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An investigation of permanent and transient changes in flood distribution and outflows in the Okavango Delta, Botswana

机译:博茨瓦纳奥卡万戈三角洲洪水分布和流出量的永久和短暂变化调查

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The annual flood cycle in the Okavango Delta is the basis of subsistence of the local population, providing water, arable land and wetland resources. Additionally, it forms the basis of a large tourism industry. Flooding in the Okavango Delta is, however, very variable both at short and long term time scales. Past research suggested the influence of factors such as tectonic activity, sedimentation, vegetation change or human influence on the spatial distribution of floodwaters. Change in the flooding regime at any given site is thus often perceived as an effect of permanent change in the system, and this perception results in unnecessary demands for engineering interventions in the system. However, it is possible that some of the perceived changes in flood regime are apparent transient effects of non-linearity of the system and variation in hydrological inputs. Hydrometric data and satellite-derived flood maps are analysed here using statistical methods (covariance analysis and double mass analysis) to distinguish between temporal and permanent changes in various parts of the Okavango Delta. The analyses reveal that system non-linearity causes the hydrological responses of the Okavango Delta to be non-proportional to the inputs. Periods of one to several consecutive years are present when flood extents and outflows are either considerably higher or lower (flow or flood regimes) than what would be expected considering the magnitude of inflow. Such effects are visible throughout the entire system, or only in some distributaries, and do not, as previously thought, represent permanent change in flood distribution. However, flood regime change that appears to result from a physical change in the system has been detected. This change has a nature of shift in flood distribution between the Thaoge and the Xudum, with the latter receiving more water after 1997 at the expense of the former and causing 2004 re-flooding of Lake Ngami. (c) 2007 Elsevier Ltd. All rights reserved.
机译:奥卡万戈三角洲的年度洪水周期是当地人口赖以生存的基础,提供水,耕地和湿地资源。此外,它构成了大型旅游业的基础。但是,在奥卡万戈三角洲,无论是短期还是长期,洪水都变化很大。过去的研究表明,构造活动,沉积,植被变化或人为因素等因素对洪水的空间分布有影响。因此,通常将任何给定站点的洪水状态的变化视为系统中永久性变化的结果,这种感知导致对系统中的工程干预产生不必要的需求。但是,洪水状态的某些感知变化可能是系统非线性和水文输入变化的明显瞬时影响。这里使用统计方法(协方差分析和双重质量分析)分析了水文数据和卫星衍生的洪水地图,以区分奥卡万戈三角洲各个地区的时间变化和永久变化。分析表明,系统非线性导致Okavango三角洲的水文响应与输入不成比例。当洪水的程度和流出量大大高于或低于考虑到流入量的预期水平时,存在连续一到几年的时期。这样的影响在整个系统中可见,或者仅在某些分配区域可见,并且不像以前所认为的那样代表洪水分布的永久变化。但是,已经检测到似乎由系统的物理变化导致的洪水状态变化。这种变化具有Thaoge和Xudum之间的洪水分布转移的性质,后者在1997年后以牺牲前者的代价接收了更多的水,并导致2004年Ngami湖重新洪水。 (c)2007 Elsevier Ltd.保留所有权利。

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