Is Urban Heat Island intensity higher during hot spells and heat waves (Dijon, France, 2014–2019)?

The Urban Heat Island (UHI) phenomenon is frequently associated with heat waves, both in scientific literature and in the media. Health problems and other issues often result from the co-occurrence of these two phenomena. Previous studies have not yet provided sufficient evidence to validate potenti...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Urban climate 2021-01, Vol.35, p.100747, Article 100747
Hauptverfasser: Richard, Yves, Pohl, Benjamin, Rega, Mario, Pergaud, Julien, Thevenin, Thomas, Emery, Justin, Dudek, Julita, Vairet, Thibaut, Zito, Sébastien, Chateau-Smith, Carmela
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page
container_issue
container_start_page 100747
container_title Urban climate
container_volume 35
creator Richard, Yves
Pohl, Benjamin
Rega, Mario
Pergaud, Julien
Thevenin, Thomas
Emery, Justin
Dudek, Julita
Vairet, Thibaut
Zito, Sébastien
Chateau-Smith, Carmela
description The Urban Heat Island (UHI) phenomenon is frequently associated with heat waves, both in scientific literature and in the media. Health problems and other issues often result from the co-occurrence of these two phenomena. Previous studies have not yet provided sufficient evidence to validate potential links between UHIs and heat waves. The MUSTARDijon network was set up in 2014, in Dijon, France. Its spatial density (60 sensors) and temporal depth (6 summers) provide information about several Hot Spells and Heat Waves (HS&HW), as well as the daily intensity of UHIs. For the period from June to August (the warmer months), no statistical relationship could be established between temperature and UHI intensity. The UHI phenomenon is strong when days are sunny and not very windy; these two conditions are frequently met during HS&HW, but not systematically. By contrast, these conditions can be fulfilled even without high temperatures. Strong UHIs can thus develop outside Hot Spell/Heat Wave (HS/HW) events. These HS&HW are not necessarily in phase with UHIs: maximum UHI intensity tends to occur before the onset or during the first few days of HS&HW. The intensity of the UHI decreases during HS&HW because nocturnal urban temperature generally remains stationary, whereas rural temperature tends to increase at night. The hypothesis proposed is that this increase in rural night temperature during HS&HW could be linked to the decrease in Actual Evapotranspiration (ETa) and soil wetness. •MUSTARDijon is a dense new meteorological network in a medium-sized European city.•Six long Hot Spells & Heat Waves (HS&HW) are identified in Dijon from 2014 to 2019.•Observational and reanalysis data are combined to study UHI intensity during HS&HW.•No synchronicity is observed between UHI intensity and temperature during HS&HW.•Low soil moisture and low evapotranspiration favor high rural temperatures at night.
doi_str_mv 10.1016/j.uclim.2020.100747
format Article
fullrecord <record><control><sourceid>elsevier_hal_p</sourceid><recordid>TN_cdi_hal_primary_oai_HAL_hal_03058359v1</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S2212095520306611</els_id><sourcerecordid>S2212095520306611</sourcerecordid><originalsourceid>FETCH-LOGICAL-c448t-113ca06256c7d854ca8a67f8b3c85305120fa858f53958ac4cbc59249193bf253</originalsourceid><addsrcrecordid>eNp9kM1Kw0AUhQdRsGifwM0sLbR1fjLJzEKkVGsLBTd2PUwmk2ZCmpSZtNKd7-Ab-iROjIgrV-dyON-93APADUZTjHB8V04PurK7KUGkc1ASJWdgQAgmEyQYO_8zX4Kh9yVCIYmJiPEAZCsPNy5VNVwa1cKVr1SdQVu3pva2PcHCbgvjYHZwtt7Commh35uq8rCLFR3ypo7Gw9tHWzb1GC6cqrUZw3Ag-nz_CCJGD9fgIleVN8MfvQKbxdPrfDlZvzyv5rP1REcRbycYU61QTFisk4yzSCuu4iTnKdWcUcQwQbnijOeMCsaVjnSqmSCRwIKmOWH0Coz6vYWq5N7ZnXIn2Sgrl7O17DwUtnDKxBGHLO2z2jXeO5P_AhjJrldZyu9eZder7HsN1H1PmfDG0RonvbYmfJxZZ3Qrs8b-y38BKRJ-vg</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Is Urban Heat Island intensity higher during hot spells and heat waves (Dijon, France, 2014–2019)?</title><source>Alma/SFX Local Collection</source><creator>Richard, Yves ; Pohl, Benjamin ; Rega, Mario ; Pergaud, Julien ; Thevenin, Thomas ; Emery, Justin ; Dudek, Julita ; Vairet, Thibaut ; Zito, Sébastien ; Chateau-Smith, Carmela</creator><creatorcontrib>Richard, Yves ; Pohl, Benjamin ; Rega, Mario ; Pergaud, Julien ; Thevenin, Thomas ; Emery, Justin ; Dudek, Julita ; Vairet, Thibaut ; Zito, Sébastien ; Chateau-Smith, Carmela</creatorcontrib><description><![CDATA[The Urban Heat Island (UHI) phenomenon is frequently associated with heat waves, both in scientific literature and in the media. Health problems and other issues often result from the co-occurrence of these two phenomena. Previous studies have not yet provided sufficient evidence to validate potential links between UHIs and heat waves. The MUSTARDijon network was set up in 2014, in Dijon, France. Its spatial density (60 sensors) and temporal depth (6 summers) provide information about several Hot Spells and Heat Waves (HS&HW), as well as the daily intensity of UHIs. For the period from June to August (the warmer months), no statistical relationship could be established between temperature and UHI intensity. The UHI phenomenon is strong when days are sunny and not very windy; these two conditions are frequently met during HS&HW, but not systematically. By contrast, these conditions can be fulfilled even without high temperatures. Strong UHIs can thus develop outside Hot Spell/Heat Wave (HS/HW) events. These HS&HW are not necessarily in phase with UHIs: maximum UHI intensity tends to occur before the onset or during the first few days of HS&HW. The intensity of the UHI decreases during HS&HW because nocturnal urban temperature generally remains stationary, whereas rural temperature tends to increase at night. The hypothesis proposed is that this increase in rural night temperature during HS&HW could be linked to the decrease in Actual Evapotranspiration (ETa) and soil wetness. •MUSTARDijon is a dense new meteorological network in a medium-sized European city.•Six long Hot Spells & Heat Waves (HS&HW) are identified in Dijon from 2014 to 2019.•Observational and reanalysis data are combined to study UHI intensity during HS&HW.•No synchronicity is observed between UHI intensity and temperature during HS&HW.•Low soil moisture and low evapotranspiration favor high rural temperatures at night.]]></description><identifier>ISSN: 2212-0955</identifier><identifier>EISSN: 2212-0955</identifier><identifier>DOI: 10.1016/j.uclim.2020.100747</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Climatology ; Earth Sciences ; Environmental Sciences ; Evapotranspiration ; Hot day ; Hot spells &amp; heat waves ; Medium-sized city ; Sciences of the Universe ; Soil moisture ; Urban Heat Island intensity</subject><ispartof>Urban climate, 2021-01, Vol.35, p.100747, Article 100747</ispartof><rights>2020 Elsevier B.V.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c448t-113ca06256c7d854ca8a67f8b3c85305120fa858f53958ac4cbc59249193bf253</citedby><cites>FETCH-LOGICAL-c448t-113ca06256c7d854ca8a67f8b3c85305120fa858f53958ac4cbc59249193bf253</cites><orcidid>0000-0002-9339-797X ; 0000-0002-9203-0922 ; 0000-0001-6995-1670 ; 0000-0003-1114-7377 ; 0000-0002-8869-8719 ; 0000-0003-3579-4990</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,314,776,780,881,4010,27900,27901,27902</link.rule.ids><backlink>$$Uhttps://hal.science/hal-03058359$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Richard, Yves</creatorcontrib><creatorcontrib>Pohl, Benjamin</creatorcontrib><creatorcontrib>Rega, Mario</creatorcontrib><creatorcontrib>Pergaud, Julien</creatorcontrib><creatorcontrib>Thevenin, Thomas</creatorcontrib><creatorcontrib>Emery, Justin</creatorcontrib><creatorcontrib>Dudek, Julita</creatorcontrib><creatorcontrib>Vairet, Thibaut</creatorcontrib><creatorcontrib>Zito, Sébastien</creatorcontrib><creatorcontrib>Chateau-Smith, Carmela</creatorcontrib><title>Is Urban Heat Island intensity higher during hot spells and heat waves (Dijon, France, 2014–2019)?</title><title>Urban climate</title><description><![CDATA[The Urban Heat Island (UHI) phenomenon is frequently associated with heat waves, both in scientific literature and in the media. Health problems and other issues often result from the co-occurrence of these two phenomena. Previous studies have not yet provided sufficient evidence to validate potential links between UHIs and heat waves. The MUSTARDijon network was set up in 2014, in Dijon, France. Its spatial density (60 sensors) and temporal depth (6 summers) provide information about several Hot Spells and Heat Waves (HS&HW), as well as the daily intensity of UHIs. For the period from June to August (the warmer months), no statistical relationship could be established between temperature and UHI intensity. The UHI phenomenon is strong when days are sunny and not very windy; these two conditions are frequently met during HS&HW, but not systematically. By contrast, these conditions can be fulfilled even without high temperatures. Strong UHIs can thus develop outside Hot Spell/Heat Wave (HS/HW) events. These HS&HW are not necessarily in phase with UHIs: maximum UHI intensity tends to occur before the onset or during the first few days of HS&HW. The intensity of the UHI decreases during HS&HW because nocturnal urban temperature generally remains stationary, whereas rural temperature tends to increase at night. The hypothesis proposed is that this increase in rural night temperature during HS&HW could be linked to the decrease in Actual Evapotranspiration (ETa) and soil wetness. •MUSTARDijon is a dense new meteorological network in a medium-sized European city.•Six long Hot Spells & Heat Waves (HS&HW) are identified in Dijon from 2014 to 2019.•Observational and reanalysis data are combined to study UHI intensity during HS&HW.•No synchronicity is observed between UHI intensity and temperature during HS&HW.•Low soil moisture and low evapotranspiration favor high rural temperatures at night.]]></description><subject>Climatology</subject><subject>Earth Sciences</subject><subject>Environmental Sciences</subject><subject>Evapotranspiration</subject><subject>Hot day</subject><subject>Hot spells &amp; heat waves</subject><subject>Medium-sized city</subject><subject>Sciences of the Universe</subject><subject>Soil moisture</subject><subject>Urban Heat Island intensity</subject><issn>2212-0955</issn><issn>2212-0955</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp9kM1Kw0AUhQdRsGifwM0sLbR1fjLJzEKkVGsLBTd2PUwmk2ZCmpSZtNKd7-Ab-iROjIgrV-dyON-93APADUZTjHB8V04PurK7KUGkc1ASJWdgQAgmEyQYO_8zX4Kh9yVCIYmJiPEAZCsPNy5VNVwa1cKVr1SdQVu3pva2PcHCbgvjYHZwtt7Commh35uq8rCLFR3ypo7Gw9tHWzb1GC6cqrUZw3Ag-nz_CCJGD9fgIleVN8MfvQKbxdPrfDlZvzyv5rP1REcRbycYU61QTFisk4yzSCuu4iTnKdWcUcQwQbnijOeMCsaVjnSqmSCRwIKmOWH0Coz6vYWq5N7ZnXIn2Sgrl7O17DwUtnDKxBGHLO2z2jXeO5P_AhjJrldZyu9eZder7HsN1H1PmfDG0RonvbYmfJxZZ3Qrs8b-y38BKRJ-vg</recordid><startdate>202101</startdate><enddate>202101</enddate><creator>Richard, Yves</creator><creator>Pohl, Benjamin</creator><creator>Rega, Mario</creator><creator>Pergaud, Julien</creator><creator>Thevenin, Thomas</creator><creator>Emery, Justin</creator><creator>Dudek, Julita</creator><creator>Vairet, Thibaut</creator><creator>Zito, Sébastien</creator><creator>Chateau-Smith, Carmela</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>AAYXX</scope><scope>CITATION</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0002-9339-797X</orcidid><orcidid>https://orcid.org/0000-0002-9203-0922</orcidid><orcidid>https://orcid.org/0000-0001-6995-1670</orcidid><orcidid>https://orcid.org/0000-0003-1114-7377</orcidid><orcidid>https://orcid.org/0000-0002-8869-8719</orcidid><orcidid>https://orcid.org/0000-0003-3579-4990</orcidid></search><sort><creationdate>202101</creationdate><title>Is Urban Heat Island intensity higher during hot spells and heat waves (Dijon, France, 2014–2019)?</title><author>Richard, Yves ; Pohl, Benjamin ; Rega, Mario ; Pergaud, Julien ; Thevenin, Thomas ; Emery, Justin ; Dudek, Julita ; Vairet, Thibaut ; Zito, Sébastien ; Chateau-Smith, Carmela</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c448t-113ca06256c7d854ca8a67f8b3c85305120fa858f53958ac4cbc59249193bf253</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Climatology</topic><topic>Earth Sciences</topic><topic>Environmental Sciences</topic><topic>Evapotranspiration</topic><topic>Hot day</topic><topic>Hot spells &amp; heat waves</topic><topic>Medium-sized city</topic><topic>Sciences of the Universe</topic><topic>Soil moisture</topic><topic>Urban Heat Island intensity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Richard, Yves</creatorcontrib><creatorcontrib>Pohl, Benjamin</creatorcontrib><creatorcontrib>Rega, Mario</creatorcontrib><creatorcontrib>Pergaud, Julien</creatorcontrib><creatorcontrib>Thevenin, Thomas</creatorcontrib><creatorcontrib>Emery, Justin</creatorcontrib><creatorcontrib>Dudek, Julita</creatorcontrib><creatorcontrib>Vairet, Thibaut</creatorcontrib><creatorcontrib>Zito, Sébastien</creatorcontrib><creatorcontrib>Chateau-Smith, Carmela</creatorcontrib><collection>CrossRef</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Urban climate</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Richard, Yves</au><au>Pohl, Benjamin</au><au>Rega, Mario</au><au>Pergaud, Julien</au><au>Thevenin, Thomas</au><au>Emery, Justin</au><au>Dudek, Julita</au><au>Vairet, Thibaut</au><au>Zito, Sébastien</au><au>Chateau-Smith, Carmela</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Is Urban Heat Island intensity higher during hot spells and heat waves (Dijon, France, 2014–2019)?</atitle><jtitle>Urban climate</jtitle><date>2021-01</date><risdate>2021</risdate><volume>35</volume><spage>100747</spage><pages>100747-</pages><artnum>100747</artnum><issn>2212-0955</issn><eissn>2212-0955</eissn><abstract><![CDATA[The Urban Heat Island (UHI) phenomenon is frequently associated with heat waves, both in scientific literature and in the media. Health problems and other issues often result from the co-occurrence of these two phenomena. Previous studies have not yet provided sufficient evidence to validate potential links between UHIs and heat waves. The MUSTARDijon network was set up in 2014, in Dijon, France. Its spatial density (60 sensors) and temporal depth (6 summers) provide information about several Hot Spells and Heat Waves (HS&HW), as well as the daily intensity of UHIs. For the period from June to August (the warmer months), no statistical relationship could be established between temperature and UHI intensity. The UHI phenomenon is strong when days are sunny and not very windy; these two conditions are frequently met during HS&HW, but not systematically. By contrast, these conditions can be fulfilled even without high temperatures. Strong UHIs can thus develop outside Hot Spell/Heat Wave (HS/HW) events. These HS&HW are not necessarily in phase with UHIs: maximum UHI intensity tends to occur before the onset or during the first few days of HS&HW. The intensity of the UHI decreases during HS&HW because nocturnal urban temperature generally remains stationary, whereas rural temperature tends to increase at night. The hypothesis proposed is that this increase in rural night temperature during HS&HW could be linked to the decrease in Actual Evapotranspiration (ETa) and soil wetness. •MUSTARDijon is a dense new meteorological network in a medium-sized European city.•Six long Hot Spells & Heat Waves (HS&HW) are identified in Dijon from 2014 to 2019.•Observational and reanalysis data are combined to study UHI intensity during HS&HW.•No synchronicity is observed between UHI intensity and temperature during HS&HW.•Low soil moisture and low evapotranspiration favor high rural temperatures at night.]]></abstract><pub>Elsevier B.V</pub><doi>10.1016/j.uclim.2020.100747</doi><orcidid>https://orcid.org/0000-0002-9339-797X</orcidid><orcidid>https://orcid.org/0000-0002-9203-0922</orcidid><orcidid>https://orcid.org/0000-0001-6995-1670</orcidid><orcidid>https://orcid.org/0000-0003-1114-7377</orcidid><orcidid>https://orcid.org/0000-0002-8869-8719</orcidid><orcidid>https://orcid.org/0000-0003-3579-4990</orcidid><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 2212-0955
ispartof Urban climate, 2021-01, Vol.35, p.100747, Article 100747
issn 2212-0955
2212-0955
language eng
recordid cdi_hal_primary_oai_HAL_hal_03058359v1
source Alma/SFX Local Collection
subjects Climatology
Earth Sciences
Environmental Sciences
Evapotranspiration
Hot day
Hot spells & heat waves
Medium-sized city
Sciences of the Universe
Soil moisture
Urban Heat Island intensity
title Is Urban Heat Island intensity higher during hot spells and heat waves (Dijon, France, 2014–2019)?
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-04T23%3A47%3A31IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-elsevier_hal_p&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Is%20Urban%20Heat%20Island%20intensity%20higher%20during%20hot%20spells%20and%20heat%20waves%20(Dijon,%20France,%202014%E2%80%932019)?&rft.jtitle=Urban%20climate&rft.au=Richard,%20Yves&rft.date=2021-01&rft.volume=35&rft.spage=100747&rft.pages=100747-&rft.artnum=100747&rft.issn=2212-0955&rft.eissn=2212-0955&rft_id=info:doi/10.1016/j.uclim.2020.100747&rft_dat=%3Celsevier_hal_p%3ES2212095520306611%3C/elsevier_hal_p%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_els_id=S2212095520306611&rfr_iscdi=true