cloud microphysical properties measured from commercial aircraft karl beswick and martin gallagher...
TRANSCRIPT
Cloud Microphysical Properties Measured from Commercial Aircraft
Karl Beswick and Martin GallagherUniversity of Manchester, United Kingdom
Darrel BaumgardnerCentro de Ciencias de la Atmósfera, UNAM, México
Roy NewtonDroplet Measurement Technologies, USA
3rd International Conference on Transport, Atmosphere and Climate25-28 June 2012
Prien am Chiemsee, Germany
Acknowledgements
• IAGOS• Mike Poellet and David Delene
University of North Dakota• Bill Dawson
Droplet Measurement Technologies• Sarah Lance
NOAA/CIRES• UK Facility for Ground based Measurements
A facility of the UK National Centre for Atmospheric Science• This work has been supported in the UK by the
NERC and FAAM.
Presentation Guide
• Background
• Instrument Description
• Laboratory Studies
• Preliminary Results
• Next Generation BCP
Background
• IAGOSis a program for long-term observations of atmospheric composition on a global scale from a fleet of long-range aircraft.
• Allows the collection of observations on a scale impossible to achieve using research aircraft.
• Large scale measurements of cloud microphysical properties will help climate modelers improve and validate their models and provide extensive data to improve retrieval algorithms for satellite measurements.
• Particles pass through open laser beam
• Scattered light in the 144-156° cone is collected by photo-detector
• Signal is amplified, digitised and sized into size bins, size range 5-75µm diameter.
• No sample volume qualification: mathematical inversion is required.
BCP (Backscatter Cloud Probe)
12.5 cm
Flight Testing FAAM BAe 146
CDP 2-50 µmBCP 5-75 µmCAS 0.6-50 µmBCPD 1-50 µm
Example Data Sets NOTE: “Liquid Water” traces are NOT fully corrected
and NOT relevant to cirrus ice clouds – only used as indicator of relative volume changes.
No T-Matrix corrections applied to size distributions for suspected ice conditions.
Particle Size Distribution data is currently produced using Version 2 of the backscatter retrieval algorithm.
sizing camera
diagnostic camera
Evaporation tube, containing droplet generator
precision X-Y adjustable platform
water and air supplies
Beam mapping with droplet stream was conducted at the NOAA/Boulder Laboratory (courtesy of Sara Lance)
Computer controlled 3D micro-positioning stages (0.5 µm
accuracy)
Piezo electric droplet generator
High speed CCD imaging camera and microscope objective
Glare CCD
camera
Air drier
Liquid pump and solution reservoir
Auto-scanning micro-positioner to direct mono-disperse dropletsReproducible size AND Concentration. IAGOS Facility – Manchester (with thanks to Sara Lance)
Positioner rodSheath air
intake
Sheath flow
straighter
Evaporation flow tubeFlow tube nozzle
Interchangeable
Glare CCD
camera
Two Sizing Methods
fringe separation glare technique
15 µm dropsConstant inter-arrival time
Δt
Wave-form generator
Low Resolution Map of Cloud Spectrometer Sample Volume (no pin-hole mask used) Spatial resolution – 50 µm data
Medium Resolution Map – 10 µm spatial data completed
Data being processed
System has been automated based on initial input of of sample area location. Time for auto-scanning of sample area varies depending on instrument used (CDP, BCP
or CAS) and scan resolution used.50 µm displacement takes 1-2 hours. 10 µm takes 10-12 hours.
Inversion uses modified Twomy algorithm (Markowski, 1987, AST)
• Laser isn’t eyesafe• Operated with weight-on-wheels interlock switch
IAGOS-ERI Annual Meeting 2012, Lake Constance, June 18-20, 2012
Current well characterized Cloud Droplet Spectrometers
Test Flights on the North Dakota CitationSeptember-November. 2011
DMT LWC and CDP
Total number concentrations from BCP show reasonable agreement with CDP even with the sample volume close to the aircraft skin.
Yaw angle change?
The averaged size distribution, derived by inversion of the measured spectrum, agrees quite well with the CDP
The IAGOS instrument package was installed on board Lufthansa’s A340-300 'Viersen’. The maiden test flight was
launched from Frankfurt in July 2011
Summary of cloud concentrations : September, 2011 to May, 2012
Particle Characteristics
Take Offs and Landngs
Mid-Flight
Total Cloud Events
66% 54%
Cloud: Low Concentration
(<100 L-1)11% 28%
Cloud: High Concentration
(>100 L-1)50% 26%
Dust 14% 1%
Cloud/Dust Particle Encounters: 319 FlightsAverage Flight Duration > 8 Hours
Analysis of Luana, Angola to Frankfurt Flight, May 18, 2012
Maximum concentration > 300,000 per liter over Nigeria
Maximum ice water content > 2 grams per cubic meter(assumes spherical ice crystals (unrealistic)
Recent cloud particle measurements on May 18, 2012, Luanda, Angola to Frankfurt, Germany. More than 100,000 particles per liter at estimated temperature of -500 C !
Note: Temperatures not corrected for dynamic heating.
Large fluctuations of temperature in cloud!
30 Kt airspeed change
Aircraft takes avoidance action but remains in cloud for nearly half an hour and temperature measurements from IAGOS package remain corrupted by melted ice crystals.
High ice crystal concentrations corrupt temperature measurements by melting and wetting the sensor.
Average diameters are dominated by small crystalsMedian volume diameters are biased by very largest crystals
Average size distribution during cloud encounter: Bimodal with maximum number at 10 m but maximum LWC at 70 m
Vertical Profiles During Take Off and LandingShow Cloud Structure (Landing in Frankfurt Shown Here)
MultipleCloudLayers
Next Generation Instrument
The Backscatter Cloud Probe with Depolarization
(BCPD)
Measurements with the Cloud Aerosol Spectrometer with Depolarization (CAS-DPOL) distinguish droplets from crystals (courtesy James Dorsey, U. Manchester)
Polarization Detector to Sizing Detector
Pola
riza
tion R
ati
o
The BCPD, under development for IAGOS, will measure the perpendicular and parallel components of the polarized scattered light and identfy water droplets, ice crystals and ash/dust.
BCP-DPOL
Photo M. Gallagher, Manchester
BCD-D First test Flight March 2012. Photo M. Gallagher, Manchester
Cloud Tunnel results are encouraging.
A) The MVD as a function of time for the BCP-PD (red curve) and CDP (black),
B) LWC, C) Number
concentration and polarization ratio (blue curve) and D) average size distribution over the whole time period.
Ice phase
Water phase
Ottawa Cloud Tunnel Data: Courtesy DMT
Summary
• The BCP is currently taking detailed size-resolved cloud measurements that will enhance the current data base and lead to a better understanding of how clouds form, evolve and impact climate, e.g. microphysical properties of Contrails and Contrail induced cirrus Cirrus and Sub-visible cirrus
• The BCP cloud data base will be available for comparisons with satellite-derived cloud products.
• BCPs can warn flight crews of very high ice crystal concentrations.
• The next generation BCP, BCP-D may distinguish water droplets, ice, volcanic ash and dust.
For more information on the BCP/BCPD:
Thank you for your interest.
BCP-100 V1 Brief Summary1.Software for assimilation and analysis of BCP database complete. Currently accepts, aircraft GPS position, altitude and temperature for interpretation. Software able to access multiple BCP data bases.2.Database for BCP complete – includes UK BAe 146, Viersen, Falcon, and two US aircraft studies. 3.Data seems consistent. Lower threshold may be higher than expected 6 µm as opposed to 5 µm under operational conditions.4.Intercomparison with BAe 146 CAPS-CAS, CDP-100 V2 complete. Data analysed and will be included in joint technical paper with DMT on BCP (in preparation, Baumgardner, Beswick et al.) together with data from US aircraft flights.5.New pylon canister mount being purchased to allow for parallel mounting of BCP and CDP on BAe 46 for better intercomparison checks (NERC FAAM-Manchester MSc Student)6.Routine detection over prevalent cloud regions e.g. Atlantic ITCZ. Profile data suggest consistent results.7.BCP appears able to detect dust particles based on consistent Middle East profile data under cloudless skies.8.Awaiting return of Viersen BCP to check
1. Calibration drift – this will be checked/validated using the new automated droplet gun calibration facility for sizing and absolute concentration. Two independent sizing methods – glare and interference fringe methods.
2. Diagnostics and laser inhomogeneity3. Power supply check etc.
9.NERC Grant awarded to develop BCP 2nd Generation instrument with polarisation capability. Delivery expected end 2012.