V E Ostroumov
Biographic Data
| ID | 5810830 |
|---|---|
| NAME | V E Ostroumov |
| GIVEN NAMES | V E |
| FAMILY NAME | Ostroumov |
| SIGNATURE | OSTROUMOV V E |
| AFFILIATIONS | Institute of Physical-Chemical and Biological Problems in Soil Science |
| ORCID | 0000-0002-6127-4203 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1996 |
| LATEST PUBLICATION YEAR | 2019 |
| H-INDEX | 0 |
Two decades of active layer thickness monitoring in northeastern Asia
This study summarizes seasonal thawing data collected in different permafrost regions of northeast Asia over the 1995–2018 period. Empirical observations were undertaken under the Circumpolar Active Layer Monitoring (CALM) program at a range of sites across the permafrost landscapes of the Yana-Indigirka and Kolyma lowlands and the Chukotka Peninsula, and supplemented with 10 years of observations from volcanic mountainous areas of the Kamchatka …
Spatial and Temporal Observations of Seasonal Thaw in the Northern Kolyma Lowland
Observations carried out in 1996-2002 in the northern part of the Kolyma Lowland reveal spatial and temporal regularities in the seasonal thawing of tundra and northern taiga soils. The main factor determining differences in active-layer thickness in zonal tundra landscapes is the texture (mechanical composition) of soil parent material. Summer thaw in sandy soils is 2-3 times deeper than in loamy soils. The distribution of maximum seasonal thaw …
Effect of Permafrost and Palaeo-Environmental History on Soil Formation in the lower Kolyma Lowland, Siberia
Danish Journal of Geography 96: 40–50, 1996. The Geography of soils has been studied in the tundra of the sandy Kolyma Lowland between latitudes 69 ° and 70 ° N. Generally, soils show characteristics indicative of variable intensity of previous fossil Podzol formation in the present day cryoturbated active layer. Hence, the transformation, transfer and segregation of chemical substances in the soil profile can be interpreted as evidence of palaeo…
No prominent works on this page.
Effect of Permafrost and Palaeo-Environmental History on Soil Formation in the lower Kolyma Lowland, Siberia
Danish Journal of Geography 96: 40–50, 1996. The Geography of soils has been studied in the tundra of the sandy Kolyma Lowland between latitudes 69 ° and 70 ° N. Generally, soils show characteristics indicative of variable intensity of previous fossil Podzol formation in the present day cryoturbated active layer. Hence, the transformation, transfer and segregation of chemical substances in the soil profile can be interpreted as evidence of palaeo…
Spatial and Temporal Observations of Seasonal Thaw in the Northern Kolyma Lowland
Observations carried out in 1996-2002 in the northern part of the Kolyma Lowland reveal spatial and temporal regularities in the seasonal thawing of tundra and northern taiga soils. The main factor determining differences in active-layer thickness in zonal tundra landscapes is the texture (mechanical composition) of soil parent material. Summer thaw in sandy soils is 2-3 times deeper than in loamy soils. The distribution of maximum seasonal thaw …
Two decades of active layer thickness monitoring in northeastern Asia
This study summarizes seasonal thawing data collected in different permafrost regions of northeast Asia over the 1995–2018 period. Empirical observations were undertaken under the Circumpolar Active Layer Monitoring (CALM) program at a range of sites across the permafrost landscapes of the Yana-Indigirka and Kolyma lowlands and the Chukotka Peninsula, and supplemented with 10 years of observations from volcanic mountainous areas of the Kamchatka …
Climate change and permafrost (3 works) · Geography (3 works) · Geology (3 works) · Oceanography (3 works) · Permafrost (3 works) · Physical geography (3 works) · Arctic (2 works) · Bog (2 works) · Ecology (2 works) · Geochemistry (2 works)