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Continuous and Discontinuous Permafrost in Central Asia/Mongolia
Entry ID:
ggd28
Summary
Abstract:
This data set consists of permafrost measurements taken in Central Asia and Mongolia during the summer seasons of 1974, 1977, and 1978. The study regions have a cold continental climate that is favorable for the development of continuous permafrost in the upper altitudes, and discontinuous permafrost in the lower altitudes which are exposed to the south. The Mongolian mountain areas near the southern boundary of permafrost are shaped by cryogenic processes, forming cryoplanation terraces, active solifluction valleys, cryopediments and solifluction cirques.
Geographic Coverage
(Click for Interactive Map)
Spatial coordinates
Data Set Citation
Dataset Originator/Creator:
Kazimierz Pekala
Dataset Title:
Continuous and Discontinuous Permafrost in Central Asia/Mongolia
Dataset Publisher:
National Snow and Ice Data Center (NSIDC)
Online Resource:
http://nsidc.org/data/ggd28.html
Temporal Coverage
Start Date:
1974-01-01
Stop Date:
1978-12-31
Location Keywords
ISO Topic Category
Platform
Ancillary Keywords
Data Center
Personnel
Role:
INVESTIGATOR
Phone:
48-81-375-915
Fax:
48-81-375-102
Email:
geomorf at biotop.umcs.lublin.pl
Contact Address:
University of Maria Curie-Sklodowska
Department of Geomorphology
ul. Akademicka 19
City:
Lublin
Postal Code:
20-033
Country:
Poland
Publications/References
Dzulynski, S., Pekala, K. 1980. Bog cirques and solifluction valley in granitic rocks. Z. f. Geomorphologie N.F. 24(2), p. 219-235. (in English) Pekala, K. 1975. Contemporary morphogenetic processes in the Sant Valley. Bull. Acad. Pol. Sci. Ser. Sci. Terre 23(3-4), p. 221-224 (in English). Pekala, K. 1977/1978. Cryoplanation terraces in the area of the southern Khangai, Mongolia. Annales ...
![]() Creation and Review Dates
Last DIF Revision Date:
2010-12-28
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