Acceleration of U.S. Southeast and gulf coast sea-level rise: Forced and unforced contributions

While there is evidence for an acceleration in global mean sea-level (MSL) since the 1960s, its detection at local levels has been hampered by the considerable influence of natural variability on the rate of MSL change. Here we report an MSL acceleration in tide gauge records along the U.S. Southeas...

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Main Authors: Dangendorf, S., Hendricks, N., Sun, Q.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016759
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5016759 2023-10-09T21:54:00+02:00 Acceleration of U.S. Southeast and gulf coast sea-level rise: Forced and unforced contributions Dangendorf, S. Hendricks, N. Sun, Q. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016759 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-0729 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016759 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-0729 2023-09-17T23:43:20Z While there is evidence for an acceleration in global mean sea-level (MSL) since the 1960s, its detection at local levels has been hampered by the considerable influence of natural variability on the rate of MSL change. Here we report an MSL acceleration in tide gauge records along the U.S. Southeast and Gulf coasts that has led to rates (>10 mmyr-1 since 2010) that are unprecedented in at least 120 years. Using a variety of remote sensing and in-situ measurements in combination with climate model outputs, we show that this acceleration is primarily induced by an ocean dynamic signal exceeding the externally forced response from historical climate model simulations. However, when the simulated forced response is removed from observations, the residuals are neither historically unprecedented nor inconsistent with unforced variability in simulations. Furthermore, a large fraction of the residuals can be explained by remote wind forcing (via Rossby waves) over the tropical North Atlantic. This indicates that the acceleration represents the compounding effects of external forcing and internal climate variability. 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 While there is evidence for an acceleration in global mean sea-level (MSL) since the 1960s, its detection at local levels has been hampered by the considerable influence of natural variability on the rate of MSL change. Here we report an MSL acceleration in tide gauge records along the U.S. Southeast and Gulf coasts that has led to rates (>10 mmyr-1 since 2010) that are unprecedented in at least 120 years. Using a variety of remote sensing and in-situ measurements in combination with climate model outputs, we show that this acceleration is primarily induced by an ocean dynamic signal exceeding the externally forced response from historical climate model simulations. However, when the simulated forced response is removed from observations, the residuals are neither historically unprecedented nor inconsistent with unforced variability in simulations. Furthermore, a large fraction of the residuals can be explained by remote wind forcing (via Rossby waves) over the tropical North Atlantic. This indicates that the acceleration represents the compounding effects of external forcing and internal climate variability.
format Conference Object
author Dangendorf, S.
Hendricks, N.
Sun, Q.
spellingShingle Dangendorf, S.
Hendricks, N.
Sun, Q.
Acceleration of U.S. Southeast and gulf coast sea-level rise: Forced and unforced contributions
author_facet Dangendorf, S.
Hendricks, N.
Sun, Q.
author_sort Dangendorf, S.
title Acceleration of U.S. Southeast and gulf coast sea-level rise: Forced and unforced contributions
title_short Acceleration of U.S. Southeast and gulf coast sea-level rise: Forced and unforced contributions
title_full Acceleration of U.S. Southeast and gulf coast sea-level rise: Forced and unforced contributions
title_fullStr Acceleration of U.S. Southeast and gulf coast sea-level rise: Forced and unforced contributions
title_full_unstemmed Acceleration of U.S. Southeast and gulf coast sea-level rise: Forced and unforced contributions
title_sort acceleration of u.s. southeast and gulf coast sea-level rise: forced and unforced contributions
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016759
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/IUGG23-0729
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016759
op_doi https://doi.org/10.57757/IUGG23-0729
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