Consistency of spatiotemporal variability of MODIS and ERA5-Land surface warming trends over complex topography
dc.authorid | Yilmaz, Meric/0000-0001-6921-7687 | |
dc.authorscopusid | 57214083722 | |
dc.authorwosid | Yilmaz, Meric/G-5145-2017 | |
dc.contributor.author | Yilmaz, Meric | |
dc.contributor.other | Civil Engineering | |
dc.date.accessioned | 2024-07-05T15:21:53Z | |
dc.date.available | 2024-07-05T15:21:53Z | |
dc.date.issued | 2023 | |
dc.department | Atılım University | en_US |
dc.department-temp | [Yilmaz, Meric] Atilim Univ, Dept Civil Engn, Ankara, Turkiye | en_US |
dc.description | Yilmaz, Meric/0000-0001-6921-7687 | en_US |
dc.description.abstract | In 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.citation | 2 | |
dc.identifier.doi | 10.1007/s11356-023-28983-y | |
dc.identifier.endpage | 94435 | en_US |
dc.identifier.issn | 0944-1344 | |
dc.identifier.issn | 1614-7499 | |
dc.identifier.issue | 41 | en_US |
dc.identifier.pmid | 37531063 | |
dc.identifier.scopus | 2-s2.0-85166302305 | |
dc.identifier.startpage | 94414 | en_US |
dc.identifier.uri | https://doi.org/10.1007/s11356-023-28983-y | |
dc.identifier.uri | https://hdl.handle.net/20.500.14411/2139 | |
dc.identifier.volume | 30 | en_US |
dc.identifier.wos | WOS:001041862000011 | |
dc.identifier.wosquality | Q1 | |
dc.institutionauthor | Yılmaz, Meriç | |
dc.language.iso | en | en_US |
dc.publisher | Springer Heidelberg | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |
dc.rights | info:eu-repo/semantics/closedAccess | en_US |
dc.subject | Surface temperature | en_US |
dc.subject | Warming trend | en_US |
dc.subject | MxD11 | en_US |
dc.subject | MxD21 | en_US |
dc.subject | ERA5-Land | en_US |
dc.title | Consistency of spatiotemporal variability of MODIS and ERA5-Land surface warming trends over complex topography | en_US |
dc.type | Article | en_US |
dspace.entity.type | Publication | |
relation.isAuthorOfPublication | 9ffb7c9c-733c-406c-891a-31d933a5152e | |
relation.isAuthorOfPublication.latestForDiscovery | 9ffb7c9c-733c-406c-891a-31d933a5152e | |
relation.isOrgUnitOfPublication | 01fb4c5b-b45f-40c0-9a74-f0b3b6265a0d | |
relation.isOrgUnitOfPublication.latestForDiscovery | 01fb4c5b-b45f-40c0-9a74-f0b3b6265a0d |
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