Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia
Abstract Deciduous forest covers vast areas of permafrost under severe dry climate in eastern Siberia. Understanding the water cycle in this forest ecosystem is quite important for climate projection. In this study, diurnal variations in isotopic compositions of atmospheric water vapour were observe...
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crwiley:10.1002/hyp.9361 2024-06-02T08:13:08+00:00 Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia Ueta, Akihiro Sugimoto, Atsuko Iijima, Yoshihiro Yabuki, Hironori Maximov, Trofim C. Velivetskaya, Tatiana A. Ignatiev, Alexander V. 2012 http://dx.doi.org/10.1002/hyp.9361 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9361 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.9361 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 27, issue 16, page 2295-2305 ISSN 0885-6087 1099-1085 journal-article 2012 crwiley https://doi.org/10.1002/hyp.9361 2024-05-03T11:54:08Z Abstract Deciduous forest covers vast areas of permafrost under severe dry climate in eastern Siberia. Understanding the water cycle in this forest ecosystem is quite important for climate projection. In this study, diurnal variations in isotopic compositions of atmospheric water vapour were observed in eastern Siberia with isotope analyses of precipitation, sap water of larch trees, soil water, and water in surface organic layer during the late summer periods of 2006, 2007, and 2008. In these years, the soil moisture content was considerably high due to unusually large amounts of summer rainfall and winter snowfall. The observed sap water δ 18 O ranged from −17.9‰ to −13.3‰, which was close to that of summer precipitation and soil water in the shallow layer, and represents that of transpired water vapour. On sunny days, as the air temperature and mixing ratio rose from predawn to morning, the atmospheric water vapour δ 18 O increased by 1‰ to 5‰ and then decreased by about 2‰ from morning to afternoon with the mixing ratio. On cloudy days, by contrast, the afternoon decrease in δ 18 O and the mixing ratio was not observed. These results show that water vapour that transpired from plants, with higher δ 18 O than the atmospheric water vapour, contributes to the increase in δ 18 O in the morning, whereas water vapour in the free atmosphere, with lower δ 18 O, contributes to the decrease in the afternoon on sunny days. The observed results reveal the significance of transpired water vapour, with relatively high δ 18 O, in the water cycle on a short diurnal time scale and confirm the importance of the recycling of precipitation through transpiration in continental forest environments such as the eastern Siberian taiga. Copyright © 2012 John Wiley & Sons, Ltd. Article in Journal/Newspaper permafrost taiga Siberia Wiley Online Library Hydrological Processes 27 16 2295 2305 |
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English |
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Abstract Deciduous forest covers vast areas of permafrost under severe dry climate in eastern Siberia. Understanding the water cycle in this forest ecosystem is quite important for climate projection. In this study, diurnal variations in isotopic compositions of atmospheric water vapour were observed in eastern Siberia with isotope analyses of precipitation, sap water of larch trees, soil water, and water in surface organic layer during the late summer periods of 2006, 2007, and 2008. In these years, the soil moisture content was considerably high due to unusually large amounts of summer rainfall and winter snowfall. The observed sap water δ 18 O ranged from −17.9‰ to −13.3‰, which was close to that of summer precipitation and soil water in the shallow layer, and represents that of transpired water vapour. On sunny days, as the air temperature and mixing ratio rose from predawn to morning, the atmospheric water vapour δ 18 O increased by 1‰ to 5‰ and then decreased by about 2‰ from morning to afternoon with the mixing ratio. On cloudy days, by contrast, the afternoon decrease in δ 18 O and the mixing ratio was not observed. These results show that water vapour that transpired from plants, with higher δ 18 O than the atmospheric water vapour, contributes to the increase in δ 18 O in the morning, whereas water vapour in the free atmosphere, with lower δ 18 O, contributes to the decrease in the afternoon on sunny days. The observed results reveal the significance of transpired water vapour, with relatively high δ 18 O, in the water cycle on a short diurnal time scale and confirm the importance of the recycling of precipitation through transpiration in continental forest environments such as the eastern Siberian taiga. Copyright © 2012 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Ueta, Akihiro Sugimoto, Atsuko Iijima, Yoshihiro Yabuki, Hironori Maximov, Trofim C. Velivetskaya, Tatiana A. Ignatiev, Alexander V. |
spellingShingle |
Ueta, Akihiro Sugimoto, Atsuko Iijima, Yoshihiro Yabuki, Hironori Maximov, Trofim C. Velivetskaya, Tatiana A. Ignatiev, Alexander V. Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia |
author_facet |
Ueta, Akihiro Sugimoto, Atsuko Iijima, Yoshihiro Yabuki, Hironori Maximov, Trofim C. Velivetskaya, Tatiana A. Ignatiev, Alexander V. |
author_sort |
Ueta, Akihiro |
title |
Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia |
title_short |
Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia |
title_full |
Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia |
title_fullStr |
Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia |
title_full_unstemmed |
Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia |
title_sort |
factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern siberia |
publisher |
Wiley |
publishDate |
2012 |
url |
http://dx.doi.org/10.1002/hyp.9361 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9361 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.9361 |
genre |
permafrost taiga Siberia |
genre_facet |
permafrost taiga Siberia |
op_source |
Hydrological Processes volume 27, issue 16, page 2295-2305 ISSN 0885-6087 1099-1085 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/hyp.9361 |
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Hydrological Processes |
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27 |
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16 |
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2295 |
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2305 |
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1800759793526243328 |