SEATTLE, Washington -- On a recent expedition to the inhospitable North Atlantic Ocean,
scientists at the University of Washington and collaborators studying
the annual growth of tiny plants were stumped to discover that the
plankton had started growing before the sun had a chance to offer the
light they need for their growth spurt.
For decades, scientists have known that
springtime brings the longer days and calmer seas that force
phytoplankton near the surface, where they get the sunlight they need to
flourish.
But in research results published this week in the journal Science, scientists report evidence of another trigger.
Eric D'Asaro and Craig Lee, oceanographers in the UW's Applied Physics Laboratory and School of Oceanography,
are among the researchers who found that whirlpools, or eddies, that
swirl across the North Atlantic sustain phytoplankton in the ocean's
shallower waters, where the plankton can get plenty of sunlight to fuel
their growth even before the longer days of spring start.
The eddies form when heavier, colder water from
the north slips under the lighter, warmer water from the south. The
researchers found that the eddies cause the bloom to happen around three
weeks earlier than it would if it was spurred just by spring's longer
days.
"That timing makes a significant difference if
you think about the animals that eat the phytoplankton," said D'Asaro,
the corresponding author on the paper.
Many small sea animals spend the winter dozing in the deep ocean, emerging in the spring and summer to feed on the phytoplankton.
"If they get the timing wrong, they'll starve,"
Lee said. Since fish eat the animals, a reduction in their number could
harm the fish population.
Scientists believe that climate change may affect oceanic circulation patterns
such as the one that causes the eddies. They've found some evidence
that warm waters from the subtropics are penetrating further to the
north, Lee said.
"If the climate alters the circulation patterns,
it might alter the timing of the bloom, which could impact which
animals grow and which die out," he said.
Learning about the circulation of the ocean also helps scientists forecast changes in the ocean, a bit like meteorologists are able to forecast the weather, said D'Asaro.
The scientists didn't set out to look at the
kind of large-scale mixing that they found. In April 2008, Lee and
co-author Mary Jane Perry of the University of Maine arrived in a
storm-lashed North Atlantic aboard an Icelandic research vessel.
They launched robots (specially designed by Lee
and D'Asaro) in the rough seas. A float that hovered below the water's
surface followed the motion of the ocean, moving around "like a giant
phytoplankton," said D'Asaro.
Lurking alongside the float were 6-foot-long,
teardrop-shaped Seagliders, also designed at the UW, that dove to depths
of up to 1,000 meters, or 3,280 feet. After each dive, working in areas
20 to 50 kilometers, or 12 to 31 miles, around the float, the gliders
rose to the surface, pointed their antennas skyward and transmitted
their stored data back to shore via satellite.
The float and gliders measured the temperature,
salinity and speed of the water, and gathered information about the
chemistry and biology of the bloom itself. Soon after measurements from
the float and gliders started coming in, the scientists saw that the
bloom had started, even though conditions still looked winter-like.
"It was apparent that some new mechanism, other than surface warming, was behind the bloom's initiation," said D'Asaro.
To find out what, the researchers needed sophisticated computer modeling.
Enter first author Amala Mahadevan, with Woods Hole Oceanographic Institution, who used 3-D computer models to look at information collected at sea by Perry, D'Asaro and Lee.
She generated eddies in a model using the
north-to-south oceanic temperature variation. Without eddies, the bloom
happened several weeks later and didn't have the space and time
structures actually observed in the North Atlantic.
In the future, the scientists hope to put the
North Atlantic bloom into a broader context. They believe much can be
learned by following the phytoplankton's evolution across an entire
year, especially with gliders and floats outfitted with new sensors. The
sensors would look at the tiny animals that graze on the phytoplankton.
"What we're learning about eddies is that they're a critical part of life in the ocean," said Perry. "They shape ocean ecosystems in countless ways."
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