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dc.contributor.authorSvendsen, Lea
dc.date.accessioned2016-06-07T11:21:36Z
dc.date.available2016-06-07T11:21:36Z
dc.date.issued2016-06-03
dc.identifier.urihttps://hdl.handle.net/1956/12075
dc.description.abstractEarlier studies have shown that Atlantic multi-decadal variability (AMY) can impact climate variability globally. However the instrumental records are short compared to the timescale of AMY, and mechanisms for these impacts are unresolved. This thesis deals with impacts of AMY on the Indo-Pacific region and over the Northern Hemisphere, investigating both the persistence of multi-decadal variability in the two phenomena and possible mechanisms for interactions between them. Coupled climate models are the main tools used in this study, in the form of output from the Coupled Model Intercomparison Project 5 (CMIP5) ensembles, a freshwater hosing experiment with the Bergen Climate Model (BCM), and partially coupled ensemble simulations with the Norwegian Earth System Model (NorESM). In addition proxy records are used to assess persistence in both AMY and its relation to regional variability in the Indo-Pacific. The results of this thesis are presented in five papers. In the first paper a new marine- based multi-proxy reconstruction for AMY is produced and presented, showing persistent multi-decadal variability 90 years further back in time than the instrumental records. The second paper evaluates multi-decadal variability in several proxy reconstructions of the Indian summer monsoon (ISM) and compares it with different AMY reconstructions, including the marine-based record from the first paper. Multi- decadal variability is found in ISM reconstructions back to the 15th century, but the relation with AMY is not clear. The AMY-ISM relation is further investigated in CMIP5 simulations in the third paper. While none of the models capture the observed significant AMY-ISM relation in the pre-industrial control simulations, one model simulates the observed correlation in the 20th century historical ensemble, indicating that the observed relation could be externally forced. In the fourth paper of this thesis it is found that changes in North Atlantic SSTs due to variations in the thermohaline circulation can impact variability in the equatorial Atlantic and change the inter-basin relation between Atlantic and Pacific Ninos. The fifth paper introduces a novel approach for investigating large-scale impacts in a coupled model, by separating radiative forced and dynamically driven variability. Ensembles of partially coupled 20th century historical simulations indicate that AMY may not have been a key contributor in Northern Hemisphere surface trends on decadal timescales. Collectively these papers indicate that the AMY is a persistent signal of the climate system, but the impacts on multi-decadal variability in the Indo-Pacific and the Northern Hemisphere may not be as strong as previous studies suggest. AMY can modulate interannual variability and inter-basin teleconnections in the tropics, but the correlation with the ISM could be due to external forcing, and the Pacific seems to make a larger contribution to decadal trends in Northern Hemisphere climate than the Atlantic.en_US
dc.language.isoengeng
dc.publisherThe University of Bergenen_US
dc.relation.haspartPaper I: Svendsen, L., S. Hetzinger, N. Keenlyside, and Y. Gao (2014), Marine-based multiproxy reconstruction of Atlantic multidecadal variability, Geophysical Research letters, 41(4), 2013GL059076. The article is available in BORA at: <a href="http://hdl.handle.net/1956/9369" target="blank">http://hdl.handle.net/1956/9369</a>en_US
dc.relation.haspartPaper II: Sankar, S., L. Svendsen, G. Bindu, P. V. Joseph, and 0. M. Johannessen, Teleconnections between Indian summer monsoon rainfall and Atlantic multidecadal variability over the last 500 years (manuscript in preparation). This article is not available in BORA.en_US
dc.relation.haspartPaper III: Luo F., Y. Gao, L. Svendsen, N. Keenlyside, S. Li and T. Furevik, External forcing synchronizes Atlantic multidecadal variability and the Indian summer monsoon (manuscript in preparation). This article is not available in BORA.en_US
dc.relation.haspartPaper IV: Svendsen, L., N. G. Kvamst0, and N. Keenlyside (2013), Weakening AM0C connects equatorial Atlantic and Pacific interannual variability, Climate Dynamics, 43(11), 2931-2941. This article is not available in BORA. The published version is available at: <a href="http://dx.doi.org/10.1007/s00382-013-1904-8" target="blank">10.1007/s00382-013-1904-8</a>en_US
dc.relation.haspartPaper V: Svendsen, L., N. Keenlyside, I. Bethke, and Y. Gao, Investigating the role of the Atlantic and Pacific in the early 20th century warming trend (manuscript in preparation). This article is not available in BORA.en_US
dc.titleImpacts of Atlantic multi-decadal variability on the Indo-Pacific and Northern Hemisphere climateen_US
dc.typeDoctoral thesis
dc.rights.holderCopyright the author. All rights reserved.en_US
dc.identifier.cristin1372664


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