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Combining Top-Down and Bottom-Up Approaches to Evaluate Recent Trends and Seasonal Patterns in UK N2O Emissions

Saboya, Eric ; Manning, Alistair J. ; Levy, Peter ; Stanley, Kieran M. ; Pitt, Joseph ; Young, Dickon ; Say, Daniel ; Grant, Aoife ; Arnold, Tim LU and Rennick, Chris , et al. (2024) In Journal of Geophysical Research: Atmospheres 129(14).
Abstract

Atmospheric trace gas measurements can be used to independently assess national greenhouse gas inventories through inverse modeling. Atmospheric nitrous oxide (N2O) measurements made in the United Kingdom (UK) and Republic of Ireland are used to derive monthly N2O emissions for 2013–2022 using two different inverse methods. We find mean UK emissions of 90.5 ± 23.0 (1σ) and 111.7 ± 32.1 (1σ) Gg N2O yr−1 for 2013–2022, and corresponding trends of −0.68 ± 0.48 (1σ) Gg N2O yr−2 and −2.10 ± 0.72 (1σ) Gg N2O yr−2, respectively, for the two inverse methods. The UK National Atmospheric Emissions Inventory (NAEI) reported mean N2O emissions of 73.9... (More)

Atmospheric trace gas measurements can be used to independently assess national greenhouse gas inventories through inverse modeling. Atmospheric nitrous oxide (N2O) measurements made in the United Kingdom (UK) and Republic of Ireland are used to derive monthly N2O emissions for 2013–2022 using two different inverse methods. We find mean UK emissions of 90.5 ± 23.0 (1σ) and 111.7 ± 32.1 (1σ) Gg N2O yr−1 for 2013–2022, and corresponding trends of −0.68 ± 0.48 (1σ) Gg N2O yr−2 and −2.10 ± 0.72 (1σ) Gg N2O yr−2, respectively, for the two inverse methods. The UK National Atmospheric Emissions Inventory (NAEI) reported mean N2O emissions of 73.9 ± 1.7 (1σ) Gg N2O yr−1 across this period, which is 22%–51% smaller than the emissions derived from atmospheric data. We infer a pronounced seasonal cycle in N2O emissions, with a peak occurring in the spring and a second smaller peak in the late summer for certain years. The springtime peak has a long seasonal decline that contrasts with the sharp rise and fall of N2O emissions estimated from the bottom-up UK Emissions Model (UKEM). Bayesian inference is used to minimize the seasonal cycle mismatch between the average top-down (atmospheric data-based) and bottom-up (process model and inventory-based) seasonal emissions at a sub-sector level. Increasing agricultural manure management and decreasing synthetic fertilizer N2O emissions reduces some of the discrepancy between the average top-down and bottom-up seasonal cycles. Other possibilities could also explain these discrepancies, such as missing emissions from NH3 deposition, but these require further investigation.

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organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
greenhouse gases, NO, regional inverse modeling, seasonal cycle, top-down bottom-up evaluation
in
Journal of Geophysical Research: Atmospheres
volume
129
issue
14
article number
e2024JD040785
publisher
Wiley-Blackwell
external identifiers
  • scopus:85199308170
ISSN
2169-897X
DOI
10.1029/2024JD040785
language
English
LU publication?
yes
id
0b748bbc-cf51-4593-81bd-103d4c524a8d
date added to LUP
2024-09-13 14:36:58
date last changed
2024-09-13 14:38:15
@article{0b748bbc-cf51-4593-81bd-103d4c524a8d,
  abstract     = {{<p>Atmospheric trace gas measurements can be used to independently assess national greenhouse gas inventories through inverse modeling. Atmospheric nitrous oxide (N<sub>2</sub>O) measurements made in the United Kingdom (UK) and Republic of Ireland are used to derive monthly N<sub>2</sub>O emissions for 2013–2022 using two different inverse methods. We find mean UK emissions of 90.5 ± 23.0 (1σ) and 111.7 ± 32.1 (1σ) Gg N<sub>2</sub>O yr<sup>−1</sup> for 2013–2022, and corresponding trends of −0.68 ± 0.48 (1σ) Gg N<sub>2</sub>O yr<sup>−2</sup> and −2.10 ± 0.72 (1σ) Gg N<sub>2</sub>O yr<sup>−2</sup>, respectively, for the two inverse methods. The UK National Atmospheric Emissions Inventory (NAEI) reported mean N<sub>2</sub>O emissions of 73.9 ± 1.7 (1σ) Gg N<sub>2</sub>O yr<sup>−1</sup> across this period, which is 22%–51% smaller than the emissions derived from atmospheric data. We infer a pronounced seasonal cycle in N<sub>2</sub>O emissions, with a peak occurring in the spring and a second smaller peak in the late summer for certain years. The springtime peak has a long seasonal decline that contrasts with the sharp rise and fall of N<sub>2</sub>O emissions estimated from the bottom-up UK Emissions Model (UKEM). Bayesian inference is used to minimize the seasonal cycle mismatch between the average top-down (atmospheric data-based) and bottom-up (process model and inventory-based) seasonal emissions at a sub-sector level. Increasing agricultural manure management and decreasing synthetic fertilizer N<sub>2</sub>O emissions reduces some of the discrepancy between the average top-down and bottom-up seasonal cycles. Other possibilities could also explain these discrepancies, such as missing emissions from NH<sub>3</sub> deposition, but these require further investigation.</p>}},
  author       = {{Saboya, Eric and Manning, Alistair J. and Levy, Peter and Stanley, Kieran M. and Pitt, Joseph and Young, Dickon and Say, Daniel and Grant, Aoife and Arnold, Tim and Rennick, Chris and Tomlinson, Samuel J. and Carnell, Edward J. and Artoli, Yuri and Stavart, Ann and Spain, T. Gerard and O’Doherty, Simon and Rigby, Matthew and Ganesan, Anita L.}},
  issn         = {{2169-897X}},
  keywords     = {{greenhouse gases; NO; regional inverse modeling; seasonal cycle; top-down bottom-up evaluation}},
  language     = {{eng}},
  number       = {{14}},
  publisher    = {{Wiley-Blackwell}},
  series       = {{Journal of Geophysical Research: Atmospheres}},
  title        = {{Combining Top-Down and Bottom-Up Approaches to Evaluate Recent Trends and Seasonal Patterns in UK N<sub>2</sub>O Emissions}},
  url          = {{http://dx.doi.org/10.1029/2024JD040785}},
  doi          = {{10.1029/2024JD040785}},
  volume       = {{129}},
  year         = {{2024}},
}