North American cold-climate forests are already absorbing less carbon,
study shows

Date:
August 17, 2020
Source:
University of Michigan
Summary:
Trees are one of humans' biggest allies in the fight against
climate change, soaking up around 30% of the carbon we pump into
the atmosphere by burning fossil fuel.



FULL STORY ========================================================================== Trees are one of humans' biggest allies in the fight against climate
change, soaking up around 30% of the carbon we pump into the atmosphere
by burning fossil fuel.


==========================================================================
And over the past several decades, it has appeared that cold-climate
forests at high latitudes have become even more effective carbon sinks as rising temperatures and higher CO2 levels have made them more productive.

But a new study led by University of Michigan researchers gives a
clearer picture of what's happening in different regions, and it has
cast additional uncertainty on whether those ecosystems will continue
to absorb carbon as they become hotter and drier in the decades ahead.

Published in PNAS and involving experts from around the globe, the
study shows that the amount of carbon Siberian forests contribute to the planet's seasonal carbon flux has increased much more than that of other forests at similar latitudes. Since the early 1980s, the seasonal carbon
uptake in Siberian forests has increased four times more than that of
North American boreal forests like those in Alaska and western Canada,
for example.

The study is the first to quantify how carbon emitted from specific
surface regions during the annual carbon flux affects the seasonal
cycle of CO2 in the atmosphere: The planet essentially "breathes in"
carbon during the spring and summer when trees and plants grow leaves
and photosynthesize. It exhales in winter when vegetation goes dormant.

Knowing this seasonal flux gives researchers a picture of how productive different forest regions are and how much carbon they remove from the atmosphere.



==========================================================================
The varied carbon flux across different forests of similar latitudes
suggests that, while some forests, like those in Siberia, are continuing
to increase their carbon uptake, others, like those in North America,
may not. They may even absorb less as the climate changes.

"This research shows that we need to be thinking differently about
how we understand the carbon cycle," said study co-author Gretchen Keppel-Aleks, U- M assistant professor of climate and space sciences and engineering. "We can't just lump ecosystems together by their latitude. We
need to be thinking about individual species and specific seasonal cycles
of temperature and precipitation." Researchers know that the swings
in annual seasonal carbon flux have increased substantially in the past
several decades. In the Northern Hemisphere, the intensity of the flux
has gone up 30-50% since the 1960s, suggesting widespread ecological
change. But because previous studies have focused on planetwide or
hemisphere average fluxes, it has been unclear exactly what's driving
the increase.

There's been a simple narrative that warmer temperatures have been
universally fueling plant photosynthesis across the high latitudes,
said Brendan Rogers of Woodwell Climate Research Center (formerly Woods
Hole Research Center).

"While that's true on the whole, we found starkly divergent responses
across regions," Rogers said. "Siberia has been greening, strengthening
its carbon sink and driving increases in seasonal CO2 exchange, but Arctic-boreal North America is showing much more browning under worsening stresses like fires, pests, and droughts.



========================================================================== "Going forward, we need to make sure our carbon budgets and models are
fully incorporating what's happening in Alaska and Canada, as these
patterns are largely not captured in models and the region may soon
transition from a carbon sink to a source." To produce their findings,
the team began with actual measurements of atmospheric CO2, collected
over decades by the National Oceanic and Atmospheric Administration.

They then worked backwards, using a computer model to calculate the
regional surface emissions that would result in atmospheric carbon levels
that matched the actual observations.

"We used these realistic surface fluxes and released them to the
atmosphere in our model, and what's unique is that we tagged individual
regions differently," Keppel-Aleks said. "We could watch red CO2
originating from Siberia, blue CO2 originating from North America,
green CO2 originating from lower latitude ecosystems. That allowed
us to figure out which regions are responsible for this increase in
the seasonal cycle." NOAA doesn't measure fluxes but instead measures
carbon dioxide in the atmosphere and has been tracking the increase in the seasonal cycle since 1976 at sites like the Barrow Observatory in Alaska.

"These observations and the magnitude of the change we have measured are unparalleled compared with the many other sites across the globe where
we track CO2 in the atmosphere -- suggesting that something dramatic is happening in the Arctic that is not happening anywhere else," said study co-author Colm Sweeney, associate director of the NOAA Global Monitoring Laboratory. "This study has helped us better understand and pinpoint the
source of these dramatic observations." The research also corroborates
earlier data that shows significant greening in Siberian forests alongside
much less greening at similar latitudes in North America.

"It's really significant that, using completely independent atmospheric
data, we're corroborating the browning and greening trends in the remote sensing data and showing that Siberian ecosystems do in fact seem to be
growing more productive in the summer," Keppel-Aleks said.

"It's another unambiguous sign that humans are causing changes in
the Earth's ecosystems, and it shows that we need to develop a better understanding of those ecosystems if we want to predict what's in store
for the planet."

========================================================================== Story Source: Materials provided by University_of_Michigan. Original
written by Gabe Cherry.

Note: Content may be edited for style and length.


========================================================================== Journal Reference:
1. Xin Lin, Brendan M. Rogers, Colm Sweeney, Fre'de'ric Chevallier,
Mikhail
Arshinov, Edward Dlugokencky, Toshinobu Machida, Motoki Sasakawa,
Pieter Tans, Gretchen Keppel-Aleks. Siberian and temperate
ecosystems shape Northern Hemisphere atmospheric CO2 seasonal
amplification. Proceedings of the National Academy of Sciences,
2020; 201914135 DOI: 10.1073/ pnas.1914135117 ==========================================================================

Link to news story: https://www.sciencedaily.com/releases/2020/08/200817191756.htm

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