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UAV observations of the wintertime boundary layer over the Terra Nova Bay polynya John Cassano and Shelley Knuth Department of Atmospheric and Oceanic Sciences Cooperative Institute for Research in Environmental Sciences University of Colorado

UAV observations of the wintertime boundary layer over the Terra Nova Bay polynya

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UAV observations of the wintertime boundary layer over the Terra Nova Bay polynya. John Cassano and Shelley Knuth Department of Atmospheric and Oceanic Sciences Cooperative Institute for Research in Environmental Sciences University of Colorado. Project Overview. - PowerPoint PPT Presentation

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Page 1: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

UAV observations of the wintertime boundary layer over the Terra Nova Bay polynya

John Cassano and Shelley KnuthDepartment of Atmospheric and Oceanic Sciences

Cooperative Institute for Research in Environmental SciencesUniversity of Colorado

Page 2: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Project Overview

• Use Aerosonde unmanned aerial vehicles (UAVs) to make meteorological measurements in the vicinity of Terra Nova Bay

• Why Terra Nova Bay?– Location of recurring polynya– Region of strong katabatic winds– Source region for Antarctic bottom water

• Prior to this project there were no in-situ atmospheric measurements of the wintertime atmosphere over the Terra Nova Bay polynya

Page 3: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

MODIS-Terra 04-Oct 2005

Page 4: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Science Questions• What atmospheric processes control the size

of the Terra Nova Bay polynya?– Winds?– Surface energy budget?

• How do changes in the atmospheric state alter the amount of heat and moisture removed from the ocean in the polynya?– What impact does this have on the development

of Antarctic bottom water?• How does the presence of the polynya modify

the katabatic airstream as it passes over the polynya?

Page 5: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Aerosonde UAV

Page 6: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Wingspan 3 metersWeight 15 kgPayload Capacity

2-5 kg

Endurance 12-17+ hrsRange 1000+ km

Altitude 100-6000 m

Communications via 900 MHz radio and Iridium

Flies in fully autonomous mode with user-controlled capability

Aerosonde UAV

Page 7: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Wind Speed/Direction Pitot with GPSRH/Temp/Pressure Standard Radiosonde Met

SensorsOcean /Ice Skin

TemperatureInfrared Thermometer

Ocean/Ice Visible Imagery

Still Digital Camera

Net Shortwave Radiation

Pyranometer

Net Longwave Radiation

Pyrgeometer

RH/T/P/wind profiles DropsondesAltitude and Surface

WavesLaser Altimeter

Aerosonde Measurements

Page 8: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

The Challenges

• Cold temperatures– Impacted:• Engine• Parts failure

• Communication failures• Wind– Take-off / landing– In flight winds

• Aircraft icing

Page 9: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Aerosonde LaunchPegasus Runway (14 Sept 2009)

Page 10: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Aerosonde RecoveryPegasus Runway (7 Sept 2009)

Page 11: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

• 16 flights– 8 science flights to TNB

• 11000 km (7000 miles)• 130 flight hours

Page 12: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

14 September 2009

• First successful TNB flight

• 15 hour flight• 1230 km (750 miles)• Max wind speed

29.1 m/s (65 mph)

Page 13: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya
Page 14: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Aerial Photos

• Local test flight 9 Sept 2009

• Aerial survey of Pegasus runway

• Flown at 1000 m altitude

Page 15: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Pegasus Runway

Mosaic courtesy of Jim Maslanik

Page 16: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya
Page 17: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya
Page 18: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Aerial Photos of TNB Polynya22 September 2009

Page 19: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Complex rafting and finger rafting: Produces accumulation of ice mass within thin-ice locations

Image width: 70m

Photo location shown in MODIS satellite image

Courtesy of Jim Maslanik

Page 20: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Nilas ice forming in area of relatively calm winds. Sea smoke is also present.

Frazil ice in location of strong winds, including waves with white caps.

Courtesy of Jim Maslanik

Page 21: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Frazil and pancake ice accumulating to form a band of thicker ice

Courtesy of Jim Maslanik

Page 22: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Pancake ice, with largest floes averaging about 2m diameter

Courtesy of Jim Maslanik

Page 23: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Ridging within consolidated pack ice. Ridging indicates thicker ice compared to locations with rafted ice.

Courtesy of Jim Maslanik

Page 24: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

TNB Air Mass Modification

• 24 September 2009• Two plane mission to

Terra Nova Bay• Determine modification

of katabatic air stream as it passes over polynya

Page 25: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Cross-wind Leg: Wind Speed

Page 26: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya
Page 27: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Temperature

100-600 m layer: ~2 K warmingSHF Profile 1-2: ~608 W/m2 (10.6 km)SHF Profile 2-3: ~580 W/m2 (11.8 km)SHF Profile 3-4: ~83 W/m2 (24.1 km)SHF Profile 1-4: ~327 W/m2 (46.5 km)

Page 28: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Relative Humidity

100-600 m layer: 125% inc. in specific humidity

LHF Profile 1-2: ~63 W/m2 (10.6 km)LHF Profile 2-3: ~161 W/m2 (11.8 km)LHF Profile 3-4: ~86 W/m2 (24.1 km)LHF Profile 1-4: ~101 W/m2 (46.5 km)

Page 29: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Wind Speed

Page 30: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Future Work• Estimate surface turbulent sensible and latent heat fluxes

– Bulk method– Compare to fluxes estimated from air mass modification

(profiles)• Estimate turbulent momentum flux to surface• What are the dynamics responsible for the downwind

modification of the katabatic jet?• Is polynya opening / closing driven by winds or changes in

the surface energy budget?• Repeat UAV observations when high vertical resolution

mooring is present in TNB

Page 31: UAV observations of the wintertime boundary layer over the Terra Nova Bay  polynya

Questions?