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Arid Land Geography ›› 2023, Vol. 46 ›› Issue (12): 1939-1950.doi: 10.12118/j.issn.1000-6060.2023.105

• Original article • Previous Articles     Next Articles

Temporal and spatial evolution of relative humidity in the Loess Plateau during 1955—2021

AN Bin1,2(),XIAO Weiwei1,LIU Yufeng3,LIU Quanyu1   

  1. 1. School of Tourism & Environment, Ankang University, Ankang 725000, Shaanxi, China
    2. College of Geographical Sciences, East China Normal University, Shanghai 200241, China
    3. School of Geography and Environment, Xianyang Normal University, Xianyang 712000, Shaanxi, China
  • Received:2023-03-08 Revised:2023-04-20 Online:2023-12-25 Published:2024-01-05

Abstract:

The Loess Plateau, a region in China that is highly sensitive to climate change, serves as a focal point for investigating the spatiotemporal evolution of relative humidity (RH). Understanding the interplay between RH and geographical and meteorological factors is essential for comprehending the climate change dynamics within the plateau. This study leverages daily RH observations from 90 meteorological stations in the Loess Plateau and its environs to analyze the temporal and spatial variations in RH from 1960 to 2021, both before and after the implementation of ecological initiatives such as the conversion project of farmland to forest and grass. Using trend analysis, sensitivity analysis, and spatial interpolation, we unveil the following findings: (1) The average annual RH in the Loess Plateau exhibited a notable decrease of -0.376%·(10a)-1 (P<0.05) from 1955 to 2021, undergoing a decadal variation characterized by a “weakening-strengthening-weakening” process. While autumn experienced a slight increase, all other seasons displayed a declining trend, with the most pronounced decrease observed in spring [-0.945%·(10a)-1] and the least in winter [-0.194%·(10a)-1]. (2) Spatially, the winter average RH in the Loess Plateau peaked in the south, gradually diminishing from east to west in the central and northern regions. Conversely, other time series demonstrated a gradual decline from south to north. The spatial patterns of the annual and seasonal average RH variation trends in the Loess Plateau were different. (3) Postimplementation of the ecological project, the average RH throughout the year, as well as in spring, summer, and winter, exhibited varying degrees of decrease. The trends in annual, summer, and winter RH shifted from an increasing to a decreasing trajectory. Noteworthy differences emerged in the spatial distribution characteristics of annual and seasonal average RH, coupled with their respective trend changes. The prevailing trend change combination type for all temporal RH patterns was consistently low. (4) The primary seasonal factor influencing long-term changes in annual RH in the Loess Plateau is spring, with spatial dominance primarily by a single dominant type in spring and a combination of dominant types in spring and summer. (5) The annual and seasonal average RH in the Loess Plateau demonstrated a significant negative correlation with latitude (P<0.01) and a positive correlation with precipitation (P<0.01). The geographical factors exerted the most significant influence on summer average RH. Annual, spring, and summer average RH were most sensitive to average temperature, whereas autumn and winter were most responsive to wind speed.

Key words: relative humidity (RH), interdecadal variation, seasonal contribution rate, sensitivity analysis, the implementation of ecological project, the Loess Plateau