The evolution of the Atlantic Meridional Overturning Circulation and its implications for surface warming

The Atlantic Meridional Overturning Circulation (AMOC) is likely the most well-known system of ocean currents on Earth, redistributing heat, nutrients and carbon over a large part of the Earth’s surface and affecting global climate as a result. Due to enhanced freshwater fluxes into the subpolar North...

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Main Author: Caesar, Levke
Format: Doctoral or Postdoctoral Thesis
Language:German
Published: 2019
Subjects:
Online Access:https://publishup.uni-potsdam.de/frontdoor/index/index/docId/43795
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author Caesar, Levke
author_facet Caesar, Levke
author_sort Caesar, Levke
collection University of Potsdam: publish.UP
description The Atlantic Meridional Overturning Circulation (AMOC) is likely the most well-known system of ocean currents on Earth, redistributing heat, nutrients and carbon over a large part of the Earth’s surface and affecting global climate as a result. Due to enhanced freshwater fluxes into the subpolar North Atlantic as a response to global warming, the AMOC is expected, and may have already started, to weaken and these changes will likely have global impacts. It is therefore of considerable relevance to improve our understanding of past and future AMOC changes. My thesis tries to answer some of the open questions in this field by giving strong evidence that the AMOC has already weakened over the last century, by narrowing future projections of this slowdown and by studying the impacts on global surface warming. While there have been various studies trying to reconstruct the strength of the overturning circulation in the past, often based on model simulations in combination with observations (Jackson et al., 2016, Kanzow et al., 2010) or proxies (Frajka-Williams, 2015, Latif et al., 2006), the results so far, due to lack of direct measurements, have been inconclusive. In the first paper I build on previous work that links the anomalously low sea surface temperatures (SSTs) in the North Atlantic with the reduced meridional heat transport due to a weaker AMOC. Using the output of a high-resolution global climate model, I derive a characteristic spatial and seasonal SST fingerprint of an AMOC slowdown and an improved SST-based AMOC index. The same fingerprint is seen in the observational SSTs since the late 19th Century, giving strong evidence that since then the AMOC has slowed down. In addition, the reconstruction of the historical overturning strength with the new AMOC index agrees well with and extends the results of earlier studies as well as the direct measurements from the RAPID project and shows a strong decline of the AMOC by about 15% (3±1 Sv) since the mid-20th Century (Caesar et al., 2018). The reconstruction of the ...
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spelling ftubpotsdam:oai:kobv.de-opus4-uni-potsdam:43795 2025-04-20T14:41:36+00:00 The evolution of the Atlantic Meridional Overturning Circulation and its implications for surface warming Caesar, Levke 2019 https://publishup.uni-potsdam.de/frontdoor/index/index/docId/43795 deu ger info:eu-repo/semantics/closedAccess ddc:530 Institut für Geowissenschaften doctoralthesis doc-type:doctoralThesis 2019 ftubpotsdam 2025-03-25T05:06:48Z The Atlantic Meridional Overturning Circulation (AMOC) is likely the most well-known system of ocean currents on Earth, redistributing heat, nutrients and carbon over a large part of the Earth’s surface and affecting global climate as a result. Due to enhanced freshwater fluxes into the subpolar North Atlantic as a response to global warming, the AMOC is expected, and may have already started, to weaken and these changes will likely have global impacts. It is therefore of considerable relevance to improve our understanding of past and future AMOC changes. My thesis tries to answer some of the open questions in this field by giving strong evidence that the AMOC has already weakened over the last century, by narrowing future projections of this slowdown and by studying the impacts on global surface warming. While there have been various studies trying to reconstruct the strength of the overturning circulation in the past, often based on model simulations in combination with observations (Jackson et al., 2016, Kanzow et al., 2010) or proxies (Frajka-Williams, 2015, Latif et al., 2006), the results so far, due to lack of direct measurements, have been inconclusive. In the first paper I build on previous work that links the anomalously low sea surface temperatures (SSTs) in the North Atlantic with the reduced meridional heat transport due to a weaker AMOC. Using the output of a high-resolution global climate model, I derive a characteristic spatial and seasonal SST fingerprint of an AMOC slowdown and an improved SST-based AMOC index. The same fingerprint is seen in the observational SSTs since the late 19th Century, giving strong evidence that since then the AMOC has slowed down. In addition, the reconstruction of the historical overturning strength with the new AMOC index agrees well with and extends the results of earlier studies as well as the direct measurements from the RAPID project and shows a strong decline of the AMOC by about 15% (3±1 Sv) since the mid-20th Century (Caesar et al., 2018). The reconstruction of the ... Doctoral or Postdoctoral Thesis North Atlantic University of Potsdam: publish.UP
spellingShingle ddc:530
Institut für Geowissenschaften
Caesar, Levke
The evolution of the Atlantic Meridional Overturning Circulation and its implications for surface warming
title The evolution of the Atlantic Meridional Overturning Circulation and its implications for surface warming
title_full The evolution of the Atlantic Meridional Overturning Circulation and its implications for surface warming
title_fullStr The evolution of the Atlantic Meridional Overturning Circulation and its implications for surface warming
title_full_unstemmed The evolution of the Atlantic Meridional Overturning Circulation and its implications for surface warming
title_short The evolution of the Atlantic Meridional Overturning Circulation and its implications for surface warming
title_sort evolution of the atlantic meridional overturning circulation and its implications for surface warming
topic ddc:530
Institut für Geowissenschaften
topic_facet ddc:530
Institut für Geowissenschaften
url https://publishup.uni-potsdam.de/frontdoor/index/index/docId/43795