Cirrus Measurements during the EAQUATE Campaign
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Transcript of Cirrus Measurements during the EAQUATE Campaign
© Crown copyright 2004 Page 1
Cirrus Measurements during the EAQUATE Campaign
C. Lee, A.J. Baran, P.N. Francis, M.D. Glew, S.M. Newman and J.P. Taylor
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Outline
Overview of frontal cirrus case on 15th Sept 2004
Aircraft remote sensing and in-situ instrumentation
Measurements and preliminary resultsARIES infrared interferometer
SWS visible and NIR spectrometer
Cloud physics probes
Summary and conclusions
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IR satellite images at approx AQUA overpass times
1200 1400
Frontal cirrus case on 15th Sept 2004
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12:23:26-12:29:25 13:59:26-14:05:25
AIRS (AQUA) 11m images on 15/09/04
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FAAM BAe146-301 ARA Instrumentation
5 port turbulence probe
Total water probeJW Liq waterNevzerov total/liq water probeRosemount temp probes
Air sample inlets
FAGE InletCVI on other side
Deimos or IR Camera
TAFTS ARIES
Cloud Physics Probes
Cloud Physics Probes
MARSS
SWS on other side
BBRs
LidarSHIMS
Upward and Forward Video Cameras
BBRs
SHIMS
Rearward and Downward Video Cameras
ADA on other side
Dropsonde on other side
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Remote Sensing instrumentation on FAAMon 15/09/04
Instrument Type Spectral range
SWS Short Wave Spectrometer 0.3 - 1.7µm
ARIESAirborne Research Interferometer Evaluation System 550 - 3000cm-1
MARSSMicrowave Airborne Radiometer Scanning System
89 - 183GHz (upward and downward)
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In-situ instrumentation on FAAM
Core Chemistry O3, CO, NOxy, SO2
NephelometerTotal scattering and hemispheric backscattering coefficient at three visible wavelengths (450, 550 and 700nm)
SID1 Small Ice Detectors. Spherical Equivalent size spectrum (1 - 50µm)
PCASPAerosol Size Spectrum optical probe. Aerosol particle concentration, mean volume radius and size spectrum (0.1 - 3µm)
2DCTwo Dimension Cloud particle imaging probe. Particle number concentration, condensed water content, mean volume radius, precipitation rate and size spectrum (25 - 800µm)
2DPTwo Dimension Precipitation particle imaging probe. Particle number concentration, condensed water content, mean volume radius, precipitation rate and size spectrum (200 - 6400µm)
AVAPS (Dropsonde)Airborne Vertical Atmospheric Profiler System (Dropsonde). Profiles of pressure, temperature, relative humidity, wind speed and direction
Johnson Williams Liquid Water Content Probe Concentration of liquid water in clouds
General Eastern Hygrometer Water Vapour (damp atmosphere)
Nevzorov Liquid and Total Water Content Probe. Liquid and total water in clouds
TWC Total Water Content Probe Water (H2O)
FWVS Fluorescence Water Vapour Sensor Water Vapour (dry atmosphere)
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FAAM BAE146 flight track
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Aircraft profile
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Time
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Take Off
Transit at FL280
Profile 1 Run 1 Profile 2
2 orbit
s
500 ft/min
1000 ft/min
P 3 R 2 P 5R 2.2 P 4 R 4R 3 R 5.2Run 5.1
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ARIES average spectra at overpass 2
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Wavenumber [cm-1]
Bri
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tnes
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start of runend of run
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ARIES BTs at select wavelengths during run at 2nd overpass
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13:58:45 14:00:45 14:02:45 14:04:45 14:06:45
Time
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Tem
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8um10um11um12um8um-12um
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Modelled IR and ARIES data
Extinction optical thickness=3.7
Re=46um
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700 1200 1700 2200 2700Wavenumber [cm-1]
Bri
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tnes
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ARIES 10 cm-1 res
Edwards-Slingo Model
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SWS nadir example spectra for thin and thick cirrus
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0.4 0.6 0.8 1 1.2 1.4 1.6
Wavelength (um)
Rad
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ce [
W/m
2 /ste
r/u
m]
thick cirrusthin cirrus
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SWS radiance variation through the flight
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Time
Rad
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ce [
W/m
2 /ste
r/u
m]
0.87um1.6um
Orbitszenith zenith zenithnadir
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SWS radiance measured during the 2 orbits banked at 45 deg
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Scattering angle [degrees]
Rad
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W/m
2/s
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Orbit 1 at 0.87umOrbit 2 at 0.87umOrbit 1 at 1.6umOrbit 2 at 1.6um
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Phase functions
6-branched bullet-rosette
Dist=0.12
=0.87 μm
Orbit 1 Orbit 2
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Phase functions
Polycrystal (Macke et al. 1996)
Dm=100 μm for all ice crystals
Orbit 1 Orbit 2
=0.87 μm
First Results – Scaled Radiances at 10o - NO multiple scattering
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Phase Functions
Analytic Phase function g=0.70 (Baran et al. 2001)=0.87 μm
Orbit 1 Orbit 2
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Phase functions
Orbit 1 Orbit 2
=1.60 μm Polycrystal
50 μm100 μm800 μm
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Cloud Physics in-situ observations
Full analysis still needs to be performed
Graupel
No larger than 200um diameter seen in flight
50 to 200/litre
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Summary and conclusions
Remote sensing and in-situ measurements have been obtained using FAAM BAE-146, for a frontal cirrus case on 15 Sept 2004, coincident with 2 AIRS (AQUA) overpasses.
The effective particle radius is larger than 50um, of graupel (non-symmetrical) type, with a large variability in optical thickness.
The analysis of this data set is on going.
It demonstrates the importance of using coincident observations at wavelengths from visible to submm, to determine a wide range of cirrus parameters and check the physical consistency of the models.
Future flights - CASEAR campaign based in UK in Nov 2005, May 2006 and July 2007, coincident with Chilbolton radar, AQUA, Cloudsat.
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Acknowledgements
FAAM
Direct Flight
BAE
Met Office instrument operators
Walter Wolf
Dave Pollard
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Visible MSG satellite images at AQUA overpass times on 15 Sept 2004
1230 1400
Frontal cirrus case
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AIRS 8m -12m for 2nd overpass
13:59:26-14:05:25
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Phase functions
Distorted Aggregate (Yang and Liou 1998)
Dist=0.13
=0.87 μm
Orbit 1 Orbit 2