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Record #188731:

Significance of snowpack for root-zone water and temperature cycles in subarctic Lapland / Raimo Sutinen.

Title: Significance of snowpack for root-zone water and temperature cycles in subarctic Lapland / Raimo Sutinen.
Author(s): Sutinen, Raimo.
Date: 2009.
In: Arctic, Antarctic, and Alpine Research. (2009.), Vol. 41(3) (2009)
Abstract: Reports results of monitoring snowpack thickness, air and soil temperatures and water content in soil, sapwood and roots of downy birch (Betula pubescens) in Finnish Lapland between 1999-2003. Extreme cold event in January 1999 resulted in soil freezing (at 10-cm depth) down to T₁₀ = -26°C at snow-free site, but soil temperature beneath 50-cm-thick snowpack was T₁₀ = -0.5°C. Snowmelt water was able to infiltrate partially frozen soil sequences, such that increase in water content of soil and birch roots occurred two to six weeks before soil temperatures rose notably above 0°C.
Notes:

Arctic, Antarctic, and Alpine Research. Vol. 41(3) :373-380 (2009).

Keywords: 551.32 -- Glaciology.
57 -- Biology.
551.5 -- Meteorology.
551.52 -- Atmospheric radiation and temperature.
551.578.46 -- Snow cover and snow patches.
574.4 -- Ecology, terrestrial.
58.03/.05 -- Plants, influence of physical environment.
582.632.1 -- Betulales: Betula pubescens.
E14 -- Glaciology: biological aspects of ice and snow.
(*3) -- Arctic regions.
(*56) -- Finland.
(*561) -- Finnish Lapland.
SPRI record no.: 188731

MARCXML

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100 1# ‡aSutinen, Raimo.
245 10 ‡aSignificance of snowpack for root-zone water and temperature cycles in subarctic Lapland /‡cRaimo Sutinen.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2009.
300 ## ‡ap. 373-380 :‡bill., diags., table, map.
500 ## ‡aArctic, Antarctic, and Alpine Research. Vol. 41(3) :373-380 (2009).
520 3# ‡aReports results of monitoring snowpack thickness, air and soil temperatures and water content in soil, sapwood and roots of downy birch (Betula pubescens) in Finnish Lapland between 1999-2003. Extreme cold event in January 1999 resulted in soil freezing (at 10-cm depth) down to T₁₀ = -26°C at snow-free site, but soil temperature beneath 50-cm-thick snowpack was T₁₀ = -0.5°C. Snowmelt water was able to infiltrate partially frozen soil sequences, such that increase in water content of soil and birch roots occurred two to six weeks before soil temperatures rose notably above 0°C.
530 ## ‡aAlso issued online ‡uurn:doi:10.1657/1938-4246-41.3.373‡uhttps://dx.doi.org/10.1657/1938-4246-41.3.373
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a57 -- Biology.‡2udc
650 07 ‡a551.5 -- Meteorology.‡2udc
650 07 ‡a551.52 -- Atmospheric radiation and temperature.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a574.4 -- Ecology, terrestrial.‡2udc
650 07 ‡a58.03/.05 -- Plants, influence of physical environment.‡2udc
650 07 ‡a582.632.1 -- Betulales: Betula pubescens.‡2udc
650 07 ‡aE14 -- Glaciology: biological aspects of ice and snow.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*56) -- Finland.‡2udc
651 #7 ‡a(*561) -- Finnish Lapland.‡2udc
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916 ## ‡a2010/01/21 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221005 ‡bJW