EGU24-12997, updated on 13 Mar 2024
https://doi.org/10.5194/egusphere-egu24-12997
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Two decades of micrometeorological measurements show dynamic drivers of springtime N2O emissions

Leah Brown1, Ian B. Strachan1, David Pelster2, Stuart Admiral2, Luc Pelletier2, Brian Grant2, Ward Smith2, and Elizabeth Pattey2
Leah Brown et al.
  • 1Queen's University, Geography and Planning, Canada (leah.brown@queensu.ca)
  • 2Agriculture and Agri-Food Canada

Nitrous oxide (N2O) is a potent greenhouse gas with a global warming potential 265 times that of carbon dioxide and the ability to destroy stratospheric ozone. Agricultural soils contribute over two-thirds of anthropogenic N2O emissions. Field observations in temperate climates have commonly shown N2O emission peaks occurring in the spring during a period of snow melt and soil thaw. This freeze-thaw period typically accounts for approximately 35% of annual N2O emissions, however, current understanding of its drivers is based off of relatively short observation periods. The analysis of such data over decadal time spans is therefore needed to improve our understanding of key drivers. Here, we report on 21 years (2002-2022) of micrometeorological N2O flux data from a field site in Ottawa, Ontario. Correlation analyses were conducted between the N2O flux during the spring thaw period and variables that are commonly considered drivers. Little to no correlation was seen from linear or multilinear regressions across a range of meteorological, management, and soil variables. The non-linear response of non-growing season cumulative N2O emissions to cumulative freezing degree-days was consistent with previous studies (Wagner-Riddle et al., 2017). However, in isolating freezing degree-days we may be neglecting other possible controls. These results show that the relationship of N2O flux with environmental variables may be related to complex, potentially non-linear, interactions between agricultural practices, weather, soil quality, and other variables. We will further examine the data using other multivariate statistical methods to further investigate potential drivers of these non-growing season emissions with a focus on those emissions occurring specifically during the spring thaw. As these relationships are used in nitrification/denitrification models, improved understanding is still needed to accurately simulate these processes, which is imperative to improving nitrogen budgets and ultimately achieving climate goals.

How to cite: Brown, L., Strachan, I. B., Pelster, D., Admiral, S., Pelletier, L., Grant, B., Smith, W., and Pattey, E.: Two decades of micrometeorological measurements show dynamic drivers of springtime N2O emissions, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12997, https://doi.org/10.5194/egusphere-egu24-12997, 2024.