利用遥感技术进行短期干旱监测:以巴基斯坦Potohar地区为例

Saad-ul-Haque, B. Ghauri, M. Khan
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引用次数: 8

摘要

由于大气污染增加和气候变化等各种环境变化,该国经常发生干旱。巴基斯坦主要是干旱和半干旱地区,气候多样,农业占全国GDP的20.9%。覆盖盐岭和Potohar高原的Barani(雨养)土地(约22256平方公里,以北纬33.2°和东经72.75°为中心,海拔1200至1900英尺)。该地区更容易受到短期干旱的影响,月平均降雨量在30 - 200毫米之间,最大降雨量在200毫米之间。温度高达47°C。太阳辐射(超过3000小时的日照/年)导致较高的蒸散速率。这种情况和长期缺乏正常降雨导致干旱,影响了该国的作物产量和经济。利用MODIS卫星的NDVI产品在拉比季节(10 - 2月)调查植被状况和干旱对这些作物的影响。利用NCEP 2000-2012年全球气象资料,结合土壤水分资料分析水分亏缺模式。结果表明:2009-2010年冬季,由于降水少,平均NDVI急剧下降;与2000-2012年冬季季风月份的平均2.9相比,2009-2010年的NDVI值下降了2.2。这种关系将有助于设计一个早期预警系统来探测干旱情况的发生,并发展一个连续的干旱监测系统。在这些研究的基础上,可以制定未来的水管理和缓解战略,例如在夏季季风期间保存水,以克服即将到来的冬季的水压力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Short term drought monitoring using remote sensing technique: A case study of Potohar region, Pakistan
Drought has frequently been witnessed in the country due to various environmental changes such as rise in atmospheric pollution and climatic changes. Pakistan is predominantly arid and semi-arid with a diversified climate, where agriculture contributes 20.9 percent to national GDP. The Barani (rainfed) land covering Salt Range and Potohar Plateau (about 22,256 km2 centered at 33.2° N and 72.75° E, at an elevation of 1,200 to 1,900 feet ASL). This area is more vulnerable to short term droughts with mean monthly rainfall in this area ranges from 30 to 200 mm with max. temperature up to 47 °C. Solar radiation (over 3,000 hours of sunshine/year) results in higher rate of evapo-transpiration. Such conditions and prolonged absence of regular rainfall lead to drought conditions affecting crop yield and economy of the country. NDVI product of MODIS Satellite was used for Rabi season (October to February) in order to investigate vegetation state and effects of drought on these crop. Soil Moisture data was incorporated to analyze water deficit pattern using NCEP global weather data from 2000-2012. The results showed that, there was a drastic decrease in mean NDVI during 2009-2010 winters' months due to low rainfall. This decrease in NDVI value seen from 2.2 in 2009-2010 as compared to average mean value of 2.9 for 2000-2012 of winter Monsoon months. Such relationship would help devise an early warning system to detect the onset of drought conditions and developing a continuous drought monitoring system. Based on such studies, future strategies for water management, mitigations could be worked out, such as preservation of water during summer monsoons to overcome the water stress in the coming winter season.
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