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Interannual variability of the lake levels in northwest Russia based on satellite altimetry

机译:基于卫星测高法的俄罗斯西北部湖泊水位年际变化

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Variability of the largest lakes levels in northwest Russia, a climatic change parameter, is characterized by alternating periods of rise and fall according to altimetric measurements of the TOPEX/Poseidon and Jason-1/2 satellites. Water level was calculated with the use of a regional adaptive retracking algorithm for the lakes Il'men, Ladoga, Onega and Peipus. Applications of this algorithm considerably increase the quantity of actual data records and significantly improve the accuracy of water level evaluation. According to the results, temporal variability of Lake Ilmen, Lake Ladoga and Lake Piepus levels is characterized by a wave with a period of 4—5 years, and that of Lake Onega level is characterized by a wave with a period of 15 years. During the period from 1993 to 2011, lake level rose at a rate of 1.17±0.95 cm/year for Lake Il'men, 0.24 ± 0.10 cm/year for Lake Ladoga, 1.39 ± 0.18 cm/year for Lake Piepus and 0.18 ± 0.09 cm/year for Lake Onega.
机译:根据TOPEX / Poseidon和Jason-1 / 2卫星的高​​度测量结果,俄罗斯西北最大湖泊水位的变化是气候变化参数,其特征是交替的上升和下降时间。使用伊尔门湖,拉多加湖,奥涅加河和佩皮斯湖的区域自适应跟踪算法,计算了水位。该算法的应用大大增加了实际数据记录的数量,并显着提高了水位评估的准确性。根据结果​​,伊尔门湖,拉多加湖和皮耶普斯湖水平面的时变性以4-5年的波浪为特征,而奥涅加湖水平面的特征为15年的波浪。从1993年到2011年,伊尔门湖的水位上升速度为1.17±0.95厘米/年,拉多加湖的水位上升为0.24±0.10厘米/年,皮耶普斯湖的水位上升为1.39±0.18厘米/年,0.18±0.09厘米/年的奥涅加湖。

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