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冰川
glacier
DISCUSSION ON SOME HYDROLOGICAL FEATURES OF THE BATURA GLACIER, KARAKORAM 喀喇昆仑山巴托拉冰川水文某些特征的探讨 短句来源 PROGRESS AND PROBLEMS OF GLACIER INVENTORY IN CHINA 中国冰川目录的进展与问题 短句来源 ANALYSIS OF TRACE ELEMENTS IN SNOW AND ICE ON THE HANS GLACIER OF MT.YOUYI IN ALTAY MOUNTAINS 阿尔泰山友谊峰哈拉斯冰川冰雪痕量元素分析 短句来源 Observation on the Changes of the Batura Glacier Terminus in 1980 1980年巴托拉冰川末端变化的观测 短句来源 Relations Between Meteorological Conditions and Mass Balance of a Glacier on the North Slope of Mt. Bogda, Tian Shan 天山博格达峰北坡气象条件与冰川物质平衡的关系(英文) 短句来源 更多 glaciers
Structural Observations of the Glaciers on the North Slope of Mt. Bogda, Tian Shan 天山博格达北坡冰川结构观测(英文) 短句来源 Preliminary Study of the Rock Glaciers in the Gongga Mt. Area 贡嘎山山地石冰川的初步研究 短句来源 A Numerical Classification of Glaciers by Means of Specific Relief Parameters 特征地形参数的冰川数值分类法(英文) 短句来源 A Study of Relationship Between Climate and Mountain Glaciers 冰川与气候关系的研究 短句来源 Cause and Mechanism of Fluctuation of Alpine Glaciers 山地冰川波动的原因和机制 短句来源 更多 glaciation
A View on Quaternary Glaciation in Lushan from the Results of Some Modern Glacial Researches 从我国现代冰川研究的一些结果看庐山第四纪冰川问题 短句来源 On Advancement in Study of Quaternary Glaciation in Recent 20 Years 近20年来中国第四纪冰川研究的进展 短句来源 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 Review and Prospects of Quaternary Glaciation Research in China 中国第四纪冰川研究的回顾与展望 短句来源 THE EFFECT OF THE NEOPROTEROZOIC GLOBAL GLACIATION ON THE EARLY BIOLOGICAL EVOLUTION 新元古代全球冰川事件对早期生物演化的影响 短句来源 更多 glacial
A View on Quaternary Glaciation in Lushan from the Results of Some Modern Glacial Researches 从我国现代冰川研究的一些结果看庐山第四纪冰川问题 短句来源 The Glacial Resources and Their Distributive Characteristics in the Tianshan Mountains of China 中国天山冰川资源及其分布特征 短句来源 The Relationship Between Glacial Mass Balance Equilibrium Line and Climate 冰川物质平衡、零平线及气候间的关系——以天山乌鲁木齐河源1号冰川为例 短句来源 Glaciations and Glacial Landforms in Finland 芬兰的冰川作用与冰川地貌(英文) 短句来源 New Achievements of Studies on the Deposits of Moraine and Glacial Debris Flow 冰碛与冰川泥石流堆积研究的若干新成果 短句来源 更多 
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Microorganisms Found in the Basal Horizons of the Antarctic Glacier above Lake Vostok
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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].
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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.
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Here we examine the nonstationary response of a glacier to small deviations of the system parameters from critical values corresponding to the stationary state.
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Numerical investigation and self-similar solutions of the glacier-ocean interaction problem
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The distribution of Abies was deeply influenced by geological events such as the uplift of Himalaya, the Alps, the Rocky Mountains, the occurrence of the Asian Monsoon as well as the Quaternary glaciers.
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The problem of stationary inner heating of cold glaciers is considered in [1, 2].
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The mathematical modeling of the heat and mass transfer processes in glaciers is an effective means of investigating and predicting their development.
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The Pechora till formed in the course of motions of glaciers from the northeast.
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The advances and retreats of glaciers and the accompanying regressions and transgressions of the ocean level caused isolation of chum salmon in the refugia belonging hypothetically to the paleo-Shuifen and paleo-Amur regions.
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These data suggest that the subspecies has been rapidly spreading northwards since the Pleistocene glaciation (about 15,000 years ago).
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In our view, microgeographic subdivision of the populations is caused by recurrent fragmentation of habitats during the Pleistocene glaciation of the Bale Massif and subsequent prolonged isolation of local populations.
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The types of mtDNA genetic variability and mismatch distribution between haplotypes in the populations indicate that the southern regions of the Sea of Okhotsk and Sea of Japan served as refugia for chum salmon during glaciation periods.
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Differences between the seasonal races of the Amur chum salmon are insignificant, and their emergence dates back to the period of the last Wisconsinian glaciation.
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Chromosomal inversion polymorphism was studied in a natural population of Drosophila subobscura from the Djerdap gorge of the Danube River, which is one of southeastern European continental refugia during the last glaciation period.
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These corresponding chalcones were reacted with phenyl hydrazide in glacial acetic acid, which led to the formation of novel 4-[5-(substituted phenyl)-1-phenyl-4,5-dihydro-1H-3-pyrazolyl]-2-methylphenol derivatives.
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15 m/ka occurred in the mono-depositional sink of the former Changjiang River mouth during 10 000-8000 aBP, when post-glacial transgression happened and the Changjiang water level remained at lower stand.
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The Role of Glacial Epochs in the Formation of Chromosomal Polymorphism in the Common Shrew Sorex araneus L.
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Lemmings of Bolshevik Island (the Severnaya Zemlya Archipelago) is a Relict of the Last Glacial Epoch
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A procedure for the determination of sodium salts of methyl sulfamic acid as tertiary amines by acidimétrie titration in glacial acetic acid was developed.
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Firn stratigraphic studies of glaciers in the eastern Tian Shan were carried out during the summer of 1981. 1981年夏天对东天山冰川进行了粒雪层研究。 本文系通过对从冰川上取得的雪-冰岩芯进行分析来解释长期气候变化的初步研究。粒雪岩芯取自博格达峰北坡D-4冰川和乌鲁木齐河源1号冰川西支,深度为表面以下2—6米,工具为手摇钻。 对冰雪样品进行了地层学描述和物理性质测量,还做了氧同位素含量分析。应用这些资料,试图就年层的估算和附加冰的形成给予地层学解释。在D-4冰川几个不同点上,发现年净平衡的在1000毫米附近变动,和以前在邻近冰川区得到的降水量相比是一个意外的值。 用花杆法在D-4冰川上测量了物质平衡,发现在最暖季节,该冰川的物质平衡与海拔高度之间具有线性关系。 文摘来源 On glaciers in the eastern Tianshan Mountains, separate measurements of amounts of accumulation and abation are difficult, since accumulation and ablation occur simultaneously in the warm season. To estimate accumulation and ablation independently, meteorological observations around Glacier D-5 were made in summer. In comparison with air temperature on the ground, much lowering of that and smaller diurnal range were seen on the glacier. From the analysis of upper weather charts, the main cause of precipitat... 在东天山冰川上,积累和消融是在暖季同时发生的,故分别对积累量和消融量的测量是困难的。为了单独估算积累和消融,夏天我们在D-5冰川附近进行了气象观测。与地面气温相比较,发现冰川上气温比较低,且具有较小的日变化幅度。由高空天气图的分析可知,降水的主要原因可归结于来自极地的冷槽。固态降水发生的频数(S:%)和地面气温(T:℃)之间的关系对冰川积累很重要,这种关系(S=25T+108)可由观测结果得到。消融(a:厘米水层)和日积温(∑T:日平均气温之和,℃·日)也可由关系式(a=1.5∑T)得到。通过这些关系的应用,我们可以估算冰川上积累、消融和物质平衡。除冰川为具有高反射率的新雪所覆盖面外,计算的物质平衡和观测结果很吻合,气象条件和物质平衡与尼伯尔喜马拉雅山冰川进行了简要的比较。 文摘来源 Preliminary structural glaciological studies of the glaciers on the north slope, of Mt. Bogda were carried out during July-August, 1981. 1981年7月至8月,我们对博格达北坡冰川进行了初步的结构冰川学研究。 结构要素,诸如沉积和动力结构以及冰川波动所造成的结构,分别在4号和5号冰川的表面做了观测,并绘制了这两条冰川的结构图。 4号冰川结构简单,而5号冰川则比较复杂。我们对5号冰川的内部结构分类做了尝试。 观测了这两条冰川的冰面运动和冰层中岩屑的产生。测量了5号冰川表面变形和末端位置的变化。该冰川平均日变化速度5—10厘米,从1981年的8月初到9月初其末端后退约1—3米。 文摘来源 << 更多相关文摘 
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