[ Derived from parent entry - See data hierarchy tab ] ECHO-G (ECHAM4/HOPE-G) 300-year control simulations ("CTL") were performed with the same initial condition with SRES "A2Ga" and "B2Ga" simulations but with fixed GHG concentration values at 1990. Initial condition was obtained by spinning up the ECHO-G for five years with the restart file of HOPE-G at the model year 311 in the 1000-year control runs (Min et al. 2004, M&D Tech. Report No. 2, http://www.mad.zmaw.de/Pingo/reports/TeReport_Web02.pdf) and climatology of ECHAM4. Flux corrections are applied only for annual mean heat and moisture fluxes, but no corrections for momentum flux. The model was run on a NEC SX-4 at the KMA, Seoul, Korea.
[1] DOIMin, Seung-Ki; Legutke, Stephanie; Hense, Andreas; Kwon, Won-Tae. (2005). Internal variability in a 1000-yr control simulation with the coupled climate model ECHO-G — I. Near-surface temperature, precipitation and mean sea level pressure. doi:10.3402/tellusa.v57i4.14712
[2] DOIMin, Seung-Ki; Legutke, Stephanie; Hense, Andreas; Kwon, Won-Tae. (2005). Internal variability in a 1000-yr control simulation with the coupled climate model ECHO-G — II. El Niño Southern Oscillation and North Atlantic Oscillation. doi:10.3402/tellusa.v57i4.14711
[3] DOIMin, Seung-Ki; Legutke, Stephanie; Hense, Andreas; Cubasch, Ulrich; Kwon, Won-Tae; Oh, Jae-Ho; Schlese, Ulrich. (2006). East Asian Climate Change in the 21st Century as Simulated by the Coupled Climate Model ECHO-G under IPCC SRES Scenarios. doi:10.2151/jmsj.84.1
Parent
ECHOG_SRES_CTL_MM: 300 years control run monthly mean values