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Ocean Mixing Experiment. Tommi Bergman, Ambarish Karmalkar, Shreethala C., Abubakr Salih. Modifications. Vertical mixing coefficients (ABACK and DBACK) increased by factor of 25 No other modifications. Hypotheses. Increased vertical mixing Mixed layer thickness increase
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Ocean Mixing Experiment Tommi Bergman, Ambarish Karmalkar, Shreethala C., Abubakr Salih
Modifications • Vertical mixing coefficients (ABACK and DBACK) increased by factor of 25 • No other modifications
Hypotheses • Increased vertical mixing • Mixed layer thickness increase • SST and SAT decrease • Build-up of sea ice at high latitudes • Salinity profile change
Mixed layer thickness • Mixed layer thickens • Some anomalies especially around Antarctica
Sea temperature • Equatorial surface layer cools • At larger depths water temperature increases
SAT Control • Global temp reduces, but polar temp increases
Salinity vertical profile Salinity increases at poles, especially north pole
Ocean circulation • Compared to the control run the poleward mass transport increases m3s-1 Time
CO2 response • CO2 burden has a increasing trend all through the 20 years