A seasonality of δD of water vapor (850-500 hPa) observed from space over Jeju Island, Korea

Jeonghoon Lee; John Worden; Dong Chan Koh; Kei Yoshimura; Jung Eun Lee

doi:10.1007/s12303-013-0003-5

A seasonality of δD of water vapor (850-500 hPa) observed from space over Jeju Island, Korea

Jeonghoon Lee, John Worden, Dong Chan Koh, Kei Yoshimura, Jung Eun Lee

Department of Science Education

Research output: Contribution to journal › Article › peer-review

14 Scopus citations

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. We ran an isotope-enabled general circulation model (IsoGSM) and calculated 120-hr reverse-calculated trajectories for air parcels corresponding to the TES observations to better understand the seasonal variations of δD of water vapor in the lower troposphere. δD of precipitation by previous studies and the model results show winter-enriched, while summer-enriched water vapor isotope is observed by the TES observations, which may require a validation campaign using in-situ measurements or continuous monitoring of water vapor isotopes around Jeju Island.

Original language	English
Pages (from-to)	87-95
Number of pages	9
Journal	Geosciences Journal
Volume	17
Issue number	1
DOIs	https://doi.org/10.1007/s12303-013-0003-5
State	Published - Mar 2013

Bibliographical note

Funding Information:
ACKNOWLEDGMENTS: The research described in this paper was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration. This work was partially supported by KOPRI research grant (PE12070). Valuable comments from an anonymous reviewer and Dr. Kwang-Sik Lee have improved the quality of this paper.

Keywords

Jeju Island
isotope
seasonality
water vapor

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title = "A seasonality of δD of water vapor (850-500 hPa) observed from space over Jeju Island, Korea",

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. We ran an isotope-enabled general circulation model (IsoGSM) and calculated 120-hr reverse-calculated trajectories for air parcels corresponding to the TES observations to better understand the seasonal variations of δD of water vapor in the lower troposphere. δD of precipitation by previous studies and the model results show winter-enriched, while summer-enriched water vapor isotope is observed by the TES observations, which may require a validation campaign using in-situ measurements or continuous monitoring of water vapor isotopes around Jeju Island.",

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author = "Jeonghoon Lee and John Worden and Koh, {Dong Chan} and Kei Yoshimura and Lee, {Jung Eun}",

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AU - Koh, Dong Chan

AU - Yoshimura, Kei

AU - Lee, Jung Eun

N1 - Funding Information: ACKNOWLEDGMENTS: The research described in this paper was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration. This work was partially supported by KOPRI research grant (PE12070). Valuable comments from an anonymous reviewer and Dr. Kwang-Sik Lee have improved the quality of this paper.

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N2 - 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. We ran an isotope-enabled general circulation model (IsoGSM) and calculated 120-hr reverse-calculated trajectories for air parcels corresponding to the TES observations to better understand the seasonal variations of δD of water vapor in the lower troposphere. δD of precipitation by previous studies and the model results show winter-enriched, while summer-enriched water vapor isotope is observed by the TES observations, which may require a validation campaign using in-situ measurements or continuous monitoring of water vapor isotopes around Jeju Island.

AB - 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. We ran an isotope-enabled general circulation model (IsoGSM) and calculated 120-hr reverse-calculated trajectories for air parcels corresponding to the TES observations to better understand the seasonal variations of δD of water vapor in the lower troposphere. δD of precipitation by previous studies and the model results show winter-enriched, while summer-enriched water vapor isotope is observed by the TES observations, which may require a validation campaign using in-situ measurements or continuous monitoring of water vapor isotopes around Jeju Island.

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ER -

A seasonality of δD of water vapor (850-500 hPa) observed from space over Jeju Island, Korea

Abstract

Bibliographical note

Keywords

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