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Identification and quantitative assessment of permafrost hazards to land resources in the central Part of Yamal Peninsula

机译:确定和定量评估亚马尔半岛中部地区多年冻土对土地资源的危害

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In the north of Western Siberia the air temperature increase trend is one of the greatest in Russia for the 1960-95 yy. period (0.05°C/year-up summer and 0.07°C/year-up winter). During 1965-2003 the regional trend of the ground temperature was 0.02°C/year (Pavlov, 2008). Locally the ground temperature response to the climate change can be quite different depending on superficial landscape and hydrogeological conditions. Completed investigations included the numerical modeling of permafrost reaction to the climate changes. In so doing the "nontemperature" climate factors of heat exchange through the surface have been taken into account also. The different climate factors were put into model as linear trends to predict the permafrost condition in the next 50 years. The climate scenarios were obtained from observation data of different duration. This modeling helps to evaluate possible land resource damages from the natural gas field exploration and to develop the effective environmental program including the land reclamation. The results will be used at the design, construction processes and environmental monitoring stages of the land reclamation.
机译:在西西伯利亚北部,气温升高趋势是1960-95年度俄罗斯最大的趋势之一。期间(夏季为0.05°C /年,冬季为0.07°C /年)。在1965-2003年期间,地温的区域趋势为0.02°C /年(Pavlov,2008)。在局部,地表温度对气候变化的响应可能会有所不同,这取决于表面景观和水文地质条件。已完成的研究包括多年冻土对气候变化反应的数值模拟。这样做时,还考虑了通过表面进行热交换的“非温度”气候因素。将不同的气候因素作为线性趋势纳入模型,以预测未来50年的多年冻土状况。从不同持续时间的观测数据获得了气候情景。该模型有助于评估天然气田勘探可能造成的土地资源损害,并制定包括土地开垦在内的有效环境计划。结果将用于土地开垦的设计,施工过程和环境监测阶段。

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