ACTA OCEANOLOGICA SINICA——Subject index to Vol. 10, 1991

Marine Hydrologyl···························……Estjmatjon of water volume transPQrts through the main straits of the East China Sea z加0 Ba,e:(赵保仁)andFa即Gooho叩(方国洪)15··········……、··········……The effect of internal tides on the vertical structure of tjdal eurrent in the North Huangha1S比 z俪了。:s加二,(赵俊生),‘e叩sh”、,,(耿世江),s。二万朋,l二二夕(孙洪亮)andz加即z,l:(张自历)37··················……,··……Sur…     

Study on dynamics of shear waves——Ⅰ. Scale analysis and dispersion relation

- Starting from satellite remote sensing data, the dynamical processes of shear waves occurring at the boundary between the western boundary current and the shelf slope water are studied and dynamically analyzed in this study. The average wavelength is 75 km, and the average amplitude (from crest to trough )17 km. the average phase speed 100 cms-1 for the shear waves along the north wall of the Gulf Stream to the east of Cape Hatteras measured from NOAA satellite IR (infrared ) images. The average wavelength of shear waves along the north wall of the Kuroshio Current is 57 km, and the average amplitude 17 km. For the shear waves occurring along the west wall of the Gulf Stream to the south of Cape Hatteras, the average wavelength is 131 km, and the average amplitude 33 km measured from Seasat SAR (synthetic aperture radar )images. The time for one cycle of shear wave event is about one week.In order to explore the dynamical mechanisms of shear waves, we solved the vorticity equation for a stratified flu     

Ultrastructure study of the diatom——Ⅱ. Synedra, Cyclophora, Plagiogramma, Opephora, Fragilaria and Pseudostaurosira

Ｕｌｔｒａｓｔｒｕｃｔｕｒｅｓｔｕｄｙｏｆｔｈｅｄｉａｔｏｍ──Ⅱ．Ｓｙｎｅｄｒａ，Ｃｙｃｌｏｐｈｏｒａ，Ｐｌａｇｉｏｇｒａｍｍａ，Ｏｐｅｐｈｏｒａ，ＦｒａｇｉｌａｒｉａａｎｄＰｓｅｕｄｏｓｔａｕｒｏｓｉｒａ￥ＬｉｕＳｈｉｃｈｅｎｇ（Ｒｅｃｅｉｖｅｄ...