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Palaeoclimatological perspective on river basin hydrometeorology: Case of the Mekong Basin

机译:流域水文气象的古气候学观点:以湄公河流域为例

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Globally, there have been many extreme weather events in recent decades. A challenge has been to determine whether these extreme weather events have increased in number and intensity compared to the past. This challenge is made more difficult due to the lack of long-term instrumental data, particularly in terms of river discharge, in many regions including Southeast Asia. Thus our main aim in this paper is to develop a river basin scale approach for assessing interannual hydrometeorological and discharge variability on long, palaeological, time scales. For the development of the basin-wide approach, we used the Mekong River basin as a case study area, although the approach is also intended to be applicable to other basins. Firstly, we derived a basin-wide Palmer Drought Severity Index (PDSI) from the Monsoon Asia Drought Atlas (MADA). Secondly, we compared the basin-wide PDSI with measured discharge to validate our approach. Thirdly, we used basin-wide PDSI to analyse the hydrometeorology and discharge of the case study area over the study period of 1300-2005. For the discharge-MADA comparison and hydrometeorological analyses, we used methods such as linear correlations, smoothing, moving window variances, Levene type tests for variances, and wavelet analyses. We found that the developed basin-wide approach based on MADA can be used for assessing long-term average conditions and interannual variability for river basin hydrometeorology and discharge. It provides a tool for studying interannual discharge variability on a palaeological time scale, and therefore the approach contributes to a better understanding of discharge variability during the most recent decades. Our case study revealed that the Mekong has experienced exceptional levels of interannual variability during the post-1950 period, which could not be observed in any other part of the study period. The increased variability was found to be at least partly associated with increased El Ni?o Southern Oscillation (ENSO) activity.
机译:在全球范围内,近几十年来发生了许多极端天气事件。确定这些极端天气事件与过去相比是否数量和强度有所增加是一个挑战。由于缺少包括东南亚在内的许多地区的长期仪器数据,尤其是在河流流量方面,这使挑战变得更加困难。因此,本文的主要目的是开发一种流域尺度方法,以评估长期,古生物学尺度上的年际水文气象和流量变化。为了开发全流域方法,我们以湄公河流域为案例研究区域,尽管该方法也打算适用于其他流域。首先,我们从季风亚洲干旱地图集(MADA)得出了全盆地范围内的Palmer干旱严重度指数(PDSI)。其次,我们将流域范围的PDSI与实测流量进行了比较,以验证我们的方法。第三,我们使用流域范围的PDSI分析了案例研究区域1300-2005年的水文气象和流量。对于流量-MADA比较和水文气象分析,我们使用了线性相关,平滑,移动窗口方差,方差的Levene类型检验和小波分析等方法。我们发现,基于MADA的已开发流域范围的方法可用于评估流域水文气象和流量的长期平均条件和年际变化。它提供了一种在古生物学时间尺度上研究年际排放变化的工具,因此,该方法有助于更好地了解最近几十年来的排放变化。我们的案例研究显示,湄公河在1950年以后的时期经历了异常的年际变化水平,而在研究的任何其他时期都无法观察到。发现增加的可变性至少部分与增加的厄尔尼诺南部涛动(ENSO)活动有关。

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