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Published byJeremy Robertson Modified over 6 years ago
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ORCA-LIM experiments with the interannual Large & Yeager forcing
Claus Böning, Arne Biastoch, Ulf Schweckendiek, Sabine Hüttl, Joke Lübbecke (IFM-GEOMAR, Kiel) with special thanks to our French colleagues collaborating in the DRAKKAR project
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Examples of interannual-decadal variability in ORCA2 and ORCA05:
Tropical oceans: EUC and STC-transports, SST ACC (Drake Passage) transport Atlantic MOC transport [Sea ice coverage] Question: effect of long-term drifts in the CNYF-runs ?
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Tropical circulation: examples of spin-up behaviors (CORE-1)
EUC transports Sv GFDL Pacific ORCA2 years ORCA2 Atlantic ORCA05
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Pacific SST anomalies
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CORE-2: Pacific SST variability (Nino3): ORCA05 , ORCA2 vs. Data
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SST variability (Nino3-region) in ORCA05 vs. SOI index
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Pacific Subtropical-Tropical overturning Cells (STCs): Equatorward transports across 10°N/10°S
Sv ORCA05 ORCA2 robust trend ! (-14 Sv) shown here: Deviations from long-term means: 59 Sv (ORCA2), 67 Sv (ORCA05)
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Atlantic: SST anomalies after 50 yrs spin-up (CORE-1)
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SST variability (ATL4-region): ORCA05 vs. Reynolds
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Atlantic STC-index (8°N/8°S) ORCA05 – ORCA05 – ORCA2 – FLAME(1/3)
- trend: robust (+2 Sv) - year-to-year var.: differing - decadal variab. (> 5 yrs): fairly robust
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ORCA2 and MICOM (W.Hazeleger, KNMI)
Annual cycle of the EUC at 23°W (after 50-yr spin-up) ORCA and MICOM (W.Hazeleger, KNMI)
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ORCA2 - MICOM - ORCA05
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EUC (23°W) ORCA2 – MICOM - ORCA05 - FLAME1/12
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Regarding simulations of tropical variability:
CORE-II experiments help to identify where models are robust and where results are sensitive to model choices: - (inter-)decadal transport changes are very robust - seasonal-interannual variability: differs between realizations
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Drake Passage transport (two ORCA05-cases)
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Drake Passage transport anomalies (deviations from the climatological reference runs)
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Atlantic MOC (45°N)
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MOC anomalies (deviations from the climatological reference runs)
ORCA05 – 3 realizations FLAME-1/3° ORCA2 ORCA05
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