Nitrous Oxide and Climate
C. A. de Lange, J. D. Ferguson, W. Happer, W. A. van Wijngaarden

TL;DR
This paper explains that nitrous oxide's contribution to global warming is relatively small compared to CO2, and restrictions on N2O emissions are unjustified and could harm food security.
Contribution
It provides a detailed analysis of N2O's radiative forcing and argues that restricting N2O emissions is not justified based on its minimal impact on climate change.
Findings
N2O's radiative forcing per molecule is 230 times that of CO2.
The increase rate of N2O is much slower than CO2, leading to a smaller overall warming contribution.
Restricting N2O emissions could harm global food supplies without significant climate benefits.
Abstract
Higher concentrations of atmospheric nitrous oxide (N2O) are expected to slightly warm Earth's surface because of increases in radiative forcing. Radiative forcing is the difference in the net upward thermal radiation flux from the Earth through a transparent atmosphere and radiation through an otherwise identical atmosphere with greenhouse gases. Radiative forcing, normally measured in W/m^2, depends on latitude, longitude and altitude, but it is often quoted for the tropopause, about 11 km of altitude for temperate latitudes, or for the top of the atmosphere at around 90 km. For current concentrations of greenhouse gases, the radiative forcing per added N2O molecule is about 230 times larger than the forcing per added carbon dioxide (CO2) molecule. This is due to the heavy saturation of the absorption band of the relatively abundant greenhouse gas, CO2, compared to the much smaller…
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Taxonomy
TopicsAtmospheric and Environmental Gas Dynamics · Atmospheric Ozone and Climate
