|
|
| [Science] [BAS home] [Met home] [Beowulf home] | Antarctic Meteorology |
jobsheet
The ocean to ice heat flux is calculated as:
OI_hf = OI_hf_hadcm3 * (ocean_ice_shear) / tie_point_speedIn this run the tie point is set at 5 cm/s: where the shear is greater than this, the OI flux is higher; where less, lower. At most points away from the coastline around Antarctica, its higher. See Fortran mods for the code (hand-edit to 5 cm/s not 10).
| Past last modified: 9/12/2002 / wmc@bas.ac.uk |
© Copyright Natural Environment Research Council - British Antarctic Survey 2002 |