Many publications of pointology have been conflicted to define fixed positions of acu-points. These underlying cause results from the historical fact that most of acu-points and meridian systems began at anonymous experiences of many generations. However, if we would believe that the acupoints and meridian systems exit clearly in all of the organism, there were exit the fixed position of acupoints. In this study, we performed bibliographically the investigation fixing the position of CV16. From the investigation, although supported that it exit 1.6 chon (寸) below CV17 in human being, we suggest that CV16 exit below the sternum met with the 7th rib, or the joined point between the sternum and the xiphoid process.

Horizontal scale and movement of tidal front zone, front in the western regions of Korea in summer are studied in conjunction with numerical model and NOAH-11 satellite data analysis(AVHRR multi -channel sea surface temperature). In numerical model result, tidal mixing is dominant in the southeast region of Hwanghae, near field of Taean, Kyunggi bay, near field of Jangsan cape, Seoan bay, mid-east Chinese coast. But the results of the NOAH infra-red image analysis show that low surface temperature by tidal mixing is clear in the southeast region of Hwanghae, near field of Taean, near field of Jangsan cape but not in the Kyunggi bay, Seoan bay and mid- east Chinese coast in August and September, temperature gradient of frontal zone in the southwest region of Hwanghae is 0.05°∼0.1℃/㎞ and tidal mixing is dominant in the near field of Maenggal kundo and Hajodo and low surface temperature extends southwesrward. Early in August, west-east front(0.2°∼0.6℃/㎞) on the south region of Jindo moves northward and persists at east half on the joining line of Jindo and Sohuksando late September. The axis of front on the west region of Jindo is northeast~sorthwest early in August and moves westward until late September The tidal mixing in the near field of Jangsan cape is dominant in the region between Jangsan cape and Baengyougdo early in August and between Baengyougdo and Daechungkundo in late September. The axis of front on the west region of Jangsan cape is south-north and its temperature gradient is 0.2°∼0.4℃/㎞.

This research was conducted by the request of the Ministry of Education as a part of $quot;The investigation of the priority (of Oceangraphy field) of the long term education loan project$quot;, which is promoted in order to find the ways) to reinforce the Oceanography education. The first Oceanography department in Korea was established in 1968 at Seoul National University. During the last 20 years, 10 Oceanography departments, 5 ocean engineering departments and 1 ocean development department were established at 8 universities and 4 colleges. However, the education facilities and the quality of education were not sufficiently improved. Furthermore, an Oceanography research vessel was not built for those ocean related departments up to now. The authority of the Ministry of Education, which foresaw the fast-changing marine policy of each nation and the rapid technological advances of ocean development, prepared a plan to search a way to reinforce the college level Oceanography education so as to secure the future survival of this nation. Therefore, through this investigation a reinforce plan of Oceanography education in Korea was formalized.

The structure and change of the salinity front formed by the outflow of Keum River into the adjacent sea is investigated through the analysis of some possible data. The outflow of the river has no peculiar direction and controlled by the various factors. The analysis of data which are obtained at March and October show that at March, the salinity front is weakened as compared with October. The outflow pattern is not uniform but varies significantly with time period less than one week.