Cipunagara河和Cimanuk河河口变化的Landsat影像空间分析

W. H. Nur, M. Hendrizan, A. Nurhidayati, A. F. Ismayanto
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引用次数: 1

摘要

位于西爪哇的北海岸爪哇,特别是在锡雷本、因德拉玛尤和苏邦等地,通过磨蚀和增生过程发生了损失和形成新陆地的过程。利用卫星图像观测可以作为确定北部沿海地区磨损和吸积分布的初始阶段。利用1978 - 2020年的Landsat影像对土地变化进行观测。结果表明,内陆变化受磨蚀和增生控制。它发生在Indramayu和Subang,特别是在大型河流周围的几个地区,如Cipunegara河和Cimanuk河。Cipunegara河和Cimanuk河的河口变化受河口高通量泥沙沉积的控制,河口泥沙淤积影响了新陆的形成。1978年至2020年对奇邦加拉河的Landsat卫星图像监测显示,有205公顷的新土地。对Cimanuk河区域的遥感分析表明,1978 - 2020年,该河口线经历了629 Ha的增积或新陆形成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estuary Changes of Cipunagara and Cimanuk River Using Landsat Imagery Spatial Analysis
The north coastal Java located in the West Java, especially in Cirebon, Indramayu, and Subang, occurs loss and forming new land by abrasion and accretion processes. Observation using satellite imagery can be used as an initial stage to determine the distribution of abrasion and accretion around the north coastal area. Observation of land changes was assigned using Landsat imagery from 1978 to 2020. The result shows that inland change was controlled by abrasion and accretion. It is occurred in Indramayu and Subang, especially in several areas around large rivers e.g. Cipunegara and Cimanuk Rivers. Estuary changes in the Cipunegara and Cimanuk Rivers were controlled by the high flux sediment deposition of the river mouths affecting the new land forming due to the accretion process. Monitoring through Landsat satellite imagery on the Cipunagara River from 1978 to 2020 shows that there was 205 Ha of new land. Remote sensing analysis in the Cimanuk River area shows that the estuary line from 1978 to 2020 experienced accretion or new land forming for 629 Ha.
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