Acta Geographica Sinica ›› 2014, Vol. 69 ›› Issue (7): 958-968.doi: 10.11821/dlxb201407008
• Orginal Article • Previous Articles Next Articles
Wei ZHANG1(), Beibei LIU1(
), Zhijiu CUI2, Yangyang LI1, Liang LIU1
Received:
2014-01-16
Revised:
2014-05-19
Online:
2014-07-20
Published:
2014-07-20
Supported by:
Wei ZHANG, Beibei LIU, Zhijiu CUI, Yangyang LI, Liang LIU. Theoretical glacial equilibrium line altitudes and their influencing factors in the typical mountains of China[J].Acta Geographica Sinica, 2014, 69(7): 958-968.
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Tab. 1
The altitude, summer temperature and precipitation at ELAs using different methods
方法 | MPC | MPF | WPF | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
山体 | 地理 坐标 (N,E) | 气象站高度 (m) | 气象站6-8月气温(oC) | 气象站年降水 (mm) | 实际平衡线高度(m) | 冰川平衡线高度(m) | 气温 (oC) | 降水 (mm) | 冰川平衡线高度(m) | 气温 (oC) | 降水 (mm) | 冰川平衡线高度(m) | 气温 (oC) | 降水 (mm) | 气象资料来源 |
阿尔泰山 | 47°, 88° | 1900 | 11.9 | 664 | 3320 | 3688 | 1.17 | 689 | 3750 | 0.8 | 689 | 3873 | 0.06 | 664 | [35] |
天山 | 43°, 86° | 3539 | 4.3 | 454 | 4056 | 4239 | 0.1 | 454 | 4294 | -0.23 | 454 | 4365 | -0.66 | 454 | [36] |
长白山 | 42°, 128° | 2624 | 6.9 | 1340 | 3290 | 2.9 | 1340 | 3364 | 2.46 | 1340 | 3407 | 2.2 | 1340 | [1] | |
贺兰山 | 38°, 106° | 2901 | 10.6 | 430.2 | 4654 | 0.08 | 430.2 | 4727 | -0.36 | 430 | 4791 | -0.74 | 430.2 | [37] | |
玛雅雪山 | 37°, 102° | 3045 | 10.3 | 355.4 | 4856 | -0.57 | 355.4 | 4900 | -0.83 | 355 | 4928 | -1 | 355.4 | [23] | |
泰山 | 117°, 36° | 1534 | 16.8 | 1132 | 3867 | 2.8 | 1267 | 3949 | 2.31 | 1267 | 4072 | 1.57 | 1132 | [1] | |
马衔山 | 36°, 103° | 1800 | 19 | 494.8 | 4883 | 0.5 | 536.8 | 4935 | 0.19 | 537 | 5050 | -0.5 | 494.8 | [38] | |
太白山 | 34°, 107° | 1543 | 19.3 | 752.6 | 4451 | 1.85 | 876 | 4526 | 1.4 | 876 | 4700 | 0.36 | 752.6 | [39] | |
五台山 | 113°, 39° | 2898 | 9.5 | 828.5 | 4198 | 1.7 | 828.5 | 4271 | 1.26 | 829 | 4380 | 0.61 | 828.5 | [40] | |
黄山 | 118°, 30° | 1840 | 16.6 | 2394 | 3906 | 4.2 | 2461 | 3946 | 3.96 | 2461 | 3756 | 5.1 | 2394 | [1] | |
白马雪山 | 28°, 99° | 4292 | 5.1 | 807.1 | 4800 | 4867 | 1.65 | 807.1 | 4942 | 1.2 | 807 | 5054 | 0.53 | 807.1 | [34] |
千湖山 | 27°, 99° | 3276 | 12.9 | 849.8 | 5134 | 1.75 | 849.8 | 5206 | 1.32 | 850 | 5312 | 0.68 | 849.8 | [41、42] | |
玉龙雪山 | 27°, 100° | 2393 | 17.7 | 950 | 4800 | 5026 | 1.9 | 950 | 5076 | 1.6 | 950 | 5176 | 1 | 950 | [43] |
螺髻山 | 27°, 102° | 2640 | 15.8 | 956 | 4940 | 2.0 | 956 | 5005 | 1.61 | 956 | 5103 | 1.02 | 956 | * | |
点苍山 | 100°, 26° | 1990 | 19.8 | 1054 | 4905 | 2.31 | 1054 | 4980 | 1.86 | 1054 | 5068 | 1.33 | 1054 | [41] | |
拱王山 | 26°, 103° | 3900 | 6.8 | 1570 | 4488 | 3.27 | 1570 | 4558 | 2.85 | 4558 | 4553 | 2.88 | 1570 | [44] | |
台湾玉山 | 23°, 120° | 3845 | 7.4 | 3054 | 4361 | 4.3 | 3054 | 4328 | 4.5 | 3054 | 3953 | 6.75 | 3054 | [14] |
Tab. 2
Meteorological data of different meteorological stations and modern theory ELAs using WPF
观测站 | 海拔 (m) | 年降水量 (mm) | 夏季气温 (oC) | 现代理论平衡线处气温值 (oC) | 夏季气温递减率 (oC/100m) | 现代理论平衡线高程 (m) |
---|---|---|---|---|---|---|
奔子栏 | 2050 | 285.6 | 23.7 | -1.3 | 0.75 | 5378 |
东竹林 | 2988 | 532.8 | 16.5 | -0.4 | 0.78 | 5152 |
122道班 | 3760 | 946.1 | 10.0 | 1.0 | 0.75 | 4961 |
白马雪山垭口 | 4292 | 807.1 | 5.1 | 0.5 | 0.76 | 4893 |
飞来寺 | 3485 | 513.8 | 11.3 | -0.4 | 0.72 | 5117 |
向阳坡 | 2747 | 410.6 | 17.4 | -0.8 | 0.69 | 5386 |
日嘴 | 2080 | 425.0 | 21.7 | -0.8 | 0.69 | 5335 |
布尔津 | 474 | 117.4 | 22.5 | -1.9 | 0.59 | 4609 |
哈巴河 | 533 | 172.0 | 21.6 | -1.7 | 0.59 | 4479 |
阿勒泰 | 735 | 174.0 | 21.2 | -1.7 | 0.59 | 4611 |
富蕴 | 803 | 157.7 | 22.8 | -1.7 | 0.59 | 4962 |
青河 | 1218 | 158.9 | 18.6 | -1.7 | 0.59 | 4663 |
森塔斯 | 1900 | 664.0 | 11.9 | 0.1 | 0.59 | 3907 |
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