Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia
Article first published online: 24 MAY 2012
Copyright © 2012 John Wiley & Sons, Ltd.
Volume 27, Issue 16, pages 2295–2305, 30 July 2013
How to Cite
Ueta, A., Sugimoto, A., Iijima, Y., Yabuki, H., Maximov, T. C., Velivetskaya, T. A. and Ignatiev, A. V. (2013), Factors controlling diurnal variation in the isotopic composition of atmospheric water vapour observed in the taiga, eastern Siberia. Hydrol. Process., 27: 2295–2305. doi: 10.1002/hyp.9361
- Issue published online: 11 JUL 2013
- Article first published online: 24 MAY 2012
- Accepted manuscript online: 24 APR 2012 09:50PM EST
- Manuscript Accepted: 20 APR 2012
- Manuscript Received: 22 SEP 2011
- eastern Siberia;
- stable isotope;
- atmospheric water vapour;
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 δ18O 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 δ18O 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 δ18O and the mixing ratio was not observed. These results show that water vapour that transpired from plants, with higher δ18O than the atmospheric water vapour, contributes to the increase in δ18O in the morning, whereas water vapour in the free atmosphere, with lower δ18O, contributes to the decrease in the afternoon on sunny days. The observed results reveal the significance of transpired water vapour, with relatively high δ18O, 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.