Formulation of the Dutch Atmospheric Large-Eddy Simulation (DALES) and overview of its applications

被引：211

作者：

Heus, T. ^{[1
,7
]}

van Heerwaarden, C. C. ^{[2
]}

Jonker, H. J. J. ^{[3
]}

Siebesma, A. Pier ^{[1
,3
]}

Axelsen, S. ^{[4
]}

van den Dries, K. ^{[2
]}

Geoffroy, O. ^{[1
]}

Moene, A. F. ^{[2
]}

Pino, D. ^{[5
,6
]}

de Roode, S. R. ^{[3
]}

Vila-Guerau de Arellano, J. ^{[2
]}

机构：

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

[2] Wageningen Univ, Meteorol & Air Qual Sect, Wageningen, Netherlands

[3] Delft Univ Technol, Dept Multiscale Phys, Delft, Netherlands

[4] Univ Utrecht, Inst Marine & Atmospher Res Utrecht, Utrecht, Netherlands

[5] Tech Univ Catalonia, Dept Appl Phys, Barcelona, Spain

[6] Inst Space Studies Catalonia IEEC, Barcelona, Spain

[7] Max Planck Inst Meteorol, D-20146 Hamburg, Germany

来源：

GEOSCIENTIFIC MODEL DEVELOPMENT | 2010年 / 3卷 / 02期

关键词：

CONVECTIVE BOUNDARY-LAYER; SHALLOW CUMULUS CONVECTION; LIQUID WATER PATH; AIRCRAFT OBSERVATIONS; TURBULENT DISPERSION; SIZE DISTRIBUTIONS; RADIATIVE-TRANSFER; DIURNAL CYCLE; MIXED LAYERS; STIFF ODES;

D O I：

10.5194/gmd-3-415-2010

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The current version of the Dutch Atmospheric Large-Eddy Simulation (DALES) is presented. DALES is a large-eddy simulation code designed for studies of the physics of the atmospheric boundary layer, including convective and stable boundary layers as well as cloudy boundary layers. In addition, DALES can be used for studies of more specific cases, such as flow over sloping or heterogeneous terrain, and dispersion of inert and chemically active species. This paper contains an extensive description of the physical and numerical formulation of the code, and gives an overview of its applications and accomplishments in recent years.

引用

页码：415 / 444

页数：30

共 166 条

[1] Large-Eddy Simulations of a Drizzling, Stratocumulus-Topped Marine Boundary Layer [J].

Ackerman, Andrew S. ;

vanZanten, Margreet C. ;

Stevens, Bjorn ;

Savic-Jovcic, Verica ;

Bretherton, Christopher S. ;

Chlond, Andreas ;

Golaz, Jean-Christophe ;

Jiang, Hongli ;

Khairoutdinov, Marat ;

Krueger, Steven K. ;

Lewellen, David C. ;

Lock, Adrian ;

Moeng, Chin-Hoh ;

Nakamura, Kozo ;

Petters, Markus D. ;

Snider, Jefferson R. ;

Weinbrecht, Sonja ;

Zulauf, Mike .

MONTHLY WEATHER REVIEW, 2009, 137 (03) :1083-1110

[2] The impact of humidity above stratiform clouds on indirect aerosol climate forcing [J].

Ackerman, AS ;

Kirkpatrick, MP ;

Stevens, DE ;

Toon, OB .

NATURE, 2004, 432 (7020) :1014-1017

[3]

[Anonymous], 2004, 16 S BOUND LAYERS TU

[4]

AXELSEN SL, 2009, ACTA GEOPHYS, V57, P853

[5]

BASU S, 2008, 18 S BOUND LAYERS TU

[6] An intercomparison of large-eddy simulations of the stable boundary layer [J].

Beare, RJ ;

MacVean, MK ;

Holtslag, AAM ;

Cuxart, J ;

Esau, I ;

Golaz, JC ;

Jimenez, MA ;

Khairoutdinov, M ;

Kosovic, B ;

Lewellen, D ;

Lund, TS ;

Lundquist, JK ;

McCabe, A ;

Moene, AF ;

Noh, Y ;

Raasch, S ;

Sullivan, P .

BOUNDARY-LAYER METEOROLOGY, 2006, 118 (02) :247-272

[7]

BELJAARS ACM, 1991, P ECMWF SEM NUM METH, P1

[8]

BETTS AK, 1975, J ATMOS SCI, V32, P1934, DOI 10.1175/1520-0469(1975)032<1934:PIOTWC>2.0.CO

[9]

[10] A scale-dependent Lagrangian dynamic model for large eddy simulation of complex turbulent flows [J].

Bou-Zeid, E ;

Meneveau, C ;

Parlange, M .

PHYSICS OF FLUIDS, 2005, 17 (02) :1-18

← 1 2 3 4 5 6 7 8 9 10 →