Total solar eclipse over Antarctica on 23 November 2003 and its effects on the atmosphere and snow near the ice sheet surface at Dome Fuji

The Moon cast a long shadow over Antarctica on 23 November 2003 in a total solar eclipse. The eclipse was observed at Dome Fuji Station, located at the highest point of East Dronning Maud Land, Antarctica, and lasted 1 h 41 min 37 s in a cloudless condition, during which the Sun was completely obscu...

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Published in:Journal of Geophysical Research
Main Authors: Takao, Kameda, Koji, Fujita, Okimasa, Sugita, Naohiko, Hirasawa, Shuhei, Takahashi
Language:English
Published: American Geophysical Union. 2009
Subjects:
Online Access:https://kitami-it.repo.nii.ac.jp/record/7656/files/No59.pdf
https://kitami-it.repo.nii.ac.jp/records/7656
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author Takao, Kameda
Koji, Fujita
Okimasa, Sugita
Naohiko, Hirasawa
Shuhei, Takahashi
author_facet Takao, Kameda
Koji, Fujita
Okimasa, Sugita
Naohiko, Hirasawa
Shuhei, Takahashi
author_sort Takao, Kameda
collection Kitami Institute of Technology Repository (KIT-R)
container_issue D18
container_title Journal of Geophysical Research
container_volume 114
description The Moon cast a long shadow over Antarctica on 23 November 2003 in a total solar eclipse. The eclipse was observed at Dome Fuji Station, located at the highest point of East Dronning Maud Land, Antarctica, and lasted 1 h 41 min 37 s in a cloudless condition, during which the Sun was completely obscured for 1 min 43 s. This was the first total solar eclipse to be observed in the Antarctic ice sheet. During the eclipse at Dome Fuji, the air temperature at 1.5 m above the snow surface and the subsurface snow temperature decreased by 3.0 K and 1.8 K, respectively. Estimated surface snow temperatures decreased by 4.6 K. Atmospheric pressure and wind direction did not change, but the wind speed possibly decreased by 0.3 m/s with decreasing air temperature; natural variations in wind speed before and after the eclipse made it difficult to identify a true effect of the solar eclipse. Variations of energy components (net shortwave and longwave radiations, sensible and latent heat fluxes, and geothermal heat) during the eclipse were investigated. The total loss of global solar radiation during the eclipse was 0.60 MJ m?2, equaling 1.6% of the total daily global solar radiation. Regional effects of the eclipse due to a reduction of global solar radiation for air temperature and snow temperature ranged from 0.015 to 0.020 K (W m?2)?1. We additionally examined the relation between eclipse obscuration (the fraction of the Sun's surface area occulted by the Moon) and the reduction of global solar radiation from the first to second contacts. The eclipse was also observed from space by the Moderate Resolution Imaging Spectroradiometer (MODIS) sensors onboard NASA's Terra and Aqua satellites. The observational results of this study will contribute to detailed model calculations for clarifying the meteorological effects of eclipses. journal article
genre Antarc*
Antarctic
Antarctica
Dronning Maud Land
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Dronning Maud Land
Ice Sheet
geographic Antarctic
Dome Fuji
Dome Fuji Station
Dronning Maud Land
The Antarctic
geographic_facet Antarctic
Dome Fuji
Dome Fuji Station
Dronning Maud Land
The Antarctic
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institution Open Polar
language English
long_lat ENVELOPE(39.700,39.700,-77.317,-77.317)
ENVELOPE(39.703,39.703,-77.317,-77.317)
op_collection_id ftkitamiit
op_doi https://doi.org/10.1029/2009JD011886
op_relation http://doi.org/10.1029/2009JD011886
Journal of Geophysical Research
D18115
114
1
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op_rights Copyright 2009 by the American Geophysical Union.
open access
publishDate 2009
publisher American Geophysical Union.
record_format openpolar
spelling ftkitamiit:oai:kitami-it.repo.nii.ac.jp:00007656 2025-04-06T14:38:26+00:00 Total solar eclipse over Antarctica on 23 November 2003 and its effects on the atmosphere and snow near the ice sheet surface at Dome Fuji Takao, Kameda Koji, Fujita Okimasa, Sugita Naohiko, Hirasawa Shuhei, Takahashi 2009-09 application/pdf https://kitami-it.repo.nii.ac.jp/record/7656/files/No59.pdf https://kitami-it.repo.nii.ac.jp/records/7656 eng eng American Geophysical Union. http://doi.org/10.1029/2009JD011886 Journal of Geophysical Research D18115 114 1 15 Copyright 2009 by the American Geophysical Union. open access 2009 ftkitamiit https://doi.org/10.1029/2009JD011886 2025-03-10T11:33:07Z The Moon cast a long shadow over Antarctica on 23 November 2003 in a total solar eclipse. The eclipse was observed at Dome Fuji Station, located at the highest point of East Dronning Maud Land, Antarctica, and lasted 1 h 41 min 37 s in a cloudless condition, during which the Sun was completely obscured for 1 min 43 s. This was the first total solar eclipse to be observed in the Antarctic ice sheet. During the eclipse at Dome Fuji, the air temperature at 1.5 m above the snow surface and the subsurface snow temperature decreased by 3.0 K and 1.8 K, respectively. Estimated surface snow temperatures decreased by 4.6 K. Atmospheric pressure and wind direction did not change, but the wind speed possibly decreased by 0.3 m/s with decreasing air temperature; natural variations in wind speed before and after the eclipse made it difficult to identify a true effect of the solar eclipse. Variations of energy components (net shortwave and longwave radiations, sensible and latent heat fluxes, and geothermal heat) during the eclipse were investigated. The total loss of global solar radiation during the eclipse was 0.60 MJ m?2, equaling 1.6% of the total daily global solar radiation. Regional effects of the eclipse due to a reduction of global solar radiation for air temperature and snow temperature ranged from 0.015 to 0.020 K (W m?2)?1. We additionally examined the relation between eclipse obscuration (the fraction of the Sun's surface area occulted by the Moon) and the reduction of global solar radiation from the first to second contacts. The eclipse was also observed from space by the Moderate Resolution Imaging Spectroradiometer (MODIS) sensors onboard NASA's Terra and Aqua satellites. The observational results of this study will contribute to detailed model calculations for clarifying the meteorological effects of eclipses. journal article Other/Unknown Material Antarc* Antarctic Antarctica Dronning Maud Land Ice Sheet Kitami Institute of Technology Repository (KIT-R) Antarctic Dome Fuji ENVELOPE(39.700,39.700,-77.317,-77.317) Dome Fuji Station ENVELOPE(39.703,39.703,-77.317,-77.317) Dronning Maud Land The Antarctic Journal of Geophysical Research 114 D18
spellingShingle Takao, Kameda
Koji, Fujita
Okimasa, Sugita
Naohiko, Hirasawa
Shuhei, Takahashi
Total solar eclipse over Antarctica on 23 November 2003 and its effects on the atmosphere and snow near the ice sheet surface at Dome Fuji
title Total solar eclipse over Antarctica on 23 November 2003 and its effects on the atmosphere and snow near the ice sheet surface at Dome Fuji
title_full Total solar eclipse over Antarctica on 23 November 2003 and its effects on the atmosphere and snow near the ice sheet surface at Dome Fuji
title_fullStr Total solar eclipse over Antarctica on 23 November 2003 and its effects on the atmosphere and snow near the ice sheet surface at Dome Fuji
title_full_unstemmed Total solar eclipse over Antarctica on 23 November 2003 and its effects on the atmosphere and snow near the ice sheet surface at Dome Fuji
title_short Total solar eclipse over Antarctica on 23 November 2003 and its effects on the atmosphere and snow near the ice sheet surface at Dome Fuji
title_sort total solar eclipse over antarctica on 23 november 2003 and its effects on the atmosphere and snow near the ice sheet surface at dome fuji
url https://kitami-it.repo.nii.ac.jp/record/7656/files/No59.pdf
https://kitami-it.repo.nii.ac.jp/records/7656