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A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China

叶佰生 陈克恭

叶佰生, 陈克恭. A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China[J]. 中国地理科学, 1997, 7(3): 243-250.
引用本文: 叶佰生, 陈克恭. A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China[J]. 中国地理科学, 1997, 7(3): 243-250.
Ye Baisheng, Chen Kegong. A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China[J]. Chinese Geographical Science, 1997, 7(3): 243-250.
Citation: Ye Baisheng, Chen Kegong. A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China[J]. Chinese Geographical Science, 1997, 7(3): 243-250.

A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China

基金项目: The project supported by the National Natural Science Foundation of China

A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China

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出版历程
  • 收稿日期:  1997-01-08
  • 刊出日期:  1997-09-20

A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China

    基金项目:  The project supported by the National Natural Science Foundation of China

摘要: This paper presents a dynamic glacier model that simulates the processes in response of Glacier No. 1 in headwaters of the Urumqi River to various future climatic scenarios The results indicate that the Glader No. 1 will continue retreating if current climatic conditions prevail, until it reaches an equilibrium state of 1600 m in length after 700 to 800 years. If air temperature raise 1℃, the glacier would become a hanging glacier with a length of 300 m after 700 to 800 years. Due to its retreat, cooling function of the glacier would be weakened, resulting in the air temperature in glaciated area higher than that in ice-free areas. The results also indicate that the current glacier melt runoff is in higher value period in comparison with the runoff in the equilibrium state under the current climatic condition. If the air temperature continues increasing, however, the runoff would still increase to a new peak and then decrease rapidly.

English Abstract

叶佰生, 陈克恭. A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China[J]. 中国地理科学, 1997, 7(3): 243-250.
引用本文: 叶佰生, 陈克恭. A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China[J]. 中国地理科学, 1997, 7(3): 243-250.
Ye Baisheng, Chen Kegong. A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China[J]. Chinese Geographical Science, 1997, 7(3): 243-250.
Citation: Ye Baisheng, Chen Kegong. A MODEL SIMULATING THE PROCESSES IN RESPONSES OF GLACIER AND RUNOFF TO CLIMATIC CHANGE─A Case Study of Glacier No. 1 in the ürümqi River, China[J]. Chinese Geographical Science, 1997, 7(3): 243-250.

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