Ocean Color Time Series

Like plants on land, phytoplankton need sunlight and nutrients to bloom. The main source of ocean nutrients comes from cold, deep ocean water that wells up to the surface, called upwelling. The circulation of the ocean and atmosphere determine where nutrients upwell. Areas of upwelling, and thus phytoplankton productivity, include the subpolar gyres, along the equator, along the west coast of continents, along western boundary currents (e.g., Gulf Stream) and near islands. Other sources of nutrients to the ocean surface include run-off from land and atmospheric deposition of minerals (e.g., desert dust).

Phytoplankton bloom patterns change with short-term weather systems (e.g., the passage of tropical storms), with the seasons, and with longer-term climate patterns such as El Niño. Ocean color satellite data such as these allow scientists to study global phytoplankton distribution, crucial for understanding the differences between long-term trends caused by natural oscillations and anthropogenic climate changes (i.e., ocean warming, stratification, acidification).

The Ocean Biology Processing Group at NASA’s Goddard Space Flight Center processed the data and the Environmental Visualization Lab at NOAA’s National Environmental Satellite, Data and Information Service (NESDIS) produced the monthly maps.