Dynamics and Driving Forces of the Alpine Wetlands in the Yarlung Zangbo River Basin of Tibet, China
Based on the field investigation and long term remote
sensing data, the dynamics of the alpine wetland in the river basin and
their response to climate change were studied. Results showed the
alpine wetlands accounted for 3.73% of total basin in 2010. Lake and
river appeared an increasing trend in the past 30 years, with an
increase of 34.36 % and 24.57%. However, swamp exhibited a
tendency of decreasing with 233.74 km2. Annual average temperature,
maximum temperature, minimum temperature and precipitation in the
river basin all exhibited an increasing trend, whereas relative humidity
exhibited a decreasing trend. Ice and snow melting are main reasons of
lake and river area enhancement and swamp area descend. There
existed 91.78%-97.86% of reduced swamp converted into lakes on the
basis of remote sensing image interpretation. China-s government
policy of implementing development in the river basin is the major
driving force of artificial wetland growth.
[1] J. T. Freymueller, "A new mechanical model for Tibet," Nature, vol. 472, pp.
48-49, 2011.
[2] J. Wischnewski, A. Kramer, Z. C. Kong, A.W. Mackay, G. L. Simpson, S.
Mischke, U. Herzschuh, "Terrestrial and aquatic responses to climate change
and human impact on the southeastern Tibetan Plateau during the past two
centuries," Global Change Biology, vol. 17, no.11, pp. 3376-3391, 2011.
[3] Q. C. Tang, Y. Xiong, "River Hydrology in China," Beijing: Science Press,
1998 (in Chinese).
[4] Y. Y. Chen, "Research of China-s wetland," Jilin Sciencific Press: Changchun,
1995 (in Chinese).
[5] Q. L. You, S. C. Kang, Y. H. Wu, Y. P. Yan, "Climate change over the Yarlung
Zangbo River Basin during 1961-2005," Journal of Geographical Sciences,
vol. 17, no. 4, pp. 409-420, 2007.
[6] The Comprehensive Scientific Exploration Team to the Qinghai-Xizang
Plateau, 1984. Rivers and Lakes of Xizang.Beijing: Science Press (in
Chinese).
[7] X. F. Fu, S. T. Yang, C. M. Liu, "Changes of NDVI and their relations with
principal climatic factors in the Yarlung Zangbo River Basin," Geographical
Research, vol. 1, no.1, pp. 60-66, 2007 (in Chinese with English abstract).
[8] H. D. Li, W. S. Shen, C. X. Zou, L. Yuan, "Soil erosion in the source area of
the Yarlung Zangbo in China", Journal of Ecology and Rural Environment,
vol. 26, no.1, pp. 25-30, 2010 (in Chinese with English abstract).
[9] J. H. Jiang, Q. Huang, "Distribution and variation of lakes in Tibetan Plateau
and their comparison with lakes in other part of China," Water Resources
Protection, vol. 6, pp. 24-27, 2004 (in Chinese with English abstract).
[10] W. S. Shen, H. D. Li, M. Sun, J. Jiang, "Dynamics of aeolian sandy land in the
Yarlung Zangbo River basin of Tibet, China from 1975 to 2008," Global and
Planetary Change, vol. 86-87, pp. 37-44, 2012.
[11] L. Yuan, W. S. Shen, H. D. Li, H. Zhang, C. X. Zou, M. Sun, "Evolution and
causes of aeolian desertification of the middle reaches of Yarlung Zangbo
River, China," Journal of Ecology and Rural Environment, vol. 26, no. 4, pp.
301-305, 2010. (in Chinese with English abstract).
[12] J. H. Jiang, Q. Huang, "Distribution and variation of lakes in Tibetan Plateau
and their comparison with lakes in other part of China," Water Resources
Protection, vol. 6, pp. 24-27, 2007 (in Chinese with English abstract).
[13] W. K. Chan, T. K. L. Tong, "Multi-criteria material selections and end-of-life
product strategy: Grey relational analysis approach," Materials & Design, vol.
28, no. 5, pp.1539-1546, 2007.
[14] D. Y. Wang, F. Yang, "One river and two streams" planning in Tibet,
Hydropower of Northeast China, vol. 3, pp. 12-19, 1994 (in Chinese with
English abstract).
[15] Y. F. Niu, C. X. Li, X. H. Xi, Y. M. Deji, "Plateau lake variation monitored by
satellite remote sensing and the relation to climate change," Arid Land
Geography, vol. 31, no. 2, pp. 284-290, 2008 (in Chinese with English
abstract).
[1] J. T. Freymueller, "A new mechanical model for Tibet," Nature, vol. 472, pp.
48-49, 2011.
[2] J. Wischnewski, A. Kramer, Z. C. Kong, A.W. Mackay, G. L. Simpson, S.
Mischke, U. Herzschuh, "Terrestrial and aquatic responses to climate change
and human impact on the southeastern Tibetan Plateau during the past two
centuries," Global Change Biology, vol. 17, no.11, pp. 3376-3391, 2011.
[3] Q. C. Tang, Y. Xiong, "River Hydrology in China," Beijing: Science Press,
1998 (in Chinese).
[4] Y. Y. Chen, "Research of China-s wetland," Jilin Sciencific Press: Changchun,
1995 (in Chinese).
[5] Q. L. You, S. C. Kang, Y. H. Wu, Y. P. Yan, "Climate change over the Yarlung
Zangbo River Basin during 1961-2005," Journal of Geographical Sciences,
vol. 17, no. 4, pp. 409-420, 2007.
[6] The Comprehensive Scientific Exploration Team to the Qinghai-Xizang
Plateau, 1984. Rivers and Lakes of Xizang.Beijing: Science Press (in
Chinese).
[7] X. F. Fu, S. T. Yang, C. M. Liu, "Changes of NDVI and their relations with
principal climatic factors in the Yarlung Zangbo River Basin," Geographical
Research, vol. 1, no.1, pp. 60-66, 2007 (in Chinese with English abstract).
[8] H. D. Li, W. S. Shen, C. X. Zou, L. Yuan, "Soil erosion in the source area of
the Yarlung Zangbo in China", Journal of Ecology and Rural Environment,
vol. 26, no.1, pp. 25-30, 2010 (in Chinese with English abstract).
[9] J. H. Jiang, Q. Huang, "Distribution and variation of lakes in Tibetan Plateau
and their comparison with lakes in other part of China," Water Resources
Protection, vol. 6, pp. 24-27, 2004 (in Chinese with English abstract).
[10] W. S. Shen, H. D. Li, M. Sun, J. Jiang, "Dynamics of aeolian sandy land in the
Yarlung Zangbo River basin of Tibet, China from 1975 to 2008," Global and
Planetary Change, vol. 86-87, pp. 37-44, 2012.
[11] L. Yuan, W. S. Shen, H. D. Li, H. Zhang, C. X. Zou, M. Sun, "Evolution and
causes of aeolian desertification of the middle reaches of Yarlung Zangbo
River, China," Journal of Ecology and Rural Environment, vol. 26, no. 4, pp.
301-305, 2010. (in Chinese with English abstract).
[12] J. H. Jiang, Q. Huang, "Distribution and variation of lakes in Tibetan Plateau
and their comparison with lakes in other part of China," Water Resources
Protection, vol. 6, pp. 24-27, 2007 (in Chinese with English abstract).
[13] W. K. Chan, T. K. L. Tong, "Multi-criteria material selections and end-of-life
product strategy: Grey relational analysis approach," Materials & Design, vol.
28, no. 5, pp.1539-1546, 2007.
[14] D. Y. Wang, F. Yang, "One river and two streams" planning in Tibet,
Hydropower of Northeast China, vol. 3, pp. 12-19, 1994 (in Chinese with
English abstract).
[15] Y. F. Niu, C. X. Li, X. H. Xi, Y. M. Deji, "Plateau lake variation monitored by
satellite remote sensing and the relation to climate change," Arid Land
Geography, vol. 31, no. 2, pp. 284-290, 2008 (in Chinese with English
abstract).
@article{"International Journal of Earth, Energy and Environmental Sciences:61611", author = "Weishou Shen and Dong Liu and Di Ji and Haoyun Shen and Naifeng Lin", title = "Dynamics and Driving Forces of the Alpine Wetlands in the Yarlung Zangbo River Basin of Tibet, China", abstract = "Based on the field investigation and long term remote
sensing data, the dynamics of the alpine wetland in the river basin and
their response to climate change were studied. Results showed the
alpine wetlands accounted for 3.73% of total basin in 2010. Lake and
river appeared an increasing trend in the past 30 years, with an
increase of 34.36 % and 24.57%. However, swamp exhibited a
tendency of decreasing with 233.74 km2. Annual average temperature,
maximum temperature, minimum temperature and precipitation in the
river basin all exhibited an increasing trend, whereas relative humidity
exhibited a decreasing trend. Ice and snow melting are main reasons of
lake and river area enhancement and swamp area descend. There
existed 91.78%-97.86% of reduced swamp converted into lakes on the
basis of remote sensing image interpretation. China-s government
policy of implementing development in the river basin is the major
driving force of artificial wetland growth.", keywords = "alpine wetland dynamics, climate change, Yarlung
Zangbo River basin", volume = "6", number = "7", pages = "447-6", }