Will storm track changes impact UK storm surges?

We present results of a storm surge simulation driven by the atmosphere of a climate model in which a catastrophic shutdown of the Atlantic Meridional Overturning Circulation (AMOC) is induced. Projections of change in the North Atlantic storm tracks in a warming world are highly uncertain and clima...

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Main Authors: Howard, T., Palmer, M.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015928
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5015928 2023-06-11T04:14:49+02:00 Will storm track changes impact UK storm surges? Howard, T. Palmer, M. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015928 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-0488 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015928 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-0488 2023-04-23T23:38:34Z We present results of a storm surge simulation driven by the atmosphere of a climate model in which a catastrophic shutdown of the Atlantic Meridional Overturning Circulation (AMOC) is induced. Projections of change in the North Atlantic storm tracks in a warming world are highly uncertain and climate models show various responses. Atmospheric storms drive storm surges which are a major component of UK coastal flooding hazard, so it is important to ask how this process may be affected by climate change — not only what change is probable, but also what is possible? Our simulation is a contribution to answering that question. We also consider an ensemble simulation with a high-climate-sensitivity model under Representative Concentration Pathway 8.5 (RCP 8.5). We find significant simulated increases for some sites: up to about 0.4 metres increase (approximately 25%) in the expected annual maximum. In both the AMOC-collapse and the ensemble simulation, the largest projected increases appear at some west coast sites, associated with a growth in the strongest westerly winds. Projected changes on the south-east coast are smaller in the AMOC-collapse simulation and generally negative in the ensemble simulation, which exhibits a decrease in strong northerly winds in addition to the growth in westerlies. Overall, these increases due to atmospheric storminess change are smaller than the expected contribution from mean sea-level rise over the 21st century, but larger than the “high-end” changes due to atmospheric storminess change which were reported in UKCP18. Conference Object North Atlantic GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description We present results of a storm surge simulation driven by the atmosphere of a climate model in which a catastrophic shutdown of the Atlantic Meridional Overturning Circulation (AMOC) is induced. Projections of change in the North Atlantic storm tracks in a warming world are highly uncertain and climate models show various responses. Atmospheric storms drive storm surges which are a major component of UK coastal flooding hazard, so it is important to ask how this process may be affected by climate change — not only what change is probable, but also what is possible? Our simulation is a contribution to answering that question. We also consider an ensemble simulation with a high-climate-sensitivity model under Representative Concentration Pathway 8.5 (RCP 8.5). We find significant simulated increases for some sites: up to about 0.4 metres increase (approximately 25%) in the expected annual maximum. In both the AMOC-collapse and the ensemble simulation, the largest projected increases appear at some west coast sites, associated with a growth in the strongest westerly winds. Projected changes on the south-east coast are smaller in the AMOC-collapse simulation and generally negative in the ensemble simulation, which exhibits a decrease in strong northerly winds in addition to the growth in westerlies. Overall, these increases due to atmospheric storminess change are smaller than the expected contribution from mean sea-level rise over the 21st century, but larger than the “high-end” changes due to atmospheric storminess change which were reported in UKCP18.
format Conference Object
author Howard, T.
Palmer, M.
spellingShingle Howard, T.
Palmer, M.
Will storm track changes impact UK storm surges?
author_facet Howard, T.
Palmer, M.
author_sort Howard, T.
title Will storm track changes impact UK storm surges?
title_short Will storm track changes impact UK storm surges?
title_full Will storm track changes impact UK storm surges?
title_fullStr Will storm track changes impact UK storm surges?
title_full_unstemmed Will storm track changes impact UK storm surges?
title_sort will storm track changes impact uk storm surges?
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015928
genre North Atlantic
genre_facet North Atlantic
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-0488
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015928
op_doi https://doi.org/10.57757/IUGG23-0488
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