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Record #125810:

A numerical simulation of coastal retreat and permafrost conditions, Mackenzie delta region, Canada / Baolai Wang.

Title: A numerical simulation of coastal retreat and permafrost conditions, Mackenzie delta region, Canada / Baolai Wang.
Author(s): Wang, Baolai.
Date: 1993.
Publisher: Wushan, Guangzhou: South China University of Technology Press
In: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China. (1993.),
Abstract: Numerical model, applicable to littoral zone of delta region, is developed and used to simulate ground thermal regime of nearshore permafrost under influence of continuous coastal retreat. Model predicts preservation of this permafrost; it will vary in thickness, depending on distance offshore, and its temperature will be 3 to 5°C warmer than adjacent terrestrial permafrost.
Notes:

In: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China / International Conference on Permafrost.

Keywords: 551.34 -- Geocryology. Frozen ground.
551.345 -- Permafrost. Cryopedology.
536 -- Heat.
551.345.2 -- Permafrost, formation and decay.
519.673 -- Modelling.
E8 -- Glaciology: frost action and permafrost.
(*41) -- Canada.
(*440) -- Northwest Territories.
(*470) -- Mackenzie District.
(*60) -- Arctic Ocean and adjacent waters.
(*628) -- Beaufort Sea.
SPRI record no.: 125810

MARCXML

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100 1# ‡aWang, Baolai.
245 12 ‡aA numerical simulation of coastal retreat and permafrost conditions, Mackenzie delta region, Canada /‡cBaolai Wang.
260 ## ‡aWushan, Guangzhou :‡bSouth China University of Technology Press,‡c1993.
300 ## ‡ap. 664-669 :‡bill., diags., map.
500 ## ‡aIn: Permafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China / International Conference on Permafrost.
520 3# ‡aNumerical model, applicable to littoral zone of delta region, is developed and used to simulate ground thermal regime of nearshore permafrost under influence of continuous coastal retreat. Model predicts preservation of this permafrost; it will vary in thickness, depending on distance offshore, and its temperature will be 3 to 5°C warmer than adjacent terrestrial permafrost.
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 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*440) -- Northwest Territories.‡2udc
651 #7 ‡a(*470) -- Mackenzie District.‡2udc
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*628) -- Beaufort Sea.‡2udc
773 0# ‡7m2am ‡aInternational Conference on Permafrost. ‡tPermafrost. Sixth International Conference. Proceedings (Vol. 1), July 5-9, 1993, Beijing China. ‡dWushan, Guangzhou : South China University of Technology Press, 1993. ‡wSPRI-125499
917 ## ‡aUnenhanced record from Muscat, imported 2019
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