[Climate changes in southern Taihang Mountain area from 1980 to 2019]

Ying Yong Sheng Tai Xue Bao. 2022 Aug;33(8):2139-2145. doi: 10.13287/j.1001-9332.202208.025.
[Article in Chinese]

Abstract

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)-1 and 14.21 mm·(10 a)-1, 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)-1, 4 d·(10 a)-1, and 5 d·(10 a)-1, 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.

南太行地区是我国黄河重点生态区的重要组成部分,研究该区域气候变化趋势对我国黄河流域生态安全维护、重大生态工程计划决策具有重要意义。本研究以南太行地区济源市为研究区,基于1980—2019年气象资料,分析了该地区气候变化趋势。结果表明: 研究期间,济源气候变化整体趋于暖湿化,气温和降水量的变化率分别为0.48 ℃·(10 a)-1、14.21 mm·(10 a)-1。春、夏季增温高于秋、冬季,春季气候变化趋势为暖干化,夏、秋、冬季趋于暖湿化。潜在蒸散和干燥度分别为增加和下降趋势,均值分别为748 mm、1.36。≥10 ℃初、终日每10年分别提前3 d、延迟1 d,≥10 ℃有效积温、≥10 ℃持续日数和高温日数的变化趋势分别为116.57 ℃·(10 a)-1、4 d·(10 a)-1和5 d·(10 a)-1。20世纪90年代是研究期间济源最干旱的10年,升温最快,有一半年份表现出半干旱区气候特征。2010—2019年,济源气候暖湿化趋势明显加快,为研究期间最暖最湿润的10年,这10年的≥10 ℃持续日数增长28 d,有效积温增加389.36 ℃,高温天气发生频率和强度明显增加。.

Keywords: aridity index; climate change; effective accumulated temperature; high temperature days; potential evapotranspiration.

MeSH terms

  • China
  • Climate Change*
  • Ecosystem*
  • Rivers
  • Seasons
  • Temperature