I have written
on this blog about the global warming potential (GWP) of nitrogen
oxides, including nitrous oxides (N2O) from fertilizer, and about the photochemical
smog (ozone) precursor nitrogen oxide (NOx) gases. It has been recently shown
via a paper in Nature by scientists from the Max Planck Institute for
Biogeochemistry in Jena, Germany, that the fine suspended particles of reactive
nitrogen compounds mostly from combustion, which are short-lived in the
atmosphere, are the biggest contributor to a net cooling effect of anthropogenic
reactive nitrogen by shielding sunlight as does gaseous ammonia (NH3), also
emitted by the agriculture sector. These gases are forms of reactive nitrogen (Nr)
that appear in the biosphere on land and in the atmosphere. Nitrogen gas (N2), is non-reactive, or inert but all other nitrogen
compounds are reactive (Nr).
The global
nitrogen cycle includes the growing amounts of anthropogenic nitrogen oxide
gases (NOx, N2O) and gaseous ammonia (NH3) being emitted into the atmosphere. The
authors of the paper summarized the results in the abstract:
“This net cooling effect is the result of increased
aerosol loading, reduced methane lifetime and increased terrestrial carbon
sequestration associated with increases in anthropogenic Nr, which are not
offset by the warming effects of enhanced atmospheric nitrous oxide and ozone.
Future predictions using three representative scenarios show that this cooling
effect may be weakened primarily as a result of reduced aerosol loading and
increased lifetime of methane, whereas in particular N2O-induced warming will
probably continue to increase under all scenarios. Our results indicate that
future reductions in anthropogenic Nr to achieve environmental protection goals
need to be accompanied by enhanced efforts to reduce anthropogenic greenhouse
gas emissions to achieve climate change mitigation in line with the Paris
Agreement.”
Combustion of
fossil fuels and application of fertilizers are the two biggest sources of Nr. The
study involved modeling the chemical reactions in the land biosphere and atmosphere
to arrive at a flow chart or Nr cycle. They utilized terrestrial
biogeochemistry and atmospheric chemistry. The authors admit, however, that there
is still considerable uncertainty in the calculations and potentially a high
margin of error since net warming and cooling effects can vary
considerably in different regions.
It is well
known that NOx, N2O, and NH3 form aerosol particles in the atmosphere and that
these aerosol particles block sunlight thereby decreasing solar radiative
forcing. They also contribute to smog in the lower atmosphere that has a similar
effect. N2O remains long in the atmosphere like CO2, while NOx and NH3 are
short-lived in the atmosphere, more like methane. Thus, N2O has a net warming effect
but the shorter-lived gases have a net cooling effect due to the aerosol
particles. All of these factors are accounted for in the models. Nr gases also have
different individual aerosol effects and affect one another in different ways. The
paper gives the equations and reactions used as model assumptions in the study.
Lest we forget, air pollution does indeed slow global warming, but only for a
short time. This includes the considerable aerosols from burning coal and
biomass. Thus, it should perhaps be pointed out that this study only considers Nr
aerosols and not all aerosol particles which also include particulate matter
and sulfur oxide and sulfate compounds. When the world finally moves away from
coal after China’s and India’s consumption peaks and begins to drop, the amount
of combustion aerosols in the atmosphere will drop as well. Better pollution
abatement equipment on coal and wood power plants, especially, but also natural
gas plants can decrease aerosol production as well.
References:
Net effects of man-made nitrogen attenuate global
warming, researchers find. Eberhard Fritz. Phys.org. July 24, 2024. Net
effects of man-made nitrogen attenuate global warming, researchers find
(msn.com)
Global
net climate effects of anthropogenic reactive nitrogen. Cheng Gong, Hanqin
Tian, Hong Liao, Naiqing Pan, Shufen Pan, Akihiko Ito, Atul K. Jain, Sian
Kou-Giesbrecht, Fortunat Joos, Qing Sun, Hao Shi, Nicolas Vuichard, Qing Zhu,
Changhui Peng, Federico Maggi, Fiona H. M. Tang & Sönke Zaehle. Nature
(2024). Global net
climate effects of anthropogenic reactive nitrogen | Nature
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