{"title":"Chemical components in rime and snow collected from the mountains in Kinki, Chubu and Chugoku regions","authors":"H. Kono, R. Inoue, K. Eguti","doi":"10.5331/SEPPYO.68.481","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.481","url":null,"abstract":"冬季山岳において樹氷と雪を採取し,その溶解成分濃度を測定した.対象とした山岳は奈良県大峰山系(標高1700m),同大台ケ原山系(標高1600m),滋賀県伊吹山(標高1377m),同比良山(標高1200m),長野県北アルプスの霞沢岳(標高2646m),同八ヶ岳(標高2998m),同御嶽山・田の原(標高2400m),同中央アルプス宝剣岳(標高2650m),鳥取県大山(標高1700m)である.測定データから次のような結果が得られた.標高が1000m-1800mの低い山岳では標高が2400m-3000mの高い山岳と比べると,樹氷に関して人為的発生源に起因するイオン成分の濃度及び海塩粒子に起因するイオン成分濃度が高い,雪に関しては,標高による差は樹氷より小さい. 樹氷のイオン成分濃度間の相関は, NO3-濃度とSO42-濃度の相関が高い. これは大気汚染濃度に対応していると思われる. 海塩粒子に起源を持つNa+濃度, Cl-濃度の相関が極めて高い. 人為発生源をもつNH4+, Ca2+, Mg2+についても相関は比較的高い. 上記の結果が, 一般的に成立するかについては, 更に多くのデータで追試が必要である. 樹氷中のイオン成分濃度は雪と比べると数倍から10倍の値を示す.","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"103 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133384509","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Chemical dynamics of snow and stream water in the Japanese Alps","authors":"T. Kuramoto, Keisuke Suzuki","doi":"10.5331/SEPPYO.68.467","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.467","url":null,"abstract":"積雪中の化学物質の動態と融雪期の河川水質の変化の特徴を明らかにすることを目的として,北アルプスの東側に位置する,信濃川水系高瀬川の源流域において,積雪の化学的特性と河川水質に関する調査を行った.調査期間は2004年12月から2005年4月である.積雪調査の結果,積雪中のpHは低く,多くの試料で酸性降水の基準となるpH5.62を下回った.積雪中の化学物質は,降雪時の気圧配置によって,層ごとにイオン含有量が異なっていた.積雪中に含まれる化学物質の多くは,融雪期まで保存されており,融雪とともに積雪から流出していた.河川水質は,融雪期に大きく変化した.河川水のpHと電気伝導度は,流出高の増加に伴って低下した.融雪期前半の流出高の増加時には,河川水中のCl-濃度とNO3-濃度が高くなった.融雪期後半には,融雪にともなう流出高の日変動が観測され,河川水質も日変動を示した.河川水中の陰イオン組成では,流出高が増加する前はHCO3-が約50%を占めていた.しかし,陰イオン組成に占めるHCO3-の割合は,流出高の増加前後で約23%減少した.一方,流出高が増加する前と比べて,流出高増加時には陰イオン組成に占めるCl-+NO3-とSO42-の割合は,それぞれ約12%増加していた.","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"104 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132792171","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Duration of forest floor snow cover in forest zone along an altitudinal gradient in Toyama prefecture, central Japan","authors":"M. Ishida","doi":"10.5331/SEPPYO.68.489","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.489","url":null,"abstract":"積雪時の地表面温度の特性を明らかにする目的で,超音波積雪深計によって観測された積雪の有無と地表面温度(1時間インターバル)との関連について検討した.その結果,積雪時の地表面温度は,0.5±1.0℃(平均±標準偏差,最小-0.4℃,最大3.2℃)であった.地表面温度3.2℃以下,前後5時間の標準偏差が±0.22℃以下の条件を積雪下とみなした場合の積雪の有無の判定的中率は95%であった.この判別条件を用い,2003年10月上旬から2004年6月下旬までの一冬季間,富山県下の暖帯から高山帯に至る主要森林タイプ19地点で林床の地表面温度の計測を行い積雪日数の推定を行った.その結果,各地点の積雪日数は,暖温帯常緑―落葉広葉樹林:22.5日/年,暖温帯落葉広葉樹林:58.4~104.5日/年,温帯落葉広葉樹林:113.3~158.6日/年,温帯針広混交林:150.3~158.7日/年,温帯―亜高山移行帯林:167.0日/年,亜高山帯林:214.5日/年,高山帯林:200.4~207.1日/年と推定された.暖帯から亜高山帯の森林では,標高と積雪日数の間に高い相関関係が認められた.","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"36 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"117308411","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Adhesion and friction of ice","authors":"N. Maeno","doi":"10.5331/SEPPYO.68.449","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.449","url":null,"abstract":"","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"101 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124136914","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Climatological characteristics corresponding to the occurrence of precipitation resulting in snow accretion in Japan","authors":"H. Matsushita, F. Nishio","doi":"10.5331/SEPPYO.68.421","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.421","url":null,"abstract":"気象庁の地上気象観測資料を基に,着雪現象に寄与する降水発生の気候学的特徴を明らかにすることを目的とした.本論文では,気温0℃以上で着雪現象を生じうる降水を湿降雪と定義して,地上気温と相対湿度を指標とした湿降雪の発生条件を示した.この発生条件は,電線着雪の重大事故時の状況とも対応した.湿降雪の発生条件に基づき,13冬季(1991年10月~2004年5月)における湿降雪の気候学的な発生実態を調べた.その結果,本州の日本海側地域や東北地方南部の内陸地域で,湿降雪日数が多く湿降雪日率(降水が湿降雪になる割合)が高いが,風が弱く地物に対する衝突降水強度が小さい.一方,関東地方の太平洋沿岸地域と北海道東部では湿降雪日数は少ないが,風や衝突降水強度が強い.この湿降雪の地域性は,従来の電線着雪の北陸型(弱風型)着雪と北海道型(強風型)着雪を気候的な地域分布として示した.特に,関東地方や北海道東部では湿降雪の発生頻度は少ないが,一度の発生によって着雪が顕著に発達する可能性があると考えられる.","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"6 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131062917","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Measures of icing and snow accretion on transmission line","authors":"Takehiko Kikuchi, Kazushige Tanaka, T. Saito","doi":"10.5331/SEPPYO.68.457","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.457","url":null,"abstract":"東京電力(株)が過去40年以上にわたって実施してきた送電設備に関する着氷雪対策技術の状況についてまとめた.本報告書では着氷雪現象のうち特に樹氷型着氷と湿型着雪を対象とした.現象の把握や送電設備への機械的影響,その影響を軽減するための対策技術について述べる.観測データは,現地での有人による直接的な調査や実規模試験線などを用いた調査結果である.着氷雪現象の物理的理論や数値解析,対策技術(偏心重量錐と回転自在型スペーサ,ルーズスペーサなど)の基本的考え方は,各検討段階において学識者やメーカ各社と協働で蓄積した.それらの技術が現実的に有効であるか否かについて,現地で自然発生する着氷雪や強風に曝される実規模試験線(高石山試験線,最上試験線)を用いて観測した.観測の結果,送電線への着氷雪に伴う荷重の増加量や振動抑止装置の効果を再現性あるデータで示すことができた.これらの成果は,現在運用されている送電設備に適用され,安定運用に貢献している.","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"17 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114973262","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Evaluation of snow entrainment coefficient based on the fluid dynamical analysis of snowdrift","authors":"T. Kikuchi, Y. Fukushima","doi":"10.5331/SEPPYO.68.267","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.267","url":null,"abstract":"乱流拡散方程式を用いて吹雪の流動解析を行う場合には,底面における濃度の境界条件の設定が重要となる.境界条件としては濃度勾配や濃度フラックスを規定するが,その際雪の連行係数の概念を用いるのが有効である.雪の連行係数は,流れの特性量と雪粒子の特性量の関数となることが期待される.吹雪流の数値解析モデルとしてκ-e乱流モデルを適用し,低温風洞実験の風速分布と飛雪流量分布のデータとの比較を行った.GarciaのパラメータZに用いる直径の算定にあたり,雪粒子の抗力と重力,浮力の釣り合いによる算出法を提案した.スノーパーティクルカウンター(SPC)を用いた直径と今回新たに求めた直径を用いて,砂の連行係数,雪の連行係数とZの関係を比較した.","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"69 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-07-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129126849","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Characteristics of new snow density and compressive viscosity in the Arctic region","authors":"M. Kajikawa, N. Sato, Y. Asuma, K. Kikuchi","doi":"10.5331/SEPPYO.68.277","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.277","url":null,"abstract":"","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"23 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-07-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122971692","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
J. Mori, T. Sone, J. Strelin, Cesar A. Torielli, K. Fukui
{"title":"Characteristics of air and ground temperatures and the reconstruction of active layer thickness on the Rink Plateau, James Ross Island, Antarctic Peninsula","authors":"J. Mori, T. Sone, J. Strelin, Cesar A. Torielli, K. Fukui","doi":"10.5331/SEPPYO.68.287","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.287","url":null,"abstract":"","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"99 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-07-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115163643","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Sea ice variation in Lützow-Holmbukta, Antarctica, during the last fifty years","authors":"S. Ushio, H. Wakabayashi, F. Nishio","doi":"10.5331/SEPPYO.68.299","DOIUrl":"https://doi.org/10.5331/SEPPYO.68.299","url":null,"abstract":"1990年代後半から2005年までの間,南極リュツォ・ホルム湾では沿岸定着氷の崩壊・流出が頻繁に観測されている.南極沿岸海氷の変動特性を把握するために,同湾で生じる海氷流出の履歴に着目して衛星画像を解析した.その結果,流出発生の有無,つまり海氷の安定/不安定は数年間ずつ続いていること,それらの発現時期は海氷上積雪深や地上気温・風系の年々変化の傾向と符合していることが見出された.また,同湾南端に流れ込む白瀬氷河の浮氷舌の動態を加えて,過去50年間の沿岸定着氷の変動を推定したところ,1980年代初期以降の約25年間は不安定で,それ以前に長期間続いた安定な氷状と顕著に異なることがわかった.南極リュツォ・ホルム湾の沿岸定着氷の変動を解析した結果,以下のことがわかった.","PeriodicalId":331826,"journal":{"name":"Journal of the Japanese Society of Snow and Ice","volume":"30 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2006-07-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115475668","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}