\u672c\u5e74\u6700\u521d\u306e\u30bb\u30df\u30ca\u30fc\u306e\u6848\u5185\u3092\u304a\u9001\u308a\u3057\u307e\u3059\u3002
\n_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/
\n_\/
\n_\/ \u6d41\u4f53\u529b\u5b66\u30bb\u30df\u30ca\u30fc \uff12\uff10\uff10\uff14 No. \uff11\uff11
\n_\/
\n_\/ \u65e5 \u6642 : \uff10\uff15\u5e74 \uff11\u6708 \uff11\uff17\u65e5 (\u6708) \uff11\uff15\uff1a\uff10\uff10\u301c\uff11\uff16\uff1a\uff13\uff10
\n_\/
\n_\/ \u5834 \u6240 : \u4eac\u5927\u6570\u7406\u7814 \uff10\uff10\uff19\u53f7\u5ba4
\n_\/
\n_\/ \u8b1b \u5e2b : Dongliang Zhao \uff08\u8d99 \u68df\u6881\uff09 \u6c0f
\n_\/ \uff08\u4eac\u5927\u5927\u5b66\u9662\u5de5\u5b66\u7814\u7a76\u79d1\/\u4e2d\u56fd\u6d77\u6d0b\u5927\u5b66\u7269\u7406\u6d77\u6d0b\u7814\u7a76\u6240\uff09
\n_\/
\n_\/ \u984c \u76ee : \u98a8\u6ce2\u3068Langmuir\u5faa\u74b0\u306b\u3088\u308b\u6d77\u6d0b\u6df7\u5408\u5c64\u306e\u5909\u52d5
\n_\/
\n_\/ \u5185 \u5bb9 :
\n_\/ The oceanic mixed layer refers to the upper layer of the ocean that is
\n_\/ in direct contact with the atmosphere and is usually observed to be mixed
\n_\/ thoroughly by turbulent mixing. Models of the oceanic mixed layer usually
\n_\/ ignore the presence of wind waves at the air-sea interface, and assumed
\n_\/ they obey the law of the wall, in which the turbulence is equilibrated
\n_\/ between shear production and dissipation. However, wind waves are at least
\n_\/ important for two reasons. First, wave breaking transfers wave energy into
\n_\/ turbulence and is thus an energy source for boundary layer turbulence.
\n_\/ Second, direct interactions between Stokes drift that is resulted from
\n_\/ wind waves and wind-driven current can produce Langmuir circulation,
\n_\/ which has the capability to transport suspended matter vertically downward
\n_\/ deep into the oceanic mixed layer and modifying the circulation and
\n_\/ turbulence characteristics in the upper ocean layer.
\n_\/ I will first introduce the wind wave models briefly, and suggest that
\n_\/ wind wave forecast has been well developed compared to the other ocean
\n_\/ environmental factor predictions. Then, based on a second order turbulent
\n_\/ closure scheme, Mellor-Yamada model, the influence of wind waves on
\n_\/ oceanic mixed layer is investigated from three aspects including air-sea
\n_\/ flux algorithms, turbulence induced by wave breaking, and Langmuir
\n_\/ circulation, all of them depend on the development degree
\n_\/ of wind waves. The detail will be reported at the presentation.
\n_\/
\n_\/ \u5099\u8003\uff1a\u8b1b\u5e2b\u306f\u6a5f\u68b0\u5de5\u5b66\u5c02\u653b\u6d41\u4f53\u5de5\u5b66 \u5c0f\u68ee\u7814\u7a76\u5ba4\u306b\u6ede\u5728\u4e2d\u3067\u3059\u3002
\n_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/
\n\u4e16\u8a71\u4eba\uff1a\u5927\u6728\u8c37 \u8015\u53f8(\u4eac\u5927\u6570\u7814)\u3001\u85e4 \u5b9a\u7fa9(\u4eac\u5927\u7406)\u3001\u677e\u672c \u525b(\u4eac\u5927\u7406)\u3001
\n\u5c71\u7530 \u9053\u592b(\u4eac\u5927\u6570\u7814)
\n\u30a2\u30c9\u30d0\u30a4\u30b6\u30fc\uff1a\u6cb3\u539f \u6e90\u592a(\u4eac\u5927\u5de5)\u3001\u5c0f\u68ee \u609f\uff08\u4eac\u5927\u5de5\uff09\u3001\u85e4\u5742\u535a\u4e00\uff08\u4eac\u5927\u60c5\u5831\u5b66\uff09\u3001
\n\u8239\u8d8a \u6e80\u660e\uff08\u4eac\u5927\u60c5\u5831\u5b66\uff09\u3001\u6c34\u5cf6 \u4e8c\u90ce(\u540c\u5fd7\u793e\u5927\u5de5)\u3001\u4f59\u7530 \u6210\u7537\uff08\u4eac\u5927\u7406\uff09
\n\u9023\u7d61\u5148\uff1aohkitani@kurims.kyoto-u.ac.jp
\n\u30e1\u30fc\u30eb\u30ea\u30b9\u30c8\u9023\u7d61\u5148\uff1a semi-adm@kyoryu.scphys.kyoto-u.ac.jp<\/p>\n","protected":false},"excerpt":{"rendered":"
\u672c\u5e74\u6700\u521d\u306e\u30bb\u30df\u30ca\u30fc\u306e\u6848\u5185\u3092\u304a\u9001\u308a\u3057\u307e\u3059\u3002 _\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/_\/ _\/ _\/ \u6d41\u4f53\u529b\u5b66 […]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[16,28],"tags":[],"class_list":["post-569","post","type-post","status-publish","format-standard","hentry","category-16","category-28"],"_links":{"self":[{"href":"http:\/\/kyoryu.scphys.kyoto-u.ac.jp\/index.php?rest_route=\/wp\/v2\/posts\/569","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/kyoryu.scphys.kyoto-u.ac.jp\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/kyoryu.scphys.kyoto-u.ac.jp\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/kyoryu.scphys.kyoto-u.ac.jp\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/kyoryu.scphys.kyoto-u.ac.jp\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=569"}],"version-history":[{"count":0,"href":"http:\/\/kyoryu.scphys.kyoto-u.ac.jp\/index.php?rest_route=\/wp\/v2\/posts\/569\/revisions"}],"wp:attachment":[{"href":"http:\/\/kyoryu.scphys.kyoto-u.ac.jp\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=569"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/kyoryu.scphys.kyoto-u.ac.jp\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=569"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/kyoryu.scphys.kyoto-u.ac.jp\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=569"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}