liess@umn_edu
New Member
Hi,
We are running CAM3-1.1.p1 on a 10 node dual quadcore 3.0GHz Xeon/16GB RAM system with PGI 7.1-5 and 1 MPI process per compute node and 8 OpenMP threads (OpenMPI 1.2.5) per node.
Validating the first couple of days of our climatological SST runs with the procedure described in http://www.ccsm.ucar.edu/models/atm-cam/port/ results in reasonable results within the specified error range. Also global averages of years 6-15 (we omitted the first 5 years due to spin-up) are similar to the climatology at http://www.ccsm.ucar.edu/models/atm-cam/sims/cam3.0/eul128x256_d50/climo_files/ .
However, when plotting global maps for each month, we see differences of 5K in Surface Temperature and Reference Height Temperature with one negative peak over Siberia and a positive peak over Alaska during DJF and a similar pattern over the same longitudes over the Antarctic in JJA when comparing our results to the monthly mean climo_files mentioned above. Should we concerned about this or is it part of model uncertainties, when running on different architectures? The radiation budget (FSNT and FSNTOA) shows a few differences over 20 W/m**2, but looks generally OK. We are especially interested in results over the Arctic.
Thanks in advance and best regards,
Stefan
We are running CAM3-1.1.p1 on a 10 node dual quadcore 3.0GHz Xeon/16GB RAM system with PGI 7.1-5 and 1 MPI process per compute node and 8 OpenMP threads (OpenMPI 1.2.5) per node.
Validating the first couple of days of our climatological SST runs with the procedure described in http://www.ccsm.ucar.edu/models/atm-cam/port/ results in reasonable results within the specified error range. Also global averages of years 6-15 (we omitted the first 5 years due to spin-up) are similar to the climatology at http://www.ccsm.ucar.edu/models/atm-cam/sims/cam3.0/eul128x256_d50/climo_files/ .
However, when plotting global maps for each month, we see differences of 5K in Surface Temperature and Reference Height Temperature with one negative peak over Siberia and a positive peak over Alaska during DJF and a similar pattern over the same longitudes over the Antarctic in JJA when comparing our results to the monthly mean climo_files mentioned above. Should we concerned about this or is it part of model uncertainties, when running on different architectures? The radiation budget (FSNT and FSNTOA) shows a few differences over 20 W/m**2, but looks generally OK. We are especially interested in results over the Arctic.
Thanks in advance and best regards,
Stefan