1990
DOI: 10.1061/(asce)0887-381x(1990)4:1(6)
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Cold Regions Engineering: Climatic Warming Concerns for Alaska

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Cited by 43 publications
(13 citation statements)
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“…Based on their review of climatological data, Esch and Osterkamp (1990) have suggested that the average air temperature at these latitudes can be expected to increase about 1°C/decade. As shown in Fig. 14, if the average annual air temperature was to increase by 2"C, the maximum depth of annual thaw would increase from about 1 to 1.3 m. Calculations were also carried out to determine the effect which failure of one or more thermosyphons would have on the operation of the system.…”
Section: Results Of Analysesmentioning
confidence: 98%
“…Based on their review of climatological data, Esch and Osterkamp (1990) have suggested that the average air temperature at these latitudes can be expected to increase about 1°C/decade. As shown in Fig. 14, if the average annual air temperature was to increase by 2"C, the maximum depth of annual thaw would increase from about 1 to 1.3 m. Calculations were also carried out to determine the effect which failure of one or more thermosyphons would have on the operation of the system.…”
Section: Results Of Analysesmentioning
confidence: 98%
“…During the interactive processes between the permafrost environment and permafrost engineering, the thermal regimes of foundation soils are easily affected by engineering activities and/or climate changes (Esch and OsterKamp, 1990;Fortier et al, 2011;Harris et al, 2009;Mu et al, 2012;Smith and Riseborough, 2010;Wu et al, 2002). The thermal impacts either from engineering activities or climate changes can cause various complications for permafrost engineering stability (Instanes et al, 2005;Ma et al, 2009;Nelson et al, 2002;Wu and Niu, 2014).…”
Section: Introductionmentioning
confidence: 97%
“…Accurate simulation of the thermal regime in frozen soil models plays an important role in the prediction of global climate changes [ Ling and Zhang , 2004], and temperature variation can affect the performance of structures constructed in cold regions [ Esch and Osterkamp , 1990; Lunardini , 1996]. A frozen soil model with realistic simulation of soil temperature, liquid water content, and ice content also improved the climate model's ability to simulate greenhouse gas exchange processes in cold regions [ Mikan et al , 2002].…”
Section: Introductionmentioning
confidence: 99%