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Fluxes and Gradients in the Convective Surface Layer and the Possible Role of Boundary-Layer Depth and Entrainment Flux

机译：对流表面层的通量和梯度以及边界层深度和夹带通量的可能作用

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Steeneveld G.J.; Holtslag A.A.M.; Debruin H.A.R.;
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年度 2005
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1. Fluxes and Gradients in the Convective Surface Layer and the Possible Role of Boundary-Layer Depth and Entrainment Flux [J] . G. J. Steeneveld, A. A. M. Holtslag, H. A. R. Debruin Boundary-Layer Meteorology . 2005,第2期

机译：对流表面层的通量和梯度以及边界层深度和夹带通量的可能作用
2. COUNTERGRADIENT FLUXES OF CONSERVED VARIABLES IN THE CLEAR CONVECTIVE AND STRATOCUMULUS-TOPPED BOUNDARY LAYER: THE ROLE OF THE ENTRAINMENT FLUX [J] . STEPHAN R. DE ROODE, HARM J.J. JONKER, PETER G. DUYNKERKE, Boundary-layer Meteorology . 2004,第1期

机译：清晰的对流和斜纹顶边界层中守恒变量的对立通量：入流的作用
3. Countergradient Fluxes of Conserved Variables in the Clear convective and Stratocumulus-topped Boundary Layer: The role of the Entrainment Flux [J] . Boundary-Layer Meteorology . 2004,第1期

机译：对流和平顶积层边界层中守恒变量的反梯度通量：夹带通量的作用
4. Non-local vertical transport in the shear-free convective surface layer: new theory and improved parameterization of turbulent fluxes [C] . Sergej Zilitinkevich, A.A.Grachev, J.C.R.Hunt, NATO/CCMS international technical meetings on air pollution modeling and its application . 1998

机译：剪切式对流表面层中的非局部垂直传输：新理论和湍流通量的改进参数化
5. Importance of boundary layer entrainment for surface fluxes over land. [D] . McGrath-Spangler, Erica L. 2011

机译：边界层夹带对于陆地表面通量的重要性。
6. Episodic organic carbon fluxes from surface ocean to abyssal depths during long-term monitoring in NE Pacific [O] . Kenneth L. Smith Jr., Henry A. Ruhl, Christine L. Huffard, 2018

机译：在东北太平洋进行长期监测期间从表面海洋到深渊的间歇性有机碳通量
7. FLUXES AND GRADIENTS IN THE CONVECTIVE SURFACE LAYER AND THE POSSIBLE ROLE OF BOUNDARY-LAYER DEPTH AND ENTRAINMENT FLUX [O] . G. J. Steeneveld, A. A. M. Holtslag, H. A. R. Debruin 2004

机译：对流面层中的通量和梯度以及边界层深度和渗透通量的可能作用
8. Surface Fluxes of Trace Gases Derived from Convective-Layer Profiles [R] . Davis, K. J. 1992

机译：从对流层剖面得到的痕量气体的表面通量

Fluxes and Gradients in the Convective Surface Layer and the Possible Role of Boundary-Layer Depth and Entrainment Flux

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