We present a new version of the global
atmospheric tracer transport model driven by analyzed meteorology with
diurnally varying mixing in the boundary layer capable of running globally at
resolutions up to quarter degree longitude-latitude or higher. The impact of
the higher resolution model can be visible in resolving city plumes, airmass
boundaries, diurnal cycle, fronts and synoptic scale events often observed in
continuous CO2 monitoring site data.
Author: S. Maksyutov, R. Onishi, G. Inoue, P.K. Patra, et al (onishi dot ryo at nies dot go dot jp)
Filesize: 53.22 Kb