Parameterization of the atmospheric boundary layer

被引：73

作者：

Teixeira, J. ^{[1
,2
]}

Stevens, B. ^{[3
]}

Bretherton, C. S. ^{[4
]}

Cederwall, R. ^{[5
]}

Doyle, J. D. ^{[6
]}

Golaz, J. C. ^{[6
,7
]}

Holtslag, A. A. M. ^{[8
]}

Klein, S. A. ^{[5
]}

Lundquist, J. K. ^{[5
]}

Randall, D. A. ^{[9
]}

Siebesma, A. R. ^{[10
]}

Soares, P. M. M. ^{[11
,12
]}

机构：

[1] Naval Res Lab, Monterey, CA USA

[2] NATO Undersea Res Ctr, La Spezia, Italy

[3] Univ Calif Los Angeles, Los Angeles, CA USA

[4] Univ Washington, Seattle, WA 98195 USA

[5] Lawrence Livermore Natl Lab, Livermore, CA USA

[6] USN, Res Lab, Monterey, CA USA

[7] Geophys Fluid Dynam Lab, Princeton, NJ USA

[8] Wageningen Univ, Wageningen, Netherlands

[9] Colorado State Univ, Ft Collins, CO 80523 USA

[10] Royal Netherlands Meteorol Inst, NL-3730 AE De Bilt, Netherlands

[11] Univ Lisbon, P-1699 Lisbon, Portugal

[12] Inst Super Engn Lisboa, Lisbon, Portugal

来源：

BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY | 2008年 / 89卷 / 04期

关键词：

D O I：

10.1175/BAMS-89-4-453

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

Since the atmospheric boundary layer is one of the main components of the climate system, its realistic parameterization can yield better climate prediction models. However, there are relevant issues that need to be addressed to improve boundary layer parameterization like how to represent subgrid vertical fluxes, how to represent cloud fraction and cloud water, how to solve the equations efficiently and how to develop more general parameterizations that represent all types of boundary layers. As such, the Parameterization of the Atmospheric Boundary Layer was held in June 2005 at the UCL conference Center in California to tackle this issue. It discussed issues regarding boundary layer clouds, stable boundary layer, interaction with the surface, and interaction with deep convection.

引用

页码：453 / 458

页数：6

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