Studying the Dynamics of Lake Sevan Water Surface Temperature Using Landsat8 Sateliite Imagery

Azatuhi Hovsepyan, V. Muradyan, G. Tepanosyan, L. Minasyan, S. Asmaryan
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引用次数: 1

Abstract

Abstract Lake Sevan being Armenia’s largest freshwater reservoir has a vital economic, recreational and cultural importance to both the catchment area and the nation as a whole. At present the Sevan which has seen the dramatic - some 20m drop - in water level entailing grave ecological consequences to the whole of its ecosystem, is at the stage of recovery. Hence, it is very important to study basic parameters describing the ecological status of the lake, and their annual and seasonal dynamics. The Sevan water surface temperature (WST) is a key parameter which influences all ecological processes that occur in the Lake. Declining lake level has brought to reduction of water volume and consequently to earlier warming of lake water in spring and its earlier cooling in the fall. Besides, more frequent becomes the complete surface freezing of Lake Sevan. Remotely sensed imagery makes it possible to get immediate information on a regular basis about WST across the entire surface of lakes. The purpose of this particular research was to study the space and time dynamics of Lake Sevan WST using Landsat 8 satellite imagery. The advantage of Landsat8 images is a regular frequency of capturing and availability of another thermal band that helps reduce the atmospheric refraction-induced errors/deviations. This research involved Landsat imagery for 2000-2018. The images underwent preprocessing steps (radiometric calibration, atmospheric correction, normalization etc) and then Lake Sevan WSTs and their monthly and annual changes over the mentioned periods were derived using both thermal bands (b10, b11). The research confirmed the fact, that Lake Sevan surface completely or partly freezing with periodicity of 2-3 years, whereas before the water drop the periodicity was 15-20 years. The study of spatial distribution of WST data derived from remote sensing shows that the temperature data corresponds to the overall general picture of temperature for Lake Sevan. This research has indicated that remotely sensed images and Landsat 8 imagery in particular allow derive both WST data on a regular basis and retrospective data (since 2013).
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基于Landsat8卫星影像的塞万湖水面温度动态研究
塞万湖是亚美尼亚最大的淡水水库,对集水区和整个国家都具有重要的经济、娱乐和文化意义。目前,塞万河正处于恢复阶段,它的水位急剧下降了大约20米,对整个生态系统造成了严重的生态后果。因此,研究湖泊生态状况及其年、季动态的基本参数具有重要意义。湖面温度(WST)是影响湖泊生态过程的关键参数。湖泊水位下降导致湖水水量减少,导致湖水春季较早升温,秋季较早降温。此外,更频繁地成为塞万湖的完全表面冻结。遥感图像使我们有可能定期获得整个湖泊表面WST的即时信息。本研究的目的是利用Landsat 8卫星图像研究塞万湖西湖的时空动态。Landsat8图像的优点是捕获频率固定,并且另一个热波段的可用性有助于减少大气折射引起的误差/偏差。这项研究涉及2000-2018年的陆地卫星图像。对图像进行预处理(辐射定标、大气校正、归一化等),然后利用两个热波段(b10、b11)得到Sevan湖WSTs及其在上述时间段内的月、年变化。研究证实,塞万湖表面完全或部分结冰的周期为2 ~ 3年,而降水前的周期为15 ~ 20年。对遥感WST数据的空间分布研究表明,温度数据与塞万湖的温度总体情况相对应。该研究表明,特别是遥感图像和Landsat 8图像可以获得常规WST数据和回顾性数据(自2013年以来)。
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