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Land use change and hydrological response in the Camel catchment, Cornwall

机译:康沃尔骆驼流域的土地利用变化和水文响应

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The paper attempts to determine the extent to which rainfall trends and land use changes influence the river flow regime and flood response of a predominantly agricultural catchment (210 km~2) in southwest England. Temporal changes in daily rainfall totals were analysed over annual, seasonal and monthly timescales but although annual average October rainfalls exhibited a weak rising trend (r= 0.3, p > 0.05), no long-term patterns were observed. Analysis of daily mean discharge data for the River Camel over the period 1965-2000, using the Gumbel distribution, revealed an increase in the magnitude and frequency of peak flows. Land use changes were examined using Agricultural Census Data for 1969, 1979, 1988, 1997 and 2000. Both the number of stock andthe area under cereals increased from 1969 to 1997, but ceieal production declined substantially between 1997 and 2000. Spatial response patterns were also examined through a comparison of the flow response of the entire Camel catchment with its more complex land use, with the predominantly pastoral De Lank headwater sub-catchment (22 km~2), to ascertain the amount of change due to increased livestock numbers alone. No single factor was found to be responsible for the increases in flood frequency and magnitude in the River Camel. Rather, long-term changes in the response of the Camel system appear to emanate from the cumulative impact of subtle changes in climate, combined with increased farming activity plus urban expansion. The paper highlights theinherent difficulties of attempting to disentangle the precise effects of individual land uses on flood responses at the catchment scale and underlines the need for a holistic approach to the management of floods. By the same token, sustainable catchmentmanagement can only be achieved through greater awareness of the potential for complex, small-scale land use decisions to result in large-scale hydrological changes.Keywords Landuse; Runoff; Catchment; Flooding; Agriculture
机译:本文试图确定降雨趋势和土地利用变化在多大程度上影响英格兰西南部一个主要农业流域(210 km〜2)的河流流量状况和洪水响应。分析了年度,季节和每月时间尺度上日降雨总量的时间变化,但尽管年平均十月降雨表现出较弱的上升趋势(r = 0.3,p> 0.05),但未观察到长期格局。使用Gumbel分布对1965-2000年期间骆驼河的日均流量数据进行分析,发现峰值流量的幅度和频率均有所增加。使用1969年,1979年,1988年,1997年和2000年的农业普查数据检查了土地利用的变化。从1969年到1997年,谷物的库存数量和谷物种植面积都增加了,但1997年至2000年间,谷物的产量大幅度下降了。通过比较整个骆驼流域与其更复杂的土地利用以及主要是田园牧歌德兰克水源流域(22 km〜2)的流量响应,来确定仅由于牲畜数量增加而引起的变化量。在骆驼河中,没有任何单一因素导致洪水频率和洪水强度的增加。相反,骆驼系统响应的长期变化似乎源于气候细微变化的累积影响,加上农业活动的增加和城市的扩张。本文着重指出了试图在流域尺度上试图区分个别土地用途对洪水响应的确切影响所固有的困难,并强调了需要采用整体方法来管理洪水。同样,可持续的集水区管理只能通过对复杂的小规模土地利用决策可能导致大规模水文变化的潜力的更多认识来实现。径流;集水;洪水;农业

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