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SATELLITE ALTIMETRY FOR MONITORING LAKE LEVEL CHANGES

机译:卫星测高仪监测湖泊水位变化

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Accurate and continuous monitoring of lakes and inland seas is possible since 1991 thanks to the recent missions of satellite altimetry (Topex-Poseidon, ERS-1, ERS-2, Jason-1 and Envisat). Global processing of the data of these satellites could provide temporal and spatial times series of lakes water level from 1991 to 2003 on the whole Earth with a decimeter precision. The response of water level to regional hydrology is particularly marked for lakes and inland seas of semi-arid regions. Altimetry data can provide an invaluable source of information in hydrology sciences, but in-situ data (rivers runoff, temperature, precipitation etc.) are still strongly needed to study the evolution of water mass balance of each lake. Moreover, sea level variations that result from variation of hydrological parameters such as river discharge, precipitation and evaporation, are very sensitive indicators of regional climate variations. Recent results obtained on Aral Sea and Issykkul Lake are presented here. Inter - annual changes of water level have been obtained over these lakes that must be interpreted in term of hydrological water balance. Since 1960 the Aral sea has been drying and since 1989 it is divided into two lakes that follow different evolution, the Big Aral in the south which continuously dried up the last 10 years, while the so-called Small Aral in the north presented large inter-annual fluctuations related to constructions and destructions of a dam in the Berg's strait retaining the water from the Syr Darya. For Issykkul, a slow decrease of the level has been observed over the last hundreds years (4 cm / year), followed by an abrupt and bigger increase of the level of around 10 cm/yr since 1998. The impact on local populations and infra-structures of these fluctuations are dramatic in the case of Aral, much less in the case of Issykkul, but comparative study of both water bodies may help in the future to understand the respective consequences of human-induced activities from the natural changes. It is also the task of a new project recently submitted and accepted by the NATO with scientists from Uzbekistan and Kyrgyz Republic.
机译:自1991年以来,由于最近的卫星测高任务(Topex-Poseidon,ERS-1,ERS-2,Jason-1和Envisat),对湖泊和内陆海域进行准确和连续的监测成为可能。这些卫星数据的全球处理可以提供1991年至2003年整个地球上湖泊水位的时间和空间时间序列,精确度为10米。对于半干旱地区的湖泊和内海,水位对区域水文学的响应尤为明显。高程数据可以为水文学提供宝贵的信息来源,但是仍然很需要现场数据(河流径流,温度,降水等)来研究每个湖泊水质平衡的演变。此外,由诸如河流流量,降水和蒸发等水文参数变化引起的海平面变化是区域气候变化的非常敏感的指标。这里介绍了在咸海和伊塞库尔湖获得的最新结果。这些湖泊已获得年际水位变化,必须根据水文水平衡来解释。自1960年以来,咸海一直处于干燥状态,自1989年以来,它被分为两个遵循不同演变过程的湖泊,南部的大咸海在过去的10年中不断变干,而北部的所谓小咸海则呈现出较大的干旱。 -与每年在伯格海峡修建和破坏大坝有关的年度波动,这些大坝保留了Syr Darya的水。在伊塞库尔地区,过去几百年(4厘米/年)的水平面缓慢下降,随后自1998年以来每年急剧增加,约为10厘米/年。水平对当地居民和基础设施的影响这些波动的结构在Aral的情况下是戏剧性的,在Issykkul的情况下则要少得多,但是对两个水体的比较研究可能会在将来帮助理解自然变化对人为活动的相应后果。这也是北约最近与乌兹别克斯坦和吉尔吉斯共和国的科学家提交并接受的一个新项目的任务。

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