Loading…
A recent build-up of atmospheric CO2 over Europe. Part 1: observed signals and possible explanations
We analysed interannual and decadal changes in the atmospheric CO 2 concentration gradient (ΔCO 2 ) between Europe and the Atlantic Ocean over the period 1995-2007. Fourteen measurement stations are used, with Mace-Head being used to define background conditions. The variability of ΔCO 2 reflects fo...
Saved in:
Published in: | Tellus. Series B, Chemical and physical meteorology Chemical and physical meteorology, 2010-02, Vol.62 (1), p.1-13 |
---|---|
Main Authors: | , , , , , , , , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Summary: | We analysed interannual and decadal changes in the atmospheric CO
2
concentration gradient (ΔCO
2
) between Europe and the Atlantic Ocean over the period 1995-2007. Fourteen measurement stations are used, with Mace-Head being used to define background conditions. The variability of ΔCO
2
reflects fossil fuel emissions and natural sinks activity over Europe, as well as atmospheric transport variability. The mean ΔCO
2
increased by 1-2 ppm at Eastern European stations (∼30% growth), between 1990-1995 and 2000-2005. This built up of CO
2
over the continent is predominantly a winter signal. If the observed increase of ΔCO
2
is explained by changes in ecosystem fluxes, a loss of about 0.46 Pg C per year would be required during 2000-2005. Even if severe droughts have impacted Western Europe in 2003 and 2005, a sustained CO
2
loss of that magnitude is unlikely to be true.We sought alternative explanations for the observed CO
2
build-up into transport changes and into regional redistribution of fossil fuel CO
2
emissions. Boundary layer heights becoming shallower can only explain 32% of the variance of the signal. Regional changes of emissions may explain up to 27% of the build-up. More insights are given in the Aulagnier et al. companion paper. |
---|---|
ISSN: | 0280-6509 1600-0889 |
DOI: | 10.1111/j.1600-0889.2009.00442.x |