Spectroscopic issues in the data analysis of REFIR-PAD ......Water vapor profile RS-92: high...

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Istituto di Fisica Applicata “Nello Carrara” Spectroscopic issues in the data analysis of REFIR-PAD measurements performed during the 2009 ground- based campaigns Giovanni Bianchini, Luca Palchetti Istituto di Fisica Applicata “Nello Carrara”, Firenze, Italy

Transcript of Spectroscopic issues in the data analysis of REFIR-PAD ......Water vapor profile RS-92: high...

Page 1: Spectroscopic issues in the data analysis of REFIR-PAD ......Water vapor profile RS-92: high vertical resolution, but low time resolution REFIR-PAD: better suited to resolve the evolution

Istituto di Fisica Applicata “Nello Carrara”

Spectroscopic issues in the data analysis of REFIR-PAD measurements performed during the 2009 ground-

based campaigns

Giovanni Bianchini, Luca PalchettiIstituto di Fisica Applicata “Nello Carrara”, Firenze, Italy

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11th International HITRAN Conference REFIR-PAD spectroscopic issues 2

Istituto di Fisica Applicata “Nello Carrara”

Outline

● Overview of the REFIR-PAD instrument

● Analysis of spectrally resolved DLR

● Summary of 2007-2008 results

● The 2009 ground-based campaigns

● Analysis of the fitting residuals

● Conclusions

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The REFIR-PAD instrument

Compact, self-contained FTS with 100-1500 cm-1 spectral range and 0.5 cm-1 spectral resolution

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Instrument overview● Room temperature optics and

detectors (DLATGS pyroelectric)

● Suitable for balloon-borne and ground-based measurement

● Autonomous or remote controlled operation (wired or wireless ethernet link)

REFIR-PAD in the ground-basedmeasurement configuration

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Level 1 products

● NESR component obtained from measurement noise through error propagation

● Calibration component also obtained through error propagation assuming a 0.3 K error in the BB temperatures

NESR= 1N

2n S

Sh−Sc 2SF1

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Auxiliary data

● Vaisala WXT520 meteo station provides local atmospheric variables

● IR webcam (low pass filter @850 nm) monitors cloud cover

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Level 2 data analysis● LBLRTM forward

model

● MINUIT routines (from CERN) to perform 2 minimization

● Fitted variables: atmospheric profiles (H2O, T), cloud optical thickness, ILS, frequency correction

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Level 2 products

● Vertical water vapor and temperature profiles

● Integrated water vapor column, cloud optical thickness

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Water vapor profile

● RS-92: high vertical resolution, but low time resolution

● REFIR-PAD: better suited to resolve the evolution in time of the atmospheric state (but with a lower resolution of the vertical structure)

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Results from 2007-2008

● 0.5-4.0 PWV range

● LBLRTM v11.3

Sensible improvements in the 350-450 cm-1 region with LBLRTM v11.6-v11.7

Residuals still above calibraton uncertainty in the 450-550 cm-1 regionfor high PWV (2-3 mm)

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2009 measurements (I)

● High PWV measurements (PWV ~ 4-8 mm)

April 2009, Pagosa Springs Staging Facility (PSSF), Colorado, 2330 m a.s.l.

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2009 measurements (II)

● Extremely dry conditions (PWV < 0.2 mm)

● About 3 months of operation (2 unattended)

August-October 2009, RHUBC II Campaign, Cerro Toco, Chile, 5383 m a.s.l.

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4 points fitting● Fitted points unevenly

spaced to reflect weighting functions behaviour with height

ground

g+1km

g+3km

● Added 1 fitted point 50 m above ground to take into account for surface effects

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Analysis of synthetic spectra● LBLRTM

simulated spectrum

● atmosphere from radio-sounding

● no error or noise

No significant residuals due to fitting process (2<<1)

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Radiometric calibration

Calibration uncertainty (gray) corresponds to ±0.5K @ 280K

Radiometric accuracy measured in the 860-930 cm-1 region:

● ≈0.25K RMS

● >0.25K mean

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Residuals (high PWV)

● features in the 450-550 cm-1 range significant above calibration uncertainty

● above 550 cm-1 model is validated with the REFIR-PAD measurement accuracy

● Spurious effects: CO2 2 Q-branch (667 cm-1), BS absorption (730 and 850 cm-1)

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Residuals (low PWV)

● features in the 300-400 cm-1 range significant above calibration uncertainty

● above 400 cm-1 model is validated with the REFIR-PAD measurement accuracy

● Spurious effects: CO2 2 Q-branch (667 cm-1), BS absorption (730 and 850 cm-1)

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Fitting issues

Actual measurement: T and H2O errors at lower altitudes

Simulated spectrum (with random noise added):

profiles are correct

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Conclusions

http://fts.ifac.cnr.it

REFIR-PAD FTS performances:

● FM validated in the 550-850 cm-1 range

● Residuals above calibration error– in the 300-400 cm-1 range for PWV < 1 mm

– in the 450-550 cm-1 range for PWV > 2 mm