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For every ton of carbon dioxide
emitted by a power plant's smokestack or a car's exhaust pipe, some
portion will stay in the Earth's atmosphere, raising global
temperatures, while the rest is absorbed by the oceans or ecosystems on
land.
But which parts of the ocean or biosphere act as net sources of carbon dioxide (CO2) and
which take up more than they emit into the atmosphere, has been an open
question. Figuring that out, as well as understanding what mechanisms
govern that interplay and how they might change along with the climate,
has been an open question and one that is key to understanding how global warming will progress.
The 2014 launch of the Orbiting Carbon Observatory-2 satellite was
aimed at beginning to piece together some answers by monitoring the
comings and goings of CO2 from the atmosphere with unprecedented
precision and over large regions. [The Reality of Climate Change: 10 Myths Busted]
So far, the mission has done that and has turned up some surprises
along the way. The mission serendipitously coincided with one of the
strongest El Niños (an
ocean and atmosphere cycle that impacts global weather) on record,
allowing scientists to see how the carbon cycle responded and pinpoint
exactly where the resulting record pulse of CO2 that entered the
atmosphere came from. The satellite's instruments also unexpectedly
proved capable of distinguishing the relatively small CO2 signatures of
cities and even volcano plumes.
"We're very, very happy with these results," deputy project scientist
Annmarie Eldering, of NASA's Jet Propulsion Laboratory, told Live
Science.
But the findings, described in series of five papers in the Oct. 13
issue of the journal Science, are just the first steps at getting a
better handle on the carbon cycle (how carbon flows through land and sea
ecosystems and the atmosphere), as OCO-2 heads into an expected
extended mission and other space-based projects are scheduled to follow
in its wake.
Luck and surprises
Carbon dioxide is added to and removed from the atmosphere by a range of competing processes. On land, for example, the photosynthesis of plants takes up CO2, while the decay of plant matter and wildfires release it back into the atmosphere. [Here's How Carbon Dioxide Warms the Planet]
Scientists knew that El Niños were another factor that caused more
CO2 to build up in the Earth's atmosphere, and from the 1997-1998 major
El Niño, they had some suspicions on why that was. For one thing, El
Niño tends to lead to drying in parts of the tropics, resulting in less
photosynthesis and less uptake of carbon dioxide.
What project scientists couldn't know when the satellite rocketed
into space on July 2, 2014, was that it would be perfectly poised to
observe how one of the strongest El Niños in the books affected the
carbon cycle.
"Sometimes you get really lucky," said Galen McKinley, a carbon cycle
scientist at Columbia University's Lamont Doherty Earth Observatory.
These effects were in evidence during the 2015-2016 event, which
caused the biggest year-over-year jump in global CO2 concentrations on
record, according to the National Oceanic and Atmospheric
Administration. But OCO-2 revealed, as is so often the case in science,
that the picture was more complicated than previously thought. [CO2 Satellite: NASA's Orbiting Carbon Observatory-2 Mission in Photos]
The satellite's observations let project scientists piece together
the sequence of events of the carbon cycle's response as the El Niño
geared up and then reached its peak. They saw that at first there was a
tiny dip in carbon dioxide levels over the tropical Pacific because of
changes in the structure of the underlying ocean that meant waters gave
off less CO2. But that slight decrease was quickly overtaken by the much
larger response from terrestrial biomass as drought, heat and wildfires
took a toll and caused less CO2 to be absorbed and more to be released.
[Top 10 Deadliest Natural Disasters in History]
The ocean signal "was really a big surprise to us," said Abhishek
Chatterjee, a scientist with University Space Research Association
working at NASA's Goddard Spaceflight Center. The response had been
inferred before, "but it was never observed to the degree that we could"
with OCO-2, he said.
The team was able to take the analysis a step further by using
OCO-2's capability to detect a signature of photosynthesis, which is a
marker of the productivity of land plants. Together, the data showed
that while the tropical areas of Southeast Asia, South America and
Africa all added about the same amount of CO2 into the atmosphere, they
did so for different reasons. In Southeast Asia, the hot, dry conditions
brought on by El Niño made the region more vulnerable to fire, which
releases CO2 into the atmosphere. In South America, dry conditions
tamped down plant productivity, meaning the biosphere took up less
carbon dioxide, so that the region became a net source of CO2. And in
Africa, while rainfall was about normal, exceptional heat increased
plant respiration, which caused more CO2 emissions.
More work to do
OCO-2 sensors were also surprisingly good at picking out much smaller
CO2 signatures, such as the plume of Vanuatu's Yasur volcano and the
contrast between Los Angeles' relatively higher CO2 levels compared with
the surrounding suburban and rural areas. [Earth from Above: 101 Stunning Images from Orbit]
The satellite could also see how the difference between the urban
core and rural areas declined in the summer because plants in the region
took up some of the excess.
The ability of satellites to pinpoint these signatures has
implications for a wide range of applications, including monitoring
emissions to make sure cities and countries are complying with their
pledges to reduce CO2. Satellite CO2 measurements could also provide
earlier warnings of volcanic eruptions, said Florian Schwandner, also of
NASA's JPL, as CO2 emissions from volcanoes increase before an
eruption.
OCO-2 has completed its initial two-year planned mission and is
expected to begin a three-year extended mission once NASA officials sign
off on it, said Eldering, the deputy project scientist.
Scientists are also hoping that two other planned missions go as
scheduled to build on OCO-2's work. One, called OCO-3, will use leftover
spare parts from OCO-2 and would be mounted on the International Space
Station to allow scientists to point at features of interest. That
mission has been slated to be cut by the Trump administration, though it
remains to be seen whether Congress will go along with that plan.
The other, called the Geostationary Carbon Cycle Observatory, would
be able to measure CO2 over continuous areas, such as the U.S.,
something OCO-2 can't do.
"It's very exciting science, [but] there's a lot more work to do," McKinley said.
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