Changes between Version 9 and Version 10 of doc/tec/topography

Timestamp:

Jun 6, 2017 2:10:27 PM (8 years ago)

Author:

suehring

Comment:

--

doc/tec/topography

@@ -217 +217 @@
 \begin{verbatim}
 TYPE surf_type
-    INTEGER(iwp), DIMENSION(:), ALLOCATABLE ::  I, j, k
-    REAL(wp), DIMENSION(:), ALLOCATABLE ::  shf
-    . 
-    . 
-    .
+    INTEGER(iwp), DIMENSION(:), ALLOCATABLE ::  i
+    INTEGER(iwp), DIMENSION(:), ALLOCATABLE ::  j
+    INTEGER(iwp), DIMENSION(:), ALLOCATABLE ::  k
+    REAL(wp),     DIMENSION(:), ALLOCATABLE ::  shf
+    ...
 END TYPE surf_type 
 \end{verbatim}
@@ -239 +239 @@
 }}}
 
-The term ''def'', ''lsm'', ''usm'' indicates the type of surface, i.e. default-type, natural-type, or urban-type, respectively, while the term at the end indicates either horizontal  ''h'' or vertical surfaces ''v''.  For the different kinds of surfaces, partly different code is executed. \\
-
-For all the different surface types, MOST (see ...) is applied to model surface fluxes of momentum. 
-For default-type surfaces, surface fluxes of latent and sensible heat as well as scalars are either prescribed or model by MOST.
-In contrast, for natural- and urban-type surfaces, an energy-balance solver is applied in order to model surface fluxes of sensible and latent heat.  \\
+The term ''def'', ''lsm'', ''usm'' indicates the type of surface, i.e. default-type, natural-type, or urban-type, respectively, while the term at the end indicates either horizontal  ''h'' or vertical surfaces ''v''.  For the different kinds of surfaces, partly different code is executed.
+For example, for natural- and urban-type surfaces, an energy-balance solver is applied according to the land-surface and urban-surface model, respectively, in order to model surface fluxes of sensible and latent heat.  \\
 
 Further, in addition to the different types of surfaces, surface elements are further distinguished according to its orientation: \\