Intercomparison of Integrated Water Vapor Measurements at High Latitudes from Co-Located and Near-Located Instruments

Data from global positioning system (GPS) ground-based receivers, ground-based microwave radiometers (MWRs), and radiosondes (RS) at two high-latitude sites were compared. At one site, the North Slope of Alaska (NSA), Barrow, Alaska (USA), the instruments were co-located, while at the other site, th...

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Published in:Remote Sensing
Main Authors: Ermanno Fionda, Maria Cadeddu, Vinia Mattioli, Rosa Pacione
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
GPS
Online Access:https://doi.org/10.3390/rs11182130
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spelling ftmdpi:oai:mdpi.com:/2072-4292/11/18/2130/ 2023-08-20T04:05:32+02:00 Intercomparison of Integrated Water Vapor Measurements at High Latitudes from Co-Located and Near-Located Instruments Ermanno Fionda Maria Cadeddu Vinia Mattioli Rosa Pacione 2019-09-13 application/pdf https://doi.org/10.3390/rs11182130 EN eng Multidisciplinary Digital Publishing Institute Atmosphere Remote Sensing https://dx.doi.org/10.3390/rs11182130 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 11; Issue 18; Pages: 2130 water vapor microwave radiometry GPS radio sounding remote sensing Text 2019 ftmdpi https://doi.org/10.3390/rs11182130 2023-07-31T22:36:23Z Data from global positioning system (GPS) ground-based receivers, ground-based microwave radiometers (MWRs), and radiosondes (RS) at two high-latitude sites were compared. At one site, the North Slope of Alaska (NSA), Barrow, Alaska (USA), the instruments were co-located, while at the other site, the second ARM Mobile Facility (AMF2), Hyytiälä, Finland, the GPS receiver was located about 20 km away from the MWRs and RS. Differences between the GPS-derived integrated water vapor (IWV) and the other three instruments were analyzed in terms of mean differences and standard deviation. A comparison of co-located and near-located independently calibrated instruments allowed us to isolate issues that may be specific to a single system and, to some extent, to isolate the effects of the distance between the GPS receiver and the remaining instruments. The results showed that at these two high-latitude sites, when the IWV was less than 15 kg/m2, the GPS agreed with other instruments within 0.5–0.7 kg/m2. When the variability of water vapor was higher, mostly in the summer months, the GPS agreed with other instruments within 0.8–1 kg/m2. The total random uncertainty between the GPS and the other systems was of the order of 0.6–1 kg/m2 and was the dominant effect when the IWV was higher than 15 kg/m2. Text Barrow north slope Alaska MDPI Open Access Publishing Remote Sensing 11 18 2130
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic water vapor
microwave radiometry
GPS
radio sounding
remote sensing
spellingShingle water vapor
microwave radiometry
GPS
radio sounding
remote sensing
Ermanno Fionda
Maria Cadeddu
Vinia Mattioli
Rosa Pacione
Intercomparison of Integrated Water Vapor Measurements at High Latitudes from Co-Located and Near-Located Instruments
topic_facet water vapor
microwave radiometry
GPS
radio sounding
remote sensing
description Data from global positioning system (GPS) ground-based receivers, ground-based microwave radiometers (MWRs), and radiosondes (RS) at two high-latitude sites were compared. At one site, the North Slope of Alaska (NSA), Barrow, Alaska (USA), the instruments were co-located, while at the other site, the second ARM Mobile Facility (AMF2), Hyytiälä, Finland, the GPS receiver was located about 20 km away from the MWRs and RS. Differences between the GPS-derived integrated water vapor (IWV) and the other three instruments were analyzed in terms of mean differences and standard deviation. A comparison of co-located and near-located independently calibrated instruments allowed us to isolate issues that may be specific to a single system and, to some extent, to isolate the effects of the distance between the GPS receiver and the remaining instruments. The results showed that at these two high-latitude sites, when the IWV was less than 15 kg/m2, the GPS agreed with other instruments within 0.5–0.7 kg/m2. When the variability of water vapor was higher, mostly in the summer months, the GPS agreed with other instruments within 0.8–1 kg/m2. The total random uncertainty between the GPS and the other systems was of the order of 0.6–1 kg/m2 and was the dominant effect when the IWV was higher than 15 kg/m2.
format Text
author Ermanno Fionda
Maria Cadeddu
Vinia Mattioli
Rosa Pacione
author_facet Ermanno Fionda
Maria Cadeddu
Vinia Mattioli
Rosa Pacione
author_sort Ermanno Fionda
title Intercomparison of Integrated Water Vapor Measurements at High Latitudes from Co-Located and Near-Located Instruments
title_short Intercomparison of Integrated Water Vapor Measurements at High Latitudes from Co-Located and Near-Located Instruments
title_full Intercomparison of Integrated Water Vapor Measurements at High Latitudes from Co-Located and Near-Located Instruments
title_fullStr Intercomparison of Integrated Water Vapor Measurements at High Latitudes from Co-Located and Near-Located Instruments
title_full_unstemmed Intercomparison of Integrated Water Vapor Measurements at High Latitudes from Co-Located and Near-Located Instruments
title_sort intercomparison of integrated water vapor measurements at high latitudes from co-located and near-located instruments
publisher Multidisciplinary Digital Publishing Institute
publishDate 2019
url https://doi.org/10.3390/rs11182130
genre Barrow
north slope
Alaska
genre_facet Barrow
north slope
Alaska
op_source Remote Sensing; Volume 11; Issue 18; Pages: 2130
op_relation Atmosphere Remote Sensing
https://dx.doi.org/10.3390/rs11182130
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs11182130
container_title Remote Sensing
container_volume 11
container_issue 18
container_start_page 2130
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