Perturbations in atmospheric gaseous components over coastal Antarctica detected in GPS signals and its natural origin to volcanic eruption

Although the variations in atmospheric water content control the perturbations in total travel time delay experienced by GPS signals during passage through the atmosphere (ZTD-Zenith Total Delay), significant changes in ZTD can also occur due to anomalous high influx of dry components into the atmos...

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Bibliographic Details
Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
GPS
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15602
http://id.nii.ac.jp/1291/00015497/
id ftnipr:oai:nipr.repo.nii.ac.jp:00015602
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00015602 2023-05-15T13:49:00+02:00 Perturbations in atmospheric gaseous components over coastal Antarctica detected in GPS signals and its natural origin to volcanic eruption 2019-03 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15602 http://id.nii.ac.jp/1291/00015497/ en eng https://doi.org/10.1016/j.polar.2018.11.009 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15602 http://id.nii.ac.jp/1291/00015497/ Polar Science, 19, 69-76(2019-03) 18739652 GPS Zenith total delay Black carbon Mt. chaiten Antarctica Journal Article 2019 ftnipr https://doi.org/10.1016/j.polar.2018.11.009 2022-12-03T19:43:10Z Although the variations in atmospheric water content control the perturbations in total travel time delay experienced by GPS signals during passage through the atmosphere (ZTD-Zenith Total Delay), significant changes in ZTD can also occur due to anomalous high influx of dry components into the atmosphere during massive volcanic eruptions. Such a possibility is illustrated here by analyzing GPS data from different locations around the Antarctic continent during the massive eruption of Mt. Chaiten volcano in Chile on 19th, February 2009. GPS derived ZTD values showed abnormal perturbation during the transition from summer to winter time in Antarctic margins. The irregular ZTD values, which existed for the short period from 19th, February to 08th, March 2009, exhibited perturbations and showed high correspondence with the abnormal atmospheric black carbon (BC) content noticed over the Indian Antarctic station (Maitri) during the same period. We therefore suggest that the anomalous ZTD changes might have resulted due to high BC influx into the atmosphere. We propose that the 19th, February 2009 massive eruption of Mt. Chaiten is the source for the BC, which moved from the volcanic front to the East Antarctica margin along with the circum polar current. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Polar Science Polar Science National Institute of Polar Research Repository, Japan Antarctic The Antarctic East Antarctica Indian Maitri ENVELOPE(11.733,11.733,-70.764,-70.764) Polar Science 19 69 76
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic GPS
Zenith total delay
Black carbon
Mt. chaiten
Antarctica
spellingShingle GPS
Zenith total delay
Black carbon
Mt. chaiten
Antarctica
Perturbations in atmospheric gaseous components over coastal Antarctica detected in GPS signals and its natural origin to volcanic eruption
topic_facet GPS
Zenith total delay
Black carbon
Mt. chaiten
Antarctica
description Although the variations in atmospheric water content control the perturbations in total travel time delay experienced by GPS signals during passage through the atmosphere (ZTD-Zenith Total Delay), significant changes in ZTD can also occur due to anomalous high influx of dry components into the atmosphere during massive volcanic eruptions. Such a possibility is illustrated here by analyzing GPS data from different locations around the Antarctic continent during the massive eruption of Mt. Chaiten volcano in Chile on 19th, February 2009. GPS derived ZTD values showed abnormal perturbation during the transition from summer to winter time in Antarctic margins. The irregular ZTD values, which existed for the short period from 19th, February to 08th, March 2009, exhibited perturbations and showed high correspondence with the abnormal atmospheric black carbon (BC) content noticed over the Indian Antarctic station (Maitri) during the same period. We therefore suggest that the anomalous ZTD changes might have resulted due to high BC influx into the atmosphere. We propose that the 19th, February 2009 massive eruption of Mt. Chaiten is the source for the BC, which moved from the volcanic front to the East Antarctica margin along with the circum polar current.
format Article in Journal/Newspaper
title Perturbations in atmospheric gaseous components over coastal Antarctica detected in GPS signals and its natural origin to volcanic eruption
title_short Perturbations in atmospheric gaseous components over coastal Antarctica detected in GPS signals and its natural origin to volcanic eruption
title_full Perturbations in atmospheric gaseous components over coastal Antarctica detected in GPS signals and its natural origin to volcanic eruption
title_fullStr Perturbations in atmospheric gaseous components over coastal Antarctica detected in GPS signals and its natural origin to volcanic eruption
title_full_unstemmed Perturbations in atmospheric gaseous components over coastal Antarctica detected in GPS signals and its natural origin to volcanic eruption
title_sort perturbations in atmospheric gaseous components over coastal antarctica detected in gps signals and its natural origin to volcanic eruption
publishDate 2019
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15602
http://id.nii.ac.jp/1291/00015497/
long_lat ENVELOPE(11.733,11.733,-70.764,-70.764)
geographic Antarctic
The Antarctic
East Antarctica
Indian
Maitri
geographic_facet Antarctic
The Antarctic
East Antarctica
Indian
Maitri
genre Antarc*
Antarctic
Antarctica
East Antarctica
Polar Science
Polar Science
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Polar Science
Polar Science
op_relation https://doi.org/10.1016/j.polar.2018.11.009
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15602
http://id.nii.ac.jp/1291/00015497/
Polar Science, 19, 69-76(2019-03)
18739652
op_doi https://doi.org/10.1016/j.polar.2018.11.009
container_title Polar Science
container_volume 19
container_start_page 69
op_container_end_page 76
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