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The second sulfur sink is pyrite burial in shelf sediments or deep seafloor sediments (4 × 10 13 g/year; δ 34 S = -20‰). [94] The total marine sulfur output flux is 1.0 × 10 14 g/year which matches the input fluxes, implying the modern marine sulfur budget is at steady state. [93] The residence time of sulfur in modern global oceans is ...
The oceans store more than 90% of the extra heat added to the climate system by Earth's energy imbalance and act as a buffer against its effects. [87] This means that the same amount of heat that would increase the average world ocean temperature by 0.01 °C (0.018 °F) would increase atmospheric temperature by approximately 10 °C (18 °F). [88]
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The World Ocean Database was first released in 1994 [3] and updates have been released approximately every four years, 1998, [4] 2001, [5] and 2005. [6] The most recent World Ocean Database series, WOD09, was released in September 2009. [7] The WOD09 has more than 9 million temperature profiles and 3.6 million salinity profiles.
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