Spatial and temporal dynamics of Pai forest vegetation in Pakistan assessed by RS and GIS

被引:0
|
作者
A.A.Siyal [1 ,2 ]
A.G.Siyal [2 ]
R.B.Mahar [1 ]
机构
[1] U.S.-Pakistan Center for Advanced Studies in Water (USPCAS-W),Mehran University of Engineering and Technology
[2] Department of Land and Water Management,Sindh Agriculture University
关键词
Landsat; Arid forest; NDVI; Deforestation; Ecosystem; Land surface temperature(LST);
D O I
暂无
中图分类号
S718.5 [森林生态学];
学科分类号
071012 ; 0713 ;
摘要
Pai, an arid forest in Sindh Province of Pakistan,is important for the environmental, social, economic development and conservation of ecosystems of the province. Considering the significance of the forest for Sindh and the calls from the local population for its deforestation,we quantified the spatial and temporal variation in the vegetation of the forest and land surface temperature(LST)using optical and thermal Landsat satellite data. Our analysis of temporal(1987–2014) images with Arc GIS10.1 revealed that the dense forest area was greatest at725 ha(37 % of the total forest area) during 2013 while it was smallest at 217 ha(11 %) in 1992. The sparse forest area peaked during 1987 at 1115 ha(58 %) under shrubs whereas it was smallest at 840 ha(43 %) in 1992, and the maximum deforestation of Pai forest occurred during 1992.Spatial change in vegetation over a period of about27 years(1987–2014) revealed that vegetation increased on an area of 735 ha(37 %), decreased on 427 ha(22 %),and there was no change on 808 ha(41 %) of the forest.Variation in temperature between shaded(dense forest) and unshaded areas(bare land) of the forest was from 6 to10 °C. While the temperature difference between areas with sparse forest and bare land ranged from 4 to 6 °C. An inverse relationship between LST and NDVI of Pai forest with coefficients of determination of 0.944 and 0.917 was observed when NDVI was plotted against minimum and maximum LST, respectively. The vegetation in the forest increased with time and the areas of more dense Pai forest supported lower surface temperature and thus air temperature.
引用
收藏
页码:593 / 603
页数:11
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