{"refrec":{"BRefID":347319,"RR":"<b>Stuart-Lee, A.E.; Mortensen, J.; van der Kaaden, A.-S.; Meire, L.</b> (2021). Seasonal hydrography of Ameralik: a southwest Greenland fjord impacted by a land‐terminating glacier. <i>JGR: Oceans 126(12)</i>: e2021JC017552. <a href=\"https://dx.doi.org/10.1029/2021jc017552\" target=\"_blank\">https://dx.doi.org/10.1029/2021jc017552</a>","BEntID":344011,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>JGR: Oceans 126(12)</i>: e2021JC017552. <a href=\"https://dx.doi.org/10.1029/2021jc017552\" target=\"_blank\">https://dx.doi.org/10.1029/2021jc017552</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Stuart-Lee, A.E.; Mortensen, J.; van der Kaaden, A.-S.; Meire, L.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Stuart-Lee, A.E. <i>et al.</i>","Englishabstract":"Greenland’s coastal zone encompasses a large number of fjords, many of which are impacted by glacial meltwater runoff from land-terminating glaciers. This type of fjord has received limited research attention, yet may represent the future of other fjords currently impacted by marine-terminating glaciers that are retreating. In this study we describe the seasonal hydrography of Ameralik, a fjord on the southwest coast of Greenland impacted by a land-terminating glacier. To complement this analysis we compare our results with observations from the neighbouring Godthåbsfjord, which receives meltwater from both land- and marine-terminating glaciers. We find that the absence of subglacial discharge and glacial ice in Ameralik has a strong impact on the inner fjord density profiles and on circulation. The mean temperature of the upper 50 m layer was lower in Ameralik than Godthåbsfjord in May, but by September was 2<sup>◦</sup>C higher in Ameralik. Dense coastal inflows occur in the late winter months in Ameralik, flushing the fjord and contributing to the return to a weakly stratified state. During the runoff period the surface waters are subject to estuarine circulation and wind forcing, while at intermediate depths a density gradient between the inner and outer fjord regions produces an intermediate baroclinic circulation, resulting in the exchange of water in this layer and the deepening of isopycnals. During summer a large fraction of the meltwater runoff is retained within the fjord rather than being exported. A substantial export of this summer accumulated freshwater occurs in connection with coastal inflows during winter.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Seasonal hydrography of Ameralik: a southwest Greenland fjord impacted by a land‐terminating glacier","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-19 01:32:13.720681","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2023-02-21","DateCreate":"2021-11-16","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000735870300044","VABBcode":null,"OpenAcc":1,"DOI":"10.1029/2021jc017552"},"refs":null,"anarec":{"AnaID":347319,"PubliDate":2021,"Pagination":"e2021JC017552","XtraPublOfAnaID":null,"ISBN":null,"Volume":"126","Issue":"12","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":272092,"SerRR":"Journal of Geophysical Research-Oceans. 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