摘要
用Niiler—Kraus类型的混合层积分模式,对TOGA—COARE强化观测期间由《实验3号》科学考察船观测资料得到的混合层深度和SST在季节内时间尺度的变化进行了模式研究。指出:1.混合层耗散参数与较长时间尺度过程风应力的变化存在着比较好的对应关系;2.模式可以较好的对风场和热通量场在季节内时间尺度的变化作出响应,模拟出季节内时间尺度SST的变化;3.Niiler,-Kraus模式在考虑耗散作用后,可用于海洋季节内时间尺度变化的模式研究。
In this paper,based on the data of SST and mixed layer depth measured by the Shiyan 3 during the TOGA-COARE IOP , we study the intraseasonal time scale variations of SST and mixed layer depth through a Niiler - Kraus type integrated mixed layer model. Our studies show that 1. there is a better correlation between the dissipation parameter and the wind speed; 2. the model is good in responding the variations of wind and heat fluxes and can simulate, to some extent, the intraseasonal time scale oscillations of SST ; 3. after adding the dissipation term, the Nuler- Kraus type model can be used to study the modelling of intraseasonal time scale variations in the upper ocean.
出处
《中国海洋大学学报(自然科学版)》
CAS
CSCD
1993年第S2期115-126,共12页
Periodical of Ocean University of China
基金
TOGA-COARE专项基金
国家教委博士点基金
关键词
混合层积分模式
混合层深度变化
耗散系数
季节内时间尺度
SST
Integrated mixed layer model
variations of mixed layer depth
dissipation parameter
intraseasonal time scale
SST