Sunlight reflects off the ocean surface near Norfolk,
Virginia, in this 1991 space shuttle image, highlighting swirling patterns
created by features such as internal waves, which are produced when the tide
moves over underwater features. Data from the international SWOT mission is
revealing the role of smaller-scale waves and eddies.
NASA
The international mission collects two-dimensional views of smaller waves
and currents that are bringing into focus the ocean’s role in supporting life
on Earth.
Small things matter, at least when
it comes to ocean features like waves and eddies. A recent NASA-led analysis
using data from the SWOT (Surface Water and Ocean Topography) satellite found
that ocean features as small as a mile across potentially have a larger impact
on the movement of nutrients and heat in marine ecosystems than previously
thought.
Too small to see well with previous
satellites but too large to see in their entirety with ship-based instruments,
these relatively small ocean features fall into a category known as the
submesoscale. The SWOT satellite, a joint effort between NASA and the French
space agency CNES (Centre National d’Études Spatiales), can observe these
features and is demonstrating just how important they are, driving much of the
vertical transport of things like nutrients, carbon, energy, and heat within
the ocean. They also influence the exchange of gases and energy between the
ocean and atmosphere.
“The role that submesoscale features play in ocean dynamics is what makes them important,” said Matthew Archer, an oceanographer at NASA’s Jet Propulsion Laboratory in Southern California. Some of these features are called out in the animation below, which was created using SWOT sea surface height data.
This animation shows small ocean features —
including internal waves and eddies — derived from SWOT observations in the
Indian, Atlantic, and Pacific oceans, as well as the Mediterranean Sea. White
and lighter blue represent higher ocean surface heights compared to darker blue
areas. The purple colors shown in one location represent ocean current speeds.
NASA’s Scientific Visualization Studio
“Vertical currents move heat
between the atmosphere and ocean, and in submesoscale eddies, can actually
bring up heat from the deep ocean to the surface, warming the atmosphere,”
added Archer, who is a coauthor on the submesoscale
analysis published
in April in the journal Nature. Vertical circulation can also bring up
nutrients from the deep sea, supplying marine food webs in surface waters like
a steady stream of food trucks supplying festivalgoers.
“Not only can we see the surface of
the ocean at 10 times the resolution of before, we can also infer how water and
materials are moving at depth,” said Nadya Vinogradova Shiffer, SWOT program
scientist at NASA Headquarters in Washington.
Fundamental
Force
Researchers have known about these
smaller eddies, or circular currents, and waves for decades. From space, Apollo
astronauts first spotted sunlight glinting off small-scale eddies about 50
years ago. And through the years, satellites have captured images of
submesoscale ocean features, providing limited information such as their
presence and size. Ship-based sensors or instruments dropped into the ocean
have yielded a more detailed view of submesoscale features, but only for
relatively small areas of the ocean and for short periods of time.
The SWOT satellite measures the
height of water on nearly all of Earth’s surface, including the ocean and
freshwater bodies, at least once every 21 days. The satellite gives researchers
a multidimensional view of water levels, which they can use to calculate, for
instance, the slope of a wave or eddy. This in turn yields information on the
amount of pressure, or force, being applied to the water in the feature. From
there, researchers can figure out how fast a current is moving, what’s driving
it and —combined with other types of information — how much energy, heat, or
nutrients those currents are transporting.
“Force is the fundamental quantity
driving fluid motion,” said study coauthor Jinbo Wang, an oceanographer at
Texas A&M University in College Station. Once that quantity is known, a
researcher can better understand how the ocean interacts with the atmosphere,
as well as how changes in one affect the other.
Prime Numbers
Not only was SWOT able to spot a
submesoscale eddy in an offshoot of the Kuroshio Current — a major current in
the western Pacific Ocean that flows past the southeast coast of Japan — but
researchers were also able to estimate the speed of the vertical circulation
within that eddy. When SWOT observed the feature, the vertical circulation was
likely 20 to 45 feet (6 to 14 meters) per day.
This is a comparatively small
amount for vertical transport. However, the ability to make those calculations
for eddies around the world, made possible by SWOT, will improve researchers’
understanding of how much energy, heat, and nutrients move between surface
waters and the deep sea.
Researchers can do similar
calculations for such submesoscale features as an internal solitary wave — a
wave driven by forces like the tide sloshing over an underwater plateau. The
SWOT satellite spotted an internal wave in the Andaman Sea, located in the
northeastern part of the Indian Ocean off Myanmar. Archer and colleagues
calculated that the energy contained in that solitary wave was at least twice
the amount of energy in a typical internal tide in that region.
This kind of information from SWOT
helps researchers refine their models of ocean circulation. A lot of ocean
models were trained to show large features, like eddies hundreds of miles
across, said Lee Fu, SWOT project scientist at JPL and a study coauthor. “Now
they have to learn to model these smaller scale features. That’s what SWOT data
is helping with.”
Researchers have already started to
incorporate SWOT ocean data into some models, including NASA’s ECCO (Estimating the Circulation and Climate of the Ocean). It may take
some time until SWOT data is fully a part of models like ECCO. But once it is,
the information will help researchers better understand how the ocean ecosystem
will react to a changing world.
More About
SWOT
The SWOT satellite was jointly
developed by NASA and CNES, with contributions from the Canadian Space Agency
(CSA) and the UK Space Agency. Managed for NASA by Caltech in Pasadena,
California, JPL leads the U.S. component of the project. For the flight system
payload, NASA provided the Ka-band radar interferometer (KaRIn) instrument, a
GPS science receiver, a laser retroreflector, a two-beam microwave radiometer,
and NASA instrument operations. The Doppler Orbitography and Radioposition
Integrated by Satellite system, the dual frequency Poseidon altimeter
(developed by Thales Alenia Space), the KaRIn radio-frequency subsystem
(together with Thales Alenia Space and with support from the UK Space Agency),
the satellite platform, and ground operations were provided by CNES. The KaRIn
high-power transmitter assembly was provided by CSA.
To learn more about SWOT, visit: https://swot.jpl.nasa.gov
Source: NASA, French SWOT Satellite Offers Big View of Small Ocean Features - NASA
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