Classification of microtopographical features along the shore of Balkhash Lake by ALOS/PRISM DSM

Y. Nakayama, Y. Hara, K. Endo
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Abstract

The purpose of this study is to analyze the distribution and the classification of gravel bar along the shore of Balkhash Lake by using the high precision DSM newly produced from the stereo pair data of PRISM carried in ALOS, and to consider the age and environment of formation of every classified gravel bar, and the long-term environmental change based on water level fluctuation of the lake. The classification of gravel bar distribution pattern based on the characteristics such as height, number and direction of the ridge line was carried out through extraction and comparative analysis of the DSM data and ALOS pan-sharpened image in eighteen areas along the shoreline. The result of this study showed that the distribution pattern of the gravel bars along the shore was classified into three typical groups. The difference in distribution of three groups is based on the influence of the waves with the strong prevailing wind. Moreover, according to the feature of the classified group, the water level change situation of Balkhash Lake was divided into three stages in the past about 26,000 years, and the tendency of drawdown was shown as the whole.
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Balkhash湖岸微地形特征的ALOS/PRISM DSM分类
利用ALOS携带的PRISM立体对数据新生成的高精度DSM,分析巴尔喀什湖岸沙砾坝的分布和分类,并考虑各分类沙砾坝形成的年代和环境,以及基于湖泊水位波动的长期环境变化。通过对海岸带18个区域的DSM数据和ALOS泛锐化图像的提取和对比分析,基于脊线高度、脊线数量、脊线方向等特征对沙砾坝分布格局进行了分类。研究结果表明,滨岸沙砾坝的分布格局可分为3个典型类群。三组的分布差异是基于强盛行风对海浪的影响。根据分类群的特征,将巴尔喀什湖近26000年来的水位变化情况划分为3个阶段,总体上呈现下降趋势。
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