[cam-users] Solar forcing
Peter Langen
plangen@gfy.ku.dk
Thu, 19 Dec 2002 10:10:03 +0100
Hi CCM (and CAM) users,
I'm running CCM366 with aqua planet/slab ocean lower boundary
conditions. I don't want an annual cycle in my experiments so I've just
set ECCEN=OBLIQ=0. However, under these conditions the solar flux at the
poles vanishes and I get an ever increasing equator-to-pole temperature
gradient. A proper way of fixing this is to use an annual mean diurnal
cycle corresponding to the pattern one obtains when averaging the
insolation at, say, 00:00 GMT each day of a year in every point. I
haven't made such at data set yet, but I don't think this will be the
problem.
The problem is how to get CCM366 to use this insolation. Also, it isn't
quite clear what to do with the zenith angle used both in the radiation
code and in the albedo calculations, since our artificial insolation
does not correspond to any physical zenith angle.
Has anybody tried working with the CCM without an annual cycle?
One other question (which I've seen also in the ccm-users archive -
without an answer): When running at T21 resolution the User's Guide says
to change the namelist variables DTIME, DIF2 and DIF4 from their default
T42 values, but the example script only changes DTIME. What about DIF2
and DIF4? In the CAM User's Guide DIF2 is left unchanged relative to the
T42 case while DIF4 is doubled. Until now I've just done the same with
CCM366, but is this the right thing to do?
Thanks
Peter Langen
--
Peter Langen
Niels Bohr Institute for Astronomy, Physics and Geophysics
Geophysical Department
University of Copenhagen