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Norwegian Meteorological Institute met.no R&D, Section Oceanography Norwegian Meteorological Institute met.no Spinning up on HYCOM at met.no: Early results with a hybrid-coordinate ocean model
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Norwegian Meteorological Institute met.no R&D, Section Oceanography ^ ^ Layer 1 target density ~ 1 Assume 1 < 1 Isopycnic interface adjustment: Hybrid coordinates Hybrid coordinate adjustment: /z-levels: sigma = D / N sigma n = max[ min,min( n, sigma )] ~ 11 00 p0p0 p1p1 p2p2
![Norwegian Meteorological Institute met.no R&D, Section Oceanography ^ ^ Layer 1 target density ~ 1 Assume 1 < 1 Isopycnic interface adjustment: Hybrid coordinates Hybrid coordinate adjustment: /z-levels: sigma = D / N sigma n = max[ min,min( n, sigma )] ~ 11 00 p0p0 p1p1 p2p2](http://images.slideplayer.com./15/4558151/slides/slide_2.jpg "Norwegian Meteorological Institute met.no R&D, Section Oceanography ^ ^ Layer 1 target density ~ 1 Assume 1 < 1 Isopycnic interface adjustment: Hybrid coordinates Hybrid coordinate adjustment: /z-levels: sigma = D / N sigma n = max[ min,min( n, sigma )] ~ 11 00 p0p0 p1p1 p2p2")
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Norwegian Meteorological Institute met.no R&D, Section Oceanography Baltic inflow Atlantic inflow Bottom topography outflow
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Norwegian Meteorological Institute met.no R&D, Section Oceanography sponge climatology weak A. inflow strong A. inflow weak A.+B. inflow strong A.+B. inflow Density cross-section (January)
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Norwegian Meteorological Institute met.no R&D, Section Oceanography climatology weak A. inflow weak A.+B. inflow spongestrong A. inflowstrong A.+B. inflow Salinity, layer 1
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Norwegian Meteorological Institute met.no R&D, Section Oceanography Density, layer 3 (target: 1.8) climatology sponge weak A. inflow strong A. inflow weak A.+B. inflow strong A.+B. inflow
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Norwegian Meteorological Institute met.no R&D, Section Oceanography climatology weak A. inflow weak A.+B. inflow spongestrong A. inflowstrong A.+B. inflow Thickness, layer 3
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Norwegian Meteorological Institute met.no R&D, Section Oceanography Density, layer 5 (target: 2.5) climatology weak A. inflow weak A.+B. inflow spongestrong A. inflowstrong A.+B. inflow
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Norwegian Meteorological Institute met.no R&D, Section Oceanography climatology weak A. inflow weak A.+B. inflow spongestrong A. inflowstrong A.+B. inflow Thickness, layer 5
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Norwegian Meteorological Institute met.no R&D, Section Oceanography Density: Climatology (top) vs. weak A. inflow (bottom) 25 4 3 6
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Norwegian Meteorological Institute met.no R&D, Section Oceanography Layer thickness: Climatology (top) vs. weak A. inflow (bottom) 25 4 3 6
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Norwegian Meteorological Institute met.no R&D, Section Oceanography Density: Climatology (top) vs. strong A.+B. inflow (bottom) 25 4 3 6
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Norwegian Meteorological Institute met.no R&D, Section Oceanography 25 4 3 6 Layer thickness: Climatology (top) vs. strong A.+B. inflow (bottom)
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Norwegian Meteorological Institute met.no R&D, Section Oceanography climatology weak A. inflow, low res. Density cross-section (January) weak A. inflow, high res.
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Norwegian Meteorological Institute met.no R&D, Section Oceanography climatology Salinity, layer 1 weak A. inflow, low res. weak A. inflow, high res.
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Norwegian Meteorological Institute met.no R&D, Section Oceanography Density: Climatology (top) vs. weak A. inflow, high res. (bottom) 25 4 3 6 Density: Weak A. inflow, high res. (top) vs. low res. (bottom)
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Norwegian Meteorological Institute met.no R&D, Section Oceanography Layer thickness: Weak A. inflow, high res. (top) vs. low res. (bottom) 25 4 3 6 Layer thickness: Climatology (top) vs. weak A. inflow, high res. (bottom)
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