• 한국항해항만학회:학술대회논문집
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• 한국항해항만학회 2019년도 춘계학술대회
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• pp.125-126
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• 2019

컨테이너 부산김해공항은 부산 경남 지역의 중요 항공 거점이며, 세계 5대 항만인 부산항과 근접해 있으면서도 그 규모나 역할에 맞지 않게 약소한 실정이다. 현재, 김해공항의 지속적인 취항 노선의 증가 및 이용 항공사가 증가하고 있지만, 포화 상태인 시설 및 군사공항을 겸하고 있어 높은 한계성에 직면하고 있다. 본 연구에서는 부산김해공항의 현 시점 및 개발 계획을 기초로 선용품물류를 중심으로 하여 부산국제공항의 발전을 예상하여, 국제공항의 시설 확충에 따른 물류비용 및 시간의 저감을 고려한다. 또한, 선용품물류를 기준으로 주요 항공노선의 우선순위를 검토하여 부산의 항만물류산업에 기여를 검토하고자 한다.

• 한국환경과학회지
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• 제13권3호
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• pp.189-196
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• 2004

Characteristics of urban wanning phenomenon were studied using degree days for three big cities(Seoul, Busan, Daegu) adjacent to airport. Time variation of the cooling and heating degree days was analyzed using the daily mean air temperature data measured at the six meteorological observatory for long-term periods(25～43years). The results for the big cities are as followings: 1) It was found that the heating degree days trended to decrease from year to year. 2) The cooling degree days were nearly unchanged during the same analysis periods. 3) The number of days calling for air-heating also tended to decrease as time passes. 4) Those of air-cooling were nearly unchanged during the same time. It suggests that the change of air-heating condition owing to urbanization came in evidence in the winter season, but that of air-cooling condition was slight in the summer season. On the other hand, the long-term trends of degree days were very small in airport areas except for Kimhae airport. Hence, the gaps of degree days between big cities and rural airport areas are increasing.

• 한국환경과학회지
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• 제10권6호
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• pp.417-422
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• 2001

The vertical structure of atmosphere was observed In investigate the variation of surface ozone concentration by vertical downward mixing of residual ozone in the atmospheric boundary layer at the Busan coastal area. Airsonde and pilot balloon measurements were made at Gamcheondong and the Kimhae airport for April 26~27, 1996. The vertical potential of potential temperature showed a residual layer between 510m and 1800m from 2100LST April 26 to 0900LST April 27. The downward mixing of ozone in the residual layer of the atmospheric boundary layer was confirmed from vertical profile of mixing ratio near 600m in the morning. The thickness of the sea breeze layer was 900m at 1500LST April 26. Thereafter, it become to be lowered with time A low level jet was measured near 900m at 0300LST on April 27 from a pibal measurement. Early morning sharp increase of surface ozone concentration at the Busan coastal area was caused by vertical downward mixing of ozone concentration rather than by photochemical reaction In the atmospheric boundary layer.