Influence of land use/land cover (LULC) changes on atmospheric dynamics over the arid region of Rajasthan state, India

被引:43
|
作者
Kharol, Shailesh Kumar [1 ,2 ]
Kaskaoutis, D. G. [3 ]
Badarinath, K. V. S. [1 ]
Sharma, Anu Rani [4 ]
Singh, R. P. [5 ]
机构
[1] Govt India, Dept Space, Natl Remote Sensing Ctr, Atmospher Sci Sect, Hyderabad 500625, Andhra Pradesh, India
[2] Dalhousie Univ, Dept Phys & Atmospher Sci, Halifax, NS B3H 3J5, Canada
[3] Sharda Univ, Res & Technol Dev Ctr, Greater Noida 201306, Ncr, India
[4] TERI Univ, Vasant Kunj Inst Area 10, New Delhi 110070, India
[5] Chapman Univ, Schmid Coll Sci & Technol, Sch Earth & Environm Sci, Orange, CA 92866 USA
关键词
Atmospheric fluxes; India; Land use/land cover (LULC) changes; Precipitation; Rajasthan; Remote sensing; INTERANNUAL VARIABILITY; VEGETATION ACTIVITY; ABSORBING AEROSOLS; SURFACE-ENERGY; CLIMATE-CHANGE; IMPACT; RAINFALL; PRECIPITATION; IRRIGATION; FLUXES;
D O I
10.1016/j.jaridenv.2012.09.006
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The present study examines the long-term effects of land use/land cover (LULC) changes in Rajasthan state, India on land-atmosphere fluxes and, possibly in precipitation and aerosol loading. By comparing the satellite observations from Landsat MSS (1972-73) and IRS-P6 AWiFS (2006-07) considerable LULC changes are observed, an increase in crop-land and vegetated areas of similar to 57% in the eastern and similar to 68% in the western Rajasthan. The increase in agriculture intensification from irrigation activities after the construction of the Indira Gandhi canal (IGC) seems to affect the land-atmosphere fluxes, i.e. increase in atmospheric humidity and latent heat and reduction in sensible heat. On the other hand, the multi-decadal variability (1951-2007) in annual rainfall amount and total number of rainy days reveals significant year-to-year fluctuations, exhibiting a slight increasing trend over arid western Rajasthan. However, the overall analysis shows that the variability in precipitation is much more influenced by the general monsoonal circulation (i.e. meteorological dynamics and intensity of the monsoon) and partly can be associated with local phenomena, such as LULC changes and modifications in land-atmosphere fluxes. Similarly to precipitation, the long-term (1979-2008) aerosol index (AI) variations over the region seem to be affected by atmospheric and meteorological dynamics and not by LULC changes. (c) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:90 / 101
页数:12
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