ndacc and water vapor raman lidars

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6 July 2006 First NDACC Water Vapor W orking Group Workshop, Be rn, Switzerland. 1 NDACC and Water Vapor Raman Lidars Thierry Leblanc JPL - Table Mountain Facility, CA [email protected]

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NDACC and Water Vapor Raman Lidars. Thierry Leblanc JPL - Table Mountain Facility, CA [email protected]. NDACC and Water Vapor Raman Lidar 1. Measuring goals. Water vapor plays significant role in radiative balance of the UTLS - PowerPoint PPT Presentation

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Page 1: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

1

NDACC and Water Vapor Raman Lidars

Thierry Leblanc

JPL - Table Mountain Facility, CA

[email protected]

Page 2: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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NDACC and Water Vapor Raman Lidar 1. Measuring goals

• Water vapor plays significant role in radiative balance of the UTLS

• Water Vapor variability is very high in both space and time

• High resolution water vapor measurements in the UTLS has remained sparse until today

2002: It was proposed to add water vapor Raman lidars to the set of NDACC instruments with the specific following

requirements:

• Capable of measuring water vapor near and above the tropopause

• Capable of measuring down to a few ppm

• Capable to sustain relatively high vertical and temporal resolution

Page 3: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

3

NDACC and Water Vapor Raman Lidar 2. Existing wv lidars

Page 4: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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NDACC and Water Vapor Raman Lidar: 3. Technique/retrieval

• Vibrational Raman backscatter technique at two wavelengths

• UV:

– Laser emission at 355 nm

– Reception at 387 nm (Raman N2) and 407.5 nm (H20)

• Visible:

– Laser emission at 532 nm

– Reception at 607 nm (Raman N2) and 660 nm (H20)

• Lidar signals corrected for background noise, saturation/pile-up effects, signal induced noise, range, Rayleigh extinction.

• Small additional correction due to temperature dependence of the H2O cross-section is needed occasionally if using very narrow filter

• After correction, the ratio of the lidar signals at the two wavelengths is proportional to water vapor mixing ratio.

Needs calibration !

Page 5: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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NDACC and Water Vapor Raman Lidar: 4. Calibration

• Calibration techniques:

– Internal/theoretical: Very challenging because requires accurate knowledge of transmission ratios of ALL the lidar optical and electro-photonic components

virtually impossible to achieve at required accuracy

– Semi-empirical: Use of a Calibration lamp to illuminate lidar receiver in conditions that mimic real measurements: Difficult, but possible

Accuracy depends mostly of lamp calibration accuracy

– External: Use of independent measurements, e.g., radiosonde, microwave

Easy to implement but accuracy limited by that of independent measurement

Page 6: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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NDACC and Water Vapor Raman Lidar 5. CONCLUSION

Important requirements for NDACC long-term measurements and associated challenges to lidar community:

1. High capability lidar

Capable of detecting a few ppm at tropopause

2. Stable calibration constant

Simultaneous multiple calibration techniques must be available to cross-validate calibration constants from each technique, and insure long-term stability

Page 7: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Overview 1

FIBER FROM0.91 m TELESCOPE

L1

B2 B3

P

P

P

P

F1

F3

F2

P

B4B4

387M Ch6Licel 5

387H Ch4Licel 3 407H Ch3

Licel 2

407M Ch5Licel 4

355H Ch1Licel 0

P

P

P

F2

F3

NEAR CHANNELSF1

407L Ch7Licel 6

387L Ch8Licel 7

355M Ch2Licel 1

SKY

Laser energy:

700 mJ/pulse

8 channels:

3 w.v. ranges

3 telescopes:

One 90 cm

Three 6 cm

Hamamatsu PMTs

Licel

photocounting

8000 7.5-m bins

Vertical resolution

75-m

Page 8: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Overview 2

• Calibration used so far:– Radiosondes: Vaisala Humicap RS-92 sensors

• Future plans:– UV lamp, GPS, Microwave– Simultaneous, multiple calibration techniques

• Important requirement for NDACC long-term measurements:– Stable calibration constant

Page 9: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Overview 3

TMF– 50 miles NE of Los Angeles– Lat: 34.4ºN– Long: 117.7ºW– Alt: 2285 m (7500 ft)

> 340 clear nights/year

Dataset

• TMF water vapor measurement program started in late 2004

• November 2004 – Present:– Radiosonde P,T, (2.3-20 km), RH (2.3-15 km)

• April 2005 – Present:– Raman Lidar (4-19 km)

• Lidar vertical resolution and accuracy:– 75 m instrumental, 2-h routine integration (5-minutes minimum)– WV total error estimated to ~5-8 ppm at tropopause

Page 10: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Overview 4

20

15

10

5

0

Alti

tude

(km

)

0.001 0.01 0.1 1 10Water Vapor Mixing Ratio (g/kg)

Page 11: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Overview 5

Page 12: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Overview 6

Water Vapor Mixing Ratio (g/kg)

Alti

tude

(km

)

0.01 0.1 1 10

11

10

9

8

7

6

5

4

3

GSFC data and this figure gracefully provided

by T. McGee, L. Twigg, G. Sumnicht, and D. Silbert

Page 13: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Overview 7

Overall mean Differences

Page 14: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Overview 8

Watch time variability!

Page 15: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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Aura/MLS - Lidar and

Aura/MLS - sonde

The Raman Lidar at Table Mountain Facility: Overview 9

Page 16: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Overview 10

Page 17: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The Raman Lidar at Table Mountain Facility: Summary

- So Far:- TMF Water Vapor Raman Lidar is doing well- Capable to reach 15-18 km for a 2-hour integration- As of today, used only radiosonde for calibration

- Next:- Introduce new calibration techniques:

- Lamp- GPS?- Microwave?

- Improve lidar power/aperture capability to reach final objectives of detection level of 2 ppm at 15 km

Page 18: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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% Difference-100 -50 0 50 100

Alt

itu

de

(km

)

3

4

5

6

7

8

9

10

116/13/2005

The Raman Lidar at Table Mountain Facility: Overview 1

6/13/2005

Red = JPL-AT

Green = Sonde-AT

Orange = STROZ-Lite – AT

From:

Tom McGee and Larry Twigg, NASA-GSFC

Page 19: NDACC and Water Vapor Raman Lidars

6 July 2006 First NDACC Water Vapor Working Group Workshop, Bern, Switzerland.

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The GSFC Raman Lidars: Overview 2

From: Tom McGee and Larry Twigg, NASA-GSFC