Changes between Version 19 and Version 20 of doc/tec/sgs

Timestamp:

Apr 7, 2020 5:09:19 AM (5 years ago)

Author:

maronga

Comment:

--

doc/tec/sgs

@@ -1 +1 @@
 = Subgrid-scale Model =
 
-One of the main challenges in LES modeling is the turbulence closure. The filtering process yields four SGS covariance terms (see the first five equations Sect. [wiki:doc/tec/gov governing equations]) that cannot be explicitly calculated. In PALM, two different subgrid-scale models are available to parameterize the SGS terms:
+One of the main challenges in LES modeling is the turbulence closure. The filtering process yields four SGS covariance terms (see the first five equations Sect. [wiki:doc/tec/gov governing equations]) that cannot be explicitly calculated. In PALM, three different subgrid-scale models are available to parameterize the SGS terms:
 * [#deardorff_sgs Deardorff subgrid-scale model]
+* [#deardorff_sgs Deardorff subgrid-scale model (modified)]
 * [#dynamic_sgs Dynamic subgrid-scale model]
- which are described below.
+
 
 Selecting one of the available SGS models is done via the namelist parameter [/wiki/doc/app/inipar#turbulence_closure turbulence_closure]. 
@@ -196 +197 @@
 == References ==
 
-* [=dai]'''Dai, Y., Basu, S., Maronga, B., de Roode, SR.''' 2020. Addressing the Grid-size Sensititivty Issue in Large-eddy Simulations of Stable Boundary Layers. Boundary-layer Meteorol., submitted. http://arxiv.org/abs/2003.09463.
+* [=#dai]'''Dai, Y., Basu, S., Maronga, B., de Roode, SR.''' 2020. Addressing the Grid-size Sensititivty Issue in Large-eddy Simulations of Stable Boundary Layers. Boundary-layer Meteorol., submitted. http://arxiv.org/abs/2003.09463.
 
 * [=#deardorff]'''Deardorff JW.''' 1980. Stratocumulus-capped mixed layers derived from a three-dimensional model. Bound.-Lay. Meteorol. 18: 495–527.