Atmospheric Circulation Drivers of Extreme High Water Level Events at Foggy Island Bay, Alaska

The northern coast of Alaska is experiencing significant climatic change enhancing hazards from reduced sea ice and increased coastal erosion. This same region is home to offshore oil/gas activities. Foggy Island Bay is one region along the Beaufort Sea coast with planned offshore oil/gas developmen...

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Published in:Atmosphere
Main Authors: Peter A. Bieniek, Li Erikson, Jeremy Kasper
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/atmos13111791
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spelling ftmdpi:oai:mdpi.com:/2073-4433/13/11/1791/ 2023-08-20T04:04:41+02:00 Atmospheric Circulation Drivers of Extreme High Water Level Events at Foggy Island Bay, Alaska Peter A. Bieniek Li Erikson Jeremy Kasper agris 2022-10-29 application/pdf https://doi.org/10.3390/atmos13111791 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos13111791 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 13; Issue 11; Pages: 1791 Arctic storms coastal flooding climate change Text 2022 ftmdpi https://doi.org/10.3390/atmos13111791 2023-08-01T07:06:27Z The northern coast of Alaska is experiencing significant climatic change enhancing hazards from reduced sea ice and increased coastal erosion. This same region is home to offshore oil/gas activities. Foggy Island Bay is one region along the Beaufort Sea coast with planned offshore oil/gas development that will need to account for the changing climate. High water levels impact infrastructure through coastal erosion and flooding hazards. In this study, 21 high water level events exceeding the top 95th percentile were identified at the gauge in Prudhoe Bay, Alaska (adjacent to Foggy Island Bay) over 1990–2018. All 21 events, and many non-extreme days with elevated water levels, were associated with strong westerly winds according to station records. Storm systems were generally found to be a key driver of westerly winds in the region according to downscaled reanalysis and storm track data. A dynamically downscaled global climate model projection from CMIP5 indicated that days with westerly wind events may become more frequent as storms strengthen and have longer durations by 2100 in the Foggy Island Bay region. Coupled with the anticipated continued decline in sea ice, the northern coast of Alaska may experience more frequent high water events over the next ~80 years. Text Arctic Beaufort Sea Climate change Prudhoe Bay Sea ice Alaska MDPI Open Access Publishing Arctic Island Bay ENVELOPE(-109.085,-109.085,59.534,59.534) Atmosphere 13 11 1791
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Arctic storms
coastal flooding
climate change
spellingShingle Arctic storms
coastal flooding
climate change
Peter A. Bieniek
Li Erikson
Jeremy Kasper
Atmospheric Circulation Drivers of Extreme High Water Level Events at Foggy Island Bay, Alaska
topic_facet Arctic storms
coastal flooding
climate change
description The northern coast of Alaska is experiencing significant climatic change enhancing hazards from reduced sea ice and increased coastal erosion. This same region is home to offshore oil/gas activities. Foggy Island Bay is one region along the Beaufort Sea coast with planned offshore oil/gas development that will need to account for the changing climate. High water levels impact infrastructure through coastal erosion and flooding hazards. In this study, 21 high water level events exceeding the top 95th percentile were identified at the gauge in Prudhoe Bay, Alaska (adjacent to Foggy Island Bay) over 1990–2018. All 21 events, and many non-extreme days with elevated water levels, were associated with strong westerly winds according to station records. Storm systems were generally found to be a key driver of westerly winds in the region according to downscaled reanalysis and storm track data. A dynamically downscaled global climate model projection from CMIP5 indicated that days with westerly wind events may become more frequent as storms strengthen and have longer durations by 2100 in the Foggy Island Bay region. Coupled with the anticipated continued decline in sea ice, the northern coast of Alaska may experience more frequent high water events over the next ~80 years.
format Text
author Peter A. Bieniek
Li Erikson
Jeremy Kasper
author_facet Peter A. Bieniek
Li Erikson
Jeremy Kasper
author_sort Peter A. Bieniek
title Atmospheric Circulation Drivers of Extreme High Water Level Events at Foggy Island Bay, Alaska
title_short Atmospheric Circulation Drivers of Extreme High Water Level Events at Foggy Island Bay, Alaska
title_full Atmospheric Circulation Drivers of Extreme High Water Level Events at Foggy Island Bay, Alaska
title_fullStr Atmospheric Circulation Drivers of Extreme High Water Level Events at Foggy Island Bay, Alaska
title_full_unstemmed Atmospheric Circulation Drivers of Extreme High Water Level Events at Foggy Island Bay, Alaska
title_sort atmospheric circulation drivers of extreme high water level events at foggy island bay, alaska
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/atmos13111791
op_coverage agris
long_lat ENVELOPE(-109.085,-109.085,59.534,59.534)
geographic Arctic
Island Bay
geographic_facet Arctic
Island Bay
genre Arctic
Beaufort Sea
Climate change
Prudhoe Bay
Sea ice
Alaska
genre_facet Arctic
Beaufort Sea
Climate change
Prudhoe Bay
Sea ice
Alaska
op_source Atmosphere; Volume 13; Issue 11; Pages: 1791
op_relation Climatology
https://dx.doi.org/10.3390/atmos13111791
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos13111791
container_title Atmosphere
container_volume 13
container_issue 11
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