The influence of 14CO2 releases from regional nuclear facilities at the Heidelberg 14CO2 sampling site (1986-2014)

Abstract. Atmospheric Δ14CO2 measurements are a well-established tool to estimate the regional fossil-fuel-derived CO2 component. However, emissions from nuclear facilities can significantly alter the regional Δ14CO2 level. In order to accurately quantify the signal originating from fossil CO2 emiss...

Full description

Saved in:
Bibliographic Details
Main Authors: Kuderer, Matthias (Author) , Hammer, Samuel (Author) , Levin, Ingeborg (Author)
Format: Article (Journal)
Language:English
Published: 2018
In: Atmospheric chemistry and physics
Year: 2018, Volume: 18, Issue: 11, Pages: 7951-7959
ISSN:1680-7324
DOI:https://doi.org/10.5194/acp-18-7951-2018
Online Access:Verlag, kostenfrei, Volltext: http://dx.doi.org/https://doi.org/10.5194/acp-18-7951-2018
Verlag, kostenfrei, Volltext: https://www.atmos-chem-phys.net/18/7951/2018/
Get full text
Author Notes:Matthias Kuderer, Samuel Hammer, and Ingeborg Levin
Description
Summary:Abstract. Atmospheric Δ14CO2 measurements are a well-established tool to estimate the regional fossil-fuel-derived CO2 component. However, emissions from nuclear facilities can significantly alter the regional Δ14CO2 level. In order to accurately quantify the signal originating from fossil CO2 emissions, a correction term for anthropogenic 14CO2 sources has to be determined. In this study, the HYSPLIT atmospheric dispersion model has been applied to calculate this correction for the long-term Δ14CO2 monitoring site in Heidelberg. Wind fields with a spatial resolution of 2.5° × 2.5°, 1° × 1°, and 0.5° × 0.5° show systematic deviations, with coarser resolved wind fields leading to higher mean values for the correction. The finally applied mean Δ14CO2 correction for the period from 1986-2014 is 2.3 ‰ with a standard deviation of 2.1 ‰ and maximum values up to 15.2 ‰. These results are based on the 0.5° × 0.5° wind field simulations in years when these fields were available (2009, 2011-2014), and for the other years they are based on 2.5° × 2.5° wind field simulations, corrected with a factor of 0.43. After operations at the Philippsburg boiling water reactor ceased in 2011, the monthly nuclear correction terms decreased to less than 2 ‰, with a mean value of 0.44 ± 0.32 ‰ from 2012 to 2014.</p>
Item Description:Published: 06 Jun 2018
Im Text ist 14 hochgestellt, 2 tiefgestellt
Gesehen am 29.06.2018
Physical Description:Online Resource
ISSN:1680-7324
DOI:https://doi.org/10.5194/acp-18-7951-2018