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Updated: Aug 30, 2025

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
[Climate changes in southern Taihang Mountain area from 1980 to 2019]
Hui Huang1,2, Chang-Ling Zheng3, Jin-Song Zhang1,2
1Research Institute of Forestry, Chinese Academy of Forestry/Key Laboratory of Tree Breeding and Cultivation, National Forestry and Grassland Administration, Beijing 100091, China.
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.
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