首页> 外文期刊>Earth System Science Data Discussions >Water balance and hydrology research in a mountainous permafrost watershed in upland streams of the Kolyma River, Russia: a database from the Kolyma Water-Balance Station, 1948–1997
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Water balance and hydrology research in a mountainous permafrost watershed in upland streams of the Kolyma River, Russia: a database from the Kolyma Water-Balance Station, 1948–1997

机译:俄罗斯科利马河高地河流山区多年冻土流域的水平衡和水文学研究:科利马水平衡站的数据库,1948年至1997年

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In 2018, 70?years have passed since the beginning of observations at the Kolyma Water-Balance Station (KWBS), a unique scientific research hydrological and permafrost catchment. The volume and duration (50 continuous years) of hydrometeorological standard and experimental data, characterizing the natural conditions and processes occurring in mountainous permafrost conditions, significantly exceed any counterparts elsewhere in the world. The data are representative of mountainous territory of the North-East of Russia. In 1997, the station was terminated, thereby leaving Russia without operating research watersheds in the permafrost zone. This paper describes the dataset containing the series of daily runoff from 10 watersheds with an area from 0.27 to 21.3?km2, precipitation, meteorological observations, evaporation from soil and snow, snow surveys, soil thaw and freeze depths, and soil temperature for the period 1948–1997. It also highlights the main historical stages of the station's existence, its work and scientific significance, and outlines the prospects for its future, where the Kolyma Water-Balance Station could be restored to the status of a scientific research watershed and become a valuable international centre for hydrological research in permafrost. The data are available at https://doi.org/10.1594/PANGAEA.881731.
机译:自2018年以来,科利马水平衡站(KWBS)开始观测已经过去了70年,这是一个独特的科学研究水文和多年冻土流域。水文气象标准和实验数据的数量和持续时间(连续50年),表征了山区多年冻土条件下发生的自然条件和过程,大大超过了世界其他任何地方。数据代表了俄罗斯东北部的山区。 1997年,该站被终止,从而使俄罗斯没有在永久冻土区进行任何研究分水岭。本文描述了数据集,该数据集包含10个流域(面积从0.27至21.3?km2)的每日径流系列,降水,气象观测,土壤和雪的蒸发,雪调查,土壤融化和冻结深度以及该时期的土壤温度1948年至1997年。它还突出了该站存在的主要历史阶段,其工作和科学意义,并概述了其未来的前景,在这里,科力马水平衡站可以恢复为科研分水岭的地位,并成为有价值的国际中心用于多年冻土的水文研究。数据可从https://doi.org/10.1594/PANGAEA.881731获得。

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