Ozone flux measurements over vegetation are important to estimate surface losses and ozone uptake by plants. The gradient and eddy covariance flux technique were used for measurements over grassland at a flux-monitoring site in southern Scotland during August 2007. The comparison of the two methods shows that the aerodynamic flux-gradient method provides very similar long-term average fluxes of ozone as the eddy covariance method. The eddy covariance technique is better at capturing diurnal cycles and short-term changes, but the comparison of two fast analysers illustrate that there can be considerable measurement uncertainty
Between June and September 2002, the fluxes of carbon dioxide (CO2) and ozone (O3), and nitrogen oxi...
We present a systematic intercomparison study of eddy covariance ozone flux measurements made using ...
International audienceTropospheric ozone (O 3) is a known greenhouse gas responsible for impacts on ...
Nowadays, eddy covariance is the state-of-the-art method to quantify turbulent exchange fluxes in th...
Nowadays, eddy covariance is the state-of-the-art method to quantify turbulent exchange fluxes in th...
Surface deposition is an important sink for tropospheric ozone. The rate of ozone deposition may be...
Surface deposition is an important sink for tropospheric ozone. The rate of ozone deposition may be...
Plants and soils act as major sinks for tropospheric ozone, especially during daylight hours when pl...
During the GRAMINAE Integrated Experiment between 20 May and 15 June 2000, the ozone flux was measur...
In June and July 2012, during the intensive field campaign of the ECLAIRE project, ozo...
In June and July 2012, during the intensive field campaign of the ECLAIRE project, ozo...
Ozone (O3) is a photochemically formed reactive gas responsible for a decreasing carbon assimilation...
The major objective of this research project was to measure the resistance to ozone uptake over a va...
During the GRAMINAE Integrated Experiment between 20 May and 15 June 2000, the ozone flux was measur...
During the GRAMINAE Integrated Experiment between 20 May and 15 June 2000, the ozone flux was measur...
Between June and September 2002, the fluxes of carbon dioxide (CO2) and ozone (O3), and nitrogen oxi...
We present a systematic intercomparison study of eddy covariance ozone flux measurements made using ...
International audienceTropospheric ozone (O 3) is a known greenhouse gas responsible for impacts on ...
Nowadays, eddy covariance is the state-of-the-art method to quantify turbulent exchange fluxes in th...
Nowadays, eddy covariance is the state-of-the-art method to quantify turbulent exchange fluxes in th...
Surface deposition is an important sink for tropospheric ozone. The rate of ozone deposition may be...
Surface deposition is an important sink for tropospheric ozone. The rate of ozone deposition may be...
Plants and soils act as major sinks for tropospheric ozone, especially during daylight hours when pl...
During the GRAMINAE Integrated Experiment between 20 May and 15 June 2000, the ozone flux was measur...
In June and July 2012, during the intensive field campaign of the ECLAIRE project, ozo...
In June and July 2012, during the intensive field campaign of the ECLAIRE project, ozo...
Ozone (O3) is a photochemically formed reactive gas responsible for a decreasing carbon assimilation...
The major objective of this research project was to measure the resistance to ozone uptake over a va...
During the GRAMINAE Integrated Experiment between 20 May and 15 June 2000, the ozone flux was measur...
During the GRAMINAE Integrated Experiment between 20 May and 15 June 2000, the ozone flux was measur...
Between June and September 2002, the fluxes of carbon dioxide (CO2) and ozone (O3), and nitrogen oxi...
We present a systematic intercomparison study of eddy covariance ozone flux measurements made using ...
International audienceTropospheric ozone (O 3) is a known greenhouse gas responsible for impacts on ...