Differences

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--- aerocom:indirect [2013-10-15 16:56:16]
steve.ghan@pnnl.gov
+++ aerocom:indirect [2013-10-15 23:23:37]
steve.ghan@pnnl.gov
@@ Line 194: / Line 194: @@
     f3d(nx,nz) cloud fraction
     t3d(nx,nz) temperature
-    phase3d(nx,nz) cloud thermodynamic phase (0: entire cloud consists of ice, 1: entire cloud consists of liquid water, between 0 and 1: mixed-phase)
+    phase3d(nx,nz) cloud thermodynamic phase (0: entire cloud consists of ice,
+: entire cloud consists of liquid water, between 0 and 1: mixed-phase)
+    phase3d could be from fice3d/f3d where fice3d=ice+mixed phase cloud fraction
     cdr3d(nx,nz) in-cloud  droplet effective radius
     icr3d(nx,nz) in-cloud ice crystal effective radius
@@ Line 262: / Line 264: @@
  ==== Q/A ====
- *    2D cloud fields (lwp, iwp, cdr, cdnc, ttop, cod): Please compute them from grid-box mean values at each level but DO NOT divide by the total (2D) cloud cover, which will be done in analysis after averaging in time and space.
+ *    2D cloud fields (lwp, iwp, cdr, cdnc, ttop, cod): Please save them as grid-box mean values but DO NOT divide by the total (2D) cloud cover, which will be done in analysis after averaging in time and space.
  *    The three months 1 October - 31 December 2005  are thought as spin-up, which can of course be longer. Please choose as overlap assumption the one you use in the radiation scheme.