CAJ | 학술논문

　　使用衡水市7个气象观测站1959-2010年的气温与地温资料，分析了衡水市气温与地温的变化特点．分析发现，1959-2010年的近52 a，衡水市平均气温显著升高，极端气温中，最低气温显著升高，最高气温升高的趋势还不十分显著．1965-2010年的近46 a，0 cm和20 cm的地温也在显著增暖，而10 cm地温虽然也有增暖的倾向，但趋势还不十分显著；土壤较深层40 cm,80 cm的地温的变化并不显著；地温变化主要为土壤较浅层变暖．气温与0~40 cm土壤较浅层地温的变化具有较好的一致性，与80 cm土壤较深层的温度变化一致性较差．
　　사용형수시7개기상관측참1959-2010년적기온여지온자료，분석료형수시기온여지온적변화특점．분석발현，1959-2010년적근52 a，형수시평균기온현저승고，겁단기온중，최저기온현저승고，최고기온승고적추세환불십분현저．1965-2010년적근46 a，0 cm화20 cm적지온야재현저증난，이10 cm지온수연야유증난적경향，단추세환불십분현저；토양교심층40 cm,80 cm적지온적변화병불현저；지온변화주요위토양교천층변난．기온여0~40 cm토양교천층지온적변화구유교호적일치성，여80 cm토양교심층적온도변화일치성교차．
In the article, the atmospheric and ground temperature changes in Hengshui City have been analyzed based on measured data of seven meteorological stations from 1959 to 2010. The research found that, during the 52 years in 1959-2010, the average air temperature of the city has significantly increased, and in the extreme weather, minimum temperature has greatly increased compared with the maximum temperature. During the 46 years in 1965-2010, the tendency of ground warming is very significant at the places of surface and below 20 cm rather than below 10 cm. In addition, the negligible changes of ground temperature were found in deep places of 40 and 80 cm far from surface. So the ground warming mainly origins from temperature increase of shallow soil 0 ~ 40 cm blow surface, which is also consistent with the change of air temperature. In contrast, the air temperature change is not consistent with the temperature variation of deep soil 80 cm below ground.