冰川物质平衡

冰川物质平衡及其与冰川特征的关系

Mass balance of glaciers and its relationship with characteristics of glaciers

天山地区冰川物质平衡的突变探测

Abrupt Change Detection of Glacier Mass Balance in the Tianshan Mountains

基于地理信息系统的太阳直接辐射与冰川物质平衡的关系

Potential Direct Solar Radiation Based on GIS and Glacier Mass Balance

高亚洲地区冰川物质平衡变化特征研究

Regional Characteristics of Glacier Mass Balance Variations in High Asia

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

The Relationship Between Glacial Mass Balance Equilibrium Line and Climate

天山冰川物质平衡波动和径流的同步监测

Simultaneous Monitoring of Mass Balance Fluctuations and Runoff of the Tianshan Glaciers

北半球冰川物质平衡变化的若干特征及其气候意义

Variations of Glacier Mass Balance and their climatic implication

北半球冰川物质平衡的突变

Abrupt Changes in Glacier Mass Balance Over Northern Hemisphere

冰川物质平衡的一种简单数学表述法

A Simple Method on Estimating Glacial Mass Balance

冰川物质平衡观测是探究冰川变化及其气候响应机制的桥梁。

Glacier mass balance observation is the bridge to explore the glacier change and its climate response mechanism .

七一冰川物质平衡变化与气候相互关系的初步研究

A Primary Study of the Relationship Between Glacial Mass Balance and Climate in the " July First " Glacier

乌鲁木齐河源冰川物质平衡季节变化和总消融海拔分布

Seasonal Variation of Mass Balance and Altitude Dependency of Total Melt in the Glacierized Source Area of the Urumqi River

过去44年乌鲁木齐河源一号冰川物质平衡结果及其过程研究

Study on Mass Balance and Process of Glacier No.1 at the Headwaters of the Urumqi River in the Past 44 Years

计算了稳定通过T≥0℃的气候积温，其与冰川物质平衡相关性最大。

The climate accumulated temperature of T ≥ 0 ℃ is calculated . Its correlation with glacier mass balance is the best .

冰川物质平衡变化的总趋势由南向北呈现由负平衡向正平衡发展的渐变之势。

For the tendency of mass balance variations , from south to north , mass balance appears to tend from decrease to increase .

同时，结合更多的气候数据探究冰川物质平衡与气候变化关系也是今后重要的研究内容。

Exploring the deep relationship between glacier mass balance and climatic changes combining more climate data will also an important content in the future .

冰川物质平衡是水热等气候因素对冰川综合作用的结果，其动态变化直接影响到冰川规模和径流变化。

The mass balance is the water and heat and other climatic factors combined result of the glacier , the dynamic changes directly affect the size of glacier and runoff changes .

目前对于疏勒河流域的治理和研究主要集中在水资源的开发利用、土地沙漠化、水文气候、冰川物质平衡、动植物多样性研究等几个方面，并取得了阶段性成果。

At present , the control and researches of Shule River Basin mainly concentrate on the aspects of development and utilization of water resources , desertification , hydrology , climate , glacier mass balance and plant and animal diversity , which has already yielded good results .

Lambert冰川流域物质平衡和南极冰盖变化

Mass Balance in the Lambert Glacier Basin and Variability of the Antarctic Ice Sheet

水文气象学方法计算喜马拉雅山北坡冰川流域物质平衡

Computation on the Mass Balance of Glaciers in North Himalaya with a Hydro-meteorological Method

高亚洲冰川系统物质平衡特征及其对全球变化响应研究进展与展望

Progress and Prospects of Mass Balance Characteristic and Responding to Global Change of Glacier System in High Asia

冰川的物质平衡是指一段时间内冰川的收入和支出量。

Glacier mass balance refers to the amount of income and expenditure of the glacier in a period of time .

冰川的物质平衡是联结冰川规模波动与气候变化的关键因子，冰川物质平衡变化是冰川对气候变化的直接反应。

The mass balance changes in glacier is a direct response to the climate change and also is the key factors of linking the climate change .

近期北半球大多数山地冰川的物质平衡为负，冰川普遍退缩，表明北半球气候暖化的趋势。

Most of the mountain glaciers in the Northern Hemisphere are retreating recently because of the negative mass balance , reflecting the warm tendency of the climate change .

北半球50条山地冰川近期的物质平衡状况

On the Mass Balance of 50 Mountain Glaciers in the Northern Hemisphere

山地冰川末端进退变化和冰川物质平衡与全球升温对应较好。

It is a good response between global warming and mass balance in mountain glaciers including glacial advancing and retreating .

近30年来，冰川退缩速度加快，冰川物质平衡有10年左右的波动变化，目前处于负平衡状态。

Over the recent 30 years , the retreating rate of glacier has increased , there is a fluctuation of glacier mass balance with a period of about 10 years . At the present , the glaciers are in negative balance .

本文从对物质平衡的高度结构分析着手，解释了山地冰川波动的原因和机制，引入了物质平衡形成过程多重性这一概念，总结了山地冰川物质平衡的一般规律。

The author tries to interpret the cause and mechanism of fluctuation of alpine glaciers with analysis of altitude structure of glacier mass balance . A new concept is introduced , namely , multiplicity of processes of mass balance .