Multi‐Scale Temporal Variability of Turbulent Mixing During a Monsoon Intra‐Seasonal Oscillation in the Bay of Bengal: An LES Study

Abstract

A process study using large‐eddy simulations is carried out to explore the dominant 1‐D processes that affect mixed layer (ML) properties during an event of summer Monsoon Intra‐seasonal Oscillations (MISO) in the Bay of Bengal (BOB). These simulations use realistic air‐sea fluxes and initial conditions that were collected during the summer 2018 MISO‐BOB field experiment to explore the roles of thermal inversion layer (TIL) and Langmuir turbulence (LT) in modulating ML properties. The simulations span an active period with heavy rain and strong winds and a break period with strong solar heat flux and little rain. The mixed layer depth (MLD), sea surface temperature (SST) and sea surface salinity (SSS) are most affected by the presence of near‐inertial oscillations, solar heating and precipitation, all of which occur at different timescales. The subsurface warming induced by the TIL reduces the SST variability at the MISO timescale when compared with the simulation without TIL. Comparison of simulations with and without LT indicates that LT enhances subsurface warming during the active phase and reduces diurnal SST modulation during the break phase. Simulations with 1‐D mixing models show a wide disparity in the evolution of MLD, SST, and SSS.

Scale-dependent air-sea exchange in the polar oceans: floe-floe and floe-flow coupling in the generation of ice-ocean boundary layer turbulence

“…Thus, floe-scale effects on surface flux can lead to significantly enhanced sub-grid-scale IOBL turbulence that needs to be parameterized to be able to include it in GCMs. This IOBL turbulence is involved in mixing of the upper oceans, deepening of the oceanic boundary layers, entrainment of deeper waters (conceivably including subsurface thermal maxima, e.g., Pham et al, 2023), and the shear within the upper ocean.…”

Scale‐Dependent Air‐Sea Exchange in the Polar Oceans: Floe‐Floe and Floe‐Flow Coupling in the Generation of Ice‐Ocean Boundary Layer Turbulence

“…Thus, floe‐scale effects on surface flux can lead to significantly enhanced sub‐grid‐scale IOBL turbulence that needs to be parameterized to be able to include it in GCMs. This IOBL turbulence is involved in ice‐ocean heat flux, mixing of the upper oceans, deepening of the oceanic boundary layers, entrainment of deeper waters (conceivably including subsurface thermal maxima, e.g., Pham et al., 2023), and the shear within the upper ocean.…”