一类改进的海洋罗斯贝波的线性斜压模型
class of improved linear oblique models for oceanic Rossby waves
罗斯贝波是地球自转过程中由科里奥利力引起的大尺度行星波,在海洋和大气环流中均存在。海洋罗斯贝波不仅对气候具有重要影响,而且对海洋中能量的传输、能量的再分配以及大洋环流等具有重要影响,因此加深对海洋罗斯贝波的全面认识具有重要意义。为了实现对于海洋罗斯贝波的进一步模型拟合,将1.5层海洋中经典风驱动罗斯贝波模型拓展到2.5层海洋中,得到新的模型框架下海洋罗斯贝波的主要驱动因素。研究结果表明,在新的模型框架下,海洋罗斯贝波主要受到局地埃克曼抽吸、密度变化以及东部边界强迫等因素的影响,实现了对海洋罗斯贝波的进一步探测和了解。
Rossby waves are large-scale planetary waves caused by Coriolis forces during the Earth\'s rotation, and they exist in both oceanic and atmospheric circulation. The oceanic Rossby waves not only have important effects on climate, but also on energy transport, energy redistribution and oceanic circulation in the ocean, so it is important to improve the overall understanding of oceanic Rossby waves. In order to achieve further model fitting of oceanic Rossby waves, the classical wind-driven Rossby wave model in the 1.5-layer ocean is extended to the 2.5-layer ocean to obtain the main drivers of oceanic Rossby waves under the new model framework. The results show that under the new model framework, the oceanic Rossby waves are mainly influenced by local Ekman pumping, density variation and eastern boundary forcing, achieving further detection and understanding of oceanic Rossby waves.
王非之、高猛、张爱弟
海洋学
应用数学罗斯贝波海平面高度2.5层海洋
pplied mathematicsRossby wavesSea surface height2.5-Layer ocean
王非之,高猛,张爱弟.一类改进的海洋罗斯贝波的线性斜压模型[EB/OL].(2023-06-21)[2025-08-11].http://www.paper.edu.cn/releasepaper/content/202306-64.点此复制
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