http://www.reportingclimatescience.com/news-stories/article/converting-wetlands-creates-radiative-forcing.html

26.03.2015 14:08 Age: 65 days

>From the Helmholtz Centre Potsdam

Natural wetlands usually emit methane and sequester carbon dioxide.
Anthropogenic impacts however, in particular the conversion of wetlands
into cropland, result in a significant increase in CO2 emissions, which
overcompensate potential decreases in methane emission, caused by the
reduction of wetlands.

A large international research team now calculated that the conversion of
arctic and boreal wetlands into agricultural land would result in an
additional cumulative radiative forcing of about 0,1 mJ per square meter
for the next 100 years. The conversion of temperate wetlands into
agricultural land would even result in a cumulative radiative forcing of
0,15 mJ per square meter. Converting forested wetlands into managed forests
also contributes to increased warming, albeit much less than the conversion
of non-forested wetlands.

Wetlands are unique ecosystems, which - under natural conditions - are the
single largest natural source of the greenhouse gas methane (CH4) but at
the same time an important sink for the greenhouse gas carbon dioxide
(CO2). The climate footprint of these ecosystems depends on the balance of
these two important greenhouse gases. Despite methane being 28 times more
potent as a greenhouse gas than carbon dioxide (in a 100 year time span),
the conversion of natural wetlands into agricultural or forested ecosystems
and its associated decrease in methane emissions still leads to an overall
warming effect. "The human impact on wetlands, such as drainage, results in
a shift of the climate footprint of that wetland” says Torsten Sachs at the
GFZ German Research Centre for Geosciences, co-author of the study. "The
overall balance of these two differently active greenhouse gases and thus
the climate footprint of a wetland over different time spans depend on the
relative sign and magnitude of these ecosystem-atmosphere fluxes".

The global impact is still rather uncertain due to large temporal and
spatial variability and a lack of data on the complex interactions between
environmental drivers such as temperatures of land, water, and sediment,
water levels, vegetation, nutrient availability, among others, and the
additional anthropogenic impacts such as land use change.

To calculate the net ecosystem carbon balance of wetland ecosystems, the
more than 40 member research team synthesized data from almost 30
differently affected arctic, boreal, and temperate study sites across the
globe. Simultaneous measurements of the ecosystem-atmosphere CO2 and CH4
fluxes in continental North America, Greenland, Europe, and Russia were
used for analyses and modeling. For sites with a full annual dataset of CO2
and CH4 fluxes, natural and converted sites were paired in all possible
combinations within similar ecosystem types. "To determine the climate
impact of the conversion, we used the difference of the net ecosystem
carbon balance between the site pairs as series of consecutive annual mass
pulses and integrated their effect on tropospheric greenhouse gas
concentrations” explains GFZ researcher Sachs. The different radiative
efficiencies and atmospheric residence times of the greenhouse gases were
accounted for when the radiative forcing was calculated for the period from
2000 – 2100.

This research was published in the the Proceedings of the National Academy
of Science (PNAS).

PNAS reports the significance of this research as: Wetlands are unique
ecosystems because they are in general sinks for carbon dioxide and sources
of methane. Their climate footprint therefore depends on the relative sign
and magnitude of the land–atmosphere exchange of these two major greenhouse
gases. This work presents a synthesis of simultaneous measurements of
carbon dioxide and methane fluxes to assess the radiative forcing of
natural wetlands converted to agricultural or forested land. The net
climate impact of wetlands is strongly dependent on whether they are
natural or managed. Here we show that the conversion of natural wetlands
produces a significant increase of the atmospheric radiative forcing. The
findings suggest that management plans for these complex ecosystems should
carefully account for the potential biogeochemical effects on climate.

Significant climate risks are associated with a positive carbon–temperature
feedback in northern latitude carbon-rich ecosystems, making an accurate
analysis of human impacts on the net greenhouse gas balance of wetlands a
priority. Here, we provide a coherent assessment of the climate footprint
of a network of wetland sites based on simultaneous and quasi-continuous
ecosystem observations of CO2 and CH4 fluxes. Experimental areas are
located both in natural and in managed wetlands and cover a wide range of
climatic regions, ecosystem types, and management practices. Based on
direct observations we predict that sustained CH4 emissions in natural
ecosystems are in the long term (i.e., several centuries) typically offset
by CO2 uptake, although with large spatiotemporal variability. Using a
space-for-time analogy across ecological and climatic gradients, we
represent the chronosequence from natural to managed conditions to quantify
the “cost” of CH4 emissions for the benefit of net carbon sequestration.
With a sustained pulse–response radiative forcing model, we found a
significant increase in atmospheric forcing due to land management, in
particular for wetland converted to cropland. Our results quantify the role
of human activities on the climate footprint of northern wetlands and call
for development of active mitigation strategies for managed wetlands and
new guidelines of the Intergovernmental Panel on Climate Change (IPCC)
accounting for both sustained CH4 emissions and cumulative CO2 exchange.

Uncertain climate footprint of wetlands under human pressure by Ana Maria
Roxana Petrescu et. al., published in the Proceedings of the National
Academy of Science, PNAS Early Edition, doi: 10.1073/pnas.1416267112

Read the abstract and get the paper here.

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