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\u3068\u898b\u7a4d\u3082\u3063\u305f.\u3053\u306e\u4ed6\u306b,\u30c9\u30fc\u30e0\u3075\u3058\u30671\u672c\u306e\u96ea\u5c3a\u30921\u5e74\u9593\u89b3\u6e2c\u3057\u305f\u6642\u306b\u5f97\u3089\u308c\u308b\u5e74\u5e73\u5747\u8868\u9762\u8cea\u91cf\u53ce\u652f\u306e\u8aa4\u5dee,10\u5e74\u5f8c\u306e\u518d\u6e2c\u5b9a\u3067\u5f97\u3089\u308c\u308b\u5e74\u5e73\u5747\u8868\u9762\u8cea\u91cf\u53ce\u652f\u306e\u8aa4\u5dee\u306a\u3069\u3092\u8ad6\u3058\u305f.\n\\nThis paper describes observational results of surface mass balance (SMB) at Dome Fuji (77\u00b019\u002701\u2033S, 39\u00b042\u002711\u2033E; 3810m a.s.l.), East Antarctica from 1995 to 2006. The SMB was estimated using 36 bamboo stakes (grid of 6\u00d76, placed at 20m intervals). The heights of the stake tops from the snow surface were measured at 0.5cm resolution twice monthly in 1995, 1996, 1997, and 2003, and once a year for the rest of the study period. The annual SMB from 1995 to 2006 at Dome Fuji was 27.3\u00b11.5kgm^\u003c-2\u003ea^\u003c-1\u003e. This result agrees well with the annual SMB from AD 1260 to 1993 (26.4kgm^\u003c-2\u003ea^\u003c-1\u003e), estimated from volcanic signals in the Dome Fuji ice core. From 1995 to 2006, there were 37 incidences of negative or zero annual SMB, which was 8.6%. Compared with similar studies at Vostok, South Pole and Dome C, we found that a site with SMB over 190kgm^\u003c-2\u003ea^\u003c-1\u003e is expected to have annual snow accumulation at the 95% confidence level. Sites from 1500 to 2500m above sea level fit the criteria on the Antarctic ice sheet. According to stake and snow pit observations at Vostok, we estimated that the probability of an annual layer missing (hiatus) at Dome Fuji under present-day and glacial conditions are 9.4% and 11.4%, respectively. Variations of SMB measured by 36-stakes for 12 years were also analyzed.", "subitem_description_type": "Abstract"}]}, "item_3_full_name_183": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "39209", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Kameda, Takao", "nameLang": "en"}]}, {"nameIdentifiers": [{"nameIdentifier": "39210", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Takahashi, syuhei", "nameLang": "en"}]}]}, "item_3_publisher_212": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "\u56fd\u7acb\u6975\u5730\u7814\u7a76\u6240"}]}, "item_3_rights_192": {"attribute_name": "\u6a29\u5229", "attribute_value_mlt": [{"subitem_rights": "Copyright 2008 National Institute of Polar Research"}]}, "item_3_select_195": {"attribute_name": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_3_subject_196": {"attribute_name": "\u65e5\u672c\u5341\u9032\u5206\u985e\u6cd5", "attribute_value_mlt": [{"subitem_subject": "500", "subitem_subject_scheme": "NDC"}]}, "item_access_right": {"attribute_name": "\u30a2\u30af\u30bb\u30b9\u6a29", "attribute_value_mlt": [{"subitem_access_right": "open access", "subitem_access_right_uri": "http://purl.org/coar/access_right/c_abf2"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "\u4e80\u7530, \u8cb4\u96c4", "creatorNameLang": "ja"}], "nameIdentifiers": [{"nameIdentifier": "44128", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "233974", "nameIdentifierScheme": "KAKEN", "nameIdentifierURI": "https://nrid.nii.ac.jp/ja/nrid/1000000233974"}]}, {"creatorNames": [{"creatorName": "\u672c\u5c71, \u79c0\u660e", "creatorNameLang": "ja"}], "nameIdentifiers": [{"nameIdentifier": "39206", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "\u85e4\u7530, \u79c0\u4e8c", "creatorNameLang": "ja"}], "nameIdentifiers": [{"nameIdentifier": "39207", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "\u9ad8\u6a4b, \u4fee\u5e73", "creatorNameLang": "ja"}], "nameIdentifiers": [{"nameIdentifier": "39208", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "\u30d5\u30a1\u30a4\u30eb\u60c5\u5831", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2016-11-22"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "No54.pdf", "filesize": [{"value": "528.4 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_note", "mimetype": "application/pdf", "size": 528400.0, "url": {"label": "No54.pdf", "url": "https://kitami-it.repo.nii.ac.jp/record/7654/files/No54.pdf"}, "version_id": "449f91fc-d61c-4e35-95b3-c18e3a0286aa"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "jpn"}]}, "item_resource_type": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"resourcetype": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "\u5357\u6975\u30c9\u30fc\u30e0\u3075\u3058\u306b\u304a\u3051\u308b1995\u5e74\u304b\u30892006\u5e74\u306e\u8868\u9762\u8cea\u91cf\u53ce\u652f\u306e\u7279\u5fb4", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "\u5357\u6975\u30c9\u30fc\u30e0\u3075\u3058\u306b\u304a\u3051\u308b1995\u5e74\u304b\u30892006\u5e74\u306e\u8868\u9762\u8cea\u91cf\u53ce\u652f\u306e\u7279\u5fb4", "subitem_title_language": "ja"}, {"subitem_title": "Outline of surface mass balance at Dome Fuji, East Antarctica, by the stake method from 1995 to 2006", "subitem_title_language": "en"}]}, "item_type_id": "3", "owner": "1", "path": ["1/86"], "permalink_uri": "https://kitami-it.repo.nii.ac.jp/records/7654", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2014-08-19"}, "publish_date": "2014-08-19", "publish_status": "0", "recid": "7654", "relation": {}, "relation_version_is_last": true, "title": ["\u5357\u6975\u30c9\u30fc\u30e0\u3075\u3058\u306b\u304a\u3051\u308b1995\u5e74\u304b\u30892006\u5e74\u306e\u8868\u9762\u8cea\u91cf\u53ce\u652f\u306e\u7279\u5fb4"], "weko_shared_id": -1}
  1. 学術雑誌掲載済論文
  2. 和雑誌

南極ドームふじにおける1995年から2006年の表面質量収支の特徴

https://kitami-it.repo.nii.ac.jp/records/7654
0e94a365-9c9e-4e06-bbb5-97e0f7036df8
名前 / ファイル ライセンス アクション
No54.pdf No54.pdf (528.4 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2014-08-19
タイトル
言語 ja
タイトル 南極ドームふじにおける1995年から2006年の表面質量収支の特徴
タイトル
言語 en
タイトル Outline of surface mass balance at Dome Fuji, East Antarctica, by the stake method from 1995 to 2006
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
その他のタイトル
その他のタイトル Outline of surface mass balance at Dome Fuji, East Antarctica, by the stake method from 1995 to 2006
著者 亀田, 貴雄

× 亀田, 貴雄

WEKO 44128
KAKEN 233974

ja 亀田, 貴雄

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本山, 秀明

× 本山, 秀明

WEKO 39206

ja 本山, 秀明

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藤田, 秀二

× 藤田, 秀二

WEKO 39207

ja 藤田, 秀二

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高橋, 修平

× 高橋, 修平

WEKO 39208

ja 高橋, 修平

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著者別名
姓名
姓名 Kameda, Takao
言語 en
著者別名
姓名
姓名 Takahashi, syuhei
言語 en
抄録
内容記述タイプ Abstract
内容記述 1995年1月25日に南極ドームふじに36本雪尺(20m間隔で100m×100m)が第36次南極地域観測隊により設置され,それ以来雪尺の高さが継続的に測定されてきた.ドームふじ基地で越冬観測を実施した4年間(1995年1月から1997年12月及び2003年1月から2004年1月)は月2回測定し,それ以外は年1回の測定(1月上旬が多い)を実施した.この結果,1995年から2006年までのドームふじの年平均表面質量収支は,27.3±1.5kgm^<-2>a^<-1> であることが推定できた.これは,ドームふじ浅層コアから推定された西暦1260年から1993年までの平均値(26.4kgm^<-2>a^<-1>)と近い値であった.また,ドームふじでは1年後に雪尺の高さが等しいかもしくは高くなっている「負の年間表面質量収支」が8.6%の確率で起こっていることがわかった.南極内陸に位置するボストーク,南極点,ドームCでの同様な観測結果と比較することにより,負の年間表面質量収支は年平均表面質量収支の増加とともに減少し,190kgm^<-2>a^<-1> 以上の地点ではで負の年間表面質量収支は95%の信頼水準で起こらず,正の年平均表面質量収支が期待できることがわかった.190kgm^<-2>a^<-1> 以上の年平均表面質量収支は地域により異なるが,現在の南極氷床ではおおよそ標高1500-2500mに相当するので,この標高域では毎年の積雪が氷床に記録されている地点が多いことが推定できた.一方,ボストークでのピット観測結果を参考にして,現在及び氷期のドームふじコアでの年層欠損確率をそれぞれ9.4%,11.4% と見積もった.この他に,ドームふじで1本の雪尺を1年間観測した時に得られる年平均表面質量収支の誤差,10年後の再測定で得られる年平均表面質量収支の誤差などを論じた.
\nThis paper describes observational results of surface mass balance (SMB) at Dome Fuji (77°19'01″S, 39°42'11″E; 3810m a.s.l.), East Antarctica from 1995 to 2006. The SMB was estimated using 36 bamboo stakes (grid of 6×6, placed at 20m intervals). The heights of the stake tops from the snow surface were measured at 0.5cm resolution twice monthly in 1995, 1996, 1997, and 2003, and once a year for the rest of the study period. The annual SMB from 1995 to 2006 at Dome Fuji was 27.3±1.5kgm^<-2>a^<-1>. This result agrees well with the annual SMB from AD 1260 to 1993 (26.4kgm^<-2>a^<-1>), estimated from volcanic signals in the Dome Fuji ice core. From 1995 to 2006, there were 37 incidences of negative or zero annual SMB, which was 8.6%. Compared with similar studies at Vostok, South Pole and Dome C, we found that a site with SMB over 190kgm^<-2>a^<-1> is expected to have annual snow accumulation at the 95% confidence level. Sites from 1500 to 2500m above sea level fit the criteria on the Antarctic ice sheet. According to stake and snow pit observations at Vostok, we estimated that the probability of an annual layer missing (hiatus) at Dome Fuji under present-day and glacial conditions are 9.4% and 11.4%, respectively. Variations of SMB measured by 36-stakes for 12 years were also analyzed.
書誌情報 南極資料

巻 52, 号 特集号, p. 151-158, 発行日 2008-06
権利
権利情報 Copyright 2008 National Institute of Polar Research
出版者
出版者 国立極地研究所
著者版フラグ
値 publisher
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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