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ANALYSIS OF LONG-TERM EVI FOR VARIATIONS IN THE PHENOLOGICAL TRENDS OF MAJOR VEGETATION TYPES IN WESTERN HIMALAYA

机译:Himalaya主要植被类型的长期EVI分析

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Over the past few years, extreme weather events due to global climate change and anthropogenic pressure are among the main drivers of changing vegetation cover and productivity in western Himalaya. Changes in vegetation cover, their life-cycle events and how they are influenced by climatic variations is studied by phenological trends. In a region where field-based study is challenging due to high altitude and heterogenous relief, quantifying changes in vegetation photosynthetic activity using remote sensing can provide crucial information regarding variations in vegetation cover and its linkages with climate change and anthropogenic impacts. We conducted this study to detect variations in phenological trends over Uttarakhand Himalaya using MODIS EVI time-series data (2000-2014) and examined temporal patterns in five different vegetation types over different locations. To classify vegetation cover of Uttarakhand in different forest types, we used Vegetation Cover and Land Use map of Uttarakhand. Random points were generated in these forest types and EVI values were extracted from all the layers of our stacked MODIS data. In total most of the vegetation types showed an overall negative trend in mean EVI (browning) with time and are in agreement with previous studies that report only increasing brownness detected at broader scale using much coarser spatial resolution time-series. Sal mixed moist deciduous, in particular, showed a little more negative trend at all the locations as compared to others. Negative EVI trend (browning) in this region could possibly be attributed to the fire activities and land use change at forest fringe as well as temperature induced drought stress and cooling spring temperatures. Wet grassland, on the other hand, showed a positive trend in EVI (greening) which could be attributed to climate warming and wetting at higher altitude. Climate change could result in a replacement of high quality forest with low-quality forests, which are likely to lead to a significant biodiversity loss. An interplay between anthropogenic and climatic factors was also possible to affect the regional phenology.
机译:在过去的几年里,由于全球气候变化和人为压力导致的极端天气事件是在喜马拉雅西部改变植被覆盖和生产率的主要驱动因素之一。通过酚类趋势研究了植被覆盖的变化,其生命周期事件以及如何受气候变化的影响。在基于现场的研究由于高海拔和异源性浮雕挑战的地区中,使用遥感量的植被光合作用的变化可以提供关于植被覆盖的变化及其与气候变化和人为影响的关键信息。我们进行了本研究,以检测使用MODIS EVI时间序列数据(2000-2014)和在不同地点上检查五种不同植被类型中的时间模式的象征趋势的变化。在不同森林类型中分类乌塔塔克手的植被覆盖,我们使用植被覆盖和乌塔塔克手的土地使用地图。在这些林类型中生成随机点,并且从我们堆叠的MODIS数据的所有层中提取EVI值。在总植被类型中,随着时间的推移,大部分植被类型的总体负面趋势表现出了平均eVI(褐变),并与以前的研究一致地报告在更广泛的空间分辨率时间序列中仅报告在更广泛的范围内检测到的褐变。特别是,与他人相比,SAL混合湿润落叶液在所有位置显示出更多的负面趋势。在该地区的负面EVI趋势(褐变)可能归因于森林边缘的火灾活动和土地利用变化以及温度诱导的干旱胁迫和冷却弹簧温度。另一方面,湿草地展示了EVI(绿化)的积极趋势,这可能归因于气候变暖和润湿在更高的高度。气候变化可能导致更换高质量的森林,森林很低,可能会导致大量生物多样性损失。人为和气候因子之间的相互作用也可能影响区域候选。

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