The 3 - year - mean anomalies correspond to a, b 240 — 242, c, d 243 — 245, and e, f 246 — 248 model years in
CTL run or 1 — 3, 4 — 6, and 7 — 9 years lead in the hindcast experiment.
To further elucidate at what soil depth multi-year predictability emerges, we calculated, for different depth ranges, the anomaly correlation skill between
the CTL run and the ensemble mean for the two geographic index regions.
Niño 3.4 index is obtained from SST anomalies (5 ° S — 5 ° N, 170 ° W — 120 ° W) in
the CTL run or ERSST for the 1850 — 2012 period.
We use
this CTL run as a surrogate «real» world and then evaluate the predictability by hindcasting this model simulated climate variability.
Left, center, and right panels are
the CTL run for 900 years, GPCC for the 1901 — 2012 period, and PREC / L for the 1948 — 2012 period.
Following a 100 - year coupled model spin - up, we perform a 900 - year - long pre-industrial control simulation (
CTL run) using constant greenhouse gas conditions for the year 1850 CE.
Not exact matches
Here is a nice option for those who are looking for a tablet
running Windows — the 2goPad SL10 Pro tablet from the Oregon based company
CTL.
CTL 2goPad SL10 Pro Windows tablet is comes with B / G / N wireless, 802.11 b / g / n WiFi, Bluetooth, Integrated 10/100 LAN, 3G ready with optional 3G card, Built - in HD Stereo Audio, and
runs Windows 7 Professional 32 - bit OS.
CTL is one of those elephants growing so large in the room that we have
run out of space to walk around it.
ANT = anthropogenic forcing NAT = natural forcing ALL = natural plus anthropogenic
CTL = preindustrial control
run SUL = sulfate aerosol forcings
Temporal evolution for three - year - mean anomalies of SLP (contoured) and total water storage (shaded; units are mm) in
CTL and the ensemble mean of hindcast
run initialized in 240.