Noel Gutierrez Brizuela , Matthew H Alford, Shang-Ping Xie, Janet Sprintall, Gunnar Voet , Sally Warner, Kenneth Hughes, James Moum

Tropical cyclones (TCs) mix vertical temperature gradients in the upper ocean and generate powerful near-inertial internal waves (NIWs) that propagate down into the deep ocean. Globally, downward mixing of heat during TC passage causes warming in the seasonal thermocline and pumps 0.15-0.6 PW of heat into the unventilated ocean. The final distribution of excess heat contributed by TCs is needed to understand subsequent consequences for climate; however, it is not well constrained by current observations. Here we show that NIWs generated by TCs drive thermocline mixing weeks after TC passage and thus greatly deepen the extent of downward heat transfer induced by TCs. Microstructure measurements of the turbulent diffusivity (κ) and turbulent heat flux (Jq) in the Western Pacific before and after the passage of three TCs indicate that mean thermocline values of κ and Jq increased by factors of 2-7 and 2-4 (95% confidence level) respectively after TC passage. Excess mixing is shown to be associated with the vertical shear of NIWs, demonstrating that studies of TC-climate interactions ought to represent NIWs and their mixing to accurately capture TC effects on ocean stratification.