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Validation of model-simulated sea surface current and sea surface temperature with observations in the southern Indian Ocean

机译:利用印度洋南部的观测值对模型模拟的海流和海面温度进行验证

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A 25-layer Ocean General Circulation Model has been used to investigate and analyse the model-simulated sea surface current (SSC) and sea surface temperature (SST) fields from a 26-year model simulation covering the Southern Indian Ocean region (50 degree S-10 degree N and 30-120 degree E). In general, simulated time-mean SSC and SST fields are found to agree well with the corresponding observed datasets in most parts of the model domain. All major currents such as Antarctic Circumpolar Current, Equatorial Counter Current, South Equatorial Current, North Equatorial Current and Agulhas Current are preserved in the model, as verified by the observation. However, slight variation in current intensity is reflected on monthly scale. Similarly, the pattern of time-mean monthly SST field is found to agree with Levitus climatology. However, disparities do exist as evidenced by the SST bias calculation in some parts of the model domain. The vertical profile of temperature from the model simulation is found to agree well with the Levitus climatology. It is concluded that the model is able to reproduce well, the observed structure in the ocean.
机译:一个25层的海洋总环流模型已被用来调查和分析来自印度南部海域(50度南半球)的26年模型模拟中的模型模拟海面流(SSC)和海面温度(SST)场-10度N和30-120度E)。通常,发现模拟时间均值SSC和SST字段与模型域大多数部分中的相应观测数据集非常吻合。经观测证实,所有主要水流,例如南极绕极流,赤道逆流,南赤道流,北赤道流和阿古拉斯流都保留在模型中。但是,电流强度的细微变化反映在月度尺度上。同样,发现平均每月SST场的模式与Levitus气候学一致。但是,在模型域的某些部分中确实存在差异,这可以通过SST偏差计算来证明。通过模型模拟得出的温度垂直剖面与Levitus气候学非常吻合。结论是该模型能够很好地复制海洋中观察到的结构。

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