Instrumented Balloon Launches for ATTREX Dale Hurst, Emrys Hall, Allen Jordan Global Monitoring Division, NOAA Earth System Research Laboratory and CIRES,

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Presentation transcript:

Instrumented Balloon Launches for ATTREX Dale Hurst, Emrys Hall, Allen Jordan Global Monitoring Division, NOAA Earth System Research Laboratory and CIRES, University of Colorado, Boulder Boulder Balloon Soundings … still going strong after 33 years!

Ozonesonde Radiosonde NOAA FPH Air Intake Tubes Payload Weight: 2.0 kg (4.4 lb) Payload Size: 15” x 12” x 8” Instrument Payload

Payload Measurements PrimaryDataUncertainty Instrument MeasurementProduct(Stratosphere) NOAA FPHT FP H 2 O VMR<±10% (±0.5 ppmv) (custom)P P OzonesondeP O 3 O 3 VMR <±5% (±0.3 ppmv ) (DMT) RadiosondeT<±0.5° C (Intermet)P<±0.5 hPa 403 MHz RHNA > 12 km GPSpayload location, horizontal winds

Balloon Flight Profile Ascent Rate +5 m/s (1000 ft/s) Valve opens Descent Rate -5 m/s ~ 70 minutes ~ 90 minutes

Ideally … Coordination with GH flights 1 balloon launch per GH flight 4-6 flights anticipated (4 week window) Close spatiotemporal coincidence with GH Requires launch timing and trajectory to be coordinated with GH flight plan

Balloon Trajectory Prediction (2D)

Balloon Trajectory Prediction (3D)

Potential Launch Sites Andersen AFB NWS Facility

Ballooning over the Rockies

FPH Measurement Technique Stable Frost Layer = equilibrium between frost layer and water vapor in air flow P H 2 O = f(T FP )Clausius-Clapeyron equation (P sat over ice) H 2 O VMR = P H 2 O / (P air – P H 2 O ) Calibrated NIST scale PID Temp Controller