Global distribution of CO<sub>2</sub> in the upper troposphere and stratosphere

In this study, we construct a new monthly zonal mean carbon dioxide (CO<sub>2</sub>) distribution from the upper troposphere to the stratosphere over the 2000–2010 time period. This reconstructed CO<sub>2</sub> product is based on a Lagrangian backward trajectory model driven...

Full description

Bibliographic Details
Main Authors: M. Diallo, B. Legras, E. Ray, A. Engel, J. A. Añel
Format: Article
Language:English
Published: Copernicus Publications 2017-03-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/17/3861/2017/acp-17-3861-2017.pdf
Description
Summary:In this study, we construct a new monthly zonal mean carbon dioxide (CO<sub>2</sub>) distribution from the upper troposphere to the stratosphere over the 2000–2010 time period. This reconstructed CO<sub>2</sub> product is based on a Lagrangian backward trajectory model driven by ERA-Interim reanalysis meteorology and tropospheric CO<sub>2</sub> measurements. Comparisons of our CO<sub>2</sub> product to extratropical in situ measurements from aircraft transects and balloon profiles show remarkably good agreement. The main features of the CO<sub>2</sub> distribution include (1) relatively large mixing ratios in the tropical stratosphere; (2) seasonal variability in the extratropics, with relatively high mixing ratios in the summer and autumn hemisphere in the 15–20 km altitude layer; and (3) decreasing mixing ratios with increasing altitude from the upper troposphere to the middle stratosphere ( ∼ 35 km). These features are consistent with expected variability due to the transport of long-lived trace gases by the stratospheric Brewer–Dobson circulation. The method used here to construct this CO<sub>2</sub> product is unique from other modelling efforts and should be useful for model and satellite validation in the upper troposphere and stratosphere as a prior for inversion modelling and to analyse features of stratosphere–troposphere exchange as well as the stratospheric circulation and its variability.
ISSN:1680-7316
1680-7324