A seasonality of δD of water vapor (850? 500 hPa) observed from space over Jeju Island, Korea
DC Field | Value | Language |
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dc.contributor.author | Koh, Dong-Chan | - |
dc.contributor.author | Lee, Jungeun | - |
dc.contributor.author | K.Yoshimura | - |
dc.contributor.author | J.Worden | - |
dc.contributor.author | Lee, Jeonghoon | - |
dc.date.accessioned | 2018-03-20T13:44:32Z | - |
dc.date.available | 2018-03-20T13:44:32Z | - |
dc.date.issued | 2013 | - |
dc.identifier.uri | https://repository.kopri.re.kr/handle/201206/6198 | - |
dc.description.abstract | We examined the seasonal variations of isotopic composition of water vapor in the lower troposphere (850? 500 hPa) to relate those of precipitation and groundwater using satellite observations from the Aura Tropospheric Emission Spectrometer (TES) over the volcanic Island of Jeju, Korea.ectrometer (TES) over the volcanic Island of Jeju, Korea. | - |
dc.language | English | - |
dc.publisher | Springer/The Association of Korean Geoscience Societies and Springer | - |
dc.subject | Geology | - |
dc.title | A seasonality of δD of water vapor (850? 500 hPa) observed from space over Jeju Island, Korea | - |
dc.title.alternative | JeJu 상공 수증기의 δD 값의 계절적 변동 | - |
dc.type | Article | - |
dc.identifier.bibliographicCitation | Koh, Dong-Chan, et al. 2013. "A seasonality of δD of water vapor (850? 500 hPa) observed from space over Jeju Island, Korea". <em>GEOSCIENCES JOURNAL</em>, 17(1): 87-95. | - |
dc.citation.title | GEOSCIENCES JOURNAL | - |
dc.citation.volume | 17 | - |
dc.citation.number | 1 | - |
dc.identifier.doi | 10.1007/s12303-013-0003-5 | - |
dc.citation.startPage | 87 | - |
dc.citation.endPage | 95 | - |
dc.description.articleClassification | SCIE | - |
dc.description.jcrRate | JCR 2011:78.82 | - |
dc.subject.keyword | Jeju Island | - |
dc.subject.keyword | isotope | - |
dc.subject.keyword | seasonality | - |
dc.subject.keyword | vapor | - |
dc.identifier.localId | 2013-0213 | - |
dc.identifier.scopusid | 2-s2.0-84874930229 | - |
dc.identifier.wosid | 000316121900009 | - |
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