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冰川水资源
相关语句
  glacier water resources
     Glacier Water Resources of Qilian Mountains
     祁连山冰川水资源
短句来源
  glacial water resource
     THE CONDITIONS OF THE GLACIAL WATER RESOURCE AND THE WAYS OF ITS EXPLOITATION AND UTILIZATION IN CHINA
     我国冰川水资源状况及开发利用途径
短句来源
  glacial water resources
     The Application of Water (Mass) Balance Model in Glacierized Area to Assessing the Climate Impact on Glacial Water Resources
     用冰川区水量(物质)平衡模型估计气候变化对冰川水资源影响的初步研究
短句来源
  “冰川水资源”译为未确定词的双语例句
     Features and Evaluation of Glaciation Landscape Reasources in Heishui County,Sichuan Province
     四川省黑水县冰川水资源的特征与评价
短句来源
     The spatial distribution of glacial melt water varies in different river basins. The runoff factor in the marine glacial area is much higher than that in the continental glacial area.
     青藏高原冰川水资源在各大水系的分布上不均匀 ,海洋性冰川区冰川融水径流模数远大于大陆性冰川区。
短句来源
     The expedition of glaciations in Heishui County,Sichuan Province has been first carried out in August 2001.There are 19 glaciers with area of 6.04km 2 and storage of 0.1736km 3.Its notable that two"baby glaciers"have been found in the east slope of Yanggong Mountain.
     首次专门对四川黑水县羊拱山脉等地的现代冰川水资源、第四纪古冰川以及相应的景观地貌环境进行了科学考察。 境内共发育分布现代冰川 19条 ,形态类型有悬冰川、坡面冰川、冰斗悬冰川、冰斗山谷冰川 ,总面积达 6 .0 4km2 ,冰储量为 0 .1736km3 。
短句来源
     Glacier retreat results in about 7million cubic meters losses of glacier causes water resources every year in the source regions of the Yangtze and Yellow rivers,respectively.
     冰川退缩使长江源区和黄河源区年均各自损失冰川水资源约0.7×108m3。
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      glacial water resource
    The conditions of the glacial water resource and ways of its exploitation and utilization in China
          
    China is one of the countries where there is abundant glacial water resource and glaciers exist in a vast area of mountainous regions.
          
    In this paper, a comprehensive discussion is made for the characteristics of glacial water resource, the chemical properties of meltwater and the prospects of future utilization in China.
          
    It has found that the glacial water resource is a water resource system based on the effect of a solid water reservoir.
          
    It is necessary to reconfirm the value of this water resource and conduct further studies on the fundamentals of its application in order to rationally exploit, utilize and preserve the glacial water resource.
          


    China is one of the countries where there is aboundant glacial water resource and glaciers exist in a vast area of mountainous regions. In this paper, a comprehensive discussion is made for the characteristics of glacial water resource,the chemical properties of meltwater and the prospects of the future utilization of this resource in China. It has been found that the glacial water resource is a water resource system based on the effect of a solid water reservoir. Its mineralization is low and it almost does...

    China is one of the countries where there is aboundant glacial water resource and glaciers exist in a vast area of mountainous regions. In this paper, a comprehensive discussion is made for the characteristics of glacial water resource,the chemical properties of meltwater and the prospects of the future utilization of this resource in China. It has been found that the glacial water resource is a water resource system based on the effect of a solid water reservoir. Its mineralization is low and it almost does not have any pollution. Particular by the glacial water is a high-quality fresh water resource in the inland arid region. It is necessary to reconfirm the value of this water resource and conduct further studies on the fundamentals of its application in order to rationally exploit,utilize and preserve the glacial water resource.

    我国是冰川水资源拥有大国之一。本文对我国冰川水资源特性、冰水化学特征及开发利用进行了综合分析论述。指出冰川水资源是以固体水库效应为基础的水资源体系,有必要重新认识冰川的水资源价值,并进一步开展冰川应用基础研究,为合理开发利用和保护冰川水资源提供依据。

    Glaciers on the Tibetan Plateau are calculated based on the Chinese glacier inventory.Statistics shows that that there are 36 793 existing glaciers on the Tibetan Plateau,with a total area of 49 873.44 km 2 and ice volume of 4561.3857km 3,corresponding to 79.4%,84.0% and 81.6% of the total glaciers in China respectively.Tibetan Plateau is the largest existing glaciation area in low mid latitude in the world.Glaciers are distributed mainly in Kunlun Mts.,Himalayas Mts.and karakorum Mts.,accounting...

    Glaciers on the Tibetan Plateau are calculated based on the Chinese glacier inventory.Statistics shows that that there are 36 793 existing glaciers on the Tibetan Plateau,with a total area of 49 873.44 km 2 and ice volume of 4561.3857km 3,corresponding to 79.4%,84.0% and 81.6% of the total glaciers in China respectively.Tibetan Plateau is the largest existing glaciation area in low mid latitude in the world.Glaciers are distributed mainly in Kunlun Mts.,Himalayas Mts.and karakorum Mts.,accounting for over half of the total glacier number and glacier volume on the Tibetan Plateau.The total glacier number and glacier volume in the other 8 mountains account for only less than half of the total glacier number and glacier volume on the Tibetan Plateau.Due to the influence of climate and topography,the glacier number and glacier volume is larger in the northern side of the mountains than that in the southern side,except the Nyainqenlanglha Mts.and Gangdisi Mts..There are few large valley glaciers,accounting for only 4.6% of the total glacier number on the plateau.However,the glacial area and ice volume account for 33.5% and 48.6% respectively of the total glaciers on the plateau.There are 21 large valley glaciers covering an are a of over 100km 2 each.The Yinsugaiti glacier in the northern side of the Karakorum Mts.is 42km in lenghth,with an area of 379.97km 2. The total ice volume of all the glaciers on the Tibetan Plateau is 39 228×10 8 m 3 of water equivalent,which is about 10.8 times of the annual surface runoff on the plateau.The gigantic volume of fresh water reservoir on the Tibetan Plateau can provide 504×10 8 m 3 of water to river runoff.The spatial distribution of glacial melt water varies in different river basins.The runoff factor in the marine glacial area is much higher than that in the continental glacial area.

    :在全部完成中国冰川编目的基础上 ,精确统计了青藏高原发育有现代冰川 3 6793条 ,冰川面积4 9873 4 4km2 ,冰川冰储量 4 561 3 857km3,分别占我国冰川总数的 79 4 %、84 0 %和 81 6% ,是世界上中低纬度地区最大的现代冰川分布区。青藏高原现代冰川主要分布在昆仑山、喜马拉雅山和喀喇昆仑山 ,其数量和规模占冰川总数的一半以上。由于气候和地形要素的不同组合 ,除念青唐古拉山和冈底斯山外 ,山脉北坡冰川在数量和规模上均大于南坡。青藏高原冰川形态类型齐全 ,悬冰川数量最多 ,占总数的3 9 3 % ;而大型的山谷冰川仅占高原总数的 4 6% ,但其面积和冰储量分别占高原总数的 3 3 5%和4 8 6%。大型山谷冰川面积大于 1 0 0km2 的冰川有 2 1条 ,喀喇昆仑山北坡的音苏盖堤冰川长 4 2km ,冰川面积达 3 79 97km2 。青藏高原现代冰川折合成淡水约有 3 92 2 8× 1 0 8m3,是青藏高原地表径流总量的 1 0 8倍 ,是巨大的优质淡水资源。初步计算 ,每年可提供冰川融水 50 4× 1 0 8m3补给河流。青藏高原冰川...

    :在全部完成中国冰川编目的基础上 ,精确统计了青藏高原发育有现代冰川 3 6793条 ,冰川面积4 9873 4 4km2 ,冰川冰储量 4 561 3 857km3,分别占我国冰川总数的 79 4 %、84 0 %和 81 6% ,是世界上中低纬度地区最大的现代冰川分布区。青藏高原现代冰川主要分布在昆仑山、喜马拉雅山和喀喇昆仑山 ,其数量和规模占冰川总数的一半以上。由于气候和地形要素的不同组合 ,除念青唐古拉山和冈底斯山外 ,山脉北坡冰川在数量和规模上均大于南坡。青藏高原冰川形态类型齐全 ,悬冰川数量最多 ,占总数的3 9 3 % ;而大型的山谷冰川仅占高原总数的 4 6% ,但其面积和冰储量分别占高原总数的 3 3 5%和4 8 6%。大型山谷冰川面积大于 1 0 0km2 的冰川有 2 1条 ,喀喇昆仑山北坡的音苏盖堤冰川长 4 2km ,冰川面积达 3 79 97km2 。青藏高原现代冰川折合成淡水约有 3 92 2 8× 1 0 8m3,是青藏高原地表径流总量的 1 0 8倍 ,是巨大的优质淡水资源。初步计算 ,每年可提供冰川融水 50 4× 1 0 8m3补给河流。青藏高原冰川水资源在各大水系的分布上不均匀 ,海洋性冰川区冰川融水径流模数远大于大陆性冰川区。

    The expedition of glaciations in Heishui County,Sichuan Province has been first carried out in August 2001.There are 19 glaciers with area of 6.04km 2 and storage of 0.1736km 3.Its notable that two"baby glaciers"have been found in the east slope of Yanggong Mountain.These new small glaciers are very important for the observation of local environment changes.These are also hundreds of ancient morain lakes and other various glaciation landscape in the upper reach of Dagu valley.That is a very good foundation...

    The expedition of glaciations in Heishui County,Sichuan Province has been first carried out in August 2001.There are 19 glaciers with area of 6.04km 2 and storage of 0.1736km 3.Its notable that two"baby glaciers"have been found in the east slope of Yanggong Mountain.These new small glaciers are very important for the observation of local environment changes.These are also hundreds of ancient morain lakes and other various glaciation landscape in the upper reach of Dagu valley.That is a very good foundation to develop scientific expedition and tourism in this region.

    首次专门对四川黑水县羊拱山脉等地的现代冰川水资源、第四纪古冰川以及相应的景观地貌环境进行了科学考察。境内共发育分布现代冰川 19条 ,形态类型有悬冰川、坡面冰川、冰斗悬冰川、冰斗山谷冰川 ,总面积达 6 .0 4km2 ,冰储量为 0 .1736km3 。值得注意的是在海拔 5 0 0 0m附近背阴处发现零星的婴儿冰川 (BabyGlacier)分布。这对当地区域气候环境的变化具有重要的窗口监测作用。打古冰川谷地上源的古冰蚀、冰碛湖泊星罗棋布 ,达数百个之多 ,这为当地未来的生态、环境科学探险、旅游业的开发提供了良好基础

     
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