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a Submillimeter-Wave Limb Sounder

Stefan B ¨uhler, Bj ¨orn-Martin Sinnhuber Institute of Remote Sensing

University of Bremen International Workshop on

Submillimeter-wave Observation of Earth’s Atmosphere from Space

Tokyo, January 27–29, 1999

2

2

2 2

2

2 2

2

2

(2)

Overview



Motivation



Retrieval method



Error analysis: The linear mapping method



The SOPRANO instrument



Antenna

– Antenna efficiency – Far wing knowledge



Pointing

– Pointing accuracy – Pointing stability



Radiometric errors – Baseline ripples

– Baseline discontinuities – Calibration errors



Error summary for selected species



Conclusions



Ongoing work

(3)

Motivation



Which instrument parameters are crucial for the scientific goal?



Minimize systematic errors



Optimize performance

(4)

Retrieval by optimal estimation



Described in: Rodgers, C. D., Journal of

Geophysical Research, 95, 5587–5595, 1990.



Minimize:

 2

OEM

= [~y ? F(~x)]

S

?1

~ y

[~y ? F(~x)]

+

[~x ? ~x

a

]

S

?1

~x

a

[~x ? ~x

a ]

~

x

: state vector

~ x

a

: a priori S

~x

a

: a priori covariance matrix

~

y

: measurement

F(~x)

: forward model

S

~y

: meas. covariance matrix



We use the Levenberg-Marquardt method to

find the minimum

(5)

Method of investigation



Impact of instrument parameters on the retrieval investigated by linear mapping:

D = @x=@y^

D :

Contribution function matrix

^

x :

Retrieved atmospheric profile

y :

Measured spectrum



Impact on retrieval then given as

^x = Dy



Generate ensembles of 100 or 1000 cases

and calculate RMS error.

(6)

The SOPRANO Instrument

Band f [GHz] Species

A 497.5 – 504.75 O

3

, ClO, CH

3

Cl, (BrO), N

2

O, H

2

O, (HNO

3

), (COF

2

) B1 624.6 – 626.5 HCl, O

3

, HOCl, (HNO

3

),

(BrO), (HO

2

)

B2 627.95 – 628.95 HOCl, O

3

, HNO

3

, (COF

2

) C1 635.6 – 637.4 CH

3

Cl, O

3

, HNO

3

, HOCl,

HO

2

C2 648.0 – 652.0 ClO, O

3

, N

2

O, HNO

3

, (H

2

CO), (HOCl), (HO

2

), (NO

2

), (BrO)

D 730.8 – 732.25 T, O

3

, Scan, HNO

3

, (CH

3

Cl), (HO

2

)

E 851.5 – 852.5 NO, O

3

, N

2

O, (HNO

3

), (NO

2

), (H

2

O

2

)

F 952.0 – 955.0 NO, T, Scan, O

3

, N

2

O, (HO

2

), (HNO

3

), (CH

3

Cl), (NO

2

)

G1 685.5 – 687.2 ClO, O

3

, (HNO

3

), (HOCl), (H

2

O

2

), (COF

2

), (NO

2

) G2 688.5 – 692.0 CO, CH

3

Cl, ClO, O

3

,

HNO

3

, (HO

2

), (HOCl),

(HCN), (NO

2

), (H

2

O)

(7)

Antenna

Assumed full width at -3 dB around a typical tangent point:



2.7 km. (SOPRANO antenna) (Should be about 12 % narrower for JEM/SMILES if one takes into account only platform altitude and antenna diameter.)

Investigation of:



Perfectly known antenna pattern:

How important is a good antenna efficiency (small near and far wing)?



Imperfect antenna knowledge

(8)

Near and far wings

Case Integration [%]

Near Wing Far Wing

1 1.0 0.0

2 1.0 0.4

3 4.0 0.0

4 4.0 1.0

5 10.0 0.0

6 10.0 4.0

(9)

Near and far wings: O

3

near 625 GHz

=)

Negligible, but

under the assumption that the antenna

response is perfectly known throughout

near and far wing.

(10)

Imperfect antenna knowledge

4 % near, 0 % far wing 4 % near, 1 % far wing

−500 0 50

10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Ant. 3 − Band B1 O3

n1 n2 n3 n4

−500 0 50

10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Ant. 4 − Band B1 O3

n1 n2 n3 n4



n1: Antenna pattern measured with 20 dB non-linearity, 35 dB noise



n2: Antenna pattern measured with 30 dB non-linearity, 45 dB noise



n3:

10

m antenna distortion



n4: 0.25 times the effect of n3

(11)

Imperfect knowledge: ClO near 500 GHz



4 % near wing, 1 % far wing

−50 0 0 50

10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Ant. 4 − Band A ClO

n1

n2

n3

n4

(12)

Imperfect knowledge: Conclusions



If there is a significant far wing it must be covered by the antenna measurement



An antenna distortion of 10



m is not critical

(13)

Pointing



Pointing accuracy: Two cases studied:



200 m random pointing offsets

– Correlated random pointing with 200 m RMS (convolved first case with 6 km FWHM filter and scaled to 200 m RMS)

Can be achieved technically by increased delay in antenna control loop



Pointing stability (small scale pointing variations):

– Simulated with different effective antenna patterns (



200 m)



Coregistration error: Scan offset of 200 m between different bands assumed

– With and without scan offset fit

(14)

Pointing: Ozone Band A (near 500 GHz)

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Pointing Error − Band A O3

Pointing accuracy

correlated

Pointing stability

(15)

Pointing: Ozone on 4 km retrieval grid

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Pointing Error − Band A O3 (4km)

Pointing accuracy correlated Pointing stability



4 km retrieval grid reduces impact

(16)

Pointing: ClO Band A (near 500 GHz)

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Pointing Error − Band A ClO (4km)

Pointing accuracy

correlated

Pointing stability

(17)

Pointing: Temperature Band F (near 954 GHz)

0 5 10 15

0 10 20 30 40 50 60

Error [K]

Altitude [km]

Pointing Error − Band F T

Pointing accuracy

correlated

Pointing stability

(18)

Coregistration error: Ozone Band A (near 500 GHz)

0 10 20 30 40 50

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Coregistration Error − Band A O3

without scan offset

with scan offset fit

(19)

Coregistration error: ClO Band A

0 10 20 30 40 50

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Coregistration Error − Band A ClO

without scan offset

with scan offset fit

(20)

Pointing: Conclusions

Pointing accuracy:

 

200 m has very critical impact on retrieval



Impact can be reduced by:

either

– Correlated pointing error (corresponding to increased delay in antenna control loop) or

– 4 km retrieval grid but

– Doing both gives no additional improvement

(actually 4 km grid retrievals are often even

slightly better with uncorrelated pointing

errors)

(21)

Pointing: Conclusions continued

Pointing stability:

 

200 m not critical Coregistration error:

 

200 m coregistration error has large impact



. . . but can be minimized with scan offset fit

 ?!

Not critical

(22)

Radiometric errors



Baseline ripples



Baseline discontinuities



Unwanted sideband



Calibration errors



Correlated noise

(23)

Baseline ripples

Assumptions:



Sinusoidal baseline structure



0.1 K amplitude



100 and 400 MHz periods



Phase randomly distributed



Two cases:

– Phase constant during scan

– Phase randomly distributed during scan

(24)

Baseline ripples: Ozone Band A (near 500 GHz)

0 5 10 15

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Baseline Ripples − Band A O3

100 MHz 100 MHz corr.

400 MHz

400 MHz corr.

(25)

Baseline ripples: ClO Band A

0 5 10 15

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Baseline Ripples − Band A ClO

100 MHz 100 MHz corr.

400 MHz

400 MHz corr.

(26)

Baseline ripples: Conclusions



Impact of 400 MHz periods larger than 100 MHz periods



Not critical



However: 0.1 K seems optimistic

(27)

Baseline discontinuities

... may be caused by AOS modules

Assumptions:



Simulated by sawtooth function from -0.2 K to +0.2 K every 2 GHz



Phase shifted by 100 MHz

?!

20 cases

(28)

Baseline discontinuity: O

3

Band A

498 499 500 501 502 503 504 505

−50 0 50 100 150 200 250

Frequency [GHz]

Brightness Temperature [K]

Band A (20km) − Baseline discontinuity: O3 best case

498 499 500 501 502 503 504 505

−50 0 50 100 150 200 250

Frequency [GHz]

Brightness Temperature [K]

Band A (20km) − Baseline discontinuity: O3 worst case

(29)

Baseline discontinuity: O

3

Band A

−15 0 −10 −5 0 5 10 15

10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Baseline discontinuity − Band A O3

O3 best case

O3 worst case

(30)

Baseline discontinuity: ClO Band A

−5 0 0 5 10 15 20 25

10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Baseline discontinuity − Band A ClO

ClO best case

ClO worst case

(31)

Baseline discontinuity: Conclusions



Worst case for discontinuity near center of line of interest



Impact stronger for weak lines



Impact can be minimized by appropriate

placement of AOS modules

(32)

Unwanted sideband



Nominal 20 dB suppression

 ?!

200 K line in sideband will appear with 2 K in measured spectrum!



Impact depends on LO frequencies



For SOPRANO study Dornier setup:

Band LO frequency [GHz]

A 482.25

B1 606.65

B2 606.65

F 933.50

(33)

Lower Sideband: Band A (near 500 GHz)

459 0 460 461 462 463 464 465 466 467 468 50

100 150 200 250

Frequency [GHz]

Brightness Temperature [K] (20km)

Band A − Lower Side Band (LO=482.25 GHz)



Many strong lines !

(34)

Lower Sideband: Band B1 (near 625 GHz)

586.5 0 587 587.5 588 588.5 589 589.5

50 100 150 200 250

Frequency [GHz]

Brightness Temperature [K] (20km)

Band B1 − Lower Side Band (LO=606.65 GHz)



Little structure

(35)

Lower Sideband: Band B2 (near 628 GHz)

584.6 0 584.7 584.8 584.9 585 585.1

50 100 150 200 250

Frequency [GHz]

Brightness Temperature [K] (20km)

Band B2 − Lower Side Band (LO=606.65 GHz)

(36)

Lower Sideband: Band F (near 954 GHz)

911.5 0 912 912.5 913 913.5 914 914.5 915 915.5 50

100 150 200 250

Frequency [GHz]

Brightness Temperature [K] (20km)

Band F − Lower Side Band (LO=933.50 GHz)



Moderate structure

(37)

Unwanted Sideband: Ozone Band A (near 500 GHz)

−100 0 −50 0 50 100

10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Sideband contribution − Band A O3

(38)

Unwanted Sideband: ClO Band A

−100 0 −50 0 50 100

10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Sideband contribution − Band A ClO

(39)

Unwanted Sideband: Conclusions



Severe impact if uncorrected



Dornier setup LO frequencies not optimal – Especially Band A should be optimized



Impact can be corrected to first order if sideband ratio is known



Present results can also be interpreted as

error due to 20 dB knowledge of sideband ratio

(40)

Calibration

Calibration process:

T

a

= G(T

h

? T

c

) + T

c

with

G = (V

a

? V

c

)=(V

h

? V

c )

?! T

a

= T

a

? T

c

T

h

? T

c

(T

h

? T

c

) + T

c

Three cases studied:



1 K error at 300 K



1 K offset



Quadratic error of 0.2 K at 150 K

(41)

Calibration error: Ozone Band A

−100 0 −50 0 50 100

10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Calibration Error − Band A O3

1 K at 300 K

1 K offset

quadratic 0.2 K

(42)

Calibration error: ClO Band A

−100 0 −50 0 50 100

10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Calibration Error − Band A ClO

1 K at 300 K

1 K offset

quadratic 0.2 K

(43)

Calibration error: Conclusions



1 K offset introduces errors of 10% and larger



Impact of 0.2 K quadratic error is small

(because the quadratic error itself is assumed

to be small)

(44)

Correlated noise



Noise on calibration measurements will be correlated for each level during one scan



Here an integration time of 2 sec. was

assumed (

10

atmospheric integration time) Result:



Errors same order of magnitude as measurement noise



Statistical error: Decreases with averaging

(45)

Correlated noise: ClO Band A

0 10 20 30 40 50

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Correlated Noise − Band A ClO

(46)

Temperature uncertainty

Temperature weighting function:

K

b



@F

@b

b=



b

S

S

= DK

b S

b

(DK

b )

T

Two cases for

Sb

studied:



3 K uncorrelated



3 K offset

(47)

Temperature uncertainty: Ozone Band A

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Temperature Uncertainty − Band A O3

3 K uncorrelated

3 K offset

(48)

Summary: Ozone Band A (near 500 GHz)

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Band A O3

Null space Radiometric noise Pointing Pointing c.

Antenna

Baseline

Calib. offset

Corr. noise

(49)

Summary: ClO Band A (near 500 GHz)

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Band A ClO

Null space Radiometric noise Pointing Pointing c.

Antenna

Baseline

Calib. offset

Corr. noise

(50)

Summary: Temperature Band F (near 954 GHz)

0 2 4 6 8 10

0 10 20 30 40 50 60

Error [K]

Altitude [km]

Band F T

Null space Radiometric noise Pointing Pointing c.

Antenna

Baseline

Calib. offset

Corr. noise

(51)

Summary: NO Band F (near 954 GHz)

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Band F NO

Null space Radiometric noise Pointing Pointing c.

Antenna

Baseline

Calib. offset

Corr. noise

(52)

Summary: HCl Band B1 (near 626 GHz)

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Band B1 HCl

Null space Radiometric noise Pointing Pointing c.

Antenna

Baseline

Calib. offset

Corr. noise

(53)

Summary: HOCl Band B2 (near 628 GHz)

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Band B2 HOCl

Null space Radiometric noise Pointing Pointing c.

Antenna

Baseline

Calib. offset

Corr. noise

(54)

Summary: H

2

O Band A (near 500 GHz)

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Band A H2O(l)

Null space Radiometric noise Pointing Pointing c.

Antenna

Baseline

Calib. offset

Corr. noise

(55)

Summary: N

2

O Band A (near 500 GHz)

0 20 40 60 80 100

0 10 20 30 40 50 60

Relative Error [%]

Altitude [km]

Band A N2O

Null space Radiometric noise Pointing Pointing c.

Antenna

Baseline

Calib. offset

Corr. noise

(56)

Conclusions (1)

Most critical parameters:



Antenna pattern knowledge (far wing must be covered, requires



35 dB noise)



Pointing accuracy (should be better than



200 m RMS, increased delay in antenna control loop helps)



Unwanted sideband (should be significantly better than 20 dB if there are strong lines in the sideband)

– Can be optimized if other sideband is not used for measurements



Atmospheric Temperature uncertainty

– Temperature retrieval schemes are currently

investigated

(57)

Conclusions (2)

Slightly less critical parameters:



Baseline ripples



Calibration errors

But SOPRANO radiometric requirements are stringent (one could also say optimistic):



0.1 K amplitude of baseline ripples



1 K hot and cold load temperature errors



0.2 K non-linearity

More significant for SMILES because radiometric noise is lower

From all our practical experience, baseline

ripples are likely to be a problem with the actual

instrument.

(58)

Conclusions (3)

Relatively uncritical parameters:



Actual shape of antenna pattern (investigated 1–10 % near wing, 0–4 % far wing)

– provided it is well known

– provided FWHM stays the same

– provided the scan goes down into the opaque region



Pointing stability

– Leads to slightly increased width of effective antenna pattern



200 m is tolerable



Baseline discontinuities (0.4 K every 2 GHz is tolerable)

– Can be optimized (disc. not on line centers)



Correlated noise

– Same order of magnitude as measurement noise (for integration time 10



atmospheric) – Statistical error, i.e., goes down when data

is averaged

(59)

Conclusion of the conclusions

Crucial!



Pointing accuracy



Baseline



Knowledge of instrument parameters, in particular

– Antenna pattern

– Sideband ratio

(60)

Ongoing work

The study has been extended by ESTEC. Issues:



Temperature / pointing retrieval (in particular from bands without oxygen lines):

IFE Bremen



Dedicated study for the retrieval of very weak species, e.g., BrO:

Observatoire de Bordeaux

References

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