极海洋型冰川是什么冰川——与景才瑞先生商榷

doi:10.7522/j.issn.1000-0240.2017.0327

冰川冻土 ›› 2018, Vol. 40 ›› Issue (1): 1-6.doi: 10.7522/j.issn.1000-0240.2017.0327

极海洋型冰川是什么冰川——与景才瑞先生商榷

李吉均^1,2, 周尚哲³

1. 兰州大学资源环境学院, 甘肃兰州 730000;
2. 南京师范大学地理科学学院, 江苏南京 210023;
3. 华南师范大学地理科学学院, 广东广州 510631

收稿日期:2017-12-05 修回日期:2018-01-11 出版日期:2018-02-25 发布日期:2018-04-13
通讯作者: 周尚哲,E-mail:szzhou@scnu.edu.cn E-mail:szzhou@scnu.edu.cn
作者简介:李吉均(1933-),男,四川彭县人,教授,中国科学院院士,地理与地貌学家,冰川学家,主要从事冰川学、地貌学、第四纪以及干旱区人地关系等方面的研究工作.E-mail:Lijj@lzb.ac.cn
基金资助:
国家自然科学基金重点项目（41330745；41171014）资助

What glacier is the “ultra-maritime glacier”? A discussion with Professor Jing Cairui

LI Jijun^1,2, ZHOU Shangzhe³

1. College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China;
2. School of Geography Science, Nanjing Normal University, Nanjing 210023, China;
3. School of Geographic Science, South China Normal University, Guangzhou 510631, China

Received:2017-12-05 Revised:2018-01-11 Online:2018-02-25 Published:2018-04-13

摘要/Abstract

摘要： 施雅风和谢自楚曾将中国现代冰川分为极大陆型冰川、亚大陆型冰川和海洋型冰川。这个分类方案因符合中国现代冰川的基本特征而得到广泛承认与应用。近年，景才瑞提出“极海洋型冰川”的概念，示意第四纪冰期时中国东部中低山地既然不存在基本的冰川类型，则可能存在一种比海洋型冰川更加高温湿润的特殊冰川。本文认为，这样类型的冰川是不存在的。海洋型冰川已经涵盖了处于融点冰温的临界冰川，即使再多的降水，也不能在正温条件下演变成冰川。故“极海洋型冰川”的概念是不能成立的。第四纪环境研究表明，冰期时大陆架广泛出露，西伯利亚-蒙古高压强迫下的冬季风加强，中国东部气候是朝着更加干旱的方向变化的，其海洋型特征也要大大降低。

关键词: “极海洋型冰川”, 冰川分类问题, 干旱的冰期气候

Abstract: Shi Yafeng and Xie Zichu have classified the contemporary glaciers of China into ultra-continental glacier, sub-continental glacier and maritime glacier. This classification has been widely accepted and applied because it accords with the essential characteristics of Chinese glaciers. Recently, Professor Jing Cairui proposes a new term, "ultra-maritime glacier", to support the hypothesis of glaciations of the East China, meaning that even if the regular glaciers were not present on the middle-lower mountains in East China during Quaternary, there would existed a special kind of glaciers that were more warm and more humid than maritime glaciers. It is difficult to think such glacier is present in the world, because the term "maritime glaciers" contains all the glaciers with 0℃ temperate ice and it is impossible for water to crystallize into glacial ice under the temperature higher than 0℃ even more precipitation. So the concept "ultra-maritime glacier" is invalid. In addition, a lot of studies on Quaternary environment have indicated that in ice ages, continental shelf exposed extensively, the winter monsoon was dominant forced by the intensified Siberia-Mongolia high pressure. So the climate shifted to drier and the maritime climate was weakened during ice ages in the East China.

Key words: “ultra-maritime glacier”, glacial classification, dried climate in ice ages

中图分类号:

P343.6

李吉均, 周尚哲. 极海洋型冰川是什么冰川——与景才瑞先生商榷[J]. 冰川冻土, 2018, 40(1): 1-6.

LI Jijun, ZHOU Shangzhe. What glacier is the “ultra-maritime glacier”? A discussion with Professor Jing Cairui[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2018, 40(1): 1-6.

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极海洋型冰川是什么冰川——与景才瑞先生商榷

What glacier is the “ultra-maritime glacier”? A discussion with Professor Jing Cairui

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