马拉维奇克瓦瓦地区夏尔河流域洪水发生的趋势和影响:历史视角(1980 - 2019)

Daniel Nakapu Hussein, Professor Maarifa Ali Mwakumanya, Professor Mwakio Mwakio Tole
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引用次数: 0

摘要

目的:本研究的目的是研究马拉维郡河流域(SRB)洪水的历史趋势。该盆地容易发生严重洪灾,是全国受灾最严重的地区。多年来,洪水对盆地内外的社区构成了重大威胁。因此,本研究的主要目的是记录1980年至2019年马拉维奇克瓦瓦区夏尔河流域洪水发生的频率和影响的历史角度。方法:本研究采用混合调查设计。采用随机抽样和有目的抽样来确定参与者。共有384名受访者参与了这项研究。这项研究收集了第一手资料和第二手资料。主要数据来源是通过家庭调查、对关键举报人的访谈和焦点小组讨论收集的,而次要数据来源是通过非政府和马拉维政府部门和机构(MDAs)的文件以及现有文献收集的。焦点小组讨论(fgd)、社区长者访谈(CEIs)和关键信息提供者访谈(KIIs)的数据在奇切瓦语用录音机记录下来,用奇切瓦语转录,然后翻译成英语。采用SPSS (Statistical Package for Social Scientists)第25版对住户调查数据进行处理,并将二次数据转换为时间序列数据,然后使用STATA软件进行分析,生成图表。结果表明:年平均气温、年平均降雨量和基流指数3个水文气象极端事件均有所增加,表明齐克瓦瓦地区夏尔河流域洪水发生的强度和频率在绝对值上均有所增加;人们对洪水的认知表明,奇克瓦瓦地区的夏尔河流域每5年就会发生一次过度洪水。除其他因素外,这个5年周期是研究区域气候变化和森林损失的结果,导致河流沉积增加。建议:本文发现,奇克瓦瓦区夏尔河流域的当地人将永远生活在日益严重的洪水中。因此,他们应该积极主动地进行洪水管理,并将这一过程理解为未来风险评估的持续活动。分析流域洪水的历史非常重要,因为它有助于马拉维灾害管理事务部(DoDMA)官员提高警惕,并估计奇克瓦瓦地区夏尔河流域下一次洪水的时间框架,从而加强洪水预报的准确性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Trends and Effects of Flood Occurrences in the Shire River Basin in Chikwawa District of Malawi: A Historical Perspective (1980 - 2019)
Purpose: The purpose of this study was to examine historical trends in flooding in Malawi’s Shire River Basin (SRB). The basin is prone to severe flooding and most affected in the country. For many years, flooding has posed a significant threat to communities in and around the basin. Therefore, the main objective of the study was to document the historical perspective of flood occurrences in terms of frequency and impact in the Shire River Basin of Chikwawa District, Malawi, from 1980 to 2019.      Methodology: A mixed survey design was used for the study. Both random and purposive sampling were used to identify participants. A total of 384 respondents took part in the study. The study collected both primary and secondary data. Primary sources of data were collected using household surveys, interviews with key informants, and focus group discussions, while secondary sources of data were collected using documents from both non-governmental and Malawian governmental departments and agencies (MDAs) as well as existing literature. Data from focus group discussions (FGDs), interviews with community elders (CEIs), and key informant interviews (KIIs) were recorded in Chichewa with a voice recorder, transcribed in Chichewa, and then translated into English. Household survey data were processed using Statistical Package for Social Scientists (SPSS) version 25 and secondary data were converted to time series data and then analysed using STATA software to produce charts and graphs.   Findings: The results showed that all three hydrometeorological extremes (mean annual temperature, average rainfall and baseflow index) increased, suggesting that both the intensity and frequency of flooding in the Shire River Basin of Chikwawa District were also increasing in absolute terms. People’s perceptions of flooding showed that the Shire River Basin in Chikwawa District experienced excessive flooding every 5 years. This 5-year cycle was, among other factors the result of climate change and forest loss in the study area, leading to an increase in river sedimentation. Recommendations: This article found that the local people in the Shire River Basin of Chikwawa District will always live with increasing levels of flooding. Therefore, they should be proactive in flood management and understand the process as an ongoing activity for future risk assessment. Analysing the history of river basin flooding is important as it helps the Malawi's Department of Disaster Management Affairs (DoDMA) officials to be alert and estimate the time frame for the next flood in the Shire River Basin of Chikwawa District to strengthen the flood forecasting accuracy.  
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