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Systematic lidar measurements of water vapor at Jungfraujoch

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J.-D.Bonjour, SI-DGR. 13.4.93. Systematic lidar measurements of water vapor at Jungfraujoch ... J.-D.Bonjour, SI-DGR. 13.4.93. Water vapour Raman lidar at IMAA ... – PowerPoint PPT presentation

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Title: Systematic lidar measurements of water vapor at Jungfraujoch


1
Systematic lidar measurements of water vapor at
Jungfraujoch V. Simeonov, B. Calpini, H. van den
Bergh I. Balin, P. Ristori, R. Nessler,
  • Lidar parameters
  • Measurements
  • -Water vapor
  • -Relative humidity
  • -Comparison with radiosonde, GPS, PFR
  • -Special events
  • Future plans
  • EARLINET

2
Jungfraujoch multiwavelength lidar
Water vapour Vibrational Raman 408 nm and
387nm Temperature Pure-rotational Raman
Relative humidity profile Aerosol Elastic
channels Aerosol extinction _at_ 355, 532, 1064
nm Aerosol backscatter _at_ 355 and 532 nm Raman
channels Vibrational_at_ 387nm, 408nm,
607nm Pure-rotational excitation l 532 nm 4
channels from Stokes and Anti Stokes
bands Transmitter NdYAG 400 mJ _at_ 1064 nm /100
Hz Receiver 20 cm F/4 Newtonian telescope
3
Water vapor mixing ratio and temperature profiles
Snow white sonde
SRS 400 (hygristor)
4
Lidar and radiosonde (SRS 400) measurements
5
Lidar GPS and PFR integrated water vapor
measurements
6
Water vapor mixing ratio and relative humidity
profiles
Dry Oct. May
Wet and layered
High boundary layer
7
High boundary layer
H2O vertical profiles
H2O horizontal profiles
8
High boundary layer - aerosol
ABL daytime
RL nighttime
9
Water flow rate and water temperature measured
at Massen
August
April
10
Future plans
11
European Aerosol Research LIdar NETwork EARLINET
  • GOALS
  • Creating a comprehensive database of the vertical
    aerosol distribution over Europe
  • Quantification of the aerosol load, its radiative
    properties, sources, sinks and long range
    transport
  • GOALS
  • Creating a comprehensive database of the vertical
    aerosol distribution over Europe
  • Quantification of the aerosol load, its radiative
    properties, sources, sinks and long range
    transport

Water vapor
12
Water vapour Raman lidar at IMAA-CNR Tito Scalo
(POTENZA) Italy
13
Water vapour Raman lidar at IMAA-CNR Tito Scalo
(POTENZA) Italy
DAY TIME CONDITIONS
5 September 2002
Typical vertical resolutions between 15 m and
300 m. Maximum height range about 5000
m. Statistical errors within 10 up to about
3000 m height and within a maximum of 50 at
5000 m.
14
Water vapour Raman lidar at IMAA-CNR Tito Scalo
(POTENZA) Italy
Typical vertical resolutions between 15 m and
300 m. Maximum height range about 12000
m. Statistical errors within
10 up to about 7000 m height and within a
maximum of 25 at 12000 m.
15
Summary
  • Raman lidar water vapor mixing ratio nigthtime
    profiles up to 10-11000 m
  • since 2000
  • Raman lidar relative humidity and temperature
    profiles since 2002
  • Water vapor mixing ratio and temperature profiles
    compared with radiosonde measurements
  • The integrated water vapor column compared with
    GPS and PFR data
  • 4 EARLINET stations ready to contribute to COST
    723 action
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