Seasonal variations in the surface energy and CO2 flux over a high‐rise, high‐population, residential urban area in the East Asian monsoon region
Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea. The study area is affected by the Asian mo...
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description | Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea. The study area is affected by the Asian monsoon, which is accompanied by long rain spells and a related mid‐season depression of solar radiation in the summer. Our analysis shows that the urban surface energy balance and turbulence characteristics demonstrate typical urban properties. Unstable conditions dominate all day, and the storage heat flux (night‐time and morning) and sensible heat flux (afternoon) significantly affect the diurnal variations in the urban surface energy balance. Owing to the rough urban surface, the turbulence intensities are higher than those reported previously in other cities. The annual CO2 emission rate is approximately 13.1 kg CO2 m−2⋅year−1 with traffic, which is the major source of CO2 (+2.3 μmol⋅m−2⋅s−1 per 100 vehicles). Ecosystem respiration, including that by vegetation, soil, and humans, becomes dominant in the night‐time (00:00–05:00), thus contributing significantly to the annual CO2 budget. Further analysis indicates a unique coupling of urban surface energy partitioning and CO2 emission rates with the seasonal progression of the Asian monsoon: (a) surface albedo has annual minima in late summer when the sun elevation angle, is relatively higher and the urban surface condition is wetter than in other seasons; (b) the Bowen ratio ranges from 1.7 (summer) to 7.0 (winter); and (c) CO2 emission rates show seasonal variations with the progress of the summer monsoon.
Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea. |
doi_str_mv | 10.1002/joc.6463 |
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Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea.</description><identifier>ISSN: 0899-8418</identifier><identifier>EISSN: 1097-0088</identifier><identifier>DOI: 10.1002/joc.6463</identifier><language>eng</language><publisher>Chichester, UK: John Wiley & Sons, Ltd</publisher><subject>Albedo ; Albedo (solar) ; Asian monsoon ; Bowen ratio ; Carbon dioxide ; Carbon dioxide emissions ; Carbon dioxide flux ; CO2 emission ; Covariance ; Diurnal variations ; East Asian monsoon ; Eddy covariance ; eddy covariance method ; Elevation angle ; Emission ; Energy balance ; Enthalpy ; Fluctuations ; Heat flux ; Heat transfer ; high‐rise residential area ; Momentum ; Monsoons ; Night ; Residential areas ; Seasonal variation ; Seasonal variations ; Seasons ; Sensible heat ; Sensible heat flux ; Sensible heat transfer ; Seoul ; Soil ; Solar radiation ; Storage ; Summer ; Summer monsoon ; Surface energy ; Surface energy balance ; Surface properties ; Turbulence ; Turbulence intensities ; Turbulent fluxes ; Urban areas ; urban climate ; Wind</subject><ispartof>International journal of climatology, 2020-08, Vol.40 (10), p.4384-4407</ispartof><rights>2019 The Authors. International Journal of Climatology published by John Wiley & Sons Ltd on behalf of the Royal Meteorological Society.</rights><rights>2019. This article is published under http://creativecommons.org/licenses/by-nc/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><orcidid>0000-0001-8769-0312 ; 0000-0003-0139-602X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fjoc.6463$$EPDF$$P50$$Gwiley$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fjoc.6463$$EHTML$$P50$$Gwiley$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids></links><search><creatorcontrib>Hong, Je‐Woo</creatorcontrib><creatorcontrib>Lee, Sang‐Dae</creatorcontrib><creatorcontrib>Lee, Keunmin</creatorcontrib><creatorcontrib>Hong, Jinkyu</creatorcontrib><title>Seasonal variations in the surface energy and CO2 flux over a high‐rise, high‐population, residential urban area in the East Asian monsoon region</title><title>International journal of climatology</title><description>Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea. The study area is affected by the Asian monsoon, which is accompanied by long rain spells and a related mid‐season depression of solar radiation in the summer. Our analysis shows that the urban surface energy balance and turbulence characteristics demonstrate typical urban properties. Unstable conditions dominate all day, and the storage heat flux (night‐time and morning) and sensible heat flux (afternoon) significantly affect the diurnal variations in the urban surface energy balance. Owing to the rough urban surface, the turbulence intensities are higher than those reported previously in other cities. The annual CO2 emission rate is approximately 13.1 kg CO2 m−2⋅year−1 with traffic, which is the major source of CO2 (+2.3 μmol⋅m−2⋅s−1 per 100 vehicles). Ecosystem respiration, including that by vegetation, soil, and humans, becomes dominant in the night‐time (00:00–05:00), thus contributing significantly to the annual CO2 budget. Further analysis indicates a unique coupling of urban surface energy partitioning and CO2 emission rates with the seasonal progression of the Asian monsoon: (a) surface albedo has annual minima in late summer when the sun elevation angle, is relatively higher and the urban surface condition is wetter than in other seasons; (b) the Bowen ratio ranges from 1.7 (summer) to 7.0 (winter); and (c) CO2 emission rates show seasonal variations with the progress of the summer monsoon.
Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea.</description><subject>Albedo</subject><subject>Albedo (solar)</subject><subject>Asian monsoon</subject><subject>Bowen ratio</subject><subject>Carbon dioxide</subject><subject>Carbon dioxide emissions</subject><subject>Carbon dioxide flux</subject><subject>CO2 emission</subject><subject>Covariance</subject><subject>Diurnal variations</subject><subject>East Asian monsoon</subject><subject>Eddy covariance</subject><subject>eddy covariance method</subject><subject>Elevation angle</subject><subject>Emission</subject><subject>Energy balance</subject><subject>Enthalpy</subject><subject>Fluctuations</subject><subject>Heat flux</subject><subject>Heat transfer</subject><subject>high‐rise residential area</subject><subject>Momentum</subject><subject>Monsoons</subject><subject>Night</subject><subject>Residential areas</subject><subject>Seasonal variation</subject><subject>Seasonal variations</subject><subject>Seasons</subject><subject>Sensible heat</subject><subject>Sensible heat flux</subject><subject>Sensible heat transfer</subject><subject>Seoul</subject><subject>Soil</subject><subject>Solar radiation</subject><subject>Storage</subject><subject>Summer</subject><subject>Summer monsoon</subject><subject>Surface energy</subject><subject>Surface energy balance</subject><subject>Surface properties</subject><subject>Turbulence</subject><subject>Turbulence intensities</subject><subject>Turbulent fluxes</subject><subject>Urban areas</subject><subject>urban climate</subject><subject>Wind</subject><issn>0899-8418</issn><issn>1097-0088</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><recordid>eNo1UEtOwzAUtBBIlILEESyxbYo_sWMvq6r8VKkLYB05idO6Su1gJ4XuOAIbLshJcCldjd7TfDQDwDVGY4wQuV27csxTTk_AACOZJQgJcQoGSEiZiBSLc3ARwhohJCXmA_D9rFVwVjVwq7xRnXE2QGNht9Iw9L5WpYbaar_cQWUrOF0QWDf9B3Rb7aGCK7Nc_Xx-eRP06Hi0ru2bP6cR9DqYStvOxIDeF8pC5bU6BsxU6OAkmPjexFznbBQso_ASnNWqCfrqH4fg9W72Mn1I5ov7x-lknrSEMZpgkXGdCl6QrKJ1RilhIk2ZlDSLfasMIaVlJSkuClZhgVkpZMkrEkllyRmnQ3Bz8G29e-t16PK1631cI-QkJZIzmWEWWcmB9W4avctbbzbK73KM8v3iUVLm-8Xzp8V0j_QXppR3cw</recordid><startdate>202008</startdate><enddate>202008</enddate><creator>Hong, Je‐Woo</creator><creator>Lee, Sang‐Dae</creator><creator>Lee, Keunmin</creator><creator>Hong, Jinkyu</creator><general>John Wiley & Sons, Ltd</general><general>Wiley Subscription Services, Inc</general><scope>24P</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0001-8769-0312</orcidid><orcidid>https://orcid.org/0000-0003-0139-602X</orcidid></search><sort><creationdate>202008</creationdate><title>Seasonal variations in the surface energy and CO2 flux over a high‐rise, high‐population, residential urban area in the East Asian monsoon region</title><author>Hong, Je‐Woo ; Lee, Sang‐Dae ; Lee, Keunmin ; Hong, Jinkyu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p2553-1876e486b27d3f7332584459937089d700ae9d931bb5d1815c89c6d2844cc6563</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Albedo</topic><topic>Albedo (solar)</topic><topic>Asian monsoon</topic><topic>Bowen ratio</topic><topic>Carbon dioxide</topic><topic>Carbon dioxide emissions</topic><topic>Carbon dioxide flux</topic><topic>CO2 emission</topic><topic>Covariance</topic><topic>Diurnal variations</topic><topic>East Asian monsoon</topic><topic>Eddy covariance</topic><topic>eddy covariance method</topic><topic>Elevation angle</topic><topic>Emission</topic><topic>Energy balance</topic><topic>Enthalpy</topic><topic>Fluctuations</topic><topic>Heat flux</topic><topic>Heat transfer</topic><topic>high‐rise residential area</topic><topic>Momentum</topic><topic>Monsoons</topic><topic>Night</topic><topic>Residential areas</topic><topic>Seasonal variation</topic><topic>Seasonal variations</topic><topic>Seasons</topic><topic>Sensible heat</topic><topic>Sensible heat flux</topic><topic>Sensible heat transfer</topic><topic>Seoul</topic><topic>Soil</topic><topic>Solar radiation</topic><topic>Storage</topic><topic>Summer</topic><topic>Summer monsoon</topic><topic>Surface energy</topic><topic>Surface energy balance</topic><topic>Surface properties</topic><topic>Turbulence</topic><topic>Turbulence intensities</topic><topic>Turbulent fluxes</topic><topic>Urban areas</topic><topic>urban climate</topic><topic>Wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hong, Je‐Woo</creatorcontrib><creatorcontrib>Lee, Sang‐Dae</creatorcontrib><creatorcontrib>Lee, Keunmin</creatorcontrib><creatorcontrib>Hong, Jinkyu</creatorcontrib><collection>Wiley Online Library Open Access</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>International journal of climatology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hong, Je‐Woo</au><au>Lee, Sang‐Dae</au><au>Lee, Keunmin</au><au>Hong, Jinkyu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Seasonal variations in the surface energy and CO2 flux over a high‐rise, high‐population, residential urban area in the East Asian monsoon region</atitle><jtitle>International journal of climatology</jtitle><date>2020-08</date><risdate>2020</risdate><volume>40</volume><issue>10</issue><spage>4384</spage><epage>4407</epage><pages>4384-4407</pages><issn>0899-8418</issn><eissn>1097-0088</eissn><abstract>Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea. The study area is affected by the Asian monsoon, which is accompanied by long rain spells and a related mid‐season depression of solar radiation in the summer. Our analysis shows that the urban surface energy balance and turbulence characteristics demonstrate typical urban properties. Unstable conditions dominate all day, and the storage heat flux (night‐time and morning) and sensible heat flux (afternoon) significantly affect the diurnal variations in the urban surface energy balance. Owing to the rough urban surface, the turbulence intensities are higher than those reported previously in other cities. The annual CO2 emission rate is approximately 13.1 kg CO2 m−2⋅year−1 with traffic, which is the major source of CO2 (+2.3 μmol⋅m−2⋅s−1 per 100 vehicles). Ecosystem respiration, including that by vegetation, soil, and humans, becomes dominant in the night‐time (00:00–05:00), thus contributing significantly to the annual CO2 budget. Further analysis indicates a unique coupling of urban surface energy partitioning and CO2 emission rates with the seasonal progression of the Asian monsoon: (a) surface albedo has annual minima in late summer when the sun elevation angle, is relatively higher and the urban surface condition is wetter than in other seasons; (b) the Bowen ratio ranges from 1.7 (summer) to 7.0 (winter); and (c) CO2 emission rates show seasonal variations with the progress of the summer monsoon.
Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea.</abstract><cop>Chichester, UK</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/joc.6463</doi><tpages>24</tpages><orcidid>https://orcid.org/0000-0001-8769-0312</orcidid><orcidid>https://orcid.org/0000-0003-0139-602X</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Albedo Albedo (solar) Asian monsoon Bowen ratio Carbon dioxide Carbon dioxide emissions Carbon dioxide flux CO2 emission Covariance Diurnal variations East Asian monsoon Eddy covariance eddy covariance method Elevation angle Emission Energy balance Enthalpy Fluctuations Heat flux Heat transfer high‐rise residential area Momentum Monsoons Night Residential areas Seasonal variation Seasonal variations Seasons Sensible heat Sensible heat flux Sensible heat transfer Seoul Soil Solar radiation Storage Summer Summer monsoon Surface energy Surface energy balance Surface properties Turbulence Turbulence intensities Turbulent fluxes Urban areas urban climate Wind |
title | Seasonal variations in the surface energy and CO2 flux over a high‐rise, high‐population, residential urban area in the East Asian monsoon region |
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