Solar penetration depths

Posted by on Aug 28, 2015 in Abstracts, Abstracts 2015

Impact of different solar penetration depths on climate simulations


Three different estimates of shortwave attenuation depth (SWAD) of photosynthetically active radiation (PAR) derived from remotely sensed ocean colour data have been tested in an ocean general circulation model (OGCM) forced with interannual atmospheric forcings.  Two estimates (referred to as Kd(PAR]_1^-1 and Kd(PAR]_2^-1 are calculated from different algorithms based on the diffusive attenuation coefficient at 490 nm and the third one (Kd(AVE]_1^-1) is just an average of Kd(PAR]_1^-1 and Kd(PAR]_2^-1.  Kd(PAR]_2^-1 is larger than Kd(PAR]_1^-1 almost everywhere in the tropical oceans.

Our results show that the OGCM with Kd(PAR]_2^-1 produces warmer sea surface temperature (SST) in the eastern equatorial Pacific and Atlantic and leads to reduce a cold bias in the equatorial cold tongue regions. It has warmer subsurface temperatures in the low latitude, a slower meridional velocity and Pacific equatorial undercurrent (EUC) than the model with Kd(PAR]_1^-1.  These results are similar to previous studies, although we use a different model and different methods. This study has further analysis and firstly reveals that slower EUC and meridional velocity in the model with Kd(PAR]_2^-1 are mainly related to the changes of the acceleration due to zonal density gradient.  This acceleration driving the EUC eastward in the subsurface becomes smaller in the subsurface along the equatorial Pacific. However, near the sea surface, the zonally averaged accelerations over the different ocean basins are larger in the model with Kd(PAR]_2^-1 than that with Kd(PAR]_1^-1, which pushes back the poleward meridional transport. The interannual variability in the model with Kd(PAR]_2^-1 is generally weaker than that in the experiment with Kd(PAR]_1^-1 due to a deeper mixed layer depth. The vertical temperature errors averaged horizontally within the domain of 30degS to 30degN in the experiment with (Kd(AVE]_1^-1) are almost in the middle of errors of the other two experiments. This indicates that the effect of the SWAD on the simulation of the vertical temperature profile is largely linear.