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Record #199797:
Thermal erosion of a permafrost coastline: improving process-based models using time-lapse photography / Cameron Wobus, and 5 others.
Title: | Thermal erosion of a permafrost coastline: improving process-based models using time-lapse photography / Cameron Wobus, and 5 others. |
Author(s): | Wobus, Cameron. |
Date: | 2011. |
In: | Arctic, Antarctic, and Alpine Research. (2011.), Vol. 43(3) (2011) |
Abstract: | Observes and quantifies coastal erosion of permafrost coastline in Northern Petroleum Reserve, northern Alaska, directly via time-lapse photography in combination with meteorological data. Observations indicate that erosion of permafrost bluffs is thermally driven, but that surface winds play crucial role in exposing bluffs to radiatively warmed seawater that drives melting of interstitial ice. |
Notes: | Arctic, Antarctic, and Alpine Research. Vol. 43(3) :474-484 (2011). |
Keywords: | 551.345 -- Permafrost. Cryopedology. 551.345.2 -- Permafrost, formation and decay. 551.58 -- Climatology. 551.506 -- Meteorological data. 551.5 -- Meteorology. 551.417 -- Coasts and beaches. 778 -- Photography, applications. E9 -- Glaciology: meteorology and climatology. (*3) -- Arctic regions. (*49) -- Alaska. (*494) -- Alaska, northwestern. (*628.1) -- Canadian Beaufort Sea. |
SPRI record no.: | 199797 |
LDR 01770naa#a2200000#a#4500 001 SPRI-199797 005 20231001191354.0 007 ta 008 231001s2011####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-199797 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aWobus, Cameron. 245 10 ‡aThermal erosion of a permafrost coastline :‡bimproving process-based models using time-lapse photography /‡cCameron Wobus, and 5 others. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2011. 300 ## ‡ap. 474-484 :‡bill. (some col.), diags., table, map. 500 ## ‡aArctic, Antarctic, and Alpine Research. Vol. 43(3) :474-484 (2011). 520 3# ‡aObserves and quantifies coastal erosion of permafrost coastline in Northern Petroleum Reserve, northern Alaska, directly via time-lapse photography in combination with meteorological data. Observations indicate that erosion of permafrost bluffs is thermally driven, but that surface winds play crucial role in exposing bluffs to radiatively warmed seawater that drives melting of interstitial ice. 530 ## ‡aAlso issued online ‡uurn:doi:10.1657/1938-4246-43.3.474‡uhttps://dx.doi.org/10.1657/1938-4246-43.3.474 650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc 650 07 ‡a551.345.2 -- Permafrost, formation and decay.‡2udc 650 07 ‡a551.58 -- Climatology.‡2udc 650 07 ‡a551.506 -- Meteorological data.‡2udc 650 07 ‡a551.5 -- Meteorology.‡2udc 650 07 ‡a551.417 -- Coasts and beaches.‡2udc 650 07 ‡a778 -- Photography, applications.‡2udc 650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*49) -- Alaska.‡2udc 651 #7 ‡a(*494) -- Alaska, northwestern.‡2udc 651 #7 ‡a(*628.1) -- Canadian Beaufort Sea.‡2udc 773 0# ‡7nnas ‡tArctic, Antarctic, and Alpine Research. ‡gVol. 43(3) (2011) ‡wSPRI-211524 916 ## ‡a2012/07/16 -- JW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231001 ‡bJW