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Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation • Detection of NLIW by Seafloor Pressure Measurement bottom landers with high-res pressure sensors Moum

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Page 1: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

• Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation

• Detection of NLIW by Seafloor Pressure Measurement

bottom landers with high-res pressure sensors

Moum

Page 2: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Named Waves Tracked• Alfred• Betty• Carlton• Debby• Elvin• Florence• George• Holly• Isaac• Jasmine• Kevin• Lola• Mika• Natalie• Oscar • …• Anya

NLIWI/SW06R/V Oceanus30 July – 26 Aug 2006

Science Party

Jim Moum OSUAlexander Perlin OSUGreg Avicola OSUEmily Shroyer OSUSam Kelly OSUMike Neeley-Brown OSURay Kreth OSU

Karen Fisher Los AlamosDezhang Chu WHOIDoris Leong DalhousiePaul Heslinga Falmouth Academy

Page 3: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

approaching wave train – < 5 kt windsview from flying bridge

Page 4: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Mika

Page 5: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Tonya / wave group interaction group-group interactions

wave-wave interactions

Page 6: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

SW37

SW38

SW39SW40

Page 7: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Oops! accidental sound source 02 August 2006 23:04:54

Page 8: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

high turbulence at interface

interfacial jets?

Page 9: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Shipboard profiling measurements

Page 10: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Varicose waveJasmine

Page 11: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Seafloor pressure measurements of nonlinear internal waves, submitted to J.Phys.Oceanogr., December 2006 (Moum & Nash)

Page 12: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Shoaling nonlinear internal waves: transition from depression to elevation waves. in prep, J.Phys.Oceanogr. (Shroyer, Moum & Nash)

Emily Shroyer

Knorr

Knorr

Page 13: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

120 kHz backscatter

successive transits along 300/120, 0.5 nm SW of main array axis

Page 14: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

pre-wave state

120 kHz backscatter

successive transits along 300/120, 0.5 nm SW of main array axis

Page 15: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

1200 kHz backscatter

successive transits along 300/120, 0.5 nm SW of main array axis

Page 16: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

Page 17: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

Page 18: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

Page 19: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

Page 20: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

Page 21: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

Page 22: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Wave Florence

Florence time/position diagrammean propagation speed 0.90 ms-1

Florence’s speed projected backward in time

We project the measured locations of the wave backward in space/time using the wave speed determined from the slope of the wave’s x-t plot to get an idea of what/where the wave was before it was clearly a wave. The result is the pre-wave state indicated several slides previous to this. This is helping us to decide what to look for in the generation region.

Page 23: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

pre-wave state

Wave Florence

Page 24: Wave-tracking Experiment to Assess NLIW Generation, Structure, Evolution and Dissipation Detection of NLIW by Seafloor Pressure Measurement bottom landers

Summary Topics of Interest

• wave pressure signature – submitted (Moum/Nash)

• shoaling / sign change – in prep. (Shroyer/Moum/Nash)

• physical structure – interfacial jets?

• energetics: evolution / transport / dissipation

• generation: bore / wave transition

• varicose waves

• wave-wave / group-group interactions