IWV retrieval from ground GNSS receivers during NAWDEX

A ground-based network of more than 1200 Global Navigation Satellite System (GNSS) Continuously Operating Reference Stations (CORS) was analysed using GIPSY-OASIS II software package for the documentation of time and space variations of water vapor in atmosphere during the North Atlantic Waveguide a...

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Published in:Advances in Geosciences
Main Authors: Bosser, Pierre, Bock, Olivier
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/adgeo-55-13-2021
https://adgeo.copernicus.org/articles/55/13/2021/
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spelling ftcopernicus:oai:publications.copernicus.org:adgeo86668 2023-05-15T16:29:41+02:00 IWV retrieval from ground GNSS receivers during NAWDEX Bosser, Pierre Bock, Olivier 2021-02-01 application/pdf https://doi.org/10.5194/adgeo-55-13-2021 https://adgeo.copernicus.org/articles/55/13/2021/ eng eng doi:10.5194/adgeo-55-13-2021 https://adgeo.copernicus.org/articles/55/13/2021/ eISSN: 1680-7359 Text 2021 ftcopernicus https://doi.org/10.5194/adgeo-55-13-2021 2021-02-08T17:22:16Z A ground-based network of more than 1200 Global Navigation Satellite System (GNSS) Continuously Operating Reference Stations (CORS) was analysed using GIPSY-OASIS II software package for the documentation of time and space variations of water vapor in atmosphere during the North Atlantic Waveguide and Downstream impact EXperiment (NAWDEX) during fall 2016. The network extends throughout the North Atlantic, from the Caribbeans to Morocco through Greenland. This paper presents the methodology used for GNSS data processing, screening, and conversion of Zenith Tropospheric Delay (ZTD) estimates to Integrated Water Vapor content (IWV) using surface parameters from reanalysis. The retrieved IWV are used to evaluate the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalyses ERAI and ERA5. ERA5 shows an overall improvement over ERAI in representing the spatial and temporal variability of IWV over the study area. The mean bias is decreased from 0.31±0.63 to 0.19±0.56 kg m −2 (mean ±1 σ over all stations) and the standard deviation reduced from 2.17±0.67 to 1.64±0.53 kg m −2 combined with a slight improvement in correlation coefficient from 0.95 to 0.97. At regional scale, both reanalyses show a general wet bias at mid and northern latitudes but a dry bias in the Caribbeans. We hypothesize this results from the different nature of data being assimilated over the tropical oceans. This GNSS IWV data set is intended to be used for a better description of the high impact weather events that occurred during the NAWDEX experiment. Text Greenland North Atlantic Copernicus Publications: E-Journals Greenland Advances in Geosciences 55 13 22
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description A ground-based network of more than 1200 Global Navigation Satellite System (GNSS) Continuously Operating Reference Stations (CORS) was analysed using GIPSY-OASIS II software package for the documentation of time and space variations of water vapor in atmosphere during the North Atlantic Waveguide and Downstream impact EXperiment (NAWDEX) during fall 2016. The network extends throughout the North Atlantic, from the Caribbeans to Morocco through Greenland. This paper presents the methodology used for GNSS data processing, screening, and conversion of Zenith Tropospheric Delay (ZTD) estimates to Integrated Water Vapor content (IWV) using surface parameters from reanalysis. The retrieved IWV are used to evaluate the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalyses ERAI and ERA5. ERA5 shows an overall improvement over ERAI in representing the spatial and temporal variability of IWV over the study area. The mean bias is decreased from 0.31±0.63 to 0.19±0.56 kg m −2 (mean ±1 σ over all stations) and the standard deviation reduced from 2.17±0.67 to 1.64±0.53 kg m −2 combined with a slight improvement in correlation coefficient from 0.95 to 0.97. At regional scale, both reanalyses show a general wet bias at mid and northern latitudes but a dry bias in the Caribbeans. We hypothesize this results from the different nature of data being assimilated over the tropical oceans. This GNSS IWV data set is intended to be used for a better description of the high impact weather events that occurred during the NAWDEX experiment.
format Text
author Bosser, Pierre
Bock, Olivier
spellingShingle Bosser, Pierre
Bock, Olivier
IWV retrieval from ground GNSS receivers during NAWDEX
author_facet Bosser, Pierre
Bock, Olivier
author_sort Bosser, Pierre
title IWV retrieval from ground GNSS receivers during NAWDEX
title_short IWV retrieval from ground GNSS receivers during NAWDEX
title_full IWV retrieval from ground GNSS receivers during NAWDEX
title_fullStr IWV retrieval from ground GNSS receivers during NAWDEX
title_full_unstemmed IWV retrieval from ground GNSS receivers during NAWDEX
title_sort iwv retrieval from ground gnss receivers during nawdex
publishDate 2021
url https://doi.org/10.5194/adgeo-55-13-2021
https://adgeo.copernicus.org/articles/55/13/2021/
geographic Greenland
geographic_facet Greenland
genre Greenland
North Atlantic
genre_facet Greenland
North Atlantic
op_source eISSN: 1680-7359
op_relation doi:10.5194/adgeo-55-13-2021
https://adgeo.copernicus.org/articles/55/13/2021/
op_doi https://doi.org/10.5194/adgeo-55-13-2021
container_title Advances in Geosciences
container_volume 55
container_start_page 13
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