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Soil temperature and soil moisture dynamics in winter and spring under heavy snowfall conditions in North-Eastern Japan

机译:日本东部大雪条件下冬季和春季土壤温度与土壤水分动力学

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Abstract Warm winters and high precipitation in north‐eastern Japan generate snow covers of more than three meters depth and densities of up to 0.55 g cm−3. Under these conditions, rain/snow ratio and snowmelt have increased significantly in the last decade under increasing warm winters. This study aims at understanding the effect of rain‐on‐snow and snowmelt on soil moisture under thick snow covers in mid‐winter, taking into account that snowmelt in spring is an important source of water for forests and agriculture. The study combines three components of the Hydrosphere (precipitation, snow cover and soil moisture) in order to trace water mobility in winter, since soil temperatures remained positive in winter at nearly 0.3°C. The results showed that soil moisture increased after snowmelt and especially after rain‐on‐snow events in mid‐winter 2018/2019. Rain‐on‐snow events were firstly buffered by fresh snow, increasing the snow water equivalent (SWE), followed by water soil infiltration once the water storage capacity of the snowpack was reached. The largest increase of soil moisture was 2.35 vol%. Early snowmelt increased soil moisture with rates between 0.02 and 0.035 vol% hr−1 while, rain‐on‐snow events infiltrated snow and soil faster than snowmelt and resulted in rates of up to 1.06 vol% hr−1. These results showed the strong connection of rain, snow and soil in winter and introduce possible hydrological scenarios in the forest ecosystems of the heavy snowfall regions of north‐eastern Japan. Effects of rain‐on‐snow events and snowmelt on soil moisture were estimated for the period 2012–2018. Rain/snow ratio showed that only 30% of the total precipitation in the winter season 2011/2012 was rain events while it was 50% for the winter 2018/2019. Increasing climate warming and weakening of the Siberian winter monsoons will probably increase rain/snow ratio and the number of rain‐on‐snow events in the near future.
机译:摘要日本东北地区的温暖冬季和高降水量产生超过三米的雪覆盖,深度高达0.55克CM-3。在这些条件下,在过去十年下,雨/雪比和雪姆尔在增加温暖的冬季下降。本研究旨在了解雨雪雪橇和雪花对冬季冬季覆盖下的土壤水分的影响,考虑到春季的雪是森林和农业的重要水源。该研究结合了水液(沉淀,雪覆盖和土壤水分)的三种组分,以追踪冬季水流动性,因为土壤温度在冬季持续阳性,近0.3℃。结果表明,散热后土壤水分增加,特别是在2018/2019年中期冬季雨雪赛事之后。雨雪事件首先被新雪缓冲,增加了雪水等同(SWE),随后达到积雪的储水能力,达到水土渗透。土壤水分的最大增长率为2.35体积%。早期昼夜越来越多的土壤水分,0.02和0.035 Vol%HR-1,雨雪事件渗透到雪地和土壤的速度比散雪速度快,导致速率高达1.06 Vol%HR-1。这些结果表明,冬季雨,雪和土壤的强大联系,并在日本东北部大雪地区的森林生态系统中引入了可能的水文情景。雨雪雪地赛事和雪光对2012 - 2018年期间的影响对土壤水分的影响。雨/雪比率表明,2011/2012年冬季的总降水量只有30%是雨季事件,而2011/2019冬季为50%。增加了气候变暖和西伯利亚冬季季风的减弱可能会在不久的将来增加雨/降价和雨雪赛事的数量。

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