![Darkening of the Global Ocean. (A) The rate change (units per year) in the diffuse attenuation coefficient for downwelling irradiance at 490 nm [ΔKd(490)] measured from MODIS Aqua between 2003 and 2022 in 9 km resolution (CRS: World Mollweide, ESRI:54009). Reds indicate regions where Kd(490) is increasing (oceans are getting darker), while blues indicate regions where Kd(490) is decreasing (oceans are getting lighter). White indicates regions where there was no statistically significant change in Kd(490) over the period 2003–2022. Values of ΔKd(490) were derived for each 9 km resolution pixel using quantile regression to the median performed on the fitted values of an Autoregressive Integrated Moving Average (ARIMA) model of annual averaged Kd(490) data. (B) International Hydrographic Office sea regions ranked according to the percentage of their area over which Kd(490) is increasing. Numbers inset above bars give the absolute area where Kd(490) is increasing in 10,000 km2. Raw data are presented in Table S4. Areas were calculated in CRS World Mercator (ESRI:54004). -- Global Change Biology](https://i0.wp.com/astrobiology.com/wp-content/uploads/2025/06/Water-Planet-Dynamics-Darkening.png?resize=1200%2C719&ssl=1)
The photic zones of the oceans—where sunlight and moonlight drive ecological interactions—are one of the most productive habitats on the planet and fundamental to the maintenance of healthy global biogeochemical […]
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