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NTIS 바로가기바다 : 한국해양학회지 = The sea : the journal of the Korean society of oceanography, v.22 no.4, 2017년, pp.151 - 171
박경애 (서울대학교 지구과학교육과) , 박지은 (서울대학교 과학교육과) , 최병주 (전남대학교 해양학과) , 이상호 (군산대학교 해양학과) , 신홍렬 (공주대학교 대기과학과) , 이상룡 (부산대학교 해양학과) , 변도성 (국립해양조사원 해양과학조사연구실) , 강분순 (국립해양조사원 해양과학조사연구실) , 이은일 (국립해양조사원 해양과학조사연구실)
Most of oceanic current maps in the secondary school science and earth science textbooks have been made on the base of extensive in-situ measurements conducted by Japanese oceanographers during 1930s. According to up-to-date scientific knowledge on the currents in the Yellow Sea and the East China S...
핵심어 | 질문 | 논문에서 추출한 답변 |
---|---|---|
황해 및 동중국해의 위치와 역할은? | 황해 및 동중국해는 유라시아 대륙의 동쪽에 위치하여 대륙의 변화에 빠르게 반응하는 해역 중 하나로 대기-해양의 상호작용을 통하여 한반도의 기상과 기후변화에 큰 영향을 주고 있다. 이 해역은 동해에 비해 수심이 얕고, 겨울철 강한 바람과 조류, 양쯔강 희석수(Yangtze River (or Chiangjiang) Diluted Water)와 같은 저염수, 고온 고염의 쿠로시오해류 유입 등의 영향으로 해수 순환이 상당히 복잡하다(Park et al. | |
황해 및 동중국해를 둘러싼 해류도 제작에의 실정은? | 해류도는 실측 자료를 기반으로 제작하는 것이 바람직하지만 현재까지 황해 및 동중국해를 둘러싼 대한민국, 중국, 일본 등 여러 나라의 관측에도 해류도를 제작하는 데는 자료가 많이 부족한 실정이며 충분한 해류관측 자료가 축적되려면 상당한 시일이 요구된다. 따라서 이 연구에서는 해류도 제작의 시급성을 고려하여 지금까지의 해양 관측자료, 연구논문, 해양학자들의 전문지식과 의견을 수렴하고 여러 번의 수정 과정을 거쳐 해류도를 제작하는 방법을 고안하였다. | |
황해 및 동중국해의 해수 순환이 복잡한 이유는? | 황해 및 동중국해는 유라시아 대륙의 동쪽에 위치하여 대륙의 변화에 빠르게 반응하는 해역 중 하나로 대기-해양의 상호작용을 통하여 한반도의 기상과 기후변화에 큰 영향을 주고 있다. 이 해역은 동해에 비해 수심이 얕고, 겨울철 강한 바람과 조류, 양쯔강 희석수(Yangtze River (or Chiangjiang) Diluted Water)와 같은 저염수, 고온 고염의 쿠로시오해류 유입 등의 영향으로 해수 순환이 상당히 복잡하다(Park et al., 2014). |
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