Can radon measurements at tall towers provide information on atmospheric vertical mixing states?
- 1National Physical Laboratory, UK
- 2Met Office, UK
- 3ICOS ERIC, Carbon Portal, Lund, Sweden
- 4School of Geographical Sciences, University of Bristol, Bristol, UK
- 5School of Environmental Sciences, University of East Anglia, Norwich, UK
- 6School of Chemistry, University of Bristol, Bristol, UK
- 7School of GeoSciences, University of Edinburgh, Edinburgh, UK
The vertical mixing state of the atmosphere, as well as the atmospheric boundary layer (ABL) height, are important atmospheric transport model parameters for the accurate simulation of greenhouse gas concentrations. In order to use tall tower greenhouse gas measurements to quantify regional scale emissions (top-down, inverse estimates) an estimate of the atmospheric transport model uncertainty across the time series of study is needed. Several methods have been used to estimate this, often relying on arbitrary thresholds or a combination of parameters (such as vertical gradients if a gas is measured at multiple points). Here we study if radon has potential as an independent measurement to assess model uncertainty.
Radon is a radioactive noble gas present in our atmosphere and is a good tracer of mixing processes in the ABL due to its properties. Hence, measurements of atmospheric radon concentration can provide useful insights into the vertical mixing state of the atmosphere, and in turn may help to calibrate and validate atmospheric dispersion models.
In this study, we use high temporal resolution atmospheric measurements of radon and CH4 from four tall tower sites in the UK, which are part of the Deriving Emissions linked to Climate Change (DECC) network: Heathfield (HFD), Ridge Hill (RGH), Tacolneston (TAC) and Weybourne (WAO). At each site, CH4 is measured at two or three different heights, while radon is measured at one height.
To determine a metric whereby single-height measurements of radon can provide a proxy for vertical mixing states, we compare the diurnal cycle of the measured radon concentration with the modelled radon (calculated by the Met Office Numerical Atmospheric Modelling Environment (NAME) dispersion model and radon flux maps). The largest uncertainties are shown to be before sunrise and after sunset right before the inversion layer was formed/destroyed. The diurnal CH4 vertical gradient at these times is also compared with the modelled CH4 vertical gradient.
How to cite: Saba, M., Kikaj, D., Chung, E., Manning, A., Karstens, U., Rennick, C., Ganesan, A., Forster, G., O'Doherty, S., Wenger, A., and Arnold, T.: Can radon measurements at tall towers provide information on atmospheric vertical mixing states?, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-12151, https://doi.org/10.5194/egusphere-egu23-12151, 2023.
