShingle Zhan, R.
Lan, H.
Jiuwei, Z.
Impact of Arctic sea ice loss on tropical cyclone genesis frequency over the North Pacific
author_facet Zhan, R.
Lan, H.
Jiuwei, Z.
author_sort Zhan, R.
title Impact of Arctic sea ice loss on tropical cyclone genesis frequency over the North Pacific
title_short Impact of Arctic sea ice loss on tropical cyclone genesis frequency over the North Pacific
title_full Impact of Arctic sea ice loss on tropical cyclone genesis frequency over the North Pacific
title_fullStr Impact of Arctic sea ice loss on tropical cyclone genesis frequency over the North Pacific
title_full_unstemmed Impact of Arctic sea ice loss on tropical cyclone genesis frequency over the North Pacific
title_sort impact of arctic sea ice loss on tropical cyclone genesis frequency over the north pacific
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018324
geographic Arctic
Pacific
geographic_facet Arctic
Pacific
genre Arctic
Global warming
Sea ice
genre_facet Arctic
Global warming
Sea ice
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2418
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018324
op_doi https://doi.org/10.57757/IUGG23-2418
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