四川康定折多山末次冰盛期古冰川重建及其气候意义
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杨舒然, 杨玮琳, 韩业松, 杨彦敏, 李梦真, 崔之久, 刘耕年
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Reconstruction of glacial extent of the Zheduoshan Mountains, eastern Qinghai-Tibet Plateau and its climatic implications
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Shuran YANG, Weilin YANG, Yesong HAN, Yanmin YANG, Mengzhen LI, Zhijiu CUI, Gengnian LIU
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表1 贡嘎山冰川地貌特征值测算统计(平均值) (m)
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Table 1 Typical glacial geomorphological characteristic values in the Mt. Gongga (average value)
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| 朝向 | 冰川名称 | h1 | h2 | h3 | h4 | h5 | Ah | At | ELA | THAR |
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| 东坡 | 燕子沟G101841E29650N | 6 172 | 6 154 | 6 033 | 5 963 | 5 908 | 6 046 | 4 564 | 4 900 | 0.23 | | 燕子沟G101848E29664N | 6 256 | 6 192 | 6 172 | 5 963 | 5 945 | 6 106 | 4 413 | 4 900 | 0.29 | | G101863E29687N | 6 256 | 5 956 | 5 945 | 5 721 | 5 424 | 5 860 | 4 146 | 4 900 | 0.44 | | 燕子沟G101865E29627N | 7 484 | 6 594 | 6 144 | 5 980 | 5 951 | 6 431 | 3 729 | 4 900 | 0.43 | | G101866E29741N | 6 265 | 6 066 | 5 903 | 5 840 | 5 474 | 5 910 | 4 323 | 4 900 | 0.36 | | G101898E29758N | 6 499 | 6 265 | 6 123 | 6 077 | 5 515 | 6 096 | 3 482 | 4 900 | 0.54 | | G101914E29718N | 6 521 | 6 253 | 6 077 | 6 057 | 5 895 | 6 161 | 3 973 | 4 900 | 0.42 | | 海螺沟G101916E29584N | 7 484 | 6 620 | 6 531 | 6 323 | 5 951 | 6 582 | 2 974 | 4 900 | 0.53 | | G101919E29653N | 6 871 | 6 842 | 6 787 | 6 733 | 6 621 | 6 771 | 4 144 | 4 900 | 0.29 | | G101924E29792N | 5 840 | 5 685 | 5 608 | 5 359 | 5 353 | 5 569 | 4 716 | 4 900 | 0.22 | | G101927E29546N | 6 306 | 5 873 | 5 864 | 5 809 | 5 798 | 5 930 | 4 195 | 4 900 | 0.41 | | 磨子沟G1101943E29621N | 6 871 | 6 787 | 6 621 | 6 620 | 6 594 | 6 699 | 4 080 | 4 900 | 0.31 | | G101948E29533N | 5 695 | 5 603 | 5 583 | 5 472 | 5 328 | 5 536 | 3 741 | 4 900 | 0.65 | | G101961E29833N | 5 366 | 5 354 | 5 306 | 5 297 | 5 292 | 5 323 | 4 786 | 4 900 | 0.21 | | G101967E29818N | 5 662 | 5 583 | 5 556 | 5 426 | 5 292 | 5 504 | 4 590 | 4 900 | 0.34 | | G101975E29793N | 5 598 | 5 556 | 5 552 | 5 537 | 5 516 | 5 552 | 4 790 | 4 900 | 0.14 | | 西坡 | G101820E29645N | 6 033 | 5 905 | 5 820 | 5 794 | 5 649 | 5 840 | 4 594 | 5 100 | 0.41 | | G101820E29660N | 6 238 | 6 033 | 5 887 | 5 796 | 5 794 | 5 950 | 4 503 | 5 100 | 0.41 | | G101824E29728N | 6 059 | 5 798 | 5 787 | 5 786 | 5 582 | 5 802 | 4 633 | 5 100 | 0.40 | | G101826E29704N | 5 952 | 5 831 | 5 729 | 5 654 | 5 365 | 5 706 | 4 548 | 5 100 | 0.48 | | G101827E29632N | 6 006 | 5 905 | 5 889 | 5 444 | 5 397 | 5 728 | 4 850 | 5 100 | 0.28 | | G101828E29739N | 5 786 | 5 682 | 5 641 | 5 563 | 5 497 | 5 634 | 4 900 | 5 100 | 0.27 | | G101831E29680N | 6 364 | 6 209 | 6 026 | 5 992 | 5 715 | 6 061 | 4 466 | 5 100 | 0.40 | | 小贡巴G101848E29595N | 6 779 | 6 570 | 6 402 | 6 385 | 6 283 | 6 484 | 4 163 | 5 100 | 0.40 | | 大贡巴G101855E29563N | 6 712 | 6 599 | 6 482 | 6 414 | 6 115 | 6 464 | 3 935 | 5 100 | 0.46 | | G101885E29547N | 6 258 | 6 091 | 5 935 | 5 876 | 5 865 | 6 005 | 4 503 | 5 100 | 0.40 | | G101895E29546N | 6 399 | 6 376 | 6 349 | 6 011 | 5 865 | 6 200 | 4 842 | 5 100 | 0.19 | | G101908E29542N | 6 422 | 6 221 | 5 888 | 5 535 | 5 473 | 5 908 | 4 461 | 5 100 | 0.44 | | G101946E29512N | 5 948 | 5 859 | 5 837 | 5 759 | 5 577 | 5 796 | 3 948 | 5 100 | 0.62 | | G101878E29734N | 6 076 | 6 041 | 5 898 | 5 895 | 5 832 | 5 948 | 4 924 | 5 100 | 0.17 | | G101895E29718N | 6 099 | 6 056 | 6 019 | 5 967 | 5 859 | 6 000 | 4 592 | 5 100 | 0.36 | | G101838E29747N | 6 059 | 5 786 | 5 653 | 5 497 | 5 452 | 5 689 | 4 615 | 5 100 | 0.45 | | G101848E29756N | 5 794 | 5 693 | 5 630 | 5 549 | 5 452 | 5 624 | 4 797 | 5 100 | 0.37 | | G101852E29776N | 6 498 | 6 283 | 5 875 | 5 724 | 5 669 | 6 010 | 4 243 | 5 100 | 0.49 | | G101895E29799N | 6 438 | 6 041 | 5 840 | 5 739 | 5 584 | 5 928 | 4 403 | 5 100 | 0.46 | | G101902E29819N | 5 705 | 5 465 | 5 395 | 5 327 | 5 170 | 5 412 | 4 590 | 5 100 | 0.62 | | G101928E29829N | 5 571 | 5 510 | 5 374 | 5 355 | 5 321 | 5 426 | 4 595 | 5 100 | 0.61 | | G101950E29846N | 5 374 | 5 302 | 5 301 | 5 277 | 5 240 | 5 299 | 4 786 | 5 100 | 0.61 | | | | | | | | | | 平均值 | 0.40 |
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