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 Kulla, Christoph Ritter
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Online Access:https://doi.org/10.3390/rs11060616
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author Birte Kulla
Christoph Ritter
author_facet Birte Kulla
Christoph Ritter
author_sort Birte Kulla
collection MDPI Open Access Publishing
container_issue 6
container_start_page 616
container_title Remote Sensing
container_volume 11
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.
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spelling ftmdpi:oai:mdpi.com:/2072-4292/11/6/616/ 2025-01-16T20:41:44+00:00 Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles Birte Kulla Christoph Ritter agris 2019-03-13 application/pdf https://doi.org/10.3390/rs11060616 EN eng Multidisciplinary Digital Publishing Institute Atmospheric Remote Sensing https://dx.doi.org/10.3390/rs11060616 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 11; Issue 6; Pages: 616 lidar Raman shift AWIPEV Svalbard water vapor water vapor calibration radiosonde GRUAN Vaisala atmosphere Text 2019 ftmdpi https://doi.org/10.3390/rs11060616 2023-07-31T22:06:47Z 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. Text Arctic Svalbard MDPI Open Access Publishing Arctic Svalbard Remote Sensing 11 6 616
spellingShingle lidar
Raman shift
AWIPEV
Svalbard
water vapor
water vapor calibration
radiosonde
GRUAN
Vaisala
atmosphere
Birte Kulla
Christoph Ritter
Water Vapor Calibration: Using a Raman Lidar and Radiosoundings to Obtain Highly Resolved Water Vapor Profiles
title 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_short 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
topic lidar
Raman shift
AWIPEV
Svalbard
water vapor
water vapor calibration
radiosonde
GRUAN
Vaisala
atmosphere
topic_facet lidar
Raman shift
AWIPEV
Svalbard
water vapor
water vapor calibration
radiosonde
GRUAN
Vaisala
atmosphere
url https://doi.org/10.3390/rs11060616