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NASA Models Find Greenland Meltwater Runoff Spurs 15–40% Phytoplankton Growth

This study highlights how nutrient-rich meltwater alters local carbon dynamics in Greenland’s coastal waters

Ocean currents swirl around North America (center left) and Greenland (upper right) in this data visualization created using NASA’s ECCO model. Advanced computing is helping oceanographers decipher hot spots of phytoplankton growth. NASA’s Scientific Visualization Studio

Overview

  • Simulations on NASA’s Ames supercomputers show that nutrients carried by Greenland’s glacial meltwater boost summer phytoplankton growth by 15 to 40 percent in Jakobshavn Fjord.
  • The ECCO-Darwin model merges billions of satellite and ship-based ocean measurements to recreate how biology, chemistry and physics interact in coastal Arctic waters.
  • At peak melt, Jakobshavn Glacier releases more than 300,000 gallons of freshwater per second, contributing to Greenland’s annual loss of nearly 300 billion tons of ice.
  • Although fresh glacial runoff reduces seawater CO₂ solubility, the enlarged phytoplankton blooms compensate by absorbing increased atmospheric carbon.
  • Researchers will scale their high-resolution simulations to all of Greenland’s roughly 250 glaciers and other sensitive polar and temperate regions to evaluate ecosystem and carbon cycle feedbacks.