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The North Icelandic Jet and its contribution to the Denmark Strait overflow water in a high-resolution ocean model Carlo Corsaro, Univ. Catania (IT) Andreas Sterl, KNMI (NL)

The North Icelandic Jet and its contribution to the ... · 20.06.2013 A. Sterl; Argo Workshop, Southampton The model NEMO in ORCA025 config (0.25 deg, but higher in Nordic Seas) 46

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Page 1: The North Icelandic Jet and its contribution to the ... · 20.06.2013 A. Sterl; Argo Workshop, Southampton The model NEMO in ORCA025 config (0.25 deg, but higher in Nordic Seas) 46

The North Icelandic Jet and its contribution to the

Denmark Strait overflow water in a high-resolution

ocean model

Carlo Corsaro, Univ. Catania (IT)Andreas Sterl, KNMI (NL)

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20.06.2013A. Sterl; Argo Workshop, Southampton

1. open-ocean convection in Nordic Seas => overflow

2. via EGC; derived from boundary current

Våge et.al, (2011): large and densest part from NIJ

Mixing (no mass transport) in interior Nordic Seas => NIJ

Sinking (mass transport): NIIC => NIJ

Origin of DSOW

Våge et.al, 2011

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20.06.2013A. Sterl; Argo Workshop, Southampton

The model● NEMO in ORCA025 config (0.25 deg, but higher in Nordic Seas)● 46 layers● Stand-alone● Sub-surface restoring● 45 years (ERA-40 period)● Here: last 25 years● DFS3 forcing (derived from ERA-40)● Output: 5-day averages● Here: monthly-means

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20.06.2013A. Sterl; Argo Workshop, Southampton

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20.06.2013A. Sterl; Argo Workshop, Southampton

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20.06.2013A. Sterl; Argo Workshop, Southampton

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9 m452 m

EGCRim current

NIJ

NIIC

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Transports

observation model

NIIC 0.75 / 1.5 1.2 – 1.35

NIJ (20ºW) 1.5 ± 0.2 1.2 ± 0.3

DSOW 2.9 – 3.7 3.2 ± 0.7

... are well reproduced by the model

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20.06.2013A. Sterl; Argo Workshop, Southampton

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Atl origin: > 0 C, Norwegian continental slopeArctic origin: < 0 C, interior GIN Sea

Våge et.al, 2011

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Transports along path of NIIC and NIJ

NIIC

― NIJ (σθ > 27.8 kg/m3)

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+0.45 Sv

+ 0.16 Sv

+0.41 Sv

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NIIC● Flows eastward along north coast of Iceland● Depth range 100 – 200 m● Joins Nordic Seas rim current at the NE corner of Iceland● Cools/densifies at surface, but not at depth● Hardly looses mass (0.1 Sv sinking)● No interaction with NIJ (no correlations)

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NIJ● Flows westward along north coast of Iceland● Depth range surface to bottom, but maximum around 400 m● Does not exist east of 14-15 ºW● Increases from 0.1 to 1 Sv● Hardly any densification● Is fed by Nordic Seas rim current● Contributes about 1/3 of DSOW

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Where does DSOW come from?

1. intermediate depth (400 m), western slope

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Where does DSOW come from?

2. deep (534 m), eastern slope

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What feeds the NIJ and where does it go to?

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NIJ at 17.5˚W

NIJ at 20˚W

EGC

NIJ(20˚W)+EGC

DSOW

σθ > 27.8 kg/m3

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Summary

● No interaction between NIIC and NIJ (diff from Våge et al., 2011)

● NIJ is fed by Nordic Seas rim current - kind of loop- water from interior mixed in?

● 1/3 of DSOW from NIJ, other 2/3 from EGC