Permafrost dynamics in the north-east of European Russia at the end of the 20th century

Norsk Geografisk Tidsskrift

Volumn 55, Issue 4, 2001, Pages 241-244

  Oberman, N G ^a   Mazhitova, G G ^b  

^a Komi Territorial Center   (Russian Federation)

^b INSTITUTE OF BIOLOGY   (Russian Federation)

Author keywords

Monitoring; Natural climate warming; North East of European Russia; Permafrost

Indexed keywords

MOUNTAIN ENVIRONMENT; PERMAFROST; TEMPERATURE; WARMING;

RUSSIAN FEDERATION;

EID: 0035677324     PISSN: 00291951     EISSN: None     Source Type: Journal    
DOI: 10.1080/00291950152746595     Document Type: Article

References (11)

1. Degradation of the cryolithozone of Russia under global climatic warming
2. Monitoring of the active/seasonally frozen layer and upper layers of cryolithozone during the ongoing half-century climatic cycle in the European Northeast of Russia
3. Transient climate response to increasing sulfate aerosols and greenhouse gases
4. Geocryological specificity and current trends in natural and anthropogenic dynamics of the cryolithozone of the East-European Subarctic
5. Features of manifestation of intra-age rhythm of the characteristics of an active layer and layer of annual temperature fluctuations in main periglacial landscapes of the European Northeast of Russia
6. Monitoring of ground waters of the cryolithozone in the European part of Russia and the Urals
7. Evidence for a cyclic variation of permafrost temperature in Northern Alaska
8. Geocryological-climatic monitoring in Russia: Methodology, results and forecast
9. Long-term changes of soil temperature regime in Central Yakutia