@article{oai:nagaokaut.repo.nii.ac.jp:00000513,
 author = {中村, 由行 and 一宮, 大祐 and 早川, 典生 and 西村, 肇},
 journal = {長岡技術科学大学研究報告},
 month = {Oct},
 note = {Field data on coastal anoxia observed during nine years in Osaka Bay were analyzed and examined using a numerical method. Field data suggest that the development of thermal stratification in the middle layer and the subsequent retardation of oxygen transport to the bottom layer is the principle mechanism in the formation of anoxia in the bottom water. The numerical model, which was developed by Nakamura and Nishimura to predict the changes of temperature and oxygen distribution, has been improved by taking account of heat exchange through the air-water interface. The improved model well reproduces the characteristic temperature variation and the dissolved oxygen content in the bottom field condition during the stratification period as well as the mixing period in autumn. Important parameters for the determination of surface heat exchange have further been evaluated by sensitivity analyses. The results show that the vapor pressure in the atmosphere and the wind velocity are the most sensitive to the total heat flux.},
 pages = {69--81},
 title = {内湾の熱収支と貧酸素水塊の形成について},
 volume = {11},
 year = {1989}
}