solar occultation for ice experiment science overview
DESCRIPTION
Solar Occultation For Ice Experiment Science Overview. Larry Gordley & Mark Hervig. AIM Is a Mission to Study Noctilucent Clouds (NLCs). NLCs are the highest (83 km) clouds in our atmosphere NLCs occur pole-ward of 50 ° latitude in both hemispheres NLCs occur only during summer. - PowerPoint PPT PresentationTRANSCRIPT
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview1
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Solar Occultation For Ice Experiment
Science Overview
Larry Gordley&
Mark Hervig
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview2
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Why do they form? Why do they vary?
Is there a relationship to global change?
SOFIE will help AIM provide answers
What is the role of•Temperature•H2O•Dynamics•Chemistry?
•NLCs are the highest (83 km) clouds in our atmosphere
•NLCs occur pole-ward of 50° latitude in both hemispheres
•NLCs occur only during summer
NLC are changing:
•Increasing numbers
•Moving equatorward
•Increasing brightness
AIM Is a Mission to Study Noctilucent Clouds (NLCs)
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview3
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SOFIE Measurement Overview
SOFIE Channel Summary
channel 1 2 3 4 5 6 7 8
Target O3 particles H2O CO2 particles CH4 CO2 NO
Center (m)
Strong band
Weak band
0.290
0.328
0.862
1.031
2.60
2.45
2.77
2.94
3.06
3.19
3.37
3.51
4.25
4.63
5.32
4.98
Differential absorption measurements to determine:
•Gas abundance: H2O, O3, CH4, NO, CO2
•Particle extinction: 10 wavelengths from 0.29 to 5.3 m
•Temperature
High signal-to-noise: 106 to 109
Precise solar tracking: 1 arcsec knowledge
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview4
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Differential Absorption Measurements
Each SOFIE channel uses two detectors to make three measurements:
1. Strong band absorption
2. Weak band absorption
3. Difference signal (weak band – strong band)
Difference signal measurements
• remove atmospheric interference
• Nearly eliminate common-mode noise (e.g. tracking jitter, chopper noise, sun spots, etc..)
Simultaneous NLCs, temperature, and gas measurements
Targets the mesosphere and above,
but easily obtains stratospheric measurements
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview5
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Progress since PDR from a Scientific View Point
• Sun Sensor: Verification of 1 arcsec tracking performance
• Simplified instrument operation: A single data collection mode, command tables provide flexibility for different scenarios.
• Analysis of Signal Drifts: Beam steering, filter thermal effects, etc…, signal drifts are low risk
• Verification of Beam Defocus: Suppression of false signals due to signal gradient on non-uniform detectors.
• Spectral Performance: Predictions for all bands exceed requirements, Delivered flight filters (bands 11 – 16) exceed requirements.
• Band 1 & 2 detectors: Changed from UV-enhanced silicon to silicon carbide: relieves extraordinary out of band rejection requirements
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview6
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Silicon Carbide Detectors, Bands 1 & 2
Ozone measurements originally used UV-enhanced silicon detectors
The spectral response of UV-Si detectors is less than ideal:
•UV-Si response combined with solar spectrum = amplified out-of-band energy
•Can be addressed with stacked filters, difficult to verify
Our New Approach: Silicon Carbide (SiC) detectors
Ideal spectral response
twice as rad-hard as Si
Eliminates 2nd filter
solar source detector response
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview7
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SOFIE Spectral Response
•Drivers:
Filter Response
Preceding Optics
Detector Response
•Spectral response evaluation must consider solar source
•Out-of-band performance is critical
(OOB < 1% required)
•Predictions meet requirements
•Filters 11 - 16 are now built
they meet requirements
•Example: Band 13Band 13
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview8
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SOFIE Performance Requirements
SOFIE Measurement Requirements from the AIM SRD (short list)
Geophysical Parameter
Precision
(near 83 km)
Altitude Range (km)
Vertical Resolution
(km)
Horizontal Resolution
Temporal Resolution
Cloud extinction
NIR: 5x10-6 km-1
IR: 5x10-5 km-1
78 – 85 3 at com. vol. 1 min @ com. vol.
temperature 5 K 70 – 90 3 5lat x 24lon 1 min @ com. vol.
H2O mixing ratio
0.6 ppmv 78 – 90 3 5lat x 24lon 1 day
Performance Drivers Precision & altitude range: signal-to-noise (S/N), spectral response, pointingVertical Resolution: FOV, S/N, pointingHorizontal & Temporal Resolution: inherent to SOFIE
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview9
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SOFIE Signal-to-Noise (S/N) Exceeds Requirements
Current best estimates indicate signal to noise margin from 3.8 to 2000
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview10
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Retrieval Simulations
Retrieval simulations are used to:
•Relate measurement requirements to instrument requirements
•Track instrument performance
Retrieval simulations are based on an advanced model:
•Rigorous line-by-line calculations
•Detailed atmospheric geometry and optics
•20 year heritage (LIMS, HALOE, CLAES, CRISTA, SABER,…)
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview11
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Retrievals in the presence of clouds
Simulated SOFIE Water Vapor Retrievals
SOFIE H2O Measurement performance
Required Current Best Estimate (Margin)
Signal to Noise 2.5 104 3.1 106 (124)
Retrieval Precision 0.6 ppmv 0.02 ppmv (30)
Retrieval Altitude Range 79 – 90 km 15 – 110 km
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview12
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Based on differential CO2 absorption from 2 channels (2.8 and 4.3 m)
Simulated SOFIE Temperature Retrievals
SOFIE Temperature Measurement performance
Required Current Best Estimate (Margin)
Signal to Noise 3.0 105 2.5 106 (8.3)
Retrieval Precision 5 K 0.6 K (8.3)
Retrieval Altitude Range 70 - 90 15 – 100 km
Retrievals in the presence of clouds
Simultaneous CO2 retrievals
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview13
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Geophysical Parameter
Precision
Required / Current Margin
Altitude Range, km
Required / Current
Vertical Resolution, km
Required / Current
NIR cloud extinction 5x10-6 km-1 / >10 78 – 85 / 75 – 90 3 / 1.5
IR cloud extinction 5x10-5 km-1 / 10 78 – 85 / 75 – 90 3 / 1.5
temperature 5 K / 8.3 70 – 90 / 15 - 100 3 / 1.5
O3 mixing ratio 0.1 ppmv / 50 78 – 90 / 15 - 110 3 / 1.5
H2O mixing ratio 0.6 ppmv / 30 78 – 90 / 15 - 110 3 / 1.5
CO2 mixing ratio 10 ppmv / 6.3 80 – 100 / 15 - 105 3 / 1.5
CH4 mixing ratio 0.05 ppmv / 2.5 30 – 90 / 15 - 90 3 / 1.5
NO mixing ratio 107 cm-3 / 10 80 – 95 / 80 - 120 5 / 3
Horizontal and temporal resolution requirements are met
Predicted Performance Exceeds Requirements
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview14
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SOFIE Particle Measurements
Particle extinctions at 10 wavelengths (290 nm – 5.3 m):
•Two dedicated particle channels (4 wavelengths)
•Gas channel weak bands (6 wavelengths)
Measurements from the tropopause to the mesopause:
•Primary: NLCs
•Secondary: cosmic dust, PSCs, cirrus, SSA
Unique combination of UV thru IR wavelengths allows:
•Particle size distribution retrievals
•Inference of particle composition
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview15
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Simulated PMC Size Distribution Retrievals
SOFIE will measure PMC extinction at 10 wavelengths
These measurements will allow accurate PMC size distribution retrievals
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview16
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Cosmic Dust (Smoke) Measurements
Model predictions suggest that SOFIE may be sensitive enough to measure the smoke layer
Accounting for molecular (Rayleigh) extinction will be important
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview17
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Summary
•SOFIE will provide critical contributions to AIM science
•CBE performance meets or exceeds requirements:
Signal to noise
Pointing
Spectral response
Retrieval precision, resolution, etc…
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview18
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Supplemental Material
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview19
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Band 1 Spectral Response, SiC Detector
Predictions indicate excellent performance using silicon carbide detector
Solar out-of-band = 0.02%
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview20
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Autonomous Start and Operation
By observing a CO2 V signal for 3 consecutive events, future event initiation and termination times can be determined, along with all other event command times. This allows autonomous start-up and operations.
Use t0.5 (when CO2 V is 50% of maximum) as a reference time.
Z(t0.5) is known to ± 3km (± 1.0 seconds)
Therefore, t0.5 values observed for the first and third events allows SOFIE to determineΔtP – Orbital Period, which in combination with the second event allows times to be predicted for all future events:tI – Event Initialization TimestB – Event Balance TimestT – Event Termination TimestC’s – Other Command Times
These times are refined continuously as more events are observed.
SS Orbital Period – ΔtP
SR Orbital Period – ΔtP
tISS tB
SS
t0.5SS
tTSS tI
SR
t0.5SR
tBSR tT
SR
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview21
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Current best estimate performance
S/N: 3.0E6 (3.0E5 required, margin = 10)
Precision: 1.6 ppmv (10 ppmv required, margin = 6)
Altitude range: 15 – 105 km (80 – 100 km required)
Simulated SOFIE CO2 Retrievals
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview22
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Current best estimate performance
S/N: 2.9E6 (4.0E5 required, margin = 7.2)
Precision: 0.02 ppmv (0.05 ppmv required, margin = 2.5)
Altitude range: 15 – 90 km (30 – 90 km required)
Simulated SOFIE Methane Retrievals
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview23
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Current best estimate performance
S/N: 1.5E6 (3.0E5 required, margin = 4.1)
Precision: 9.8 x 105 cm-3 (107 cm-3 required, margin = 10)
Altitude range: 80 – 120 km (80 – 95 km required)
Simulated SOFIE Nitric Oxide Retrievals
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview24
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Current best estimate performance
S/N: 1.9E10 (1.0E4 required, margin > 1000)
Precision: 0.002 ppmv (0.1 ppmv required, margin = 50)
Altitude range: 15 - 110 km (78 – 90 km required)
Note: weak band signal will be used to retrieve O3 below 50 km
Simulated SOFIE Ozone Retrievals
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview25
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SOFIE Refraction Angle Temperature Retrievals
Measurements of solar refraction angle vs. height can be used to retrieve temperature
Refraction angle known to 0.25 arcsec from the SOFIE sun sensor
2 K precision below 35 km
SOFIE CDR, October 7 & 8, 2004
SOFIE Science Overview26
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Cosmic Dust (Smoke) Measurements?
Can SOFIE measure cosmic smoke?
Model predictions of cosmic smoke properties show an extremely tenuous layer
These predictions were used to simulate SOFIE signals