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• W2024407560 abstract "A key biological link between ocean geochemical cycles, ocean color and sea surface temperature (SST) is the nitrogen-to-chlorophyll a (N:chl a) ratio of phytoplankton. This is because nitrogen is the limiting factor over approximately 2/3 of the ocean surface and light absorption depends on the concentration of chlorophyll a. Recent work has demonstrated systematic variability in this ratio. Using one-dimensional models at two locations we show that varying N:Chl a, rather than keeping a fixed mean value (0–150m), leads to lower chlorophyll a in the mixed layer, less light absorption within the mixed layer and cooler sea surface temperatures. At the equator the temperature reduction is 0.15°C throughout the year whereas at 35°N, a temperature difference of about 1°C occurs during the summer. Although demonstrated at only two locations, this effect is likely to occur over large parts of the ocean." @default.
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• W2024407560 date "2001-04-01" @default.
• W2024407560 modified "2023-10-11" @default.
• W2024407560 title "Phytoplankton physiology can affect ocean surface temperatures" @default.
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• W2024407560 doi "https://doi.org/10.1029/2000gl011509" @default.
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