中国农业气象 ›› 2025, Vol. 46 ›› Issue (4): 459-470.doi: 10.3969/j.issn.1000-6362.2025.04.003

• 农业生态环境栏目 • 上一篇    下一篇

中国北方农牧交错带风蚀气候侵蚀力时空变化特征及其成因分析

姜婧妍,胡琦,楚希雅,周建朔,张丽娜,潘学标,王靖,黄彬香   

  1. 中国农业大学资源与环境学院/中国气象局−中国农业大学农业应对气候变化联合实验室,北京 100193
  • 收稿日期:2024-04-15 出版日期:2025-04-20 发布日期:2025-04-14
  • 作者简介:姜婧妍,E-mail:jiangjingyan2022@163.com
  • 基金资助:
    国家重点研发计划项目(2023YFD1900504;2022YFD1900302)

Spatiotemporal Variation Characteristics and Causes of Wind Erosion Climatic Erodibility in the Ecotone Between Agriculture and Animal Husbandry in Northern China

JIANG Jing-yan, HU Qi, CHU Xi-ya, ZHOU Jian-shuo, ZHANG Li-na, PAN Xue-biao, WANG Jing, HUANG Bin-xiang   

  1. College of Resources and Environment, China Agricultural University/Joint Laboratory of Agriculture Response to Climate Change, China Meteorological Administration and China Agricultural University, Beijing 100193, China
  • Received:2024-04-15 Online:2025-04-20 Published:2025-04-14

摘要:

基于中国北方农牧交错带186个气象站点1961-2020年逐日气象数据,利用气候倾向率和空间插值,分析不同时间尺度风蚀气候侵蚀力的时空分布和变化特征,定量解析风速、降水量和蒸散量(ET0)等气象因子变化对风蚀的影响,以期为改善农牧交错带的环境问题和风沙治理提供科学建议及理论支撑。结果表明:研究区土壤风蚀量呈东高西低的空间分布特征,高值区分布在内蒙古中部的通辽、赤峰与河北张家口交界处等地,主要是该地区风速大、降水量少且蒸散量大。研究区不同时段风蚀量存在显著差异,春季风蚀气候侵蚀力最大、夏季最小,东部地区季节风蚀差异最显著。近60a研究区风蚀呈显著减少趋势,风速、降水量和蒸散量的变化共同影响了风蚀气候侵蚀力的变化,其中风速起主导作用,但不同区域风蚀变化的成因存在差异,研究区中东部地区风速减少、降水量增加,导致风蚀气候侵蚀力减少;研究区西部风速和蒸散量增加,同时降水量增加,抵消了风速和蒸散变化对风蚀的影响,致使风蚀气候侵蚀力变化不显著。

关键词:

北方农牧交错带, 风速, 降水, ET0, 风蚀气候侵蚀力

Abstract:

Soil wind erosion poses a significant threat to environmental degradation and hinders the development of agriculture and animal husbandry in China. This study investigated the spatiotemporal distribution and variation characteristics of wind erosion climatic erosivity across different timescales, using daily meteorological data from 186 stations in the agro-pastoral ecotone of northern China spanning 1961−2020. It quantitatively analyzed the impacts of meteorological factors, including wind speed, precipitation, and reference evapotranspiration (ET0), on wind erosion. The results revealed a spatial pattern of soil wind erosion with higher values in the east and lower in the west, peaking in regions such as Tongliao and Chifeng in central Inner Mongolia and the border between Zhangjiakou in Hebei province, attributed primarily to high wind speeds, low precipitation, and intense evapotranspiration. Significant seasonal variations in wind erosion were observed, with the highest climatic erosivity in spring and the lowest in summer, particularly pronounced in the eastern region. Over the past 60 years, wind erosion in the study area had shown a notable decreasing trend, influenced jointly by changes in wind speed, precipitation, and ET0, with wind speed playing a dominant role. However, the drivers of wind erosion variation differed across regions; decreases in wind speed and increases in precipitation led to reduce wind erosion climatic erosivity in the central and eastern parts, while increased in wind speed and ET0, albeit accompanied by rising precipitation, counteracted each other's effects in the western region, resulting in insignificant changes in wind erosion climatic erosivity. This study, which explores the spatiotemporal variations of wind erosion in the agro-pastoral ecotone of northern China across multiple meteorological factors and timescales, provides scientific theoretical guidance for regional agricultural production, wind prevention, and erosion mitigation.

Key words:

Northern farming-pastoral ecotone, Wind speed, Precipitation, ET0, Wind erosion climatic erosivity