Page 167 - 《高原气象》2026年第2期
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2 期 王彦淇等:基于CEEMD 方法对森林下垫面湍流相干结构的通量贡献研究 467
有所差异, 水平 u 风的斜坡强度在中性条件下最 Boundary-Layer Meteorology, 47(1): 349-377. DOI: 10. 1007/
小并且随着稳定度和不稳定度的增大而增大, 但 BF00122339.
是 w 风的斜坡强度在不稳定条件下最大而随着中 Gao Z, Liu H, Katul G G, et al, 2017. Non-closure of the surface en‐
ergy balance explained by phase difference between vertical ve‐
性到稳定层结的变化, 斜坡强度转而减小, 这反
locity and scalars of large atmospheric eddies[J]. Environmental
映了不稳定层结下对于垂直相干运动的促进作
Research Letters, 12(3): 34025. DOI: 10. 1088/1748-9326/
用, 而稳定层结下抑制了这种运动。 aa625b.
Gao Z, Liu H, Missik J E C, et al, 2019. Mechanistic links between
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