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Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence Research and Development Canada SW06 Post-Experiment Meeting

Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

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Page 1: Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

Airborne Magnetic Measurements Associated with SW06 Experiment

Will AveraPat Gallacher, Wayne KinneyNaval Research Laboratory

And

Brad NelsonDefence Research and Development Canada

SW06 Post-Experiment Meeting

Page 2: Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

Objective / Purpose

• Measure magnetic fields in the vicinity of NLIW’s

• Test theoretical predictions – Internal waves can produce measurable magnetic

signatures

Page 3: Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

Plan / Measurements

• 12 flight lines were collected over NLIWs on August 2, 2006– 4 lines @ 300’ (Lines 1,2,3,4)– 4 lines @ 500’ (Lines 5,6,11,12)– 2 lines @ 1000’ (Lines 7,8)– 2 lines @ 2000’ (Lines 9,10)– each line was ~ 10 minutes in length (~ 60 km) + 3 minutes per

corner– All lines were along the same track

• 39.5317 N , 73.6478 W to 38.9560 N , 73.0213 W

• Start point and bearing for this line were given to us by Jim Moum who was on the OCEANUS

• OCEANUS was in the middle of one NLIW packet

Page 4: Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

SW06

NRC Convair flight line

Simulations and Analysis -Very high resolution -MITgcm nonhydrostatic simulation -Forced with nested NCOM -Focus on nonlinear internal wave -Based on previous work including -MITgcm simulations of Hudson Canyon generation area -Nested NCOM simulations of high amplitude internal waves on shelf and slope in SW06

SW_06_new Domain (0.5km)current simulations

LBSF Domain (0.5km)future simulations

SW06 Moorings

Page 5: Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

The NRC Convair

• Convair data acquisition system – 3 Cesium total-field magnetometers– 2 vector magnetometers for compensation– Attitude and noise sensors– Post-processed DGPS navigation @ 4 Hz

Page 6: Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

500’ Results: Track Reproducibility : Lines 5,6,11,12

• Excellent reproducibility => Good geologic noise removal

All 4 Lines OverlyLine 11

Unfiltered

So

uth

No

rth

Page 7: Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

Magnetic Results: 500’ Alt - Lines 5, 6, 11, 12

• OCEANUS located near the internal wave activity • OCEANUS location sufficiently distant not to be disturbing measurements

NLIW ?

OCEANUS

Lt. Blue = Line 11

Ships > 1 mile off line

Black = Line 5

Blue = Line 6

Green =Line 12

Magnetic DataModel : U Velocity

1700 UT

1600 UT

1500 UT

Page 8: Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

Magnetic Results: 500’ Alt - Lines 5, 6, 11, 12

• OCEANUS located near the internal wave activity • OCEANUS location sufficiently distant not to be disturbing measurements

NLIW ?

OCEANUS

Lt. Blue = Line 11

Ships > 1 mile off line

Black = Line 5

Blue = Line 6

Green =Line 12

Magnetic DataModel : W Velocity

1700 UT

1600 UT

1500 UT

Page 9: Airborne Magnetic Measurements Associated with SW06 Experiment Will Avera Pat Gallacher, Wayne Kinney Naval Research Laboratory And Brad Nelson Defence

Conclusions (So Far)

• Data processing techniques – Appear to work for external magnetic noise reduction

• Anomalous residual noise on east side of the line is good candidate for NLIW – Jim Moum claimed the ship was in the middle of the NLIW– Residual noise correlated with OCEANUS position