{"refrec":{"BRefID":306197,"RR":"<b>Shinoda, T.; Zamudio, L.; Guo, Y.; Metzger, E.J.; Fairall, C.W.</b> (2019). Ocean variability and air-sea fluxes produced by atmospheric rivers. <i>NPG Scientific Reports 9(1)</i>: 12 pp. <a href=\"https://dx.doi.org/10.1038/s41598-019-38562-2\" target=\"_blank\">https://dx.doi.org/10.1038/s41598-019-38562-2</a>","BEntID":298522,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>NPG Scientific Reports 9(1)</i>: 12 pp. <a href=\"https://dx.doi.org/10.1038/s41598-019-38562-2\" target=\"_blank\">https://dx.doi.org/10.1038/s41598-019-38562-2</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Shinoda, T.; Zamudio, L.; Guo, Y.; Metzger, E.J.; Fairall, C.W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Shinoda, T. <i>et al.</i>","Englishabstract":"Atmospheric rivers (ARs) cause heavy precipitation and flooding in the coastal areas of many mid-latitude continents, and thus the atmospheric processes associated with the AR have been intensively studied in recent years. However, AR-associated ocean variability and air-sea fluxes have received little attention because of the lack of high-resolution ocean data until recently. Here we demonstrate that typical ARs can generate strong upper ocean response and substantial air-sea fluxes using a high-resolution (1/12°) ocean reanalysis. AR events observed during the CalWater 2015 field campaign generate large-scale on-shore currents that hit the coast, generating strong narrow northward jets along the west coast of North America, in association with a substantial rise of sea level at the coast. In the open ocean, the AR generates prominent changes of mixed layer depth, especially south of 30°N due to the strong surface winds and air-sea heat fluxes. The prominent cooling of SST is observed only in the vicinity of AR upstream areas primarily due to the large latent heat flux. Using a long-term AR dataset, composite structure and variations of upper ocean and air-sea fluxes are presented, which are consistent with those found in the events during CalWater 2015.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Ocean variability and air-sea fluxes produced by atmospheric rivers","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-13 01:31:38.183266","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2019,"MonPub":null,"DateUpdate":"2019-02-21","DateCreate":"2019-02-21","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000458752600004","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s41598-019-38562-2"},"refs":null,"anarec":{"AnaID":306197,"PubliDate":2019,"Pagination":"12 pp","XtraPublOfAnaID":null,"ISBN":null,"Volume":"9","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":208093,"SerRR":"Scientific Reports (Nature Publishing Group). 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