13 |
C > 0 for increase in uVel, which is west to |
C > 0 for increase in uVel, which is west to |
14 |
C east for cartesian and spherical polar grids |
C east for cartesian and spherical polar grids |
15 |
C Typical range: -10 < uwind < 10 |
C Typical range: -10 < uwind < 10 |
|
C Southwest B-grid U point |
|
16 |
C |
C |
17 |
C vwind :: Surface (10-m) meridional wind velocity in m/s |
C vwind :: Surface (10-m) meridional wind velocity in m/s |
18 |
C > 0 for increase in vVel, which is south to |
C > 0 for increase in vVel, which is south to |
19 |
C north for cartesian and spherical polar grids |
C north for cartesian and spherical polar grids |
20 |
C Typical range: -10 < vwind < 10 |
C Typical range: -10 < vwind < 10 |
|
C Southwest B-grid V point |
|
21 |
C |
C |
22 |
C evap :: Evaporation in m/s |
C evap :: Evaporation in m/s |
23 |
C > 0 for increase in salt (ocean salinity) |
C > 0 for increase in salt (ocean salinity) |
24 |
C Typical range: 0 < evap < 2.5e-7 |
C Typical range: 0 < evap < 2.5e-7 |
|
C Southwest B-grid tracer point |
|
25 |
C |
C |
26 |
C precip :: Precipitation in m/s |
C precip :: Precipitation in m/s |
27 |
C > 0 for decrease in salt (ocean salinity) |
C > 0 for decrease in salt (ocean salinity) |
28 |
C Typical range: 0 < precip < 5e-7 |
C Typical range: 0 < precip < 5e-7 |
|
C Southwest B-grid tracer point |
|
29 |
C |
C |
30 |
C runoff :: River and glacier runoff in m/s |
C runoff :: River and glacier runoff in m/s |
31 |
C > 0 for decrease in salt (ocean salinity) |
C > 0 for decrease in salt (ocean salinity) |
32 |
C Typical range: 0 < runoff < ???? |
C Typical range: 0 < runoff < ???? |
|
C Southwest B-grid tracer point |
|
33 |
C |
C |
34 |
C atemp :: Surface (2-m) air temperature in deg K |
C atemp :: Surface (2-m) air temperature in deg K |
35 |
C Typical range: 200 < atemp < 300 |
C Typical range: 200 < atemp < 300 |
|
C Southwest B-grid tracer point |
|
36 |
C |
C |
37 |
C aqh :: Surface (2m) specific humidity in kg/kg |
C aqh :: Surface (2m) specific humidity in kg/kg |
38 |
C Typical range: 0 < aqh < 0.02 |
C Typical range: 0 < aqh < 0.02 |
|
C Southwest B-grid tracer point |
|
39 |
C |
C |
40 |
C swdown :: Downward shortwave radiation in W/m^2 |
C swdown :: Downward shortwave radiation in W/m^2 |
41 |
C > 0 for increase in theta (ocean warming) |
C > 0 for increase in theta (ocean warming) |
42 |
C Typical range: 0 < swdown < 450 |
C Typical range: 0 < swdown < 450 |
|
C Southwest B-grid tracer point |
|
43 |
C |
C |
44 |
C lwdown :: Downward longwave radiation in W/m^2 |
C lwdown :: Downward longwave radiation in W/m^2 |
45 |
C > 0 for increase in theta (ocean warming) |
C > 0 for increase in theta (ocean warming) |
46 |
C Typical range: 50 < lwdown < 450 |
C Typical range: 50 < lwdown < 450 |
|
C Southwest B-grid tracer point |
|
47 |
C |
C |
48 |
C |
C |
49 |
C NOTES: |
C NOTES: |
50 |
C ====== |
C ====== |
51 |
C |
C |
52 |
|
C All surface forcing fields are defined at the center of |
53 |
|
C each grid (the rVel location in model/inc/GRID.h). |
54 |
|
C |
55 |
C #ifdef SEAICE_EXTERNAL_FORCING, sea-ice forcing fields |
C #ifdef SEAICE_EXTERNAL_FORCING, sea-ice forcing fields |
56 |
C are defined in exf_fields.h |
C are defined in exf_fields.h |
57 |
C |
C |
58 |
C #ifdef SEAICE_EXTERNAL_FLUXES, additional forcing fields, fu, |
C #ifdef SEAICE_EXTERNAL_FLUXES, additional forcing fields, fu, |
59 |
C fv, Qnet, Qsw, and EmPmR, as defined in FFIELDS.h, are required. |
C fv, Qnet, Qsw, and EmPmR, as defined in FFIELDS.h, are required. |
60 |
C |
C |
|
C If (SEAICEwindOnCgrid .EQ. .TRUE.), uwind and vwind are |
|
|
C defined on southwest C-grid U and V points, respectively. |
|
|
C |
|
61 |
C Downward and net radiative fluxes are not the same !!! |
C Downward and net radiative fluxes are not the same !!! |
62 |
C Downward radiative fluxes, swdown and lwdown, are used by |
C Downward radiative fluxes, swdown and lwdown, are used by |
63 |
C radiation bulk formulae to compute net radiative fluxes. |
C radiation bulk formulae to compute net radiative fluxes. |