초록

AI-Helper

본 논문에서는 동해에 있어서의 오징어 채낚기어업의 조업위치선정에 필요한 해황정보인 표면수온, 중 하층수온에 주목하여 검토하였다. 표면수온으로 검토한 오징어 채낚기어업의 어장형성에 관해서는 각 어선이 조업시에 측정한 수온을 어해황속보와 대비해 보면 같은 표면수온에서도 약간 차이가 있었다. 그래서 조업위치선정에 있어서 중요한 해황정보인 조업시에 있어서의 표면수온을 사용하여 고찰한 결과 해에 따라서 해황상태가 달라도 조업척수가 가장 많은 표면수온은 대체로 $2^{\circ}C$ 범위내에 들어간다는 것을 알았다. 그러나 중 하층수온에 관해서는 선단의 각 어선이 측정하고 있지 않다는 것과 근해관측이 200해리 수역내에서만 행해졌다는 것으로부터 한정된 시기에 대해서만 검토한 결과 6월 및 7월 상순에 있어서 신나천현선단(神奈川縣船團)의 조업해역에 있어서의 50m층 수온으로 보면, 난수역과 냉수역 사이의 $10{\sim}12^{\circ}C$에서 어장이 형성되었고 그후 극전선부근의 $5{\sim}8^{\circ}C$의 해역으로 어장이 이동하는 것을 파악할 수 있었고, 연안역에서는 극전선 남쪽의 난수역의 50m층 수온이 $10{\sim}12^{\circ}C$의 해역에서 어장이 형성된다는 것을 알았다.

Abstract ▼ AI-Helper

In this paper, we analyzed the relationships between the fishing ground formation and the sea condition information, surface, mid and bottom layer temperature that is necessary for fishing point selection of angling to catch squid in the East Sea. There was a little differences between temperature m...

In this paper, we analyzed the relationships between the fishing ground formation and the sea condition information, surface, mid and bottom layer temperature that is necessary for fishing point selection of angling to catch squid in the East Sea. There was a little differences between temperature measured by every fishing boat on fishing operating and prompt reports of fishing and sea condition about fishing ground formation of angling. And then the result examined by using SST that is a important information of sea condition for the fishing position selection follows as ; We knew, even if the differencs of sea condition each year, SST with a lot of fishing boats was generally within the extnet of $2^{\circ}C$. But the result examined by the limit time about the temperature of mid and bottom layer for the groups of fishing boats not to measure and for the near sea measurement to be done only within EEZ waters follows as ; About the temperature of 50m layer on early in June and July in operating waters of the group of fishing boats, the fishing ground was formed from $10^{\circ}C$ to $12^{\circ}C$ between warm waters and cold waters, afterwards we can seize that the fishing ground was moving to waters from $5^{\circ}C$ to $8^{\circ}C$ at near of polar front. In the coastal waters, we knew that fishing ground is formed to waters from $10^{\circ}C$ to $12^{\circ}C$ at the southern of polar front about the temperature of 50m layer.