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dc.contributor.authorSakallı, Abdulla
dc.contributor.authorBaşusta, Nuri
dc.date.accessioned12.07.201910:50:10
dc.date.accessioned2019-07-12T22:06:02Z
dc.date.available12.07.201910:50:10
dc.date.available2019-07-12T22:06:02Z
dc.date.issued2018
dc.identifier.citationSakalli, A., Başusta, N. (2018). Sea surface temperature change in the Black Sea under climate change: A simulation of the sea surface temperature up to 2100. International Journal of Climatology, 38 (13), pp. 4687-4698. https://doi.org/10.1002/joc.5688en_US
dc.identifier.issn0899-8418
dc.identifier.issn1097-0088
dc.identifier.urihttps://doi.org/10.1002/joc.5688
dc.identifier.urihttps://hdl.handle.net/20.500.12508/620
dc.descriptionWOS: 000450222100002en_US
dc.description.abstractSurface temperature of the Black Sea increased due to climate change during the 20th century and continues to rise. Here we present by in situ data-corrected remote-sensed SST data covering a 34-year period (1982-2015). Using a linear black box model, we predicted the Black Sea surface temperature (SST) up to 2100. During the 34-year study period, we detected a 0.64 degrees C increase in SST per decade. The largest monthly fluctuations in SST were during late summer (August) and autumn (November). The rate of SST increase has almost caught up with the worst climate change scenario for the future. At the end of this century, the relative increase in average Black Sea SST is predicted to be 5.1 degrees C. In summary, our data show sea surface warming during recent decades, and we predict that this warming is likely to continue under the present environmental condition. The warming of the sea seems to also influence the amount of caught anchovies in the Black Sea. After 1993, the amount of captured anchovies in the southern Black Sea was drastically decreased with increased SST.en_US
dc.language.isoengen_US
dc.publisherWileyen_US
dc.relation.isversionof10.1002/joc.5688en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectAnchovyen_US
dc.subjectBlack Sea warmingen_US
dc.subjectCMEMSen_US
dc.subjectRemote sensingen_US
dc.subjectSSTen_US
dc.subject.classificationMeteorology & Atmospheric Sciencesen_US
dc.subject.classificationUpwelling | Sardinop Sagax | Pacific Decadal Oscillationen_US
dc.subject.otherLong-term trendsen_US
dc.subject.otherMediterranean seaen_US
dc.subject.otherNorth-seaen_US
dc.subject.otherAnchovyen_US
dc.subject.otherVariabilityen_US
dc.subject.otherEcosystemsen_US
dc.subject.otherSardinesen_US
dc.subject.otherImpactsen_US
dc.subject.otherLevelen_US
dc.subject.otherOceanen_US
dc.subject.otherAtmospheric temperatureen_US
dc.subject.otherClimate changeen_US
dc.subject.otherRemote sensingen_US
dc.subject.otherSubmarine geophysicsen_US
dc.subject.otherSurface propertiesen_US
dc.subject.otherSurface watersen_US
dc.subject.otherAnchovyen_US
dc.subject.otherBlack seaen_US
dc.subject.otherClimate change scenariosen_US
dc.subject.otherEnvironmental conditionsen_US
dc.subject.otherSea surface temperature (SST)en_US
dc.subject.otherSurface temperaturesen_US
dc.subject.otherOceanographyen_US
dc.subject.otherClupeoiden_US
dc.subject.otherEnvironmental conditionsen_US
dc.subject.otherRemote sensingen_US
dc.subject.otherSeasonal variationen_US
dc.subject.otherWarmingen_US
dc.subject.otherEngraulidaeen_US
dc.titleSea surface temperature change in the Black Sea under climate change: A simulation of the sea surface temperature up to 2100en_US
dc.typearticleen_US
dc.relation.journalInternational Journal of Climatologyen_US
dc.contributor.departmentMühendislik ve Doğa Bilimleri Fakültesi -- Endüstri Mühendisliği Bölümüen_US
dc.contributor.authorID0000-0002-4260-4772en_US
dc.identifier.volume38en_US
dc.identifier.issue13en_US
dc.identifier.startpage4687en_US
dc.identifier.endpage4698en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.contributor.isteauthorSakallı, Abdullaen_US
dc.relation.indexWeb of Science - Scopusen_US
dc.relation.indexWeb of Science Core Collection - Science Citation Index Expandeden_US


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