Land surface emissivity change in China from 2001 to 2010
Land surface emissivity is one of the important parameters in temperature inversion from thermal infrared remote sensing. Using MOD11C3 of Terra-MODIS L3 level products, spatio-temporal data sets of land surface emissivity in China for 10 years from 2001 to 2010 are obtained. The results show that t...
Gespeichert in:
Veröffentlicht in: | Journal of geographical sciences 2012-06, Vol.22 (3), p.407-415 |
---|---|
Hauptverfasser: | , , , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 415 |
---|---|
container_issue | 3 |
container_start_page | 407 |
container_title | Journal of geographical sciences |
container_volume | 22 |
creator | Wang, Xinsheng Fan, Jiangwen Xu, Jing Liu, Fei Gao, Shoujie Wei, Xincai |
description | Land surface emissivity is one of the important parameters in temperature inversion from thermal infrared remote sensing. Using MOD11C3 of Terra-MODIS L3 level products, spatio-temporal data sets of land surface emissivity in China for 10 years from 2001 to 2010 are obtained. The results show that the land surface emissivity in the northwest desert region is the lowest in China, with little seasonal variations. In contrast, there are significant seasonal variations in land surface emissivity in northeast China and northern Xinjiang, the Qinghai-Tibet Plateau, the Yangtze River Valley and the eastern and southern China. In winter, the land surface emissivity in the northeast China and northern Xinjiang is relatively high. The land surface emissivity of the Qinghai-Tibet Plateau region is maintained at low value from November to March, while it becomes higher in other months. The land surface emissivity of the Yangtze River Valley, eastern and southern China, and Sichuan Basin varies from July to October, and peaks in August. Land surface emissivity values could be divided into five levels low emissivity (0.6163-0.9638), moderate-low emissivity (0.9639-0.9709), moderate emissivity (0.9710-0.9724), moderate-high emissivity (0.9725-0.9738), and high emissivity (0.9739-0.9999). The percentages of areas with low emissivity, moderate-low emissivity and moderate emissivity are, respectively, about 20%, 10% and 20%. The moderate-high emissivity region makes up 40%-50% of China's land surface area. The inter-annual variation of moderate-high emissivity region is also very clear, with two peaks (in spring and autumn) and two troughs (in summer and winter). The inter-annual variation of the high emissivity region is very significant, with a peak in winter (10%), while only 1% or 2% in other seasons. There is a clear association between the spatio-temporal distribution of China's land surface emissivity and temperature: the higher the emissivity, the lower the temperature, and vice versa. Emissivity is an inherent property of any object, but the precise value of its emissivity depends very much on its surrounding environmental factors. |
doi_str_mv | 10.1007/s11442-012-0935-0 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1093472329</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>41426056</cqvip_id><sourcerecordid>2918592009</sourcerecordid><originalsourceid>FETCH-LOGICAL-c405t-8e7843915078039bc8a41da57947c53ac81a9503bdb15652c26953af666029073</originalsourceid><addsrcrecordid>eNp9kEtLAzEUhYMoWKs_wN2ICG5G781zspTiCwpuFNyFNM20U9qZmswI_fdmmFLBhYtwQ3LOyZdDyCXCHQKo-4jIOc0B09JM5HBERlhIzLWQxXHaA-hcMvV5Ss5iXAEwzSUdET219TyLXSit85nfVDFW31W7y9zS1gufVXU2WVa1zcrQbDIKgFnbpIlwTk5Ku47-Yj_H5OPp8X3ykk_fnl8nD9PccRBtXnhVcKZRgCrSozNXWI5zK5TmyglmXYFWC2Cz-QyFFNRRqdNxKaUEqkGxMbkdcreh-ep8bE2CdH69trVvumgw_ZcryqhO0us_0lXThTrRGaqxEDrx9yocVC40MQZfmm2oNjbsUpTpyzRDmSaVafoyDSTPzT7ZRmfXZbC1q-LBSIXWqHQPSwddTFepv_BL8F_41R5o2dSLr-Q7BHPkVIKQ7AcRPYmL</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2918592009</pqid></control><display><type>article</type><title>Land surface emissivity change in China from 2001 to 2010</title><source>Springer Nature - Complete Springer Journals</source><source>ProQuest Central UK/Ireland</source><source>ProQuest Central</source><creator>Wang, Xinsheng ; Fan, Jiangwen ; Xu, Jing ; Liu, Fei ; Gao, Shoujie ; Wei, Xincai</creator><creatorcontrib>Wang, Xinsheng ; Fan, Jiangwen ; Xu, Jing ; Liu, Fei ; Gao, Shoujie ; Wei, Xincai</creatorcontrib><description>Land surface emissivity is one of the important parameters in temperature inversion from thermal infrared remote sensing. Using MOD11C3 of Terra-MODIS L3 level products, spatio-temporal data sets of land surface emissivity in China for 10 years from 2001 to 2010 are obtained. The results show that the land surface emissivity in the northwest desert region is the lowest in China, with little seasonal variations. In contrast, there are significant seasonal variations in land surface emissivity in northeast China and northern Xinjiang, the Qinghai-Tibet Plateau, the Yangtze River Valley and the eastern and southern China. In winter, the land surface emissivity in the northeast China and northern Xinjiang is relatively high. The land surface emissivity of the Qinghai-Tibet Plateau region is maintained at low value from November to March, while it becomes higher in other months. The land surface emissivity of the Yangtze River Valley, eastern and southern China, and Sichuan Basin varies from July to October, and peaks in August. Land surface emissivity values could be divided into five levels low emissivity (0.6163-0.9638), moderate-low emissivity (0.9639-0.9709), moderate emissivity (0.9710-0.9724), moderate-high emissivity (0.9725-0.9738), and high emissivity (0.9739-0.9999). The percentages of areas with low emissivity, moderate-low emissivity and moderate emissivity are, respectively, about 20%, 10% and 20%. The moderate-high emissivity region makes up 40%-50% of China's land surface area. The inter-annual variation of moderate-high emissivity region is also very clear, with two peaks (in spring and autumn) and two troughs (in summer and winter). The inter-annual variation of the high emissivity region is very significant, with a peak in winter (10%), while only 1% or 2% in other seasons. There is a clear association between the spatio-temporal distribution of China's land surface emissivity and temperature: the higher the emissivity, the lower the temperature, and vice versa. Emissivity is an inherent property of any object, but the precise value of its emissivity depends very much on its surrounding environmental factors.</description><identifier>ISSN: 1009-637X</identifier><identifier>EISSN: 1861-9568</identifier><identifier>DOI: 10.1007/s11442-012-0935-0</identifier><language>eng</language><publisher>Heidelberg: SP Science Press</publisher><subject>Annual variations ; Asia ; Bgi / Prodig ; China ; Earth and Environmental Science ; Emissivity ; Environmental factors ; Geographical Information Systems/Cartography ; Geography ; Nature Conservation ; Physical Geography ; Remote sensing ; Remote Sensing/Photogrammetry ; Rivers ; Seasonal variations ; Temperature inversions ; Temporal distribution ; Winter ; 中国东部 ; 季节变化 ; 年际变化 ; 新疆北部 ; 长江流域 ; 陆地表面 ; 青藏高原地区 ; 高发射率</subject><ispartof>Journal of geographical sciences, 2012-06, Vol.22 (3), p.407-415</ispartof><rights>Science China Press and Springer-Verlag Berlin Heidelberg 2012</rights><rights>Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2012</rights><rights>Science China Press and Springer-Verlag Berlin Heidelberg 2012.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c405t-8e7843915078039bc8a41da57947c53ac81a9503bdb15652c26953af666029073</citedby><cites>FETCH-LOGICAL-c405t-8e7843915078039bc8a41da57947c53ac81a9503bdb15652c26953af666029073</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/85906X/85906X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11442-012-0935-0$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2918592009?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,776,780,21368,27903,27904,33723,33724,41467,42536,43784,51297,64361,64363,64365,72215</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=25991797$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Wang, Xinsheng</creatorcontrib><creatorcontrib>Fan, Jiangwen</creatorcontrib><creatorcontrib>Xu, Jing</creatorcontrib><creatorcontrib>Liu, Fei</creatorcontrib><creatorcontrib>Gao, Shoujie</creatorcontrib><creatorcontrib>Wei, Xincai</creatorcontrib><title>Land surface emissivity change in China from 2001 to 2010</title><title>Journal of geographical sciences</title><addtitle>J. Geogr. Sci</addtitle><addtitle>Journal of Geographical Sciences</addtitle><description>Land surface emissivity is one of the important parameters in temperature inversion from thermal infrared remote sensing. Using MOD11C3 of Terra-MODIS L3 level products, spatio-temporal data sets of land surface emissivity in China for 10 years from 2001 to 2010 are obtained. The results show that the land surface emissivity in the northwest desert region is the lowest in China, with little seasonal variations. In contrast, there are significant seasonal variations in land surface emissivity in northeast China and northern Xinjiang, the Qinghai-Tibet Plateau, the Yangtze River Valley and the eastern and southern China. In winter, the land surface emissivity in the northeast China and northern Xinjiang is relatively high. The land surface emissivity of the Qinghai-Tibet Plateau region is maintained at low value from November to March, while it becomes higher in other months. The land surface emissivity of the Yangtze River Valley, eastern and southern China, and Sichuan Basin varies from July to October, and peaks in August. Land surface emissivity values could be divided into five levels low emissivity (0.6163-0.9638), moderate-low emissivity (0.9639-0.9709), moderate emissivity (0.9710-0.9724), moderate-high emissivity (0.9725-0.9738), and high emissivity (0.9739-0.9999). The percentages of areas with low emissivity, moderate-low emissivity and moderate emissivity are, respectively, about 20%, 10% and 20%. The moderate-high emissivity region makes up 40%-50% of China's land surface area. The inter-annual variation of moderate-high emissivity region is also very clear, with two peaks (in spring and autumn) and two troughs (in summer and winter). The inter-annual variation of the high emissivity region is very significant, with a peak in winter (10%), while only 1% or 2% in other seasons. There is a clear association between the spatio-temporal distribution of China's land surface emissivity and temperature: the higher the emissivity, the lower the temperature, and vice versa. Emissivity is an inherent property of any object, but the precise value of its emissivity depends very much on its surrounding environmental factors.</description><subject>Annual variations</subject><subject>Asia</subject><subject>Bgi / Prodig</subject><subject>China</subject><subject>Earth and Environmental Science</subject><subject>Emissivity</subject><subject>Environmental factors</subject><subject>Geographical Information Systems/Cartography</subject><subject>Geography</subject><subject>Nature Conservation</subject><subject>Physical Geography</subject><subject>Remote sensing</subject><subject>Remote Sensing/Photogrammetry</subject><subject>Rivers</subject><subject>Seasonal variations</subject><subject>Temperature inversions</subject><subject>Temporal distribution</subject><subject>Winter</subject><subject>中国东部</subject><subject>季节变化</subject><subject>年际变化</subject><subject>新疆北部</subject><subject>长江流域</subject><subject>陆地表面</subject><subject>青藏高原地区</subject><subject>高发射率</subject><issn>1009-637X</issn><issn>1861-9568</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNp9kEtLAzEUhYMoWKs_wN2ICG5G781zspTiCwpuFNyFNM20U9qZmswI_fdmmFLBhYtwQ3LOyZdDyCXCHQKo-4jIOc0B09JM5HBERlhIzLWQxXHaA-hcMvV5Ss5iXAEwzSUdET219TyLXSit85nfVDFW31W7y9zS1gufVXU2WVa1zcrQbDIKgFnbpIlwTk5Ku47-Yj_H5OPp8X3ykk_fnl8nD9PccRBtXnhVcKZRgCrSozNXWI5zK5TmyglmXYFWC2Cz-QyFFNRRqdNxKaUEqkGxMbkdcreh-ep8bE2CdH69trVvumgw_ZcryqhO0us_0lXThTrRGaqxEDrx9yocVC40MQZfmm2oNjbsUpTpyzRDmSaVafoyDSTPzT7ZRmfXZbC1q-LBSIXWqHQPSwddTFepv_BL8F_41R5o2dSLr-Q7BHPkVIKQ7AcRPYmL</recordid><startdate>20120601</startdate><enddate>20120601</enddate><creator>Wang, Xinsheng</creator><creator>Fan, Jiangwen</creator><creator>Xu, Jing</creator><creator>Liu, Fei</creator><creator>Gao, Shoujie</creator><creator>Wei, Xincai</creator><general>SP Science Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>HCIFZ</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>7ST</scope><scope>7U6</scope><scope>C1K</scope></search><sort><creationdate>20120601</creationdate><title>Land surface emissivity change in China from 2001 to 2010</title><author>Wang, Xinsheng ; Fan, Jiangwen ; Xu, Jing ; Liu, Fei ; Gao, Shoujie ; Wei, Xincai</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c405t-8e7843915078039bc8a41da57947c53ac81a9503bdb15652c26953af666029073</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Annual variations</topic><topic>Asia</topic><topic>Bgi / Prodig</topic><topic>China</topic><topic>Earth and Environmental Science</topic><topic>Emissivity</topic><topic>Environmental factors</topic><topic>Geographical Information Systems/Cartography</topic><topic>Geography</topic><topic>Nature Conservation</topic><topic>Physical Geography</topic><topic>Remote sensing</topic><topic>Remote Sensing/Photogrammetry</topic><topic>Rivers</topic><topic>Seasonal variations</topic><topic>Temperature inversions</topic><topic>Temporal distribution</topic><topic>Winter</topic><topic>中国东部</topic><topic>季节变化</topic><topic>年际变化</topic><topic>新疆北部</topic><topic>长江流域</topic><topic>陆地表面</topic><topic>青藏高原地区</topic><topic>高发射率</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Xinsheng</creatorcontrib><creatorcontrib>Fan, Jiangwen</creatorcontrib><creatorcontrib>Xu, Jing</creatorcontrib><creatorcontrib>Liu, Fei</creatorcontrib><creatorcontrib>Gao, Shoujie</creatorcontrib><creatorcontrib>Wei, Xincai</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>SciTech Premium Collection</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environment Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Journal of geographical sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Xinsheng</au><au>Fan, Jiangwen</au><au>Xu, Jing</au><au>Liu, Fei</au><au>Gao, Shoujie</au><au>Wei, Xincai</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Land surface emissivity change in China from 2001 to 2010</atitle><jtitle>Journal of geographical sciences</jtitle><stitle>J. Geogr. Sci</stitle><addtitle>Journal of Geographical Sciences</addtitle><date>2012-06-01</date><risdate>2012</risdate><volume>22</volume><issue>3</issue><spage>407</spage><epage>415</epage><pages>407-415</pages><issn>1009-637X</issn><eissn>1861-9568</eissn><abstract>Land surface emissivity is one of the important parameters in temperature inversion from thermal infrared remote sensing. Using MOD11C3 of Terra-MODIS L3 level products, spatio-temporal data sets of land surface emissivity in China for 10 years from 2001 to 2010 are obtained. The results show that the land surface emissivity in the northwest desert region is the lowest in China, with little seasonal variations. In contrast, there are significant seasonal variations in land surface emissivity in northeast China and northern Xinjiang, the Qinghai-Tibet Plateau, the Yangtze River Valley and the eastern and southern China. In winter, the land surface emissivity in the northeast China and northern Xinjiang is relatively high. The land surface emissivity of the Qinghai-Tibet Plateau region is maintained at low value from November to March, while it becomes higher in other months. The land surface emissivity of the Yangtze River Valley, eastern and southern China, and Sichuan Basin varies from July to October, and peaks in August. Land surface emissivity values could be divided into five levels low emissivity (0.6163-0.9638), moderate-low emissivity (0.9639-0.9709), moderate emissivity (0.9710-0.9724), moderate-high emissivity (0.9725-0.9738), and high emissivity (0.9739-0.9999). The percentages of areas with low emissivity, moderate-low emissivity and moderate emissivity are, respectively, about 20%, 10% and 20%. The moderate-high emissivity region makes up 40%-50% of China's land surface area. The inter-annual variation of moderate-high emissivity region is also very clear, with two peaks (in spring and autumn) and two troughs (in summer and winter). The inter-annual variation of the high emissivity region is very significant, with a peak in winter (10%), while only 1% or 2% in other seasons. There is a clear association between the spatio-temporal distribution of China's land surface emissivity and temperature: the higher the emissivity, the lower the temperature, and vice versa. Emissivity is an inherent property of any object, but the precise value of its emissivity depends very much on its surrounding environmental factors.</abstract><cop>Heidelberg</cop><pub>SP Science Press</pub><doi>10.1007/s11442-012-0935-0</doi><tpages>9</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1009-637X |
ispartof | Journal of geographical sciences, 2012-06, Vol.22 (3), p.407-415 |
issn | 1009-637X 1861-9568 |
language | eng |
recordid | cdi_proquest_miscellaneous_1093472329 |
source | Springer Nature - Complete Springer Journals; ProQuest Central UK/Ireland; ProQuest Central |
subjects | Annual variations Asia Bgi / Prodig China Earth and Environmental Science Emissivity Environmental factors Geographical Information Systems/Cartography Geography Nature Conservation Physical Geography Remote sensing Remote Sensing/Photogrammetry Rivers Seasonal variations Temperature inversions Temporal distribution Winter 中国东部 季节变化 年际变化 新疆北部 长江流域 陆地表面 青藏高原地区 高发射率 |
title | Land surface emissivity change in China from 2001 to 2010 |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-24T04%3A27%3A31IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Land%20surface%20emissivity%20change%20in%20China%20from%202001%20to%202010&rft.jtitle=Journal%20of%20geographical%20sciences&rft.au=Wang,%20Xinsheng&rft.date=2012-06-01&rft.volume=22&rft.issue=3&rft.spage=407&rft.epage=415&rft.pages=407-415&rft.issn=1009-637X&rft.eissn=1861-9568&rft_id=info:doi/10.1007/s11442-012-0935-0&rft_dat=%3Cproquest_cross%3E2918592009%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2918592009&rft_id=info:pmid/&rft_cqvip_id=41426056&rfr_iscdi=true |