Climatic controls on the stable isotopic composition of precipitation in Northeast Asia
An examination of oxygen and hydrogen isotopic compositions of precipitation in NE Asia from the IAEA/WMO data set reveals that many sites have a distinct winter-summer seasonal pattern in deuterium excess (d-) values that appears to reflect different climatic conditions. To further understand this...
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| Veröffentlicht in: | Climate research 2003-01, Vol.23 (2), p.137-148 |
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| creator | Lee, Kwang-Sik Grundstein, Andrew J. Wenner, David B. Choi, Man-Sik Woo, Nam-Chil Lee, Dae-Ha |
| description | An examination of oxygen and hydrogen isotopic compositions of precipitation in NE Asia from the IAEA/WMO data set reveals that many sites have a distinct winter-summer seasonal pattern in deuterium excess (d-) values that appears to reflect different climatic conditions. To further understand this pattern, stable isotopic data were obtained for individual rainfall events over a 2 yr period at Jeju Island, Korea. The δ18O- and δD-values of precipitation at Jeju Island are not dependent upon temperature. However, the deuterium excess values, which range from 3.0 to 40.6‰, show a distinct seasonal variation with higher d-values in winter (>~15‰) and lower values in summer (~10‰). Such a seasonal variation is closely related to different air masses affecting the island during different seasons: a cold-dry continental polar air mass in winter and a hot-humid maritime tropical air mass in summer. |
| doi_str_mv | 10.3354/cr023137 |
| format | Article |
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To further understand this pattern, stable isotopic data were obtained for individual rainfall events over a 2 yr period at Jeju Island, Korea. The δ18O- and δD-values of precipitation at Jeju Island are not dependent upon temperature. However, the deuterium excess values, which range from 3.0 to 40.6‰, show a distinct seasonal variation with higher d-values in winter (>~15‰) and lower values in summer (~10‰). 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To further understand this pattern, stable isotopic data were obtained for individual rainfall events over a 2 yr period at Jeju Island, Korea. The δ18O- and δD-values of precipitation at Jeju Island are not dependent upon temperature. However, the deuterium excess values, which range from 3.0 to 40.6‰, show a distinct seasonal variation with higher d-values in winter (>~15‰) and lower values in summer (~10‰). Such a seasonal variation is closely related to different air masses affecting the island during different seasons: a cold-dry continental polar air mass in winter and a hot-humid maritime tropical air mass in summer.</description><subject>Air masses</subject><subject>Deuterium</subject><subject>Evaporation</subject><subject>Humidity</subject><subject>Oxygen</subject><subject>Precipitation</subject><subject>Rain</subject><subject>Seasons</subject><subject>Summer</subject><subject>Trajectories</subject><issn>0936-577X</issn><issn>1616-1572</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNo9kEtLAzEUhYMoWB_gHxCyEjejN7mZSWZZii8oulF0N6QxwZRpM-amC_-9Y6uuLpzznQP3MHYm4AqxVtcug0SBeo9NRCOaStRa7rMJtNhUtdZvh-yIaAkA0miYsNdZH1e2RMddWpeceuJpzcuH51Tsovc8Uipp2PqrIVEscfRT4EP2Lg6x2K0Q1_wx5TFmqfApRXvCDoLtyZ_-3mP2cnvzPLuv5k93D7PpvHKoTakQ4R2tkqLxIchW1-g9CtGGoKD1oW1ki3JR1wuhQVutlW48GKMsGnDCSjxmF7veIafPjafSrSI53_d27dOGOmG0Agl6BC93oMuJKPvQDXn8PH91Arqf5bq_5Ub0fIcuqaT8z0llGoNK4jfxiGo8</recordid><startdate>20030131</startdate><enddate>20030131</enddate><creator>Lee, Kwang-Sik</creator><creator>Grundstein, Andrew J.</creator><creator>Wenner, David B.</creator><creator>Choi, Man-Sik</creator><creator>Woo, Nam-Chil</creator><creator>Lee, Dae-Ha</creator><general>Inter-Research</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope></search><sort><creationdate>20030131</creationdate><title>Climatic controls on the stable isotopic composition of precipitation in Northeast Asia</title><author>Lee, Kwang-Sik ; Grundstein, Andrew J. ; Wenner, David B. ; Choi, Man-Sik ; Woo, Nam-Chil ; Lee, Dae-Ha</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c378t-330d3a4216eff29753ee3119ff409ef962932b55b1707a77476e0884a380c1a23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Air masses</topic><topic>Deuterium</topic><topic>Evaporation</topic><topic>Humidity</topic><topic>Oxygen</topic><topic>Precipitation</topic><topic>Rain</topic><topic>Seasons</topic><topic>Summer</topic><topic>Trajectories</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lee, Kwang-Sik</creatorcontrib><creatorcontrib>Grundstein, Andrew J.</creatorcontrib><creatorcontrib>Wenner, David B.</creatorcontrib><creatorcontrib>Choi, Man-Sik</creatorcontrib><creatorcontrib>Woo, Nam-Chil</creatorcontrib><creatorcontrib>Lee, Dae-Ha</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Climate research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lee, Kwang-Sik</au><au>Grundstein, Andrew J.</au><au>Wenner, David B.</au><au>Choi, Man-Sik</au><au>Woo, Nam-Chil</au><au>Lee, Dae-Ha</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Climatic controls on the stable isotopic composition of precipitation in Northeast Asia</atitle><jtitle>Climate research</jtitle><date>2003-01-31</date><risdate>2003</risdate><volume>23</volume><issue>2</issue><spage>137</spage><epage>148</epage><pages>137-148</pages><issn>0936-577X</issn><eissn>1616-1572</eissn><abstract>An examination of oxygen and hydrogen isotopic compositions of precipitation in NE Asia from the IAEA/WMO data set reveals that many sites have a distinct winter-summer seasonal pattern in deuterium excess (d-) values that appears to reflect different climatic conditions. To further understand this pattern, stable isotopic data were obtained for individual rainfall events over a 2 yr period at Jeju Island, Korea. The δ18O- and δD-values of precipitation at Jeju Island are not dependent upon temperature. However, the deuterium excess values, which range from 3.0 to 40.6‰, show a distinct seasonal variation with higher d-values in winter (>~15‰) and lower values in summer (~10‰). Such a seasonal variation is closely related to different air masses affecting the island during different seasons: a cold-dry continental polar air mass in winter and a hot-humid maritime tropical air mass in summer.</abstract><pub>Inter-Research</pub><doi>10.3354/cr023137</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
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| ispartof | Climate research, 2003-01, Vol.23 (2), p.137-148 |
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| language | eng |
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| source | Jstor Complete Legacy; Inter-Research; EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection |
| subjects | Air masses Deuterium Evaporation Humidity Oxygen Precipitation Rain Seasons Summer Trajectories |
| title | Climatic controls on the stable isotopic composition of precipitation in Northeast Asia |
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