英语人>词典>汉英 : 冰川 的英文翻译,例句
冰川 的英文翻译、例句

冰川

基本解释 (translations)
glacier  ·  glaciers

词组短语
ice floe
更多网络例句与冰川相关的网络例句 [注:此内容来源于网络,仅供参考]

If a nasty bergschrund is involved, the last step of an alpine approach may be the trickiest.

如果行进路线上有可怕的背隙窿(编译者注:背隙窿是较大的冰川裂缝,一般在冰川的上游可以见到,由于冰川向下流动,断裂的冰川体和上方的冰帽形成巨大的裂缝,下端比上端低很多,形成悬垂的外貌。

This paper analyzes the spatial variability characteristics of the degree-day factors obtained from the observed glaciers of different regions in western China.

本文根据中国西部不同地区数十条冰川的短期考察和观测资料,分析了西部冰川度日因子的空间变化特征,结果表明:由于青藏高原及其周围地区独特的气候和热量条件,西部冰川度日因子具有明显的区域特征。

Predictions for the Indian side are gloomier still. In April a leading Indian glaciologist, Professor Syed Iqbal Hasnain, measured the East Rathong glacier in lofty Sikkim state. It appeared to have shrunk by 2.5km, or half its length, in a decade.

对于印度境内喜马拉雅冰川的预测则更令人悲观。4月,一位资深的印度冰川地质学家, Syed Iqbal Hasnain 教授测量了 Sikkim 省的东 Rathong 冰川,发现在10年的时间内,这段冰川已经萎缩了2500公里,可以说是其长度的一半。

Scientists specialized on glaciology and geomorphology are measuring physical and chemical characteristics and taking samples on the surface of the glacier.

简要说明:波密县的嘎隆拉山季风型海洋性山谷冰川发育,科考队的冰川与地貌工作者在冰川表面作理化测量和采样,这条冰川深入森林以下,冰川表面布满冰碛石。

This paper reviews the processes in glacier hydrological model in term of runoff generation model and runoff concentration model, analyzes the runoff generation mode from two most widely ablation model (the meteorological factors statistical model and the energy balance model), and enlarges on the runoff concentration model from three sub-models: the surface routing sub-model, the englacial hydrology sub-model and the sub-glacial hydrology sub-model.

冰川产流和汇流两个水文物理过程出发,介绍了国内外冰川水文模型的研究进展,对目前应用最广的两类消融模型-基于气象因子的统计模型和基于物理机制的能量平衡模型进行了分析和讨论;从冰川表面、内部以及下部汇流3个方面阐述了冰川汇流模型所取得的成果。

This dissertation mainly discusses glacial -geomorphic process and formative mechanism in modern-glacier areas.

本文着重讨论了现代冰川区的冰川地貌过程,形成机制,从各种冰川遗迹探讨冰川底部的地质地貌作用,了解冰-岩界面的情况,配合对现代冰川的研究建立冰川底部动力模型。

The level of energy exchange is higher in sammer and winter. The sensibility of air temperature to global radiation above the glacial surface is much more low than that in free-glacier areas.

Yr,只有〓为冰川所吸收,冰川表面只有4-10月通过辐射过程吸收能量,其它季节均为支出能量,冰川表面的能量交换水平在盛夏与隆冬季节均较高,冰川表面气温对总辐射通量变化的敏感性比非冰川区要小得多。

Brief Introduction: Mount Muztag lies on the west of the Kunlun Mountains, 75.1°E, 38.5°N. It is the second highest peak of the Kunlun Mountains. Occupying an area of 258 square kilometers and with fault scarps and a relatively smooth top surface, this block mountain developed modern glaciers, the endsof which reach heights from 5020 to 3900 meters. The largest two, the Xili and Kematule Gllaciers, split the mountain body into half transversely. Slopes on west face of the mountain are even, whereas those on north and east faces are quite rugged.

简要说明:慕士塔格峰位于西昆仑山,为昆仑山第二高峰(海拔7509米),位于东经75.1度,北纬38.5度,为有断崖发育的断块山地,顶面较平,现代冰川发育,面积达258平方公里,冰川末端海拔3900~5020米,其中最大的栖力冰川和克麻土勒冰川将山体横切为两半,山峰西边坡势平缓,北边和东边却十分险峻。

Glaciers in accordance with its distribution, shape, size divided into continental glaciers and mountain glaciers, mountain glaciers can also be further divided into cirque glaciers, hanging cirques, valley glaciers, piedmont glaciers such as several types.

冰川根据其分布、形态、规模等分为大陆冰川和山岳冰川,山岳冰川又可进一步分为冰斗冰川、悬冰斗、山谷冰川、山麓冰川等几种类型。

This photo shows the end of the Muztag Glacier. Moraines are on the right of the glacier, with a small glacial lake beyond it. Submerged glacial gravels can be seen clearly.

该照片反映的是木孜塔格冰川的末端,冰川右侧为冰碛物,前下方为小型的冰川湖,冰川沉砾清晰可见。

更多网络解释与冰川相关的网络解释 [注:此内容来源于网络,仅供参考]

barranca:峡谷、冰川或陆架冰的大裂缝

barranca 峡谷;冰川或陆架冰的大裂缝 | barranca 峡谷、冰川或陆架冰的大裂缝 | barranca 峡谷冰川或陆架冰的大裂缝

cirque glacier:冰斗冰川;(冰)斗冰川

冰斗冰川 cwm glacier | 冰斗冰川;(冰)斗冰川 cirque glacier | 冰斗底 cirque floor

cwm glacier:冰斗冰川

冰斗冰川 corrie glacier | 冰斗冰川 cwm glacier | 冰斗冰川;(冰)斗冰川 cirque glacier

esker trough:蛇丘槽,蛇丘谷(冰川地形)

蛇丘脊(冰川地形) esker ridge | 蛇丘槽,蛇丘谷(冰川地形) esker trough | 蛇丘的(冰川) eskerine

esker fan:蛇丘扇(冰川地形)

蛇丘扇(冰川地形) esker fan | 蛇丘丛(冰川地形) esker knobs | 蛇丘湖(冰川地形) esker lake

esker knobs:蛇丘丛(冰川地形)

蛇丘扇(冰川地形) esker fan | 蛇丘丛(冰川地形) esker knobs | 蛇丘湖(冰川地形) esker lake

glacier:冰川

文章作者: 发布时间:2006.12.05 冰川(glacier)是一巨大的流动固体,是在高寒地区由雪再结晶聚积成巨大的冰川冰,因重力这主要因素使冰川冰流动,成为冰川.

mountain glacier:高山冰川; 山岳冰川

motor vehicle emission standard 机动车辆废气排放标准 | mountain glacier 高山冰川; 山岳冰川 | movement document.nbsp 转移文件

outwash plain:冰川沉积平原

冰川沉积 glaposition | 冰川沉积平原 outwash plain | 冰川沉积扇 outwash fan

glacier pothole:冰川壶穴

glacier mill 冰川壶穴 | glacier pothole 冰川壶穴 | glacier recession 冰川后退,冰退