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Influence of ground surface characteristics on the mean radiant temperature in urban areas
The effect of variations in land cover on mean radiant temperature ( T mrt ) is explored through a simple scheme developed within the radiation model SOLWEIG. Outgoing longwave radiation is parameterised using surface temperature observations on a grass and an asphalt surface, whereas outgoing short...
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Published in: | International journal of biometeorology 2016-09, Vol.60 (9), p.1439-1452 |
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creator | Lindberg, Fredrik Onomura, Shiho Grimmond, C. S. B. |
description | The effect of variations in land cover on mean radiant temperature (
T
mrt
) is explored through a simple scheme developed within the radiation model SOLWEIG. Outgoing longwave radiation is parameterised using surface temperature observations on a grass and an asphalt surface, whereas outgoing shortwave radiation is modelled through variations in albedo for the different surfaces. The influence of ground surface materials on
T
mrt
is small compared to the effects of shadowing. Nevertheless, altering ground surface materials could contribute to a reduction in
T
mrt
to reduce the radiant load during heat-wave episodes in locations where shadowing is not an option. Evaluation of the new scheme suggests that despite its simplicity it can simulate the outgoing fluxes well, especially during sunny conditions. However, it underestimates at night and in shadowed locations. One grass surface used to develop the parameterisation, with very different characteristics compared to an evaluation grass site, caused
T
mrt
to be underestimated. The implications of using high temporal resolution (e.g. 15 minutes) meteorological forcing data under partly cloudy conditions are demonstrated even for fairly proximal sites. |
doi_str_mv | 10.1007/s00484-016-1135-x |
format | article |
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T
mrt
) is explored through a simple scheme developed within the radiation model SOLWEIG. Outgoing longwave radiation is parameterised using surface temperature observations on a grass and an asphalt surface, whereas outgoing shortwave radiation is modelled through variations in albedo for the different surfaces. The influence of ground surface materials on
T
mrt
is small compared to the effects of shadowing. Nevertheless, altering ground surface materials could contribute to a reduction in
T
mrt
to reduce the radiant load during heat-wave episodes in locations where shadowing is not an option. Evaluation of the new scheme suggests that despite its simplicity it can simulate the outgoing fluxes well, especially during sunny conditions. However, it underestimates at night and in shadowed locations. One grass surface used to develop the parameterisation, with very different characteristics compared to an evaluation grass site, caused
T
mrt
to be underestimated. The implications of using high temporal resolution (e.g. 15 minutes) meteorological forcing data under partly cloudy conditions are demonstrated even for fairly proximal sites.</description><identifier>ISSN: 0020-7128</identifier><identifier>EISSN: 1432-1254</identifier><identifier>DOI: 10.1007/s00484-016-1135-x</identifier><identifier>PMID: 26852384</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Albedo ; Animal Physiology ; Asphalt ; Biological and Medical Physics ; Biophysics ; Earth and Environmental Science ; Earth and Related Environmental Sciences ; energy ; Environment ; Environmental Health ; environments ; fluxes ; freiburg ; Geovetenskap och relaterad miljövetenskap ; germany ; Gothenburg ; Grasses ; Hydrocarbons ; Land use ; London ; Meteorology ; Models, Theoretical ; Original Paper ; outdoor thermal comfort ; parameterization ; Plant Physiology ; Poaceae ; solar-radiation ; SOLWEIG ; street canyon ; summer ; Sunlight ; Surface mount technology ; Surface temperature ; Temperature ; Temperature effects ; Urban areas ; Water</subject><ispartof>International journal of biometeorology, 2016-09, Vol.60 (9), p.1439-1452</ispartof><rights>ISB 2016</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-p283t-a586b2ec41c7b0258482a0b65e8984b2a876b193c43ac3100306aa6af13f46b23</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/26852384$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://gup.ub.gu.se/publication/246683$$DView record from Swedish Publication Index$$Hfree_for_read</backlink></links><search><creatorcontrib>Lindberg, Fredrik</creatorcontrib><creatorcontrib>Onomura, Shiho</creatorcontrib><creatorcontrib>Grimmond, C. S. B.</creatorcontrib><title>Influence of ground surface characteristics on the mean radiant temperature in urban areas</title><title>International journal of biometeorology</title><addtitle>Int J Biometeorol</addtitle><addtitle>Int J Biometeorol</addtitle><description>The effect of variations in land cover on mean radiant temperature (
T
mrt
) is explored through a simple scheme developed within the radiation model SOLWEIG. Outgoing longwave radiation is parameterised using surface temperature observations on a grass and an asphalt surface, whereas outgoing shortwave radiation is modelled through variations in albedo for the different surfaces. The influence of ground surface materials on
T
mrt
is small compared to the effects of shadowing. Nevertheless, altering ground surface materials could contribute to a reduction in
T
mrt
to reduce the radiant load during heat-wave episodes in locations where shadowing is not an option. Evaluation of the new scheme suggests that despite its simplicity it can simulate the outgoing fluxes well, especially during sunny conditions. However, it underestimates at night and in shadowed locations. One grass surface used to develop the parameterisation, with very different characteristics compared to an evaluation grass site, caused
T
mrt
to be underestimated. The implications of using high temporal resolution (e.g. 15 minutes) meteorological forcing data under partly cloudy conditions are demonstrated even for fairly proximal sites.</description><subject>Albedo</subject><subject>Animal Physiology</subject><subject>Asphalt</subject><subject>Biological and Medical Physics</subject><subject>Biophysics</subject><subject>Earth and Environmental Science</subject><subject>Earth and Related Environmental Sciences</subject><subject>energy</subject><subject>Environment</subject><subject>Environmental Health</subject><subject>environments</subject><subject>fluxes</subject><subject>freiburg</subject><subject>Geovetenskap och relaterad miljövetenskap</subject><subject>germany</subject><subject>Gothenburg</subject><subject>Grasses</subject><subject>Hydrocarbons</subject><subject>Land use</subject><subject>London</subject><subject>Meteorology</subject><subject>Models, Theoretical</subject><subject>Original Paper</subject><subject>outdoor thermal comfort</subject><subject>parameterization</subject><subject>Plant Physiology</subject><subject>Poaceae</subject><subject>solar-radiation</subject><subject>SOLWEIG</subject><subject>street canyon</subject><subject>summer</subject><subject>Sunlight</subject><subject>Surface mount technology</subject><subject>Surface temperature</subject><subject>Temperature</subject><subject>Temperature effects</subject><subject>Urban areas</subject><subject>Water</subject><issn>0020-7128</issn><issn>1432-1254</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqNkT1PHDEQhq0oUbgAP4AGWUqTxom_11silA8kJJqkobFmfbPHolvvYq8V8u8x3IEQVaqRZp4ZzauHkBPBvwrOm2-Zc-0048IyIZRh9-_ISmglmZBGvycrziVnjZDugHzK-ZbXHWebj-RAWmekcnpFri9ivy0YA9Kpp5s0lbimuaQeaifcQIKwYBryMoRMp0iXG6QjQqQJ1gPEhS44zphgKQnpEGlJXR1CQshH5EMP24zH-3pI_vz4_vv8F7u8-nlxfnbJZunUwsA420kMWoSm49I47STwzhp0rdOdBNfYTrQqaAVB1dyKWwALvVC9rpvqkLDd3fwX59L5OQ0jpH9-gsFvyuxra1N8Ri-1tU5V_suOn9N0VzAvfhxywO0WIk4le-FEK7Q2rfkfVNvGGNVW9PMb9HYqKdbgTxS31ra2Uqd7qnQjrl9-fRZSAbkPU0dxg-nVGe4frfuddV-t-0fr_l49AASGnHU</recordid><startdate>20160901</startdate><enddate>20160901</enddate><creator>Lindberg, Fredrik</creator><creator>Onomura, Shiho</creator><creator>Grimmond, C. 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B.</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>3V.</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>7X7</scope><scope>7XB</scope><scope>88E</scope><scope>88F</scope><scope>88I</scope><scope>8FE</scope><scope>8FH</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>K9.</scope><scope>KL.</scope><scope>LK8</scope><scope>M0S</scope><scope>M1P</scope><scope>M1Q</scope><scope>M2P</scope><scope>M7P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PHGZM</scope><scope>PHGZT</scope><scope>PJZUB</scope><scope>PKEHL</scope><scope>PPXIY</scope><scope>PQEST</scope><scope>PQGLB</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7X8</scope><scope>ADTPV</scope><scope>AOWAS</scope><scope>F1U</scope></search><sort><creationdate>20160901</creationdate><title>Influence of ground surface characteristics on the mean radiant temperature in urban areas</title><author>Lindberg, Fredrik ; Onomura, Shiho ; Grimmond, C. S. B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p283t-a586b2ec41c7b0258482a0b65e8984b2a876b193c43ac3100306aa6af13f46b23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Albedo</topic><topic>Animal Physiology</topic><topic>Asphalt</topic><topic>Biological and Medical Physics</topic><topic>Biophysics</topic><topic>Earth and Environmental Science</topic><topic>Earth and Related Environmental Sciences</topic><topic>energy</topic><topic>Environment</topic><topic>Environmental Health</topic><topic>environments</topic><topic>fluxes</topic><topic>freiburg</topic><topic>Geovetenskap och relaterad miljövetenskap</topic><topic>germany</topic><topic>Gothenburg</topic><topic>Grasses</topic><topic>Hydrocarbons</topic><topic>Land use</topic><topic>London</topic><topic>Meteorology</topic><topic>Models, Theoretical</topic><topic>Original Paper</topic><topic>outdoor thermal comfort</topic><topic>parameterization</topic><topic>Plant Physiology</topic><topic>Poaceae</topic><topic>solar-radiation</topic><topic>SOLWEIG</topic><topic>street canyon</topic><topic>summer</topic><topic>Sunlight</topic><topic>Surface mount technology</topic><topic>Surface temperature</topic><topic>Temperature</topic><topic>Temperature effects</topic><topic>Urban areas</topic><topic>Water</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lindberg, Fredrik</creatorcontrib><creatorcontrib>Onomura, Shiho</creatorcontrib><creatorcontrib>Grimmond, C. 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S. B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Influence of ground surface characteristics on the mean radiant temperature in urban areas</atitle><jtitle>International journal of biometeorology</jtitle><stitle>Int J Biometeorol</stitle><addtitle>Int J Biometeorol</addtitle><date>2016-09-01</date><risdate>2016</risdate><volume>60</volume><issue>9</issue><spage>1439</spage><epage>1452</epage><pages>1439-1452</pages><issn>0020-7128</issn><eissn>1432-1254</eissn><abstract>The effect of variations in land cover on mean radiant temperature (
T
mrt
) is explored through a simple scheme developed within the radiation model SOLWEIG. Outgoing longwave radiation is parameterised using surface temperature observations on a grass and an asphalt surface, whereas outgoing shortwave radiation is modelled through variations in albedo for the different surfaces. The influence of ground surface materials on
T
mrt
is small compared to the effects of shadowing. Nevertheless, altering ground surface materials could contribute to a reduction in
T
mrt
to reduce the radiant load during heat-wave episodes in locations where shadowing is not an option. Evaluation of the new scheme suggests that despite its simplicity it can simulate the outgoing fluxes well, especially during sunny conditions. However, it underestimates at night and in shadowed locations. One grass surface used to develop the parameterisation, with very different characteristics compared to an evaluation grass site, caused
T
mrt
to be underestimated. The implications of using high temporal resolution (e.g. 15 minutes) meteorological forcing data under partly cloudy conditions are demonstrated even for fairly proximal sites.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><pmid>26852384</pmid><doi>10.1007/s00484-016-1135-x</doi><tpages>14</tpages></addata></record> |
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subjects | Albedo Animal Physiology Asphalt Biological and Medical Physics Biophysics Earth and Environmental Science Earth and Related Environmental Sciences energy Environment Environmental Health environments fluxes freiburg Geovetenskap och relaterad miljövetenskap germany Gothenburg Grasses Hydrocarbons Land use London Meteorology Models, Theoretical Original Paper outdoor thermal comfort parameterization Plant Physiology Poaceae solar-radiation SOLWEIG street canyon summer Sunlight Surface mount technology Surface temperature Temperature Temperature effects Urban areas Water |
title | Influence of ground surface characteristics on the mean radiant temperature in urban areas |
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