Abstract

Abstract. The mixing layer is an important meteorological factor that affects air pollution. In this study, the atmospheric mixing layer height (MLH) was observed in Beijing from July 2009 to December 2012 using a ceilometer. By comparison with radiosonde data, we found that the ceilometer underestimates the MLH under conditions of neutral stratification caused by strong winds, whereas it overestimates the MLH when sand-dust is crossing. Using meteorological, PM2.5, and PM10 observational data, we screened the observed MLH automatically; the ceilometer observations were fairly consistent with the radiosondes, with a correlation coefficient greater than 0.9. Further analysis indicated that the MLH is low in autumn and winter and high in spring and summer in Beijing. There is a significant correlation between the sensible heat flux and MLH, and the diurnal cycle of the MLH in summer is also affected by the circulation of mountainous plain winds. Using visibility as an index to classify the degree of air pollution, we found that the variation in the sensible heat and buoyancy term in turbulent kinetic energy (TKE) is insignificant when visibility decreases from 10 to 5 km, but the reduction of shear term in TKE is near 70 %. When visibility decreases from 5 to 1 km, the variation of the shear term in TKE is insignificant, but the decrease in the sensible heat and buoyancy term in TKE is approximately 60 %. Although the correlation between the daily variation of the MLH and visibility is very poor, the correlation between them is significantly enhanced when the relative humidity increases beyond 80 %. This indicates that humidity-related physicochemical processes is the primary source of atmospheric particles under heavy pollution and that the dissipation of atmospheric particles mainly depends on the MLH. The presented results of the atmospheric mixing layer provide useful empirical information for improving meteorological and atmospheric chemistry models and the forecasting and warning of air pollution.

Highlights

  • The mixing layer is formed when discontinuous turbulence exists due to discontinuities in temperature stratification between the upper and lower layers of the atmosphere

  • The mixing layer height (MLH) data acquired by meteorological radiosondes and by ceilometer were compared for the two types of weather conditions (Fig. 2)

  • Using the MLH calculated by the radiosondes as a reference, the comparison showed that the MLH observed from the ceilometer was overestimated or underestimated in a portion of the samples

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Summary

Introduction

The mixing layer is formed when discontinuous turbulence exists due to discontinuities in temperature stratification between the upper and lower layers of the atmosphere. The atmospheric mixing layer height (MLH) is an important meteorological factor that affects the vertical diffusion of atmospheric pollutants and water vapour concentrations; it impacts the formation and dissipation of air pollutants (Aron, 1983; Stull, 1988). Continuous observations of the MLH are helpful for improving the parameterizations of boundary layer models, and they play an important role of improving the simulation accuracy of meteorological models and optimizing the simulation results for pollutants. G. Tang et al.: Mixing layer height and air pollution over Beijing

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