Time lag analysis between air and water temperatures using buoy monitoring data
DC Field | Value | Language |
---|---|---|
dc.contributor.author | 조홍연 | - |
dc.date.accessioned | 2020-07-16T18:46:11Z | - |
dc.date.available | 2020-07-16T18:46:11Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2011-03-28 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/28441 | - |
dc.description.abstract | The time lag between air and surface water temperatures is much bigger in the falling period than the rising period of air temperature. It is reversely changedbetween surface and bottom water temperatures. In particular, the time lag of maximum temperature is more than 30 days between surface and bottom water temperatures. | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | IOC/WESTPAC | - |
dc.relation.isPartOf | IOC/WESTPAC 8th Int | - |
dc.title | Time lag analysis between air and water temperatures using buoy monitoring data | - |
dc.type | Conference | - |
dc.citation.conferencePlace | KO | - |
dc.citation.endPage | 36 | - |
dc.citation.startPage | 36 | - |
dc.citation.title | IOC/WESTPAC 8th Int | - |
dc.contributor.alternativeName | 조홍연 | - |
dc.identifier.bibliographicCitation | IOC/WESTPAC 8th Int, pp.36 | - |
dc.description.journalClass | 1 | - |