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One year of 222 Rn concentration in the atmospheric surface layer

S. Galmarini
- 19 Dec 2005 - 
- Vol. 6, Iss: 10, pp 2865-2886
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TLDR
In this article, a one-year time series of radon measured in a rural area in the North of Italy in 1997 has been analyzed, where wavelet analysis is used as one of the investigation tools of the time series.
Abstract
A one-year time series of 222 Rn measured in a rural area in the North of Italy in 1997 is analyzed. The scope of the investigation is to better understand the behavior of this common atmospheric tracer in relation to the meteorological conditions at the release site. Wavelet analysis is used as one of the investigation tools of the time series. The measurements and scalograms of 222 Rn are compared to those of wind-speed, pressure, relative humidity, temperature and NO x . The use of wavelet analysis allows the identification of the various scales controlling the influence of the meteorological variables on 222 Rn dispersion in the surface layer that are not visible through classical Fourier analysis or direct time series inspection. The analysis of the time series has identified specific periods during which the usual diurnal variation of radon is superimposed to a linear growth thus indicating the build up of concentration at the measurement level. From these specific cases an estimate of the surface flux of 222 Rn is made. By means of a simple model these special cases are reproduced.

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Review on airflow in unsaturated zones induced by natural forcings

TL;DR: In this paper, the authors synthesize the published literature on subsurface airflow driven by natural forcings such as atmospheric pressure fluctuations, topographic effect, water table fluctuations, and water infiltration.
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On the use of radon for quantifying the effects of atmospheric stability on urban emissions

TL;DR: In this article, the authors argue that single-height radon observations should not be used quantitatively as an indicator of atmospheric stability without prior conditioning of the time series to remove contributions from larger-scale "non-local" processes.
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Investigations on indoor radon in Austria, Part 1: Seasonality of indoor radon concentration.

TL;DR: The seasonality of indoor Rn concentration measured in Austria is investigated as a function of other factors that influence indoors Rn, with higher Rn levels in winter.
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Radon as a tracer of atmospheric influences on traffic-related air pollution in a small inland city

TL;DR: One year of radon, benzene and carbon monoxide (CO) concentrations were analyzed to characterise the combined influences of variations in traffic density and meteorological conditions on urban air quality in Bern, Switzerland as mentioned in this paper.
References
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Journal ArticleDOI

Factors affecting exhalation of radon from a gravelly sandy loam

TL;DR: In this article, the meteorological factors that most affected the instantaneous value of exhalation of radon were atmospheric pressure and rain, while effects due to other parameters such as wind or temperature were either comparatively small or undetectable.
Journal ArticleDOI

Wavelet Analysis of Coherent Structures at the Atmosphere-Forest Interface.

TL;DR: In this paper, a wavelet analysis was applied to turbulence data for temperature and vertical velocity within and above a deciduous forest, and the principal time scales of the structures determined by this technique were 56–60 s and 40–44 s for the vertical velocity fields, respectively.
Journal ArticleDOI

Radon global simulations with the multiscale chemistry and transport model MOCAGE

TL;DR: In this article, the authors present an evaluation of the representation of subgrid scale transport in the new multiscale global chemistry and transport model MOCAGE, which is an off-line computation of vertical mass fluxes due to convective and turbulent processes.
Journal ArticleDOI

Long period study of outdoor radon concentration in Milan and correlation between its temporal variations and dispersion properties of atmosphere

TL;DR: The long term measurements of radon have permitted us to examine the dispersion characteristics of the atmosphere over Milan, and to establish the frequency of conditions unfavourable to the dispossession of atmospheric pollutants.
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