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Spatial and temporal variability of urban fluxes of methane, carbon monoxide and carbon dioxide above London, UK.
- Source :
- Atmospheric Chemistry & Physics Discussions; 3/30/2016, p1-31, 31p
- Publication Year :
- 2016
-
Abstract
- We report on more than three years of measurements of fluxes of methane (CH<subscript>4</subscript>), carbon monoxide (CO) and carbon dioxide (CO<subscript>2</subscript>) taken by eddy-covariance in central London, UK. Inter-annual variability in the period 2012-2014 ranged from 36.3 to 40.7 ktons km<superscript>-2</superscript> y<superscript>-1</superscript> for CO<subscript>2</subscript>, and from 69 to 75 tons km<superscript>-2</superscript> y<superscript>-1</superscript> for CH<subscript>4</subscript>. Mean annual emissions of CO<subscript>2</subscript> (39.1 ± 2.4 ktons km<superscript>-2</superscript> y<superscript>-1</superscript>) and CO (89 ± 16 tons km<superscript>-2</superscript> y<superscript>-1</superscript>) were consistent (within 1% and 5% respectively) with values from the London Atmospheric Emissions Inventory, but measured CH<subscript>4</subscript> (72 ± 3 tons km<superscript>-2</superscript> y<superscript>-1</superscript>) was over two-fold larger than the inventory value. Seasonal variability was large for CO with a winter to summer reduction of 69%. Monthly fluxes of CO were strongly anti-correlated with mean air temperature, and the winter emissions accounted for 45% of the annual budget. The winter increment in CO emissions was attributed mainly to vehicle cold starts and reduced fuel combustion efficiency. CO<subscript>2</subscript> fluxes were 33% higher in winter and anti-correlated with mean air temperature, albeit to a lesser extent than for CO. This was attributed to an increased demand for natural gas for heating during the winter. Seasonality in CH<subscript>4</subscript> fluxes was moderate (21% larger in winter) and linear correlation with air temperature was only statistically significant for certain wind sectors (N, NE, E and W), which was also the case for CO<subscript>2</subscript>. Differences in resident population within the flux footprint explained ca. 90% variability by wind direction in annual CO<subscript>2</subscript> fluxes and 99% for CH<subscript>4</subscript> (wind sectors excluded from linear regressions: S for CO<subscript>2</subscript>; S, SE and E for CH<subscript>4</subscript>). Seasonality and proportionality of emissions with respect to population in the outlying wind sectors (S, SE and E) might be masked by constant sources of CO<subscript>2</subscript> and CH<subscript>4</subscript>, perhaps of industrial or biogenic origin. To our knowledge, this study is unique given the long-term, continuous dataset of urban CH<subscript>4</subscript> fluxes analysed. [ABSTRACT FROM AUTHOR]
Details
- Language :
- English
- ISSN :
- 16807367
- Database :
- Complementary Index
- Journal :
- Atmospheric Chemistry & Physics Discussions
- Publication Type :
- Academic Journal
- Accession number :
- 116978749
- Full Text :
- https://doi.org/10.5194/acp-2016-216