Changes between Version 35 and Version 36 of user/ctlod/NewSurfaceModule

Timestamp:

2008-02-14T16:30:54+01:00 (16 years ago)

Author:

ctlod

Comment:

--

user/ctlod/NewSurfaceModule

@@ -77 +77 @@
 In doing that we are closer to what is done in limdyn.F90 of the NEW SBC.[[BR]]
 It results in a sea-ice surface temperature colder O(-1/2°C) than in SDP Ref mainly in the limit sea-ice extent.[[BR]]
-And a systematic decrease of the icet thickness by O(-2/4 cm) over all the Arctic reaching in some area O(-10 cm) Hudson bay or near 
-the Bering strait.[[BR]]
-So its impact is significant and must be take into account in the rewritten of this part in the NEW _SBC.
+And a systematic decrease of the icet thickness by O(-2/4 cm) over all the Arctic reaching in some area O(-10 cm) 
+Hudson bay or near the Bering strait.[[BR]]
+So its impact is significant and must be take into account in the rewritten of this part in the NEW _SBC.[[BR]]
 [[Color(white,red,'''BUT''')]] it remains a bug in the comptutation of zt11, zt12 ..etc see SDP6 experience below[[BR]]
 
@@ -111 +111 @@
 }}}
 The impact of this modification is weak as seen on plots below change in ice thickness are O(±1/2 cm)) 
-in Arctic during winter (March). Same behaviour in summer (Sept).
+in Arctic during winter (March). Same behaviour in summer (Sept).[[BR]]
 '''Ice thickness diffs. between REF_CORE SDP4 - REF_CORE SDP / Year 10 / Winter March''':[[BR]]
 [[Image(SDP4_Ref_SDP_Ref_icethic_March.png, 90%)]]
@@ -135 +135 @@
 '''Ice thickness differences between New SDP3 - New SDP experience / Year 10 / Winter March''':[[BR]]
 ''In SDP3 the sea-ice velocity [uv]i_ice() is removed from the computation of sea-ice wind-stress and
-&  scalar wind-stress in sbc_blk_ice() whereas it is used in SDP experience, it is the only thing which changes 
-between the 2''[[BR]]
+&  scalar wind-stress in sbc_blk_ice() whereas it is used in SDP experience, it is the only thing which changes between the 2''[[BR]]
 This modification implies a weaker extension off the east Greenland coast and north to the Spitzberg.[[BR]]
 A lightly increasing of the ice thickness close to the Greenland and North to the Bering strait area O(+2cm)