菲律宾伊洛伊洛市Jaro泄洪道河口段红树林覆盖变化(1947-2018

Paul Caesar M. Flores, L. David, F. Siringan
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引用次数: 1

摘要

2012年修建的Jaro泄洪道导致海岸线在8年内迅速退化。本研究利用历史地图(1947年和1988年)和陆地卫星图像,考察了该泄洪渠河口地区红树林覆盖面积的长期和短期变化。共使用了44张Landsat图像,覆盖时间段为1998年、2000-2001年、2004年、2006年、2008年、2010-2011年、2013-2014年、2016年和2018年。每个时间段使用5张图像,并使用监督分类方案确定每张图像的红树林覆盖率。然后对每个时间段的栅格集进行平均,以生成最终的分类图。由1947年至1988年,由于在原河口兴建鱼塘而导致河道崩裂,红树林覆盖面积由7.01公顷增加至43.83公顷。然而,由于广泛的鱼塘改造,它开始减少,直到2008年(3.42公顷)。然后,在2018年迅速增加到40.05公顷。这种增加的主要原因是由于高沉积和低容纳空间造成的Jaro泄洪道泄洪区潮间带迅速扩大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mangrove Forest Cover Change (1947-2018) at The River Mouth Section of The Jaro Floodway, Iloilo City, Philippines
The construction of the Jaro Floodway in 2012 resulted to a rapid progradation of the shoreline in 8 years. This study examined the long- and short-term changes in area covered by mangroves at the river mouth area of this flood canal by utilizing historical maps (1947 and 1988), and Landsat images. A total of 44 Landsat images were used that covered the time periods 1998, 2000-2001, 2004, 2006, 2008, 2010-2011, 2013-2014, 2016, and 2018. Five images were used for each time period and the mangrove cover for each image was determined by using a supervised classification scheme. The set of rasters for each time period was then averaged to generate the final classification map. From 1947 to 1988, mangrove cover increased from 7.01 to 43.83 ha as a result of channel avulsion of the Jaro River due to fishpond construction at the former river mouth. However, it started to decrease until 2008 (3.42 ha) due to widespread fishpond conversion. Then, it rapidly increased to 40.05 ha in 2018. This increase is primarily attributed to the rapid expansion of the intertidal zone in the discharge area of the Jaro Floodway which is due to high sedimentation and low accommodation space.
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