Consistency of spatiotemporal variability of MODIS and ERA5-Land surface warming trends over complex topography

dc.authoridYilmaz, Meric/0000-0001-6921-7687
dc.authorscopusid57214083722
dc.authorwosidYilmaz, Meric/G-5145-2017
dc.contributor.authorYilmaz, Meric
dc.contributor.otherCivil Engineering
dc.date.accessioned2024-07-05T15:21:53Z
dc.date.available2024-07-05T15:21:53Z
dc.date.issued2023
dc.departmentAtılım Universityen_US
dc.department-temp[Yilmaz, Meric] Atilim Univ, Dept Civil Engn, Ankara, Turkiyeen_US
dc.descriptionYilmaz, Meric/0000-0001-6921-7687en_US
dc.description.abstractIn this study, the trend of widely used MODIS MxD11 and MxD21 Land Surface Temperature (LST) and ERA5-Land Skin Temperature (SKT) and 2 m air temperature products were validated using 2 m air temperature trends obtained by ground observations from 266 stations in 2000-2021 over Turkey, known to have complex topography. The results show that colder regions have substantially higher temporal temperature variability than warmer ones. MxD21 and MxD11 products are 4.4 & DEG;C and 2.9 & DEG;C warmer than ERA5-Land products, respectively, while ERA5-Land products (SKT and 2 m) have nearly similar averages (12.5 & DEG;C). The consistency between MODIS and ERA5-Land data is significantly lower over areas with more complex topography and irrigation activities, despite the fact that the products show a high linear relationship over the study area. While February trends are consistently much higher than other months (2.2 and 1.4 & DEG;C/decade for MODIS and ERA5-Land, respectively), overall MODIS skin temperature products (0.7 & DEG;C/decade) generally exhibit smaller trends than ERA5-Land skin and air temperature trends (0.94 & DEG;C/decade). The results suggested that MODIS and ERA5-Land trends, which are highly consistent with observations, might replace observations in the absence of long-term station-based records.en_US
dc.identifier.citation2
dc.identifier.doi10.1007/s11356-023-28983-y
dc.identifier.endpage94435en_US
dc.identifier.issn0944-1344
dc.identifier.issn1614-7499
dc.identifier.issue41en_US
dc.identifier.pmid37531063
dc.identifier.scopus2-s2.0-85166302305
dc.identifier.startpage94414en_US
dc.identifier.urihttps://doi.org/10.1007/s11356-023-28983-y
dc.identifier.urihttps://hdl.handle.net/20.500.14411/2139
dc.identifier.volume30en_US
dc.identifier.wosWOS:001041862000011
dc.identifier.wosqualityQ1
dc.institutionauthorYılmaz, Meriç
dc.language.isoenen_US
dc.publisherSpringer Heidelbergen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectSurface temperatureen_US
dc.subjectWarming trenden_US
dc.subjectMxD11en_US
dc.subjectMxD21en_US
dc.subjectERA5-Landen_US
dc.titleConsistency of spatiotemporal variability of MODIS and ERA5-Land surface warming trends over complex topographyen_US
dc.typeArticleen_US
dspace.entity.typePublication
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relation.isAuthorOfPublication.latestForDiscovery9ffb7c9c-733c-406c-891a-31d933a5152e
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