卡卢河流域的洪水与土地利用、土地覆盖变化:行动呼吁

Amarakoon V., Wickramasinghe D.D., Premasiri H.M.R., Shaw R., Mukherjee M.
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引用次数: 0

摘要

洪水是全球最常见的自然灾害之一。除降雨外,土地利用、土地覆被 (LULC) 变化也是造成洪水的一个主要因素。卡卢河流域是斯里兰卡第二大流域,也是经常发生洪水的地区,本研究试图了解洪水与 LULC 变化之间的联系。我们研究了 2001-2020 年期间快速城市化的两个地区 Rathnapura(流域上游)和 Kalutara(流域下游)的洪峰水位、洪水事件数量、土地利用类型的变化及其影响。获得了 2001 年、2009 年、2015 年和 2020 年的卫星图像(LANDSAT),并使用 ArcGIS 和遥感工具进行了土地利用分类。对主要土地利用类型及其转换进行了调查,并进行了地面实况核实。因此,确定的主要土地利用类型包括自然植被和森林(NV)、定居点(ST-住房和工业用地)、耕地(CL)、水体(WB)和裸地(BL)。结果表明,自然区(NV)的变化最为剧烈,面积有所减少,而受人类活动影响的土地(ST、CL 和 BL)则逐年增加。2001 年,自然区所占土地面积最大(42.4%),到 2020 年减少了 14.2%。ST 和 CL 分别增加了 8.6% 和 5.2%。随着时间的推移,Rathnapura 和 Kalutara 的月降雨量(资料来源:斯里兰卡气象局)有所增 加,这是这些地区最高水位不断上升的主要原因(资料来源:斯里兰卡灌溉局)。然而,居住区的变化与下游流域的河流最高水位之间也存在着明显的相关性(p=0.03,R2=99%;回归分析)。2001-2020 年间,拉斯纳普拉经历了 3 次大洪水(超过高水位警戒线的洪水),而卡卢塔拉则发生了 16 次大洪水。在 2017 年的大洪水中,Rathnapura 的儿童死亡人数为 14 人,而 Kalutara 则为 24 人。因此,整个流域的土地利用、土地利用变化和降雨似乎对卡卢塔拉的洪水严重程度影响更大,因为它位于海拔最低的地方。当自然土地转变为受人为影响的地区时,水循环受到干扰,不透水表面增加,蓄水能力降低,自然排水系统丧失,洪水风险往往会增加。由于气候变化也会引发更多的洪灾,因此迫切需要采取积极主动的方法,包括适当的土地利用规划和雨水储存。因此,应优先采取洪水缓解行动,特别是在下游流域,以确保抗灾能力和可持续性。关键词卡卢河流域 土地利用、土地覆盖(LULC)变化 洪水
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Floods and Land Use Land Cover Changes in the Kalu River Basin: A Call to Action
Floods are one of the most common natural disasters worldwide. Apart from rainfall, Land Use Land Cover (LULC) changes too are a main contributory factor for floods. This study attempted to understand the link between floods and LULC changes in Kalu river basin, which is the second largest river basin and an area that experiences recurrent floods in Sri Lanka. We studied peak water levels, number of flood events, changes in land use types and impacts in rapidly urbanizing two districts, Rathnapura (upper basin) and Kalutara (lower basin) during 2001-2020. The satellite images (LANDSAT) were obtained for 2001, 2009, 2015 and 2020 and land use classification was done using ArcGIS and Remote Sensing Tools. Main land use types and their transformations were investigated and ground-truthing was carried out. Accordingly, the main types of land uses identified were Natural Vegetation and forests (NV), Settlements (ST- housing and industrial lands), Cultivated Lands (CL), Water Bodies (WB) and Bare Lands (BL). The results indicated that the most drastic change was found in the natural areas (NV) and they have diminished while the lands with anthropogenic impacts (ST, CL and BL) have increased across years. The NV had occupied the highest land area in 2001 (42.4%) and has reduced by 14.2% by 2020. The ST and CL have increased by 8.6 % and 5.2% respectively. The monthly rainfall of Rathnapura and Kalutara (Source: Department of Meteorology, Sri Lanka) has increased with time, which is a main reason for the increasing peak water levels of these areas (Source: Department of Irrigation, Sri Lanka). However, a significant correlation also exists between the change of the settlement area with the peak river water levels in the lower basin (p=0.03, R2=99%; regression analysis). Rathnapura has experienced 3 major floods (floods above the high water alert level) from 2001-2020, while 16 major floods have occurred in Kalutara. During the major flood in 2017, the number of child deaths in Rathnapura was 14 while in Kalutara it was 24. Accordingly, the LULC changes of the whole basin along with rainfall seem to influence on the severity of floods in Kalutara more, as it is located in the lowest elevation level. When natural lands are transformed to anthropogenic- impacted areas with disturbances to the water cycle, increased impervious surfaces, reduced water storage capacities and loss of natural drainage, the flood risk tends to increase. Proactive approaches including proper land use planning and rainwater storage are urgently needed as the climate change too would trigger more floods. Thus, the flood mitigatory actions, especially, in the lower river basin should be a priority to ensure resilience and sustainability. Keywords: Kalu river basin, Land Use Land Cover (LULC) changes, Floods
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