Stratified-turbulence observations in the deep Mediterranean
Hans van Haren

TL;DR
This study uses high-resolution temperature sensors to analyze stratified turbulence in the deep Mediterranean, revealing its significance for deep-sea life and its correlation with atmospheric disturbances.
Contribution
It provides the first detailed measurements of stratified turbulence in the deep Mediterranean and compares different turbulence estimation methods under weakly stratified conditions.
Findings
Eddy-induced stratified turbulence exceeds geothermal and open-ocean turbulence.
Stratified turbulence correlates with atmospheric disturbances with about a one-week delay.
Turbulence is more energetic in winter than in summer.
Abstract
A nearly half-cubic hectometer of deep Mediterranean-Sea waters is yearlong sampled with about 3000 high-resolution temperature sensors to study different sources of turbulent waterflows, which are vital for life. Although temperature differences are never larger than 0.01degrC, daily, weekly, and seasonal variations are observed. About half the time, relatively warm stratified waters are moved from 100's of meters higher levels to near the seafloor. These internal-wave and sub-mesoscale eddy-induced motions are half an order of magnitude more turbulent than those induced via general geothermal heating from below, and about one order of magnitude more turbulent than those from open-ocean processes. A rough estimate shows that eddy-induced stratified turbulence is likely more important for deep-sea life than rare, not observed, deep dense-water formation at the abyssal-plain mooring…
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Taxonomy
TopicsOceanographic and Atmospheric Processes · Marine Invertebrate Physiology and Ecology · Geological formations and processes
