Peatland area change in the southern Altay Mountains over the last twenty years based on GIS and RS analysis
Huan LI, Dingyi XU, Yan ZHAO
Peatland area change in the southern Altay Mountains over the last twenty years based on GIS and RS analysis
Analyses results of total peatland area changes in the southern Altay Mountain region over the past 20 years are discussed in this paper. These analyses were based on remote sensing (RS) and geographical information system (GIS) studies. Possible control methods are evaluated by comparing these results to other regional records and climate data. The area of the peatland zones was calculated by overlaying a peatland layer of Landsat TM (Thematic Map) image constructed by using supervised classification with a layer of slope based on a digital elevation model (DEM). The results show that slope layer is crucial to improving the accuracy of peatland extracted from TM images. The peatland area of the Altay Mountains increased from 931.5 km2 in 1990 to 977.7 km2 in 2010. This trend is consistent with the climate change in this region, due in part to increasing temperatures and precipitation, suggesting possible climate controls on peatland expansion. The increase in the peatland area in the Altay Mountains over the last 20 years has been influenced by the westerlies. Alternatively, changes in the largest highland peatland area of the Zoige Basin, located in the eastern Tibetan Plateau have been influenced by the intensity of the Asian summer monsoons. In addition to increased temperatures, decreased precipitation in the Zoige Basin and increased precipitation in the Altay Mountains, due to varied patterns of atmospheric circulation, are the probable causes for driving the change differences in these two peatland areas.
RS image / DEM image / GIS analysis / peatland area change / the Altay Mountains
[1] |
Beilman D W, MacDonald G M, Smith L C, Reimer P J (2009). Carbon accumulation in peatlands of West Siberia over the last 2000 years. Global Biogeochem Cycles, 23(1): 1−12
CrossRef
Google scholar
|
[2] |
Braswell B H, Schimel D S, Linder E, Moore B (1997). The response of global terrestrial ecosystems to interannual temperature variability. Science, 278(5339): 870−873
CrossRef
Google scholar
|
[3] |
Cai X (1981). The formation and types of peat in China and the law of governing its distribution. Acta Geogr Sin, 36: 237−253
|
[4] |
Fu A H, Chen Y N, Li W H, Li B F, Yang Y H, Zhang S H (2013). Spatial and temporal patterns of climate variations in the Kaidu River Basin of Xinjiang, Northwest China. Quat Int, 311: 117−122
CrossRef
Google scholar
|
[5] |
Gignac L D, Vitt D H (1994). Responses of northern peatlands to climate change: effects on bryophytes. J Hattori Bot Lab, 75: 119−132
|
[6] |
Gong P, Niu Z G, Cheng X, Zhao K Y, Zhou D M (2006). Changes in landscape pattern of alpine wetlands on the Zoige Plateau in the past four decades. Acta Ecol Sin, 28(5): 2245−2252 (in Chinese)
|
[7] |
Holden J (2005). Peatland hydrology and carbon release: why small-scale process matters. Philosophical tranctions of the royal society A, 363: 2891−2913
|
[8] |
Hu G Y, Dong Z B, Lu J F, Yan C Z (2012). Driving forces of land use and land cover change (LUCC) in the Zoige Wetland, Qinghai-Tibetan Plateau. Sciences in Cold and Arid Regions, 4(5): 422−430
|
[9] |
IPCC (2007). Climate change 2007: the physical science basis, contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change. In: Solomon S, Qin D, Manning M, Marquis M, Averyt K, Tignor M, Miller H, Chen Z, eds. Cambridge University Press, Cambridge
|
[10] |
Klein E S, Yu Z C, Booth R K (2013). Recent increase in peatland carbon accumulation in a thermokarst lake basin in Southwestern Alaska. Palaeogeogr Palaeoclimatol Palaeoecol, 392: 186−195
CrossRef
Google scholar
|
[11] |
Li K, Yang Y X, Yang Y, Han D Y (2012). Degardation characteristics of swamps in Zoige Plateau induced by drainage based on quantitative classification of vegetation. J Appl Ecol, 23(7): 1781−1789
|
[12] |
Los S O, Collatz G J, Bounoua L, Sellers P J, Tucker C J (2001). Global interannual variations in sea surface temperature and land surface vegetation, air temperature, and precipitation. J Clim, 14(7): 1535−1549
CrossRef
Google scholar
|
[13] |
Lydolph P E (1977). Climates of the Soviet Union. Amsterdam: Elsevier Scientific Publishing
|
[14] |
Min W B, Peng G Z, Luo L, Guo H Y (2008). Analysis of TM imagery characteristics over Ruoergai wetland. Meteorological Science and Technology, 36: 108−111 (in Chinese)
|
[15] |
Moore T R, Knowles R (1989). The influence of water table levels on methane and carbon dioxide emissions from peatland soils. Can J Soil Sci, 69(1): 33−38
CrossRef
Google scholar
|
[16] |
Niu Z G, Gong P (2009). Wetland remote sensing mapping and geographical characteristics analysis in China. Sci China Ser D, 39: 188−203
|
[17] |
Piao S L, Fang J Y, Zhou L M, Guo Q H, Henderson M, Ji W, Li Y, Tao S (2003). Interannual variations of monthly and seasonal normalized difference vegetation index (NDVI) in China from 1982 to 1999. Journal of Geophysical Research, 108in Chinese)
CrossRef
Google scholar
|
[18] |
Ruppel M, Valiranta M, Virtanen T, Korhola A (2013). Postglacial spatiotemporal peatland initiation and lateral expansion dynamics in North America and Northern Europe. Holocene, 23(11): 1596−1606
CrossRef
Google scholar
|
[19] |
Schumann M, Thevs N, Joosten H (2008). Extent and degradation of peatlands on the Ruoergai Plateau (Tibet, China) assessed by remote sensing. Pristine Mire Landscape, 77−80
|
[20] |
Schwikowski M, Eichler A, Kalugin I, Ovtchinnikov D, Papina T (2009). Past climate variability in the Altay. Pages news, workshop reports 1(17)
|
[21] |
Sheng Y W, Smith L C, MacDonald G M, Kremenetski K, Frey K E, Velichko A A, Lee M, Beilman D W, Dubinin P (2004). A high-resolution GIS-based inventory of the west Siberian peat carbon pool. Global Biogeochem Cycles, 18(3): GB3004
CrossRef
Google scholar
|
[22] |
van Bellen S, Dallaire P L, Garneau M, Bergeron Y (2011). Quantifying spatial and temporal Holocene carbon accumulation in ombrotrophic peatlands of the Eastmain region, Quebec, Canada. Global Biogeochem Cycles, 25: GB2016
CrossRef
Google scholar
|
[23] |
Wang J, Rich P M, Price K P (2003). Temporal responses of NDVI to precipitation and temperature in the central Great Plains, USA. Int J Remote Sens, 24(11): 2345−2364
CrossRef
Google scholar
|
[24] |
Wang X N (2012). Response of glacial variation to climate change in the Southern Altay Mountians during the last 40 years. Dissertation for master degree. Lanzhou: Lanzhou University (in Chinese)
|
[25] |
Wang Y, Zhao Z Z, Qiao Y S, Li C Z (2005). Characteristics of the climatic variatation in Zoige in the past 45 years and its effects on the eco-environment in the area. Journal of Geomechanics, 11(4): 328−333 (in Chinese)
|
[26] |
Xie J L, Song X, Yan C Z (2012). Response of landscape interference pattern changes to human in Zoige Plateau. Journal of Beijing Union University (National Sciences), 3(26): 16−20 (in Chinese)
|
[27] |
Yao L, Zhao Y, Gao S J, Sun J H, Li F R (2011). The peatland area change in past 20 years in the Zoige Basin, eastern Tibetan Plateau. Front Earth Sci, 5: 271−275
|
[28] |
Yao T D, Thompson L, Yang W, Yu W S, Gao Y, Guo X J, Yang X X, Duan K Q, Zhao H B, Xu B Q, Pu J C, Lu A X, Xiang Y, Kattel D B, Joswiak D (2012). Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings. Nature Climate Change,
CrossRef
Google scholar
|
[29] |
Yong G W, Shi C C, Qiu P F (2003). Monitoring on desertification trends of the grassland and shrinking of the wetland in Ruoergai Plateau in North-west Sichuan by means of remote-sensing. Journal of Mountain Science, 6(21): 758−762 (in Chinese)
|
/
〈 | 〉 |