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<p>This circulation operates when certain currents send warm, oxygenated, nutrient-poor water into the deep ocean (<a href="page.php?w=downwelling">downwelling</a>), while the cold, oxygen-limited, nutrient-rich water travels upwards (or <a href="page.php?w=upwelling">upwells</a>) at specific points. Thermohaline circulation transports not only massive volumes of warm and cold water across the planet, but also dissolved <a href="page.php?w=oxygen">oxygen</a>, <a href="page.php?w=dissolved_organic_carbon">dissolved organic carbon</a> and other <a href="page.php?w=nutrient">nutrient</a>s</p><p>
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