1960—2020年东北黑土区水蚀动力因子时空格局及其对主要大气海洋环流模式的响应
[目的] 研究东北黑土区水蚀动力因子的时空格局及其对大气海洋环流模式的响应,对区域极端降水事件诱发的土壤侵蚀防治有重要意义。[方法] 选用降雨侵蚀力(R)、暴雨雨量(R50p)、极端强降水量(R95p)、连续5日最大降水量(R5d)表征水蚀动力因子,基于1960—2020年逐日降雨数据,采用滑动平均、小波分析、Sen斜率估计法、Mann-Kendall检验方法,分析1960—2020年东北黑土区水蚀动力因子的时空格局,解析水蚀动力因子对大气海洋环流模式的响应。[结果] (1)东北黑土区的年降雨侵蚀力(R)
高晓玉 +7 more
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