Abstract
Airborne measurements within the urban mixing layer (360 m) over Greater London are used to quantify CO2 emissions at the meso-scale. Daytime CO2 fluxes, calculated by the Integrative Mass Boundary Layer (IMBL) method, ranged from 46 to 104 μmol CO2 m−2 s−1 for four days in October 2011. The day-to-day variability of IMBL fluxes is at the same order of magnitude as for surface eddy-covariance fluxes observed in central London. Compared to fluxes derived from emissions inventory, the IMBL method gives both lower (by −37%) and higher (by 19%) estimates. The sources of uncertainty of applying the IMBL method in urban areas are discussed and guidance for future studies is given.
Original language | English |
---|---|
Pages (from-to) | 98-106 |
Number of pages | 9 |
Journal | ENVIRONMENTAL POLLUTION |
Volume | 196 |
Early online date | 13 Oct 2014 |
DOIs | |
Publication status | Published - Jan 2015 |
Keywords
- carbon dioxide
- urban fluxes
- aircraft surveys
- eddy covariance
- megacity
- emissions inventory