永久冻土
北半球
地质学
冰层
自然地理学
北极的
仰角(弹道)
纬度
气候学
海冰
海洋学
地理
大地测量学
几何学
数学
作者
Tingjun Zhang,Roger G. Barry,K. Knowles,J A Heginbottom,Jerry Brown
出处
期刊:Polar Geography
[Taylor & Francis]
日期:1999-04-01
卷期号:23 (2): 132-154
被引量:487
标识
DOI:10.1080/10889379909377670
摘要
Abstract The recently published digital version of the International Permafrost Association (IPA) Circum‐Arctic Map of Permafrost and Ground Ice Conditions (the IPA map), together with ancillary data sets of the global land cover characteristics data base and the Global Land One‐kilometer Base Elevation data base, are used to investigate the distribution of permafrost and ground ice in the Northern Hemisphere. Our study indicates that permafrost underlies approximately 22.79 × 106 km2 or 23.9% of the exposed land area of the Northern Hemisphere. Permafrost extends from 26°N in the Himalayas to 84°N in northern Greenland. Approximately 70% of the permafrost is distributed between 45°N and 67°N. Generally, permafrost with high ice content (>20% by volume) and relatively thick overburden cover (>5 to 10 m) is found at high latitudes, representing approximately 8.57% of the total permafrost area, or 2.02% of the exposed land area of the Northern Hemisphere. Permafrost with low ice content (<10% by volume with either thick or thin overburden cover) occurs mainly in mountainous regions and high plateaus, representing approximately 66.5% of the total permafrost area or 15.8% of the exposed land area. Approximately 62% of the permafrost of the Northern Hemisphere is found below 500 m a.s.l. and about 10% occurs above 3000 m a.s.l. Based on the IPA map categories, the estimated volume of ground ice in the Northern Hemisphere is between 5.63 and 15.12 × 103 km3, corresponding to ∼2–4 cm sea level equivalent. Based on alternative assumptions, the volume of ground ice may be between 11.37 and 36.55 × 103 km3, which corresponds to 3–10 cm sea‐level equivalent. Notes We acknowledge with gratitude the major contributions of E. S. Melnikov and his staff, previously at VSEGINGEO and presently at the Russian Academy of Sciences, Earth Cryosphere Institute, Moscow, Russia, in the compilation of the original, printed version of the IPA Circum‐Arctic Map of Permafrost and Ground‐ice Conditions. We wish to express our appreciation to the two reviewers for their very constructive comments and suggestions. This research was funded by the U.S. National Science Foundation through the NSF OPP‐9614557 and NSF OPP 9907541 and by the Wang Kuancheng Foundation through the Natural Science Foundation of China. The U.S. National Science Foundation also supported many aspects of map production and digitization through a grant to the American Geophysical Union. The development of the EASE‐grid versions of the maps was supported by the National Snow and Ice Data Center (NSIDC) Distributed Active Archive Centers (DAAC) at the University of Colorado at Boulder. Financial support does not constitute an endorsement of the views expressed in this article.
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