云量对祁连山老虎沟12号冰川表面能量平衡的影响
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邹小伟, 孙维君, 杨堤益, 王英珊, 李延召, 晋子振, 杜文涛, 秦翔
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Effect of cloud on surface energy balance of Laohugou Glacier No. 12, Qilian Mountains
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Xiaowei ZOU, Weijun SUN, Diyi YANG, Yingshan WANG, Yanzhao LI, Zizhen JIN, Wentao DU, Xiang QIN
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表4 全球不同类型冰川/盖表面能量平衡对比
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Table 4 Comparison of surface energy balance between different types of glaciers/ice sheet
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冰川、冰盖名称 | 海拔/m a.s.l. | S/(W⋅m-2) | L/(W⋅m-2) | H/(W⋅m-2) | LE/(W⋅m-2) | G/(W⋅m-2) | Qm/(W⋅m-2) |
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Laohugou No.12 | 4 550 | 82(92%) | -54(61%) | 7(8%) | -7(8%) | 0 | -27(31%) | Storbreen | 1 570 | 38(67%) | -20(35%) | 15(26%) | 1(2%) | 3(5%) | -37(65%) | Midtdalsbreen | 1 450 | 50(61%) | -25(31%) | 24(30%) | 4(5%) | 3(4%) | -56(69%) | S5 | 490 | 45(53%) | -39(46%) | 38(45%) | -4(5%) | 2(2%) | -41(49%) | S6 | 1 020 | 36(55%) | -42(66%) | 26(40%) | -2(3%) | 3(5%) | -20(31%) | Zhadang | 5 665 | 73(83%) | -56(69%) | 13(15%) | -11(14%) | 2(2%) | -14(17%) | Parlung No.4 | 4 800 | 78(81%) | -49(55%) | 16(17%) | -10(11%) | 2(2%) | -30(34%) | PANDA-N | 2 579 | 20(40%) | -49(98%) | 26(52%) | -1(2%) | 4(8%) | 0 | Panda-1 | 2 737 | 29(67%) | -39(87%) | 12(30%) | 2(5%) | -5(11%) | 0 |
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