| Section |
Code |
Longitude |
Name |
| M |
129 |
220 |
Potential temperature |
| M |
130 |
220 |
Salinity |
| M |
131 |
220 |
u-velocity |
| M |
132 |
220 |
v-velocity |
| M |
133 |
220 |
w-velocity |
The following accumulated fields are written once per month during the
forecasts. Monthly means can be derived from them. They are the main fields
for diagnosing the oceanic behaviour of the coupled model forecasts.
Accumulated horizontal fields are:
| Section |
Code |
Depth |
Name |
| H |
129 |
5 |
Potential temperature |
| H |
130 |
5 |
Salinity |
| H |
131 |
5 |
u-velocity |
| H |
132 |
5 |
v-velocity |
| H |
145 |
0 |
Sea level |
| H |
148 |
0 |
Mixed layer depth |
| H |
163 |
0 |
Depth of 20 deg isotherm |
| H |
164 |
0 |
T averaged over upper 300m |
| H |
175 |
0 |
S averaged over upper 300m |
| H |
153 |
0 |
Zonal wind stress |
| H |
154 |
0 |
Meridional wind stress |
| H |
156 |
0 |
Net surface heat flux |
| H |
157 |
0 |
Absorbed solar radiation |
| H |
158 |
0 |
Precipitation - Evaporation |
Accumulated vertical zonal sections are:
| Section |
Code |
Latitude |
Name |
| Z |
129 |
0 |
Potential temperature |
| Z |
130 |
0 |
Salinity |
| Z |
131 |
0 |
u-velocity |
| Z |
133 |
0 |
w-velocity |
Accumulated vertical meridional sections are:
| Section |
Code |
Longitude |
Name |
| M |
129 |
60E/90E/165E/180/140W/95W/30W/10W |
Potential temperature |
| M |
130 |
60E/90E/165E/180/140W/95W/30W/10W |
Salinity |
| M |
131 |
60E/165E/140W/30W |
u-velocity |
| M |
132 |
60E/165E/140W/30W |
v-velocity |
| M |
133 |
60E/165E/140W/30W |
w-velocity |
| M |
138 |
60E/165E/140W/30W |
Potential density |
Several so-called time series fields are also produced. These allow detailed
examination of the evolution of certain fields along given lines of latitude
or longitude. In all cases the temporal resolution is daily.
Lines of latitude are:
| Section |
Code |
Depth |
Latitude |
Name |
| Z |
129 |
5 |
0 |
Potential temperature |
| Z |
131 |
5 |
0 |
U velocity |
| Z |
145 |
0 |
0 |
Sea level |
| Z |
163 |
0 |
0 |
Depth of 20 deg isotherm |
| Z |
153 |
0 |
0 |
Zonal wind stress |
| Z |
164 |
0 |
8N/5N/0/5S/8S |
T averaged over upper 300m |
Lines of longitude are:
| Section |
Code |
Depth |
Longitude |
Name |
| M |
129 |
5 |
180/60W |
Potential temperature |
| M |
145 |
0 |
180/60W |
Sea level |
| M |
148 |
0 |
180/60W |
Mixed layer depth |
Finally, a small selection of instantaneous fields is output daily, to
allow study of the evolution of the system on synoptic timescales. The
fields concerned are:
| Section |
Code |
Depth |
Name |
| H |
129 |
5 |
Potential temperature |
| H |
145 |
0 |
Sea level |
| H |
148 |
0 |
Mixed layer depth |
| M |
129 |
0 |
Potential temperature |
Monthly archive of ocean fields (accelerated forecast):
Since the ocean analysis lags about 12 days behind real time, the ocean
model is integrated from the last ocean analysis forced by analyzed wind
stress, heat fluxes and P-E. During this "ocean forecast", teh
sea surface temperature is relaxed towards persisted SST, with a damping
rate of 100W/m2/K.
Forcing fields (type ff):
The time-averaged fields used to force the ocean during the 12 days of
ocean integration are archived on MARS:
| Section |
Code |
Depth |
Name |
| H |
157 |
0 |
Absorbed solar radiation |
| H |
161 |
0 |
Diagnosed sea surface temperature error |
| H |
162 |
0 |
Heat flux correction |
| H |
156 |
0 |
Net surface heat flux |
| H |
129 |
0 |
Ocean potential temperature |
| H |
158 |
0 |
Precipitation-evaporation |
| H |
159 |
0 |
Specified sea-surface temperature |
| H |
160 |
0 |
Specified surface heat flux |
| H |
153 |
0 |
u stress |
| H |
154 |
0 |
v stress |
Ocean Fields (type of):
Same fields as for for the operational
ocean analysis. The list includes all the fields stored during coupled
integrations but with a much larger number of levels, longitude and latitude
lines.