{"refrec":{"BRefID":336337,"RR":"<b>Frederikse, T.; Adhikari, S.; Daley, T.J.; Dangendorf, S.; Gehrels, R.; Landerer, F.W.; Marcos, M.; Newton, T.L.; Rush, G.; Slangen, A.B.A.; Wöppelmann, G.</b> (2021). Constraining 20th‐century sea‐level rise in the South Atlantic Ocean. <i>JGR: Oceans 126(3)</i>: e2020JC016970. <a href=\"https://doi.org/10.1029/2020jc016970\" target=\"_blank\">https://doi.org/10.1029/2020jc016970</a>","BEntID":332959,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>JGR: Oceans 126(3)</i>: e2020JC016970. <a href=\"https://doi.org/10.1029/2020jc016970\" target=\"_blank\">https://doi.org/10.1029/2020jc016970</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Frederikse, T.; Adhikari, S.; Daley, T.J.; Dangendorf, S.; Gehrels, R.; Landerer, F.W.; Marcos, M.; Newton, T.L.; Rush, G.; Slangen, A.B.A.; Wöppelmann, G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Frederikse, T. <i>et al.</i>","Englishabstract":"<p>    Sea level in the South Atlantic Ocean has only been measured at a small    number of tide‐gauge locations, which causes considerable uncertainty in    20th‐century sea‐level trend estimates in this basin. To obtain a    better‐constrained sea‐level trend in the South Atlantic Ocean, this study    aims to answer two questions. The first question is: can we combine new    observations, vertical land motion estimates, and information on spatial    sampling biases to obtain a likely range of 20th‐century sea‐level rise in    the South Atlantic? We combine existing observations with recovered    observations from Dakar and a high‐resolution sea‐level reconstruction    based on salt‐marsh sediments from the Falkland Islands and find that the    rate of sea‐level rise in the South Atlantic has likely been between 1.1    and 2.2 mm year<sup>−1</sup> (5%–95% confidence intervals), with a central    estimate of 1.6 mm year<sup>−1</sup>. This rate is on the high side, but    not statistically different compared to global‐mean trends from recent    reconstructions. The second question is: are there any physical processes    that could explain a large deviation from the global‐mean sea‐level trend    in the South Atlantic? Sterodynamic (changes in ocean dynamics and steric    effects) and gravitation, rotation, and deformation effects related to ice    mass loss and land water storage have probably led to a 20th‐century    sea‐level trend in the South Atlantic above the global mean. Both    observations and physical processes thus suggest that 20th‐centurysea‐level rise in the South Atlantic has been about 0.3 mm year    <sup>−1</sup> above the rate of global‐mean sea‐level rise, although even    with the additional observations, the uncertainties are still too large to    distinguish a statistically significant difference.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Constraining 20th‐century sea‐level rise in the South Atlantic Ocean","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-19 01:32:10.298501","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"data rescue; salt-marsh proxies; sea-level changes; South Atlantic; tide gauges","OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2022-02-08","DateCreate":"2021-04-12","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000636285300008","VABBcode":null,"OpenAcc":1,"DOI":"10.1029/2020jc016970"},"refs":null,"anarec":{"AnaID":336337,"PubliDate":2021,"Pagination":"e2020JC016970","XtraPublOfAnaID":null,"ISBN":null,"Volume":"126","Issue":"3","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":272092,"SerRR":"Journal of Geophysical Research-Oceans. 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