The Wind System and the Dynamic Heating in the Upper Stratosphere
抄録
In the upper stratosphere the wind components and especially the dynamic heating which occur when the upper part of the ozonoshere is heated, are studied theoretically. In the present paper a node appears between 62 km and 77km, therefore the dynamic heating obtained from the present study is out of the phase with that in the previous paper, while in resect of wind components the result obtained from this study is almost same as that obtained from the previous one by the present authors.
上部成層圏における風系と力学的加熱について
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NAOSITEについて