ミズホ カンソク キョテン ノ ニッシャ シュウシ

P(論文) The solar radiation balance on the ground surface at Mizuho Camp (70°42.6'S, 44°18.9'E, elevation 2,200m) is discussed on the basis of the observations with two pyranometers carried out during the period from July to December 1972. The daily values of the global radiation around the...

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Main Authors: 川口, 貞男, カワグチ, サダオ, 佐々木, 浩, ササキ, ヒロシ, KAWAGUCHI, Sadao, SASAKI, Hiroshi
Language:Japanese
Published: 国立極地研究所 1975
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/7831/files/KJ00002476934.pdf
https://doi.org/10.15094/00007831
https://nipr.repo.nii.ac.jp/records/7831
_version_ 1829301652868300800
author 川口, 貞男
カワグチ, サダオ
佐々木, 浩
ササキ, ヒロシ
KAWAGUCHI, Sadao
SASAKI, Hiroshi
author_facet 川口, 貞男
カワグチ, サダオ
佐々木, 浩
ササキ, ヒロシ
KAWAGUCHI, Sadao
SASAKI, Hiroshi
author_sort 川口, 貞男
collection National Institute of Polar Research Repository, Japan
description P(論文) The solar radiation balance on the ground surface at Mizuho Camp (70°42.6'S, 44°18.9'E, elevation 2,200m) is discussed on the basis of the observations with two pyranometers carried out during the period from July to December 1972. The daily values of the global radiation around the summer solstice were 950 Ly under clear sky, and 640 Ly when cloudy, giving a monthly total of 25.6 × 10^3 Ly for December. Averaged monthly values of the albedo varied from 0.86 to 0.83 in July to December, and the albedos under cloudy condition were somewhat larger than those under clear sky condition. The decrease of the global radiation by cloud cover was small, about 30%, in comparison with the case in lower latitudes. This is partly due to the high transmissibility of clouds in Antarctica, and partly due to the multiple reflection of the solar radiation between the cloud bottom and the snow surface which has large albedos. The monthly values of global radiation and albedo for January to June in 1972 were estimated; relations among the solar altitude, global radiation and albedo obtained in the observed months were taken into consideration, extrapolating the observed cloud amounts at Syowa Station (69°00'S, 39°35/E) to Mizuho Camp. The annual values of global radiation and the effective short-wave radiation were 114×10^3Ly and 19 × 10^3 Ly, respectively. departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
genre_facet Antarc*
Antarctica
East Antarctica
geographic East Antarctica
Syowa Station
Mizuho
geographic_facet East Antarctica
Syowa Station
Mizuho
id ftnipr:oai:nipr.repo.nii.ac.jp:00007831
institution Open Polar
language Japanese
long_lat ENVELOPE(44.317,44.317,-70.683,-70.683)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00007831
op_relation 南極資料
54
34
41
AN00181831
00857289
https://nipr.repo.nii.ac.jp/record/7831/files/KJ00002476934.pdf
https://doi.org/10.15094/00007831
https://nipr.repo.nii.ac.jp/records/7831
publishDate 1975
publisher 国立極地研究所
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00007831 2025-04-13T14:09:49+00:00 ミズホ カンソク キョテン ノ ニッシャ シュウシ みずほ観測拠点の日射収支 Solar Radiation Balance at Mizuho Camp, East Antarctica 川口, 貞男 カワグチ, サダオ 佐々木, 浩 ササキ, ヒロシ KAWAGUCHI, Sadao SASAKI, Hiroshi 1975-12 application/pdf https://nipr.repo.nii.ac.jp/record/7831/files/KJ00002476934.pdf https://doi.org/10.15094/00007831 https://nipr.repo.nii.ac.jp/records/7831 jpn jpn 国立極地研究所 南極資料 54 34 41 AN00181831 00857289 https://nipr.repo.nii.ac.jp/record/7831/files/KJ00002476934.pdf https://doi.org/10.15094/00007831 https://nipr.repo.nii.ac.jp/records/7831 551.5 1975 ftnipr https://doi.org/10.15094/00007831 2025-03-19T10:19:57Z P(論文) The solar radiation balance on the ground surface at Mizuho Camp (70°42.6'S, 44°18.9'E, elevation 2,200m) is discussed on the basis of the observations with two pyranometers carried out during the period from July to December 1972. The daily values of the global radiation around the summer solstice were 950 Ly under clear sky, and 640 Ly when cloudy, giving a monthly total of 25.6 × 10^3 Ly for December. Averaged monthly values of the albedo varied from 0.86 to 0.83 in July to December, and the albedos under cloudy condition were somewhat larger than those under clear sky condition. The decrease of the global radiation by cloud cover was small, about 30%, in comparison with the case in lower latitudes. This is partly due to the high transmissibility of clouds in Antarctica, and partly due to the multiple reflection of the solar radiation between the cloud bottom and the snow surface which has large albedos. The monthly values of global radiation and albedo for January to June in 1972 were estimated; relations among the solar altitude, global radiation and albedo obtained in the observed months were taken into consideration, extrapolating the observed cloud amounts at Syowa Station (69°00'S, 39°35/E) to Mizuho Camp. The annual values of global radiation and the effective short-wave radiation were 114×10^3Ly and 19 × 10^3 Ly, respectively. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica National Institute of Polar Research Repository, Japan East Antarctica Syowa Station Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683)
spellingShingle 551.5
川口, 貞男
カワグチ, サダオ
佐々木, 浩
ササキ, ヒロシ
KAWAGUCHI, Sadao
SASAKI, Hiroshi
ミズホ カンソク キョテン ノ ニッシャ シュウシ
title ミズホ カンソク キョテン ノ ニッシャ シュウシ
title_full ミズホ カンソク キョテン ノ ニッシャ シュウシ
title_fullStr ミズホ カンソク キョテン ノ ニッシャ シュウシ
title_full_unstemmed ミズホ カンソク キョテン ノ ニッシャ シュウシ
title_short ミズホ カンソク キョテン ノ ニッシャ シュウシ
title_sort ミズホ カンソク キョテン ノ ニッシャ シュウシ
topic 551.5
topic_facet 551.5
url https://nipr.repo.nii.ac.jp/record/7831/files/KJ00002476934.pdf
https://doi.org/10.15094/00007831
https://nipr.repo.nii.ac.jp/records/7831