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Record #173439:

Spatial and temporal observations of seasonal thaw in the Northern Kolyma Lowland / D.G. Fyodorov-Davydov, and 8 others.

Title: Spatial and temporal observations of seasonal thaw in the Northern Kolyma Lowland / D.G. Fyodorov-Davydov, and 8 others.
Author(s): Fyodorov-Davydov, D. G.
Date: 2004.
In: Polar Geography. (2004.), Vol. 28(4) (2004)
Abstract: Discusses first results of regional-scale analysis of active layer in Kolyma Lowland. Carried out in 1996-2002, these reveal spatial and temporal regularities in seasonal thawing of tundra and northern taiga soils. Presents air temperature and precipitation data and field observations of seasonal thaw depths. Compares mean active-layer thickness (ALT) in different landscape types. Examines correlations between ALT and climatic parameters. Finds texture (mechanical composition) of soil parent material is main factor determining differences in ALT in zonal tundra landscapes. Summer thaw in sandy soils is 2-3 times deeper than in loamy soils.
Notes:

Polar Geography. Vol. 28(4) :308-325 (2004).

In special issue Eurasian Contributions from the Circumpolar Active Layer Monitoring (CALM) Workshop.

Keywords: 551.34 -- Geocryology. Frozen ground.
551.345 -- Permafrost. Cryopedology.
551.58 -- Climatology.
551.345.1 -- Permafrost, surveys.
551.524 -- Air temperature.
551.578 -- Precipitation, particular forms.
536.421.1 -- Melting.
631.43 -- Soils, physical and mechanical properties.
581.524.444.3 -- Tayga.
581.524.444.2 -- Tundra.
E8 -- Glaciology: frost action and permafrost.
(*501) -- Russia (Federation).
(*531.3) -- Yakutiya. Respublika Sakha.
SPRI record no.: 173439

MARCXML

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100 1# ‡aFyodorov-Davydov, D. G.
245 10 ‡aSpatial and temporal observations of seasonal thaw in the Northern Kolyma Lowland /‡cD.G. Fyodorov-Davydov, and 8 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2004.
300 ## ‡ap. 308-325 :‡bill., diags., tables.
500 ## ‡aPolar Geography. Vol. 28(4) :308-325 (2004).
500 ## ‡aIn special issue Eurasian Contributions from the Circumpolar Active Layer Monitoring (CALM) Workshop.
520 3# ‡aDiscusses first results of regional-scale analysis of active layer in Kolyma Lowland. Carried out in 1996-2002, these reveal spatial and temporal regularities in seasonal thawing of tundra and northern taiga soils. Presents air temperature and precipitation data and field observations of seasonal thaw depths. Compares mean active-layer thickness (ALT) in different landscape types. Examines correlations between ALT and climatic parameters. Finds texture (mechanical composition) of soil parent material is main factor determining differences in ALT in zonal tundra landscapes. Summer thaw in sandy soils is 2-3 times deeper than in loamy soils.
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.345.1 -- Permafrost, surveys.‡2udc
650 07 ‡a551.524 -- Air temperature.‡2udc
650 07 ‡a551.578 -- Precipitation, particular forms.‡2udc
650 07 ‡a536.421.1 -- Melting.‡2udc
650 07 ‡a631.43 -- Soils, physical and mechanical properties.‡2udc
650 07 ‡a581.524.444.3 -- Tayga.‡2udc
650 07 ‡a581.524.444.2 -- Tundra.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*501) -- Russia (Federation).‡2udc
651 #7 ‡a(*531.3) -- Yakutiya. Respublika Sakha.‡2udc
773 0# ‡7nnas ‡tPolar Geography. ‡gVol. 28(4) (2004) ‡wSPRI-137181
916 ## ‡a2005/10/10 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221004 ‡bRF