Langmuir mixing effects on global climate: WAVEWATCH III in CESM. (July 2016)

• Record Type: Journal Article
• Authors: Li, Qing; Webb, Adrean; Fox-Kemper, Baylor; Craig, Anthony; Danabasoglu, Gokhan; Large, William G.; Vertenstein, Mariana
• Is Part Of: Ocean modelling. Volume 103(2016:Jul.)
• Page Start: 145
• Page End: 160
• Publication Date: 2016-07
• Subjects: Langmuir mixing -- Mixed layer -- KPP -- Climate model; Oceanography -- Periodicals; Océanographie -- Périodiques; Oceanography; Periodicals; 551.46
• DOI: 10.1016/j.ocemod.2015.07.020
• Languages: English
• ISSNs: 1463-5003

Abstract

Highlights: A third generation wave model has been incorporated into a global climate model. Langmuir mixing is parameterized empirically based on large eddy simulations. Wind-wave misalignment and Stokes drift penetration depth are considered. Mixed layer depth is deepened and improved, especially in the Southern Ocean. Ventilation and subsurface temperature are improved globally. Abstract: Large-Eddy Simulations (LES) have shown the effects of ocean surface gravity waves in enhancing the ocean boundary layer mixing through Langmuir turbulence. Neglecting this Langmuir mixing process may contribute to the common shallow bias in mixed layer depth in regions of the Southern Ocean and the Northern Atlantic in most state-of-the-art climate models. In this study, a third generation wave model, WAVEWATCH III, has been incorporated as a component of the Community Earth System Model, version 1.2 (CESM1.2). In particular, the wave model is now coupled with the ocean model through a modified version of the K-Profile Parameterization (KPP) to approximate the influence of Langmuir mixing. Unlike past studies, the wind-wave misalignment and the effects of Stokes drift penetration depth are considered through empirical scalings based on the rate of mixing in LES. Wave-Ocean only experiments show substantial improvements in the shallow biases of mixed layer depth in the Southern Ocean. Ventilation is enhanced and low concentration biases of pCFC-11 are reduced in the Southern Hemisphere. A majority of the improvements persist in the presence of other climate feedbacks in the fully coupled experiments. In addition, warming of the subsurface water over the majority of global ocean is observed in the fully coupled experiments with waves, and the cold subsurface ocean temperature biases are reduced.