Late summer chlorophyll blooms in the oligotrophic North
Pacific subtropical gyre
Cara Wilson, Ph.D.
NOAA/NMFS
Pacific Fisheries Environmental Laboratory
Wednesday, June 25, 2003
3:00 p.m. – Pacific Forum
In
the late summer of 1997, 1999, and 2000, SeaWiFS recorded large
chlorophyll blooms in the oligotrophic North Pacific subtropical gyre (NPSG)
near 30°N and 150°W. These blooms covered up to 40,000 km2
and lasted as long as 4 months. They are distinct from the surface
seasonal cycle in both timing and amplitude, and they are not associated
with either SSH or SST anomalies that would indicate changes in subsurface
structure. The chlorophyll blooms are not forced by nutrient fertilization
from dust deposition or rainfall. It is hypothesized that the chlorophyll
blooms are fueled by NO3 supplied
from summer Trichodesmium blooms, and that wind forcing could be a
factor in their development. The existence of these blooms supports
previous research indicating that there are inputs of primary production
in the NPSG outside of the understood seasonal cycle.
Next: Nanopore analysis of macromolecules