Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles

We revised the calibration of a water vapor Raman lidar by co-located radiosoundings for a site in the high European Arctic. For this purpose, we defined robust criteria for a valid calibration. One of these criteria is the logarithm of the water vapor mixing ratio between the sonde and the lidar. W...

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Published in:Remote Sensing
Main Authors: Birte Solveig Kulla, Christoph Ritter
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2019
Subjects:
Q
Online Access:https://doi.org/10.3390/rs11060616
https://doaj.org/article/9667aa3855044f27ae731d38389b614d
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spelling ftdoajarticles:oai:doaj.org/article:9667aa3855044f27ae731d38389b614d 2023-05-15T15:10:09+02:00 Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles Birte Solveig Kulla Christoph Ritter 2019-03-01T00:00:00Z https://doi.org/10.3390/rs11060616 https://doaj.org/article/9667aa3855044f27ae731d38389b614d EN eng MDPI AG http://www.mdpi.com/2072-4292/11/6/616 https://doaj.org/toc/2072-4292 2072-4292 doi:10.3390/rs11060616 https://doaj.org/article/9667aa3855044f27ae731d38389b614d Remote Sensing, Vol 11, Iss 6, p 616 (2019) lidar Raman shift AWIPEV Svalbard water vapor water vapor calibration radiosonde GRUAN Vaisala atmosphere Science Q article 2019 ftdoajarticles https://doi.org/10.3390/rs11060616 2022-12-31T11:23:31Z We revised the calibration of a water vapor Raman lidar by co-located radiosoundings for a site in the high European Arctic. For this purpose, we defined robust criteria for a valid calibration. One of these criteria is the logarithm of the water vapor mixing ratio between the sonde and the lidar. With an error analysis, we showed that for our site correlations smaller than 0.95 could be explained neither by noise in the lidar nor by wrong assumptions concerning the aerosol or Rayleigh extinction. However, highly variable correlation coefficients between sonde and consecutive lidar profiles were found, suggesting that small scale variability of the humidity was our largest source of error. Therefore, not all co-located radiosoundings are useful for lidar calibration. As we assumed these changes to be non-systematic, averaging over several independent measurements increased the calibration’s quality. The calibration of the water vapor measurements from the lidar for individual profiles varied by less than ±5%. The seasonal median, used for calibration in this study, was stable and reliable (confidence ±1% for the season with most calibration profiles). Thus, the water vapor mixing ratio profiles from the Koldewey Aerosol Raman Lidar (KARL) are very accurate. They show high temporal variability up to 4 km altitude and, therefore, provide additional, independent information to the radiosonde. Article in Journal/Newspaper Arctic Svalbard Directory of Open Access Journals: DOAJ Articles Arctic Svalbard Remote Sensing 11 6 616
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic lidar
Raman shift
AWIPEV
Svalbard
water vapor
water vapor calibration
radiosonde
GRUAN
Vaisala
atmosphere
Science
Q
spellingShingle lidar
Raman shift
AWIPEV
Svalbard
water vapor
water vapor calibration
radiosonde
GRUAN
Vaisala
atmosphere
Science
Q
Birte Solveig Kulla
Christoph Ritter
Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles
topic_facet lidar
Raman shift
AWIPEV
Svalbard
water vapor
water vapor calibration
radiosonde
GRUAN
Vaisala
atmosphere
Science
Q
description We revised the calibration of a water vapor Raman lidar by co-located radiosoundings for a site in the high European Arctic. For this purpose, we defined robust criteria for a valid calibration. One of these criteria is the logarithm of the water vapor mixing ratio between the sonde and the lidar. With an error analysis, we showed that for our site correlations smaller than 0.95 could be explained neither by noise in the lidar nor by wrong assumptions concerning the aerosol or Rayleigh extinction. However, highly variable correlation coefficients between sonde and consecutive lidar profiles were found, suggesting that small scale variability of the humidity was our largest source of error. Therefore, not all co-located radiosoundings are useful for lidar calibration. As we assumed these changes to be non-systematic, averaging over several independent measurements increased the calibration’s quality. The calibration of the water vapor measurements from the lidar for individual profiles varied by less than ±5%. The seasonal median, used for calibration in this study, was stable and reliable (confidence ±1% for the season with most calibration profiles). Thus, the water vapor mixing ratio profiles from the Koldewey Aerosol Raman Lidar (KARL) are very accurate. They show high temporal variability up to 4 km altitude and, therefore, provide additional, independent information to the radiosonde.
format Article in Journal/Newspaper
author Birte Solveig Kulla
Christoph Ritter
author_facet Birte Solveig Kulla
Christoph Ritter
author_sort Birte Solveig Kulla
title Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles
title_short Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles
title_full Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles
title_fullStr Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles
title_full_unstemmed Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles
title_sort water vapor calibration: using a raman lidar and radiosoundings to obtain highly resolved water vapor profiles
publisher MDPI AG
publishDate 2019
url https://doi.org/10.3390/rs11060616
https://doaj.org/article/9667aa3855044f27ae731d38389b614d
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Svalbard
genre_facet Arctic
Svalbard
op_source Remote Sensing, Vol 11, Iss 6, p 616 (2019)
op_relation http://www.mdpi.com/2072-4292/11/6/616
https://doaj.org/toc/2072-4292
2072-4292
doi:10.3390/rs11060616
https://doaj.org/article/9667aa3855044f27ae731d38389b614d
op_doi https://doi.org/10.3390/rs11060616
container_title Remote Sensing
container_volume 11
container_issue 6
container_start_page 616
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