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Biogeochemical evidence of vigorous mixing in the abyssal ocean
Author(s) -
Lampitt Richard S.,
Popova Ekaterina E.,
Tyrrell Toby
Publication year - 2003
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2002gl016638
Subject(s) - abyssal zone , biogeochemical cycle , seabed , water column , oceanography , geology , salinity , sink (geography) , environmental science , mixing (physics) , nutrient , chemistry , environmental chemistry , physics , quantum mechanics , cartography , organic chemistry , geography
The metabolic activities of biological communities living at the abyssal seabed create a strong source of nutrients and a sink for oxygen. If the published estimates of vertical mixing based on instantaneous microstructure measurements are correct, near to the abyssal seabed away from rough topographic features there should be enhanced concentrations of nitrate and phosphate and depletion of oxygen. Recent data on the vertical concentration profiles of inorganic nutrients and oxygen over the bottom 1000 m of the water column (World Ocean Circulation Experiment ‐ WOCE) provide no such evidence. It is concluded that the effective vertical mixing rates are much more vigorous than previously indicated and may even be higher than estimates of average basin scale rates based on temperature and salinity distributions. We propose that the enhanced mixing associated with rough topography influences the entire volume of the abyssal ocean on short time scales (e.g., one month ‐ one year).