Wind-generated near-inertial internal waves (NIWs) are characterized by dominant long-range equatorward radiation due to the gradient of the planetary vorticity, known as the β-refraction effect. In this study, we analyze the effects of horizontal model resolution on the long-range equatorward radiation of NIWs. In a high-resolution Community Earth System Model (CESM-HR) with a 0.1° oceanic resolution, about 25% (15%) of downward NIW energy flux injected at the surface boundary layer (SBL) base poleward of 30°N (30°S) radiates into the lower-latitude region. This ratio decreases to about 15% (8%) in a low-resolution CESM (CESM-LR) with a 1° oceanic resolution. The higher long-range equatorward radiation efficiency in the CESM-HR than the CESM-LR is directly attributed to the faster equatorward group velocity of the NIWs of the first three vertical modes, and essentially results from the finer oceanic resolution of the CESM-HR. In the CESM-LR, increase of equatorward wavenumber of NIWs induced by the β-refraction effect is limited by the grid size, which underrepresents the long-range equatorward radiation of NIWs. The results underscore the necessity of high-resolution ocean models in accurately simulating the spatial variabilities of NIWs and their induced turbulent diapycnal mixing in the global ocean.
Coastal Zones Under Intensifying Human Activities and Changing Climate: A Regional Programme Integrating Science, Management and Society to Support Ocean Sustainability (COASTAL-SOS)
承办单位
State Key Laboratory of Marine Environmental Science, Xiamen University College of Ocean and Earth Sciences, Xiamen University China-ASEAN College of Marine Sciences, Xiamen University Malaysia