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Shifts in stream hydrochemistry in responses to typhoon and non-typhoon precipitation

机译:在河流水平响应中转移到台风和非台风降水中

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Climate change is projected to increase the intensity and frequency of extreme climatic events such as tropical cyclones. However, few studies have examined the responses of hydrochemical processes to climate extremes. To fill this knowledge gap, we compared the relationship between stream discharge and ion input-output budget during typhoon and non-typhoon periods in four subtropical mountain watersheds with different levels of agricultural land cover in northern Taiwan. The results indicated that the high predictability of ion input-output budgets using stream discharge during the non-typhoon period largely disappeared during the typhoon periods. For ions such as Na+, NH4+, and PO43-, the typhoon period and non-typhoon period exhibited opposite discharge-budget relationships. In other cases, the discharge-budget relationship was driven by the typhoon period, which consisted of only 7 % of the total time period. The striking differences in the discharge-ion budget relationship between the two periods likely resulted from differences in the relative contributions of surface runoff, subsurface runoff and groundwater, which had different chemical compositions, to stream discharge between the two periods. Watersheds with a 17-22 % tea plantation cover showed large increases in NO3- export with increases in stream discharge. In contrast, watersheds with 93-99 % forest cover showed very mild or no increases in NO3- export with increases in discharge and very low levels of NO3- export even during typhoon storms. The results suggest that even mild disruption of the natural vegetation could largely alter hydrochemical processes. Our study clearly illustrates significant shifts in hydrochemical responses between regular and typhoon precipitation. We propose that hydrological models should separate hydrochemical processes into regular and extreme conditions to better capture the whole spectrum of hydrochemical responses to a variety of climate conditions.
机译:预计气候变化将增加热带气旋等极端气候事件的强度和频率。然而,很少有研究检测了水化工程对气候极端的反应。为了填补这一知识差距,我们将流量与台湾四大农业陆地覆盖水平不同水平的农场和非台风期间的流排放和离子投入输出预算之间的关系。结果表明,在非台风期间,在台风时期期间使用流排放的离子输入输出预算的高可预测性。对于诸如Na +,NH4 +和PO43的离子,台风周期和非台风时期表现出相反的排放预算关系。在其他情况下,排放预算关系由台风时期驱动,其中仅由总时间段的7%组成。两个时期之间的放电离子预算关系中的引人注目的差异可能是由于表面径流的相对贡献,地下径流和地下水的差异导致,其具有不同的化学组成,在两个时段之间流出放电。分水岭17-22%的茶园覆盖物显示NO3-出口的大幅增加,流量放电增加。相比之下,具有93-99%的森林覆盖的流域表现出在NO3-出口的NO3-出口时显示出非常温和或没有增加,即使在台风风暴期间,也甚至在NO 3-出口的增加而增加。结果表明,即使轻度破坏天然植被也可能大大改变水化工程。我们的研究清楚地说明了常规和台风降水之间的水化反应的显着变化。我们提出水文模型应该将水化工程分离成常规和极端条件,以更好地捕获整个气候响应的整个气候响应。

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