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glacier
相关语句
  冰川
    DERIVING GLACIER CHANGE INFORMATION ON THE XIZANG (TIBETAN) PLATEAU BY INTEGRATING RS AND GIS TECHNIQUES
    综合RS与GIS方法提取青藏高原冰川变化信息——以布喀塔格峰为例
短句来源
    Glacier has a narrow spectrum on TM5, 7 bands, but moraine and snow and ice are different in evidence, therefore, TM5, 7 are advantageous bands for extracting glacier information.
    冰川在 TM5、7 波段光谱值范围窄, 且冰碛与冰雪有明显的光谱差异, 是冰川信息提取的有利波段.
短句来源
    The last principal component image, which is brought by K-L transformation with multiple band images, including TM5, 7, is a differential image of both TM5 and TM7, and mainly reflects the glacier information of image.
    包含TM5、7的多波段图像K—L变换的最后主组分是TM5、7的差值图像, 主要反映的是图像中的冰川信息.
短句来源
    There is about 35,000 km~2 glacier in Tibet,which is the largest area of modern glacier distribution in China,as well as modern glacier lake distribution.
    西藏地区冰川面积约为35000km2,是我国现代冰川分布最多的地区,也是现代冰湖分布最多的地区。
短句来源
    RELATIONSHIP BETWEEN THE GLACIER VARIATION AND THE DEBRIS FLOW DEVELOPMENT OF THE HOLOCENE IN THE GONGGA MOUNTAINOUS REGION
    贡嘎山区全新世冰川变化与泥石流发育的关系
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  “glacier”译为未确定词的双语例句
    Preliminary study on debris flow induced by glacier lake outburst in Tibet
    西藏典型冰湖溃决型泥石流的初步研究
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    The dissertation investigates application of SAR interferometry in Antarctic inland glacier for DEM and complex ice flow measurement, also large-scale scatterometer and radiometer data for ice sheet monitoring.
    本论文开展了利用干涉雷达技术在南极内陆冰盖地区提取数字高程模型和测量复杂冰流的研究,另利用大尺度的微波散射计和辐射计数据开展了冰盖冰架地区的变化监测研究。
短句来源
  相似匹配句对
    Preliminary study on debris flow induced by glacier lake outburst in Tibet
    西藏典型冰湖溃决型泥石流的初步研究
短句来源
    DISTRIBUTION AND CHARACTERISTICS OF GLACIER DEBRIS FLOW ALONG THE DUSHANZI-KORLA HIGHWAY
    独库公路冰川泥石流分布及其特征
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  glacier
Microorganisms Found in the Basal Horizons of the Antarctic Glacier above Lake Vostok
      
Problems of such kind arise in glaciology when one estimates the stability of snow on mountain slopes or determines the catastrophic movement of a glacier; the results can also be applied to solifluction phenomena [2, 3].
      
It was assumed that the temperature at the bed of the glacier could reach the melting point due to nonstationary heating and that the conditions would be produced for motion of the glacier.
      
Here we examine the nonstationary response of a glacier to small deviations of the system parameters from critical values corresponding to the stationary state.
      
Numerical investigation and self-similar solutions of the glacier-ocean interaction problem
      
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In the Gon gga Mountainous Regioin,the relationship between the glacier variation and thedebris flow development is very close. In the carly Holocene, the climate became warm,the glaciers gradually retreated,and formedthe debris flow laver in the lower section of the fourth glaciofluvial terrace(T_4). In the Hypsithermal period of the middle Holocene(7 500-4000a BP),the glacier retreatedstrongly and formed the middle and upper sections of T_4(7500±4000a BP ) including somedebris flow layers.In...

In the Gon gga Mountainous Regioin,the relationship between the glacier variation and thedebris flow development is very close. In the carly Holocene, the climate became warm,the glaciers gradually retreated,and formedthe debris flow laver in the lower section of the fourth glaciofluvial terrace(T_4). In the Hypsithermal period of the middle Holocene(7 500-4000a BP),the glacier retreatedstrongly and formed the middle and upper sections of T_4(7500±4000a BP ) including somedebris flow layers.In the late Holocene,the climate turned into cold and the Neoglaciation can divided into 3stages of the glacier advance:the pre-Guanjingtai glacier advance(>3080±80a BP) , heGuanjingtai glacier advance( 2 35 0±65 1 530±80a BP)and the Hailougou glacier advance(84o±85-78o±90a BP). And also the 3 glaciofluvial-dedris flow terraces are formed respec-tively :T_3 4 000-3000,T_2 3 000-1200 and T_1 1200-750(a BP)。The earliest of the Modern Little Ice Age appeared in 400a BP,and thete were 3 times of Cli- mate waving.Resentily,the climate turned into warm,and the debris flow appeared much more.

贡嘎山区在全新世初期(10000-7500aBP),气候渐暖,冰川后退,泥石流发生频次剧增;中期(7500-4000aBP),出现高温气候,冰川强烈后退,沉积物则以冰水河流相为主;晚期(<4000aBP),气候转冷,出现新冰期。嗣后,气候转暖,但有三次明显的冰进过程;400aBP前,气候再度转冷,出现小冰期。大量的泥石流点是出现在气候转暖、冰川退缩的初始阶段。

The benefical conditions that debris flow is formed in Sanchahe valley along Du-ku highway of Tianshan mountains are frequent rainstorm,exposed rock and high and precipitous land form in alpine region of the drainage basin. Sustained high air temperature in summer can lead to ice-fall of glacier at backwall of the basin.Then,the ice-fall is melted qulkly and results in formation of glacier flood which the debris flow is simulated.Because the conditions mentioned above are still exist,debris flow...

The benefical conditions that debris flow is formed in Sanchahe valley along Du-ku highway of Tianshan mountains are frequent rainstorm,exposed rock and high and precipitous land form in alpine region of the drainage basin. Sustained high air temperature in summer can lead to ice-fall of glacier at backwall of the basin.Then,the ice-fall is melted qulkly and results in formation of glacier flood which the debris flow is simulated.Because the conditions mentioned above are still exist,debris flow at present,is in an active period.

三岔河流域高山带裸露的岩石地表与其35°以上的陡峻地形一同构成了迅速汇流的有利条件;夏季高山带5℃~10℃左右的持续高温天气过程,引起冰舌末端发生冰体崩解或山缘积雪发生雪崩、进入沟道,并在较短时间内融化,形成激发泥石流的冰雪消融洪水。目前,由于提供泥石流的这种水源和沟道内丰富的松散固体物质条件依然具备,所以,泥石流爆发将仍处于活跃发展阶段。

Research results show that the glacier debris flow along the Dushanzi-Korla Highway is insmall scale and has full process of development.The debris flow occurs during June-July everysummer and often destories bridges and blocks the highway.The major water source joining upwith the formation of debris fiow,first of all, is snow meltwater and ice meltwater from theicefalls during the warm summer,and secondly,the flood of storm rain and meltwater. From themass conditions for forming debris flow in 9 gullies...

Research results show that the glacier debris flow along the Dushanzi-Korla Highway is insmall scale and has full process of development.The debris flow occurs during June-July everysummer and often destories bridges and blocks the highway.The major water source joining upwith the formation of debris fiow,first of all, is snow meltwater and ice meltwater from theicefalls during the warm summer,and secondly,the flood of storm rain and meltwater. From themass conditions for forming debris flow in 9 gullies , the mass in the middle and lower reaches iseasier to develop into debris flow than that in the upper reaches.The collapse of rock banks alongthe gully following the debris flow is both main mean that moraine mass develop into debris flowand supplementary pattern of solid mass,Viscous flow by gravity is major debris flow along thehighway;the main way and features of debris flow movement are in viscous and intermittentflow. Observed maximum density of the debris flow is 24.6g /cm ̄2 which is the maximum figureamong all measured data. The glacier debris flow along the highway can be classified into 4types.

对独库公路冰川泥石流的考察及重点泥石流沟的观测,摸清了9条泥石流沟的分布,泥石流发生概况、危害和形成的水文气象条件。以实测资料分析了公路沿线冰川泥石流运动规律基本特征和形成机制。参与泥石流形成的主要水源为融雪水、冰崩和冰川融水,其次是暴雨和冰川融水的叠加所形成的洪水,实测最大容重为2.46g/cm ̄3。

 
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