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991.
In this paper, image processing technique that reduces video images of buoy motion to yield time series of image coordinates
of buoy objects will be investigated. The buoy motion images are noisy due to time-varying brightness as well as non-uniform
background illumination. The occurrence of boats, wakes, and wind-induced white caps interferes significantly in recognition
of buoy objects. Thus, semiautomated procedures consisting of object recognition and image measurement aspects will be conducted.
These offer more satisfactory results than a manual process. Spectral analysis shows that the image coordinates of buoy objects
represent wave motion well, indicating its usefulness in the analysis of wave characteristics. 相似文献
992.
Daigo Yanagimoto Masaki Kawabe 《Deep Sea Research Part I: Oceanographic Research Papers》2007,54(12):2067-2081
Direct current measurements with five moorings at 27–35°N, 165°E from 1991 to 1993 and with one mooring at 27°N, 167°E from 1989 to 1991 revealed temporal variations of deep flow at mid-latitude in the western North Pacific. The deep-circulation flow carrying the Lower Circumpolar Deep Water from the Southern Ocean passed 33°N, 165°E northwestward with a high mean velocity of 7.8 cm s−1 near the bottom and was stable enough to continue for 4–6 months between interruptions of 1- or 2-months duration. The deep-circulation flow expanded or shifted intermittently to the mooring at 31°N, 165°E but did not reach 35°N, 165°E although it shifted northward. The deep-circulation flow was not detected at the other four moorings, whereas meso-scale eddy variations were prominent at all the moorings, particularly at 35°N and 29°N, 165°E. The characteristics of current velocity and dissolved oxygen distributions led us to conclude that the deep-circulation flow takes a cyclonic pathway after passing through Wake Island Passage, passing 24°N, 169.5–173°E and 30°N, 168–169°E northward, proceeds northwestward around 33°N, 165°E, and goes westward through the south of the Shatsky Rise. We did not find that the deep-circulation flow proceeded westward along the northern side of the Mid-Pacific Seamounts and eastward between the Hess Rise and the Hawaiian Ridge toward the Northeast Pacific Basin. 相似文献
993.
Hidetaka Takeoka 《Journal of Oceanography》2002,58(1):93-107
The Seto Inland Sea is a representative coastal sea in Japan with a complicated geometry and thus a variety of marine environments.
This sea is, at the same time, one of the most industrialized areas in Japan, and its marine environment has been significantly
affected by the anthropogenic impacts over the last four decades. The wide range of marine environments in this sea and the
serious environmental issues resulting from these impacts have attracted the attention of Japanese coastal oceanographers.
It is believed that the nature and scope of these studies might be an example of the progress of Japanese coastal oceanography.
The historical changes in the Seto Inland Sea environment in the last four decades are briefly summarized, and the progress
in the studies of the Seto Inland Sea is reviewed with reference to historical changes. Some recent research topics and activities
are also mentioned.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
994.
995.
台站用百叶箱内外气温比对与分析 总被引:2,自引:0,他引:2
用双通道自动测温表对台站用的百叶箱内外气温进行了同步比对测量与分析。指出自然通风时,百叶箱对箱内气温变化产生一定程度的滞后和热辐射作用。滞后作用较明显。 相似文献
996.
杨振华 《中国海洋大学学报(自然科学版)》1997,(4)
采用声学方法精密测定汞被高压强压入储油岩样的渗入体积,对岩芯孔隙结构测定中的汞体积计量方法作了重要改进。本方法以无水酒精作为计量工作介质,在其中发射声波,通过对汞界面反射声波的识别,进行非接触的声学测量,从根本上解决了当前国内外采用的电阻法,电容法无法避免的由于汞腐蚀或油污染而要求经常进行与有毒汞接触的清洗,并且确保了计量系统工作性能的长期稳定与准确可靠。在0.01MPa至50MPa压强范围内连续计量,量程0~10ml,准确度0.01ml。 相似文献
997.
大鹏湾几种赤潮甲藻的分类学研究 总被引:24,自引:3,他引:24
对采自深圳大鹏湾的5种赤潮甲藻进行了分类学研究。其中海洋原甲藻属pro-rocentrum2种:P.micans Ehrenberg,P.minimum(Pavillard)Schiller;亚历山大属Alexandrium2种:Atamarense(Lebour)Balech,A.catenella(Whedon&Kofoid)Ba-lech;施克里普藻属Scrippsiella1种:S.tro 相似文献
998.
999.
The coastal sea level propagating westward along the south coast of Japan and the impact of the disturbance on the generation
of the Kuroshio small meander have been examined. The propagation occurs in sea level variations for periods shorter than
10 days and is remarkable for periods of 4–6 days. Characteristics of the 4–6 day component have been studied using the extended
empirical orthogonal function (EEOF). The first and second modes of EEOF are almost in-phase throughout the south coast of
Japan. The higher four modes of EEOF are significantly excited when the Kuroshio takes the non-large-meander path, and propagate
westward with phase speeds of 2.8 m s−1 (third and fourth modes) and 1.6 m s−1 (fifth and sixth modes) in the Kuroshio region west of Mera in the Boso Peninsula. The analysis shows that more than 70%
of the small meanders generate in two months after a significant propagating disturbance reaches south of Kyushu when the
velocity of the Kuroshio is high. This effect of coastal disturbance is examined by numerical experiments with a 2.5-layer
model in which coastal disturbance is excited by vertical displacement of the upper interface. The result is that offshore
displacement of the Kuroshio occurs southeast of Kyushu only in the case of significant upward displacement of the interface
under the influence of a high Kuroshio velocity. The significant coastal disturbance, which is associated with upward displacement
of the density interface, and a high Kuroshio velocity can therefore be important factors in generating small meanders. 相似文献
1000.