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根据２１４国道沿线花石峡地区的气候变化特征和自然地理及地质水文条件，以该区长石头山连续多年冻土区４０ｍ深实测地温为基础，并以年平均气温升速率０．４℃／１０ａ为前提，对该区气候变化与多年冻土退化的关系等进行了模拟预测．
According to the climate change characteristics and natural geography and geology and hydrology conditions of Huashixia region along the No.214 national highway, based on the measured ground temperature of 40m in continuous permafrost zone of Longshuishan Mountain, the annual average temperature increase rate is 0.4 ℃ / 10a As a prerequisite, the climate change in the area and the relationship between the degradation of permafrost were simulated and predicted.