Journal of Desert Research ›› 2020, Vol. 40 ›› Issue (5): 65-73.DOI: 10.7522/j.issn.1000-694X.2020.00013
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Shouxu Chen1(), Yuxiang Dong1,2(
)
Received:
2020-01-16
Revised:
2020-03-25
Online:
2020-09-28
Published:
2020-09-28
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Yuxiang Dong
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Shouxu Chen, Yuxiang Dong. A review of the research on wind erosion climatic erosivity[J]. Journal of Desert Research, 2020, 40(5): 65-73.
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URL: http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2020.00013
影响因素 | 相关性 |
---|---|
风速 | 正相关 |
风向 | 视情况而定 |
降雨量 | 负相关 |
降雪覆盖 | 负相关 |
湍流 | 负相关 |
蒸发 | 负相关 |
气温 | 正相关 |
气压 | 负相关 |
冻融过程 | 正相关 |
Table 1 Some interactive factors affecting wind erosion climatic erosivity[66-67]
影响因素 | 相关性 |
---|---|
风速 | 正相关 |
风向 | 视情况而定 |
降雨量 | 负相关 |
降雪覆盖 | 负相关 |
湍流 | 负相关 |
蒸发 | 负相关 |
气温 | 正相关 |
气压 | 负相关 |
冻融过程 | 正相关 |
计算方法 | 所需数据 | 优缺点 |
---|---|---|
Chepil公式 | 风速、降水量、气温 | 优点:计算简单,数据容易获取 缺点:不适用于寒冷、极端干旱地区 |
FAO公式 | 风速、降水量、ETP | 优点:计算简单,数据易获取,适用范围较广 缺点:暂未确定ETP的最佳计算方法 |
Skidmore公式 | 风速、大气密度、吸附水粘聚抗力、α常数、风速概率密度函数 | 优点:理论基础坚实,计算结果准确 缺点:数据获取难度大,计算方法复杂,可能不适用于中国部分地区 |
Table 2 Comparison of calculation methods of wind erosion climatic erosivity
计算方法 | 所需数据 | 优缺点 |
---|---|---|
Chepil公式 | 风速、降水量、气温 | 优点:计算简单,数据容易获取 缺点:不适用于寒冷、极端干旱地区 |
FAO公式 | 风速、降水量、ETP | 优点:计算简单,数据易获取,适用范围较广 缺点:暂未确定ETP的最佳计算方法 |
Skidmore公式 | 风速、大气密度、吸附水粘聚抗力、α常数、风速概率密度函数 | 优点:理论基础坚实,计算结果准确 缺点:数据获取难度大,计算方法复杂,可能不适用于中国部分地区 |
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