OKAYAMA University Earth Science Reports, Vol.17, No.1, 7-19, (2010) Comparison of large-scale cloud distribution and atmospheric fields around the Ak
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1 OKAYAMA University Earth Science Reports, Vol.17, No.1, 7-19, (2010) Comparison of large-scale cloud distribution and atmospheric fields around the Akisame (autumn rainfall) front in East Asia among 1993, 1994 and 1995 (Shigeko FUKUDA)* (Kuranoshin KATO)** In order to examine year-to-year variability of the Akisame (autumn rainfall) frontal zone in East Asia, large-scale cloud distribution and atmospheric fields around the frontal zone were compared among 1993, 1994 and 1995, when their characteristics were rather different among each other. While the Akisame frontal zone extended zonally and the deep convective clouds tended to appear in that frontal zone near the southern coast of the Japan Islands in 1993, the frontal zone extends from southwest to northeast and the large amount of precipitation was brought mainly in the northern Japan. In 1995, although the surface front on the weather maps appeared frequently also around the southern coast of the Japan Islands, the rainfall amount there was not so large. The area with frequent appearance of the deep convective clouds in the Akisame frontal zone was seen only to the east of the Japan Islands. As such, it is noted that the active area of the Akisame frontal zone shows rather large year-to-year variability also in the zonal direction. It is also suggested that such great variability of the Akisame frontal zone in the zonal direction seems to correspond to the variations of the subtropical high and the ITCZ in the western Pacific region around September.. Keywords: Akisame (autumn rainfall) front, STFZ in early autumn, year-to-year difference of Akisame front STFZ: subtropical frontal zone Ninomiya, 1984; Matsumoto, 1988; 2003 Murakami and Matsumoto 1994; 2004; preliminary study preliminary study Kodama 1992, 1993 SPCZ: South Pacific Convergence Zone South Atlantic Convergence Zone SPCZ SACZ SPCZ SACZ * Faculty of Education, Okayama University Ishiai Primary School ** **Graduate School of Education, Okayama University, Okayama, , Japan
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8 14 福田維子 加藤内藏進 り東側に位置していることが分かる 以上のように 秋雨前線帯に関連した広域の 雲 降水分布は 単に南北の位置だけでなく 雲 帯の走向や主たる活動域の東西の違い 更には Hc-Area で示唆されるような雲頂の高い雲域 恐 らく 積乱雲群に対応 の出現状況の違いのよう な 大きな年々の差異が見られうることが明らか になった 4.2 前線帯付近の大気場の比較 次に GANAL に基づく大気場の解析を行った 期間 A で平均した各年における海面気圧の分布の を 第 3 図に示す また 各年の期間 A で平均し た 850hPa における相当温位θe と 期間平均気温 の水平傾度の絶対値 T850 の分布を第 4 図に示 す また 26,25N 南西諸島付近の緯度 におけ る 850 hpa 面での 5 日移動平均の南北風成分 V850 の時間 経度断面を第 5 図に示す 第３図 期間 A 9 月 3 日 22 日 で平均した海面気圧の分布 hpa 左から順に 1993 年 1994 年 1995 年 第４図 期間 A 9 月 3 日 22 日 で平均した 850 hpa における相当温位θe K 実線 及び 期間平均気温の水 平傾度の絶対値 T850 /1000 km の分布 T850 については 4 /1000 km 以上の値の等値線のみ示した 左 から順に 1993 年 1994 年 1995 年 1993 年の期間 A 秋雨期 には 地上の太平洋 高気圧に対応するリッジが 冷夏であった 8 月か らあまり位置を変えず 28N に東西に伸びて停 滞していた 第 3 図(左) 8 月については 気候 系監視報告 気象庁 を参照 但し 次章の第 6 図からも 太平洋高気圧に覆われて上層雲量の 小さな領域が分かる 以下 1994 年 1995 年８月 についても同様 秋雨前線帯は 梅雨前線帯と同様に 高温多湿 な海洋性熱帯気団の北縁に位置する準定常的前線
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608 東シナ海上の梅雨前線南側における降水系の形成機構 水蒸気前線の発見 帯の併合が起こりました その際に BAND1では 反 射強度で 6dBZe 以上増加するような急激な降水強化 が起こりました その併合過程が起こる直前の12時40 において デュアルドップラーレーダー解析 ２台以上のドップ ラーレーダーによるドップラー速度データから３次元 気流場を計算する解析手法 から得られた２本の降水 帯の気流構造を示したのが第４図です
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1 2 1 847 1201 1417 1 E-mail: onitsuka@nkg-net.co.jp 2 E-mail: hara@nkg-net.co.jp B. C. 150 3 3 Key Words: Yoshinogari burial mound, Chinese burial mounds, construction technique, Hanchiku, Sochiku, Taichiku
Present Situation and Problems on Aseismic Design of Pile Foundation By H. Hokugo, F. Ohsugi, A. Omika, S. Nomura, Y. Fukuda Concrete Journal, Vol. 29
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30 2015 51-62 2015/01/17 2015/03/31 1914 * Literature Survey on Damage of Akita Mining College due to the 1914 Akita-Senboku Earthquake Toshihiko MIZUTA Center for Regional Development, Akita University
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The purpose of this study is to clarify a process that Awa dance developed into tourist resources and the factors that it spread out in all over Japan. Consideration was made with the memory magazines,
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女子短大生に対する栄養マネジメント教育とその評価
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Graduate School of Environment and Information Sciences, Yokohama National University, Yokohama 240 8501 Faculty of Education and Human Sciences, Yokohama National University, Yokohama 240 8501 Keywords:
remained dispersedly in the surrounding CBD areas. However, few hotels were located in the core of Sendai's CBD near the station because this area had
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