Huang Hui, Zheng Chang-Ling, Zhang Jin-Song, Meng Ping
Research Institute of Forestry, Chinese Academy of Forestry/Key Laboratory of Tree Breeding and Cultivation, National Forestry and Grassland Administration, Beijing 100091, China.
Collaborative Innovation Center of Sustainable Forestry in Southern China, Nanjing Forest University, Nanjing 210037, China.
Ying Yong Sheng Tai Xue Bao. 2022 Aug;33(8):2139-2145. doi: 10.13287/j.1001-9332.202208.025.
Southern Taihang Mountain area is an important part of the key ecological regions along the Yellow River in China. Understanding the climate change trend in this area is of significance for the maintenance of ecological security and the planning and decision-making of major ecological projects in the Yellow River Basin. Taking Jiyuan City in southern Taihang Mountain area as the research area, we analyzed the climate change trend in Jiyuan based on the meteorological data from 1980 to 2019. The results showed that climate in Jiyuan tended to be warmer and wetter during the study period. The change rates of temperature and precipitation were 0.48 ℃·(10 a) and 14.21 mm·(10 a), respectively. The rise of temperature in spring and summer was higher than that in autumn and winter. Climate was warmer and drier in spring, while warmer and wetter in the other three seasons. Potential evapotranspiration and aridity index showed increasing and decreasing trends, with the average value of 748 mm and 1.36, respectively. The first and last days ≥10 ℃ were about 3 days in advance and 1 day in delay every 10 years. The change rate of effective accumulated temperature ≥10 ℃, duration days ≥10 ℃ and high temperature days were 116.57 ℃·(10 a), 4 d·(10 a), and 5 d·(10 a), respectively. The 1990s was the driest decade in Jiyuan during the study period, with strongest increases of temperature. Half of the years showed the characteristics of semi-arid climate in that decade. From 2010 to 2019, the trend of climate warming and wetting in Jiyuan had accelerated significantly, which was the warmest and wettest decade. In recent 10 years, duration days ≥10 ℃ and the effective accumulated temperature increased by about 28 days and 389.36 ℃, respectively. The frequency and intensity of high temperature weather also increased significantly in this decade.
南太行山地区是中国黄河流域重点生态区域的重要组成部分。了解该地区气候变化趋势对于维护生态安全以及黄河流域重大生态工程的规划与决策具有重要意义。以南太行山地区的济源市为研究区域,基于1980年至2019年的气象数据,分析了济源市的气候变化趋势。结果表明,研究期内济源市气候呈暖湿化趋势。气温和降水的变化速率分别为0.48℃·(10年)和14.21毫米·(10年)。春季和夏季气温上升幅度高于秋季和冬季。春季气候暖干,其他三个季节暖湿。潜在蒸散量和干旱指数呈增加和减少趋势,平均值分别为748毫米和1.36。≥10℃的初日和终日每10年分别提前约3天和推迟1天。≥10℃有效积温、≥10℃持续日数和高温日数的变化速率分别为116.57℃·(10年)、4天·(10年)和5天·(10年)。20世纪90年代是研究期内济源市最干旱的十年,气温上升最为强烈。该年代半数年份呈现半干旱气候特征。2010年至2019年,济源市气候暖湿化趋势显著加速,是最暖湿的十年。近10年,≥10℃持续日数和有效积温分别增加约28天和389.36℃。该年代高温天气的频率和强度也显著增加。