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Development of Environmental Dataset of Taklamakan Desert by TERRA/AQUA MODIS Data

机译:利用TERRA / AQUA MODIS数据开发塔克拉玛干沙漠环境数据集

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摘要

The images of huge fixed type longitudinal sand dunes of eastern Taklamakan Desert acquired with Terra and Aqua MODIS indicate non negligible difference due to influence of solar illumination angles resulting from 70 minutes observation time difference in late Autumn. Analyses of the images of the same sand dunes acquired with Terra MODIS and JERS-1 OPS indicate significant difference due to spatial resolution difference (250 m vs. 18 m). The OPS image shows that when a large longitudinal sand dune grows to a certain size in width then it begins to split The space and height of huge longitudinal sand dunes in the eastern Taklamkan Desert derived from the OPS image is about 2 km and 120 m in average respectively. The OPS image also clearly shows influences of the Hotien River and Ma2artag mountain range on sand dunes of the area. In the north side of the Mazartag mountain range are transversal dunes in the west and compound (pyramidal, transversal and longitudinal) dunes in the eastern part while in the south side are longitudinal dunes. There is a good correspondence between the orientation of the huge fixed type longitudinal sand dunes and the direction of the monthly maximum winds of the sand storm months.
机译:用Terra和Aqua MODIS采集的塔克拉玛干沙漠东部巨大的固定型纵向沙丘图像表明,由于深秋70分钟观测时间差异导致的太阳照射角度的影响,这种差异不可忽略。用Terra MODIS和JERS-1 OPS采集的相同沙丘的图像分析表明,由于空间分辨率差异(250 m与18 m),差异很大。 OPS图像显示,当一个大型纵向沙丘在宽度上增长到一定大小时,便开始分裂。从OPS图像得出的塔克拉姆干沙漠东部的大型纵向沙丘的空间和高度分别约为2 km和120 m。平均。 OPS图像还清楚地显示了Hotien河和Ma2artag山脉对该地区沙丘的影响。在Mazartag山脉的北侧,西部是横向沙丘,在东部是复合(金字塔形,横向和纵向)沙丘,而在南侧则是纵向沙丘。巨大的固定型纵向沙丘的方向和沙尘暴月份的每月最大风向之间有很好的对应关系。

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