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The assumption that the coefficient  x is inde-\npendent of surface states is discussed, and it is illustrated by an example that \nthis assumption leads to a result contradictory with the observed fact. P.A. \nSheppard and others\u0027 determinations of  x from pilot balloon observations are reviewed, and it is noticed that the order of the obtained value of  K \u0027---10X  10-4 \nis reliable; and by the way the value is about one-forth of that over land. Rossby\u0027s treatment for the determination of  x from the velocity profile in the skin layer is discussed in the latter part of this paper. Noticing Rossby\u0027s results that in the upper portion of the skin layer the wind profile obeys Prandtl\u0027s formula while in the lower portion it obeys von  Karman\u0027s formula for the smooth surface, the writer of this paper supposes that the condition of the upper portion of the skin layer, shown by the available data observed at near coast, may be much modified by the neighbouring land condition without representing the true condition over the open sea, while the condition of the lower portion indicates the true condition over the open sea. 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  1. 掲載誌一覧
  2. 鹿児島大学水産学部紀要
  3. vol.4
  1. 水産学部
  2. 水産学部・紀要論文

Critical Note on the Surface Resistance Coefficient in the Atmospheric Flow over the Ocean

http://hdl.handle.net/10232/10700
http://hdl.handle.net/10232/10700
c0fddfe7-f17d-4713-a997-8d5645c81398
名前 / ファイル ライセンス アクション
無題11.pdf 無題11.pdf (571.0 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2011-03-17
タイトル
タイトル Critical Note on the Surface Resistance Coefficient in the Atmospheric Flow over the Ocean
著者 TAKAHASHI, Tadao

× TAKAHASHI, Tadao

WEKO 104427

TAKAHASHI, Tadao

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言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ departmental bulletin paper
要約(Abstract)
内容記述タイプ Other
内容記述 A determination of the coefficient of the skin friction ( x ) over the sea is
attempted in this critical note. The assumption that the coefficient x is inde-
pendent of surface states is discussed, and it is illustrated by an example that
this assumption leads to a result contradictory with the observed fact. P.A.
Sheppard and others' determinations of x from pilot balloon observations are reviewed, and it is noticed that the order of the obtained value of K '---10X 10-4
is reliable; and by the way the value is about one-forth of that over land. Rossby's treatment for the determination of x from the velocity profile in the skin layer is discussed in the latter part of this paper. Noticing Rossby's results that in the upper portion of the skin layer the wind profile obeys Prandtl's formula while in the lower portion it obeys von Karman's formula for the smooth surface, the writer of this paper supposes that the condition of the upper portion of the skin layer, shown by the available data observed at near coast, may be much modified by the neighbouring land condition without representing the true condition over the open sea, while the condition of the lower portion indicates the true condition over the open sea. In this view point, rejecting the too high values of Ic ( 20 - 33 x 10' ) obtained from the upper profiles of the skin layer, and assuming that von Karmanrs formula is available up to the top of the skin layer, the writer fixes the value rc.8x 10-4, which is comparable with the value obtained from the pilot balloon observations over the open sea.
収録雑誌名 鹿児島大学水産学部紀要=Memoirs of Faculty of Fisheries Kagoshima University

巻 4, p. 65-70
作成日
日付 1956-01-30
ISSN
収録物識別子タイプ ISSN
ISSN 0453087X
NII書誌ID(雑誌)
収録物識別子タイプ NCID
NC ID AN00040498
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
NDC
主題Scheme NDC
主題 660
NIIsubject
主題Scheme Other
主題 自然科学
公開者・出版者
出版者 鹿児島大学
公開者よみ
公開者よみ カゴシマ ダイガク
公開者別名
公開者別名 Kagoshima University
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