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Rapid urbanization induced daily maximum wind speed decline in metropolitan areas: A case study in the Yangtze River Delta (China)
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dc.contributor.authorZhang, Gangfenges_ES
dc.contributor.authorAzorín Molina, Césares_ES
dc.contributor.authorWang, Xuejiaes_ES
dc.contributor.authorChen, Delianges_ES
dc.contributor.authorMcVicar, Tim R.es_ES
dc.contributor.authorGuijarro Pastor, José Antonioes_ES
dc.contributor.authorChappell, Adrianes_ES
dc.contributor.authorDeng, Kaiqianges_ES
dc.contributor.authorMinola, Lorenzoes_ES
dc.contributor.authorKong, Fenges_ES
dc.contributor.authorWang, Shuoes_ES
dc.contributor.authorShi, Peijunes_ES
dc.date.accessioned2023-08-01T06:19:24Z-
dc.date.available2023-08-01T06:19:24Z-
dc.date.issued2022-
dc.identifier.citationUrban Climate. 2022, 43, 101147es_ES
dc.identifier.issn2212-0955-
dc.identifier.urihttp://hdl.handle.net/20.500.11765/14853-
dc.description.abstractWind extremes cause many environmental and natural hazard related problems globally, particularly in heavily populated metropolitan areas. However, the underlying causes of maximum wind speed variability in urbanized regions remain largely unknown. Here, we investigated how rapid urbanization in the Yangtze River Delta (YRD), China, impacted daily maximum wind speed (DMWS) between 1990 and 2015, based on near-surface (10 m height) DMWS observations, reanalysis datasets, and night-time lighting data (a proxy for urbanization). The station observation shows that annual DMWS in the YRD significantly (p < 0.05) declined during 1990–2015, by −0.209 m s−1 decade−1, while slightly (p > 0.1) positive trends were found in NCEP-NCAR1 (+0.048 m s−1 decade−1) and ERA5 (+0.027 m s−1 decade−1). An increasing divergence between the reanalysis output and the station observation since 2005 was found, and those stations located in areas with high rates of urbanization show the strongest negative annual DMWS trend, implying the key role of urbanization in weakening DMWS. This finding is supported by sensitivity experiments conducted using a regional climate model (RegCM4) forced with both 1990 and 2015 land-use and land-cover (LULC) data, where the simulated DMWS using the 2015 LULC data was lower than that simulated using the 1990 LULC data.es_ES
dc.description.sponsorshipThis study was supported by the Second Tibetan Plateau Scientific Expedition and Research Program (STEP, Grant No. 2019QZKK0606), the National Natural Science Foundation of China (Grant No. 42101027 and No.41621061). This work was also supported by a Swedish Research Council (2017-03780) and a Swedish Research Council for Sustainable Development (2019-00509) grant, and by the IBER-STILLING project, funded by the Spanish Ministry of Science, Innovation and Universities (RTI2018-095749-A-I00; MCIU/AEI/FEDER, UE). C.A.M. was supported by a Ramon y Cajal fellowship (RYC-2017-22830). L.M. was founded by the International Postdoc grant from the Swedish Research Council (2021-00444).es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsLicencia CC: Reconocimiento–NoComercial–SinObraDerivada CC BY-NC-NDes_ES
dc.subjectDaily maximum wind speedes_ES
dc.subjectTrendes_ES
dc.subjectUrbanizationes_ES
dc.subjectYangtze River Deltaes_ES
dc.subjectRegional climate modeles_ES
dc.titleRapid urbanization induced daily maximum wind speed decline in metropolitan areas: A case study in the Yangtze River Delta (China)es_ES
dc.typeinfo:eu-repo/semantics/preprintes_ES
dc.relation.publisherversionhttps://doi.org/10.1016/j.uclim.2022.101147es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
Colecciones: Artículos científicos 2019-2022


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