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* [2] Wang W., Yin S.*, Gao G., Papalexiou S.M., Wang Z., 2022, Increasing trends in rainfall erosivity in the Yellow River basin from 1971 to 2020, Journal of Hydrology, 610: 127851.
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* [6] Borrelli P., Alewell C., Alvarez P., et al., 2021, Soil erosion modelling: A global review and statistical analysis. Science of the Total Environment, 780: 146494.
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* [9] Yue T., Xie Y., Yin S.*, Yu B., Miao C., Wang W., 2020, Effect of time resolution of rainfall measurements on the erosivity factor in the USLE in China, International Soil and Water Conservation Research, 8(4): 373-382. DOI information: 10.1016/j.iswcr.2020.06.001.
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* [32] 高歌*，殷水清，陈涛，黄大鹏，王文婷，2022, 长江流域降雨侵蚀力时空变化及成因分析. 农业工程学报，38(3): 84-92.
* [33] 秦大河, 效存德*, 丁明虎, 王飞腾，朱志强，殷水清，任贾文，2022, 服务冬奥、支撑发展：冰冻圈科学的延拓. [[中国科学院院刊]], 37(3): 395-402.
* [34] 高歌*，韩振宇，殷水清，黄大鹏，王文婷, 2021, 黄河流域1961~2017年 [[ 降雨侵蚀力 ]] 特征与 [[ 未来变化预估]]. [[ 应用基础与工程科学学报]], 29(3): 575-590.* [35] 殷水清*, 王文婷, 2020, 土壤侵蚀研究中降雨过程随机模拟综述. 地理 [[ 科学进展]], 39(10): 1747-1757.
* [36] 谢云, 张汝正, 殷水清*, 田丹丹, 高歌，2020, 1961—2010年全球变暖背景下中国空气湿度长期变化特征. 水科学进展, 31(5): 674-684. doi: 10.14042/j.cnki.32.1309.2020.05.004.
* [37] 殷水清*, 薛筱婵, 岳天雨, 谢云, 高歌, 2019, 中国降雨侵蚀力的时空分布及重现期研究. 农业工程学报, 35(9): 105-113. DOI:10.11975/j.issn.1002-6819.2019.09.013.
* [54] 殷水清, 谢云*，2005, 黄土高原降雨侵蚀力时间分布. 水土保持通报，25(4): 29-33.
* [55] 殷水清, 谢云*，2005, 黄土高原地区中小流域日降雨空间分布特征. 北京师范大学学报(自然科学版)，41(1): 89-91.
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==获奖情况==
2018年, 中国水土保持学会科技进步奖, 一等奖（14/15）