{"refrec":{"BRefID":393607,"RR":"<b>van der Kaaden, A.-S.; van Oevelen, D.; Mohn, C.; Soetaert, K.; Rietkerk, M.; van de Koppel, J.; Gerkema, T.</b> (2024). Resemblance of the global depth distribution of internal-tide generation and cold-water coral occurrences. <i>Ocean Science Journal 20(2)</i>: 569-587. <a href=\"https://dx.doi.org/10.5194/os-20-569-2024\" target=\"_blank\">https://dx.doi.org/10.5194/os-20-569-2024</a>","BEntID":391395,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Ocean Science Journal 20(2)</i>: 569-587. <a href=\"https://dx.doi.org/10.5194/os-20-569-2024\" target=\"_blank\">https://dx.doi.org/10.5194/os-20-569-2024</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"van der Kaaden, A.-S.; van Oevelen, D.; Mohn, C.; Soetaert, K.; Rietkerk, M.; van de Koppel, J.; Gerkema, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"van der Kaaden, A.-S. <i>et al.</i>","Englishabstract":"Internal tides are known to be an important source of mixing in the oceans, especially in the bottom boundary layer. The depth of internal-tide generation therefore seems important for benthic life and the formation of cold-water coral mounds, but internal-tide conversion is generally investigated in a depth-integrated sense. Using both idealized and realistic simulations on continental slopes, we found that the depth of internal-tide generation increases with increasing slope steepness and decreases with intensified shallow stratification. The depth of internal-tide generation also shows a typical latitudinal dependency related to Coriolis effects. Using a global database of cold-water corals, we found that, especially in Northern Hemisphere autumn and winter, the global depth pattern of internal-tide generation correlates (<i>r</i><sub>autumn</sub> = 0.70, <i>r</i><sub>winter</sub> = 0.65, <i>p</i> &lt; 0.01) with that of cold-water corals: shallowest near the poles and deepest around the Equator, with a decrease in depth around 25° S and N, and shallower north of the Equator than south.We further found that cold-water corals are situated significantly more often on topography that is steeper than the internal-tide beam (i.e. where supercritical reflection of internal tides occurs) than would be expected from a random distribution: in our study, in 66.9 % of all cases, cold-water corals occurred on a topography that is supercritical to the M2 tide whereas globally only 9.4 % of all topography is supercritical. Our findings underline internal-tide generation and the occurrence of supercritical reflection of internal tides as globally important for cold-water coral growth. The energetic dynamics associated with internal-tide generation and the supercritical reflection of internal tides likely increase the food supply towards the reefs in food-limited winter months. With climate change, stratification is expected to increase. Based on our results, this would decrease the depth of internal-tide generation, possibly creating new suitable habitat for cold-water corals shallower on continental slopes.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Resemblance of the global depth distribution of internal-tide generation and cold-water coral occurrences","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2024,"MonPub":null,"DateUpdate":"2024-11-25","DateCreate":"2024-07-30","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1,"DOI":"10.5194/os-20-569-2024"},"refs":null,"anarec":{"AnaID":393607,"PubliDate":2024,"Pagination":"569-587","XtraPublOfAnaID":null,"ISBN":null,"Volume":"20","Issue":"2","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":72541,"SerRR":"Ocean Science Journal. 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ISSN 1738-5261; e-ISSN 2005-7172","StandardTitleSer":"Ocean Science Journal","ISSN":"1738-5261","AbbrevSer":"Ocean Science Journal","StandardTitleMon":null,"StartPage":569,"Pages":19,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"van der Kaaden","Firstname":"Anna-Selma","Initials":"A.-S.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":391395,"AutID":482050,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":"EDS","InsFSN":"Koninklijk Nederlands Instituut voor Onderzoek der Zee; Estuarine and Delta Systems","ORCID":"0000-0002-8814-1822","PersID":40950,"InsID":13657},{"AutName":"van Oevelen","Firstname":"Dick","Initials":"D.","Affiliation":"EDS","Discriminator":null,"CorporateFlag":0,"BEntID":391395,"AutID":342090,"OrderNr":2,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":"EDS","InsFSN":"Koninklijk Nederlands Instituut voor Onderzoek der Zee; 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