In the first phase, the model was integrated starting from an rest state over ten years under the annual mean wind stress. At the end of the first phase, a quasi-equilibrium state in the upper levels was reached.
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- 模式數值積分分兩個(gè)階段,在第一個(gè)階段,海洋環(huán)流從靜止狀態(tài)開(kāi)始,以只隨緯度變化的年平均風(fēng)應力和海表熱通量作為強迫邊條件數值積分十年,這時(shí)海洋上層的環(huán)流和溫度都趨于平穩,我們將第十年末的積分狀態(tài)作為模式氣候的準平衡態(tài)。
