{"refrec":{"BRefID":322845,"RR":"<b>Huynh, H.-N.T.; Alvera-Azcárate, A.; Beckers, J.-M.</b> (2020). Analysis of surface chlorophyll a associated with sea surface temperature and surface wind in the South China Sea. <i>Ocean Dynamics 70(1)</i>: 139-161. <a href=\"https://dx.doi.org/10.1007/s10236-019-01308-9\" target=\"_blank\">https://dx.doi.org/10.1007/s10236-019-01308-9</a>","BEntID":316316,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Ocean Dynamics 70(1)</i>: 139-161. <a href=\"https://dx.doi.org/10.1007/s10236-019-01308-9\" target=\"_blank\">https://dx.doi.org/10.1007/s10236-019-01308-9</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Huynh, H.-N.T.; Alvera-Azcárate, A.; Beckers, J.-M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Huynh, H.-N.T.; Alvera-Azcárate, A.; Beckers, J.-M.","Englishabstract":"In this study, the spatial and temporal variability in surface chlorophyll a (Chl-a) in the whole South China Sea (SCS) was investigated in detail by using 8-day, 4-km, gap-free MODIS-A data (2003–2016). Monthly climatology and empirical-orthogonal-functions analysis of Chl-a were performed in association with sea surface temperature and surface wind to aid in better understanding the physical mechanisms responsible for the Chl-a variability. The results are as follows: (1) Chl-a has out-of-phase variability between the coastal and open-sea regions due to different major factors controlling phytoplankton growth in each region; (2) in particular, Chl-a increases in the northern SCS during winter and in the western and southwestern SCS during summer mainly due to the effects of monsoons and orography; and (3) wind-driven coastal upwelling is stronger in the western SCS than in the eastern SCS. A wind-induced coastal upwelling not reported in the literature was detected along Palawan Island (8–12∘N, 117–120∘E) during winter. In the SCS, the Chl-a variability is influenced by the El Niño–Southern Oscillation with a time lag of 4–9 months, depending on the variability scales.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Analysis of surface chlorophyll a associated with sea surface temperature and surface wind in the South China Sea","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:32:52.928458","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Chlorophyll a; Sea surface temperature; Monsoon; ENSO; South China Sea;DINEOF","OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2020-04-14","DateCreate":"2020-04-07","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000499230600002","VABBcode":null,"OpenAcc":0,"DOI":"10.1007/s10236-019-01308-9"},"refs":null,"anarec":{"AnaID":322845,"PubliDate":2020,"Pagination":"139-161","XtraPublOfAnaID":null,"ISBN":null,"Volume":"70","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45486,"SerRR":"Ocean Dynamics. 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