Numerical simulation of ground thermal response in Canadian seasonal frost regions to climate warming

IF 2.6 Q2 ENGINEERING, GEOLOGICAL International Journal of Geo-Engineering Pub Date : 2023-09-27 DOI:10.1186/s40703-023-00196-9
Mohammed Yassir Marrah, Mamadou Fall, Husham Almansour
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引用次数: 1

Abstract

Abstract To ensure that public infrastructure can safely provide essential services and support economic activities in seasonal frost regions, the design of their foundation systems must be updated and/or adapted to the impacts of climate change. This objective can only be achieved, if the impact of global warming on the soil thermal behaviour in Canadian seasonal frost regions is well-known and can be predicted. In the present paper, the results of a modeling study to assess and predict the effect of global warming on the thermal regimes of grounds in three Canadian seasonal frost regions (Ottawa, Sudbury, Toronto) are presented and discussed. The results show that future climate changes will significantly affect the soil thermal regimes in seasonal frost Canadian areas. The simulation results indicated a gradual loss in the frost penetration depth due to the climate change, in the three representative sites. The frost period duration will be shorter due to climate change in the three selected regions and will completely disappear in Ottawa and Toronto. However, the impact of climate change would not appear clearly in the first 40 years “up to 2060”. The response of the ground to the effect of climate change is a function of the geotechnical characteristics of the ground and the climate conditions. The numerical tool developed and results obtained will be useful for the geotechnical design of climate-adaptive transportation structures in Canadian seasonal frost areas.

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气候变暖对加拿大季节性霜冻地区地表热响应的数值模拟
为确保公共基础设施能够在季节性霜冻地区安全地提供基本服务和支持经济活动,其基础系统的设计必须更新和/或适应气候变化的影响。这一目标只有在全球变暖对加拿大季节性霜冻地区土壤热行为的影响是众所周知和可以预测的情况下才能实现。本文介绍并讨论了全球变暖对加拿大三个季节性霜冻地区(渥太华、萨德伯里和多伦多)地表热状态影响的模拟研究结果。结果表明,未来气候变化将显著影响加拿大季节性霜冻地区的土壤热状态。模拟结果表明,在三个代表性站点,由于气候变化,霜侵深度逐渐减少。由于气候变化,这三个地区的霜冻持续时间将缩短,渥太华和多伦多的霜冻将完全消失。然而,在“到2060年”的前40年里,气候变化的影响不会明显显现。地面对气候变化影响的反应是地面岩土特性和气候条件的函数。所开发的数值工具和所得结果将为加拿大季节性霜冻地区气候适应性交通结构的岩土工程设计提供参考。
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来源期刊
International Journal of Geo-Engineering
International Journal of Geo-Engineering ENGINEERING, GEOLOGICAL-
CiteScore
3.70
自引率
0.00%
发文量
10
审稿时长
13 weeks
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