摘要
本文应用1986年11月17日至12月17日和1988年10日16日至11月21日,0°00′～22°00′N,115°00′～141°00′E和0°00′～10°00′S:141°00′～165°00′E海域的实测资料,对天气过程和海—气热量交换某些特征进行分析,得出如下结论:1)两次调查期间主要是由海洋向大气输热,占总天数的80％以上;2)调查期间海面有效回辐射Q_e、潜热通量Q_V及显热通量Q_K的总值为正值,即大气从海洋得到热量,而海洋主要是以潜热Q_V的方式把热量输送给大气;2)在不同天气过程中,海—气界面的热交换量有所不同。
Based on the data obtained during two investigation cruises in the western Pacific Ocean in the area 0°00'-22°00'N, 115°00'- 141°00' E from Nov. 17 to Dec. 17, 1986 and in the area 0°00'- 10°00'S, 141°00' -165°00' E from Oct. 16 to Nov. 21, 1988, several aspects of the air-sea thermal exchange are looked at in this paper. The caculation results of the two cruises indicate that the thermal transfer was conducted mainly from the sea to the air, as was the case for .80% of the observation days. The sum of value of sea surface effective reflex radiation (Qe) , latent thermal flux (Qv) and sensible thermal flux (Qk) was positive, which meant the heat in the air came from the sea. The exchange amount through the air-sea interface varied in different weather.
出处
《海洋通报》
CAS
CSCD
北大核心
1990年第5期17-24,共8页
Marine Science Bulletin
