• Journal of the Korean Society of Marine Environment & Safety
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• v.16 no.1
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• pp.71-80
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• 2010

This paper compares the maritime education of two traditional maritime countries, Korea and the Philippines, specifically, in their maritime transportation education. The subjects of this review focus on Mokpo National Maritime University(MMU) and the Philippine Merchant Marine Academy(PMMA). The paper presents the curricular and training programs of both institutions and shows the differences in the curriculum designs and methodology of delivery as contained in the requirements of Standards of Training, Certification and Watch keeping 1978, as amended in 1995(STCW 95). It also illustrates the social climate of the two countries and the attitude of maritime community in relation with the maritime programs offered by the institutions towards the quality of the competent maritime graduates.

• Proceedings of the Korean Institute of Navigation and Port Research Conference
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• 2016.05a
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• pp.10-12
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• 2016

이 연구는 케냐 해양대학 항해학과 교과과정의 개발을 위해 다음과 같은 다양한 연구들이 수행되었다. 먼저 2장에서 케냐의 교육 및 환경 여건을 살펴보기 위해 케냐의 전반적인 상황과 JKUAT 및 동 대학 기관공학과의 교과과정을 살펴보았다. 이어 3장에서는 항해학과 교과과정의 표준으로 삼아야 할 IMO STCW 협약 해기교육요건과 IMO 모델 코스를 살펴보았다. 이어 4장에서는 항해학과 교과과정의 개발에 참고하기 위해 모범적인 해기교육을 실시하고 있는 미국의 USMMA와 CMA, 필리핀의 PMMA와 MAAP, 한국의 한국해양대학교, 중국의 대련해사대학교, 그리고 베트남의 VIMARU와 HCMUT의 교과과정을 각각 살펴보았다. 마지막으로 5장에서는 이상의 검토 결과를 토대로 케냐 해양대학의 항해학과 교과과정을 제시하였다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.13 no.3
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• pp.190-199
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• 2008

To investigate hydrographic structure and characteristics of the tropical ocean in the eastern and the western Pacific, CTD(Conductivity-Temperature-Depth) data along $131^{\circ}W$ and $137^{\circ}-142^{\circ}E$ in July-August 2005 were analyzed. Sea surface temperature along $131.5^{\circ}W$ in summer is highest in the Equatorial Counter Current(ECC) because of the high-temperature water greater than $28^{\circ}C$ moving through the ECC from the western Pacific to the eastern Pacific in spring and summer. Based on the evidence of the presence of low salinity and high dissolved oxygen water in the North Equatorial Current(NEC), we suggested that the low salinity water moved from the Gulf of Panama to the east of Philippine along the North Equatorial Current(NEC). The South Equatorial Current(SEC) had the most saline water from surface to deep layer because the saline water from the Subtropical South Pacific Ocean moved to the north. The salinity minimum layer was observed at 500-1500 m depth along $131.5^{\circ}W$. The water mass with the salinity minimum layer in the north of $5^{\circ}N$ came from the North Pacific Intermediate Water(NPIW) and that in the south of $5^{\circ}N$ came from the Antarctic Intermediate Water(AAIW), which was more saline than the NPIW. Cyclonic cold eddy with a diameter of about 200km was found in $4-6^{\circ}N$. Sea surface temperature along $131.5^{\circ}W$ in the eastern Pacific was lower than along $137^{\circ}-142^{\circ}E$ in the western Pacific; on the other hand, sea surface salinity in the eastern Pacific was higher than in the western Pacific. Subsurface saline water from the Subtropical South Pacific Ocean was less saline in the eastern Pacific than in the western Pacific. Salinity and density(${\sigma}_{\theta}$) of the salinity minimum layer south of $14^{\circ}N$ was higher in the eastern Pacific than in the western Pacific.