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Record #110237:

Thermal response of the active layer to climatic warming in a permafrost environment / Douglas L. Kane, Larry D. Hinzman, John P. Zarling.

Title: Thermal response of the active layer to climatic warming in a permafrost environment / Douglas L. Kane, Larry D. Hinzman, John P. Zarling.
Author(s): Kane, Douglas L.
Hinzman, Larry D.
Zarling, John P.
Date: 1991.
In: Cold Regions Science and Technology. (1991.), Vol. 19(2) (1991)
Abstract: Soil temperature data collected over four-year period near Toolik Lake, northern Alaska. Finite-element, two-dimensional heat conduction model with phase change was used to predict soil temperatures at this site. After verification that model could be used to predict soil thermal regime, various climatic warming scenarios were used as inputs to estimate thermal response for next 50 years.
Notes:

Cold Regions Science and Technology. Vol. 19(2) :111-122 (1991).

Keywords: 551.32 -- Glaciology.
551.58 -- Climatology.
551.583 -- Climatic changes.
551.588 -- Climate, effect of man and environment.
551.34 -- Geocryology. Frozen ground.
551.345 -- Permafrost. Cryopedology.
536 -- Heat.
551.345.2 -- Permafrost, formation and decay.
E8 -- Glaciology: frost action and permafrost.
(*49) -- Alaska.
(*494) -- Alaska, northwestern.
SPRI record no.: 110237

MARCXML

LDR 01607naa#a2200000#a#4500
001 SPRI-110237
005 20231129160832.0
007 ta
008 231129s1991####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-110237
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aKane, Douglas L.
245 10 ‡aThermal response of the active layer to climatic warming in a permafrost environment /‡cDouglas L. Kane, Larry D. Hinzman, John P. Zarling.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 111-122 :‡bdiags., map.
500 ## ‡aCold Regions Science and Technology. Vol. 19(2) :111-122 (1991).
520 3# ‡aSoil temperature data collected over four-year period near Toolik Lake, northern Alaska. Finite-element, two-dimensional heat conduction model with phase change was used to predict soil temperatures at this site. After verification that model could be used to predict soil thermal regime, various climatic warming scenarios were used as inputs to estimate thermal response for next 50 years.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.588 -- Climate, effect of man and environment.‡2udc
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a536 -- Heat.‡2udc
650 07 ‡a551.345.2 -- Permafrost, formation and decay.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*49) -- Alaska.‡2udc
651 #7 ‡a(*494) -- Alaska, northwestern.‡2udc
700 1# ‡aHinzman, Larry D.
700 1# ‡aZarling, John P.
773 0# ‡7nnas ‡tCold Regions Science and Technology. ‡gVol. 19(2) (1991) ‡wSPRI-59075
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20231129