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比约克尼斯正反馈
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比约克尼斯正反馈
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比约克尼斯正反馈
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Bjerknes positive feedback
比约克尼斯正反馈
一种用来解释热带太平洋海表温度纬向差异与海面气压之间链式耦合并相互促进的正反馈,最早由著名的气象学家J.比约克尼斯(Jacob Bjerknes,1897~1975)在20世纪60年代提出,用来解释ENSO现象中海表面温度与低层大气环流之间耦合性的演变。
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