

FOLLOWUS
1.Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
2.Laboratory for Ocean and Climate Dynamics, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
3.University of Chinese Academy of Sciences, Beijing 100049, China
4.Center for Ocean Mega-Science, Chinese Academy of Sciences Qingdao 266071, China
XU Yongsheng, E-mail: yongsheng.xu@qdio.ac.cn
收稿:2019-05-05,
录用:2019-11-22,
网络首发:2021-01-12,
纸质出版:2021-03
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Quantification of the impact of environmental factors on chlorophyll in the open ocean[J]. 海洋湖沼学报(英文), 2021,39(2):447-457.
Dandan ZHAO, Le GAO, Yongsheng XU. Quantification of the impact of environmental factors on chlorophyll in the open ocean[J]. Journal of Oceanology and Limnology, 2021, 39(2): 447-457.
Quantification of the impact of environmental factors on chlorophyll in the open ocean[J]. 海洋湖沼学报(英文), 2021,39(2):447-457. DOI: 10.1007/s00343-020-9121-x.
Dandan ZHAO, Le GAO, Yongsheng XU. Quantification of the impact of environmental factors on chlorophyll in the open ocean[J]. Journal of Oceanology and Limnology, 2021, 39(2): 447-457. DOI: 10.1007/s00343-020-9121-x.
Many previous studies of the impact of oceanic environmental factors on chlorophyll (CHL) in a specific region focused on sea surface temperature (SST)
mixed-layer depth (MLD)
or wind stress (WS) alone. In this study
relationship between CHL and all those environmental factors (SST
MLD
and WS) in the open ocean was quantified for five regions within the subtropical gyres and the variation trend of 13-year (2003-2015) was analyzed using satellite observations and Argo measurements. The correlation analysis results show that MLD was correlated positively with CHL
SST was correlated negatively with CHL
and the correlation between CHL and WS was either positive or negative. Based on the significance of the correlations
models representing the relationships were established using the multiple linear regression and analyzed
showing that the environmental factors were the major determinants of CHL change. The regression coefficients show that both SST and MLD have remarkable effect on CHL. Our derived models could be used to diagnose the past changes
understand present variability
and predict the future state of CHL changes based on environmental factors
and help us understand the dynamics of CHL variation in the open ocean.
BehrenfeldMJ,O'MalleyRT,SiegelDA,McClainCR,SarmientoJL,FeldmanGC,MilliganAJ,FalkowskiPG,LetelierRM,BossES.2006.Climate-driventrendsincontemporaryoceanproductivity. Nature , 444 (7120):752-755,https://doi.org/10.1038/nature05317..
BentamyA,GrodskySA,CartonJA,Croizé-FillonD,ChapronB.2012.MatchingASCATandQuikSCATwinds. Journal of Geophysical Research: Oceans , 117 (C2):C02011,https://doi.org/10.1029/2011JC007479..
CheltonDB,GaubeP,SchlaxMG,EarlyJJ,SamelsonRM.2011a.Theinfluenceofnonlinearmesoscaleeddiesonnear-surfaceoceanicchlorophyll. Science , 334 (6054):328-332,https://doi.org/10.1126/science.1208897..
D'SaEJ,KorobkinM.2009.WindinfluenceonchlorophyllvariabilityalongtheLouisiana-Texascoastfromsatellitewindandoceancolordata. In :ProceedingsofSPIE7473,RemoteSensingoftheOcean,SeaIce,andLargeWaterRegions2009.SPIE,Berlin,Germany.747305p, https://doi.org/10.1117/12.830537 https://doi.org/10.1117/12.830537 ..
FayAR,McKinleyGA.2017.CorrelationsofsurfaceoceanpCO 2 tosatellitechlorophyllonmonthlytointerannualtimescales. Global Biogeochemical Cycles , 31 (3):436-455,https://doi.org/10.1002/2016GB005563..
FengJF,DurantJM,StigeLC,HessenDO,HjermannDØ,ZhuL,LlopeM,StensethNC.2015.Contrastingcorrelationpatternsbetweenenvironmentalfactorsandchlorophylllevelsintheglobalocean. Global Biogeochemical Cycles , 29 (12):2095-2107,https://doi.org/10.1002/2015GB005216..
GeorgeDG,EdwardsRW.1976.TheEffectofwindonthedistributionofchlorophyll a andcrustaceanplanktoninashalloweutrophicreservoir. Journal of Applied Ecology , 13 (3):667-690,https://doi.org/10.2307/2402246..
GreggWW,CaseyNW,McClainCR.2005.Recenttrendsinglobaloceanchlorophyll. Geophysical Research Letters , 32 (3):L03606,https://doi.org/10.1029/2004GL021808..
HuangRX,RussellS.1994.Ventilationofthesubtropicalnorthpacific. Journal of Physical Oceanography , 24 (12):2589-2605,https://doi.org/10.1175/1520-0485(1994)024 < 2589:votsnp > 2.0.co;2..
ItohS,YasudaI,SaitoH,TsudaA,KomatsuK.2015.Mixedlayerdepthandchlorophyll a :ProfilingfloatobservationsintheKuroshio-Oyashioextensionregion. Journal of Marine Systems , 151 :1-14,https://doi.org/10.1016/j.jmarsys.2015.06.004..
JiCX,ZhangYZ,ChengQM,TsouJY,JiangTC,LiangXS.2018.Evaluatingtheimpactofseasurfacetemperature(SST)onspatialdistributionofchlorophyll-aconcentrationintheEastChinaSea. International Journal of Applied Earth Observation and Geoinformation , 68 :252-261,https://doi.org/10.1016/j.jag.2018.01.020..
KavakMT,KaradoganS.2012.TherelationshipbetweenseasurfacetemperatureandchlorophyllconcentrationofphytoplanktonsintheBlackSeausingremotesensingtechniques. Journal of Environmental Biology , 33 (2Suppl.):493-498..
KillworthPD,CipolliniP,UzBM,BlundellJR.2004.Physicalandbiologicalmechanismsforplanetarywavesobservedinsatellite-derivedchlorophyll. Journal of Geophysical Research: Oceans , 109 (C7):C07002,https://doi.org/10.1029/2003JC001768..
LiuFF,ChenCQ,ZhanHG.2012.DecadalvariabilityofchlorophyllaintheSouthChinaSea: a possiblemechanism. Chinese Journal of Oceanology and Limnology , 30 (6):1054-1062,https://doi.org/10.1007/s00343-012-1282-9..
LonghurstA.1993.Seasonalcoolingandbloomingintropicaloceans. Deep Sea Research Part Ⅰ : Oceanographic Research Papers , 40 (11-12):2145-2165,https://doi.org/10.1016/0967-0637(93)90095-K..
LovenduskiNS,GruberN,DoneySC.2008.TowardamechanisticunderstandingofthedecadaltrendsintheSouthernOceancarbonsink. Global Biogeochemical Cycles , 22 (3):GB3016,https://doi.org/10.1029/2007GB003139..
McClainCR,SignoriniSR,ChristianJR.2004.Subtropicalgyrevariabilityobservedbyocean-colorsatellites. Deep Sea Research Part Ⅱ : Topical Studies in Oceanography , 51 (1-3):281-301,https://doi.org/10.1016/j.dsr2.2003.08.002..
McQuatters-GollopA,MeeLD,RaitsosDE,ShapiroGI.2008.Non-linearities,regimeshiftsandrecovery:TherecentinfluenceofclimateonBlackSeachlorophyll. Journal of Marine Systems , 74 (1-2):649-658,https://doi.org/10.1016/j.jmarsys.2008.06.002..
NezlinNP,LiBL.2003.Time-seriesanalysisofremotesensedchlorophyllandenvironmentalfactorsintheSantaMonica-SanPedroBasinoffSouthernCalifornia. Journal of Marine Systems , 39 (3-4):185-202,https://doi.org/10.1016/S0924-7963(03)00030-7..
QiuFW,FangWD,FangGH.2011.Seasonal-to-interannualvariabilityofchlorophyllincentralwesternSouthChinaSeaextractedfromSeaWiFS. Chinese Journal of Oceanology and Limnology , 29 (1):18-25,https://doi.org/10.1007/s00343-011-9931-y..
RaymontJEG.1980.PlanktonandProductivityintheOceans.Phytoplankton,vol.1.2 nd edn.Pergamon,Oxford.489p.
UzBM,YoderJA.2004.HighfrequencyandmesoscalevariabilityinSeaWiFSchlorophyllimageryanditsrelationtootherremotelysensedoceanographicvariables. Deep Sea Research Part Ⅱ : Topical Studies in Oceanography , 51 (10-11):1001-1017,https://doi.org/10.1016/j.dsr2.2004.03.003..
WangDK,WangH,LiM,LiuMM,WuXY.2013.RoleofEkmantransportversusEkmanpumpingindrivingsummerupwellingintheSouthChinaSea. Journal of Ocean University of China , 12 (3):355-365,https://doi.org/10.1007/s11802-013-1904-7..
WebsterIT,HutchinsonPA.1994.Effectofwindonthedistributionofphytoplanktoncellsinlakesrevisited. Limnology and Oceanography , 39 (2):365-373,https://doi.org/10.4319/lo.1994.39.2.0365..
WentzFJ.1997.Awell-calibratedoceanalgorithmforspecialsensormicrowave/imager. Journal of Geophysical Research: Oceans , 102 (C4):8703-8718,https://doi.org/10.1029/96JC01751..
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