Gas composition of the surface air in Moscow during the extreme summer of 2010

Abstract

In summer 2010, anomalously hot weather occurred in the European part of Russia. It was caused by a blocking anticyclone of an unusually high intensity. West winds were stopped in the whole column of the troposphere, from the Earth's surface up to the lower stratosphere, for two months. During this entire period, the concentration of gaseous and aerosol pol� lutants grew in the nearsurface air. In the end of July and the first half of August, this extreme situation become even more complicated due to the arrival of air masses from the areas of forest, peat, and grass fires to Moscow. By the measurements data from the station of the Institute of Physics of the Atmosphere, Russian Academy of Sciences (IPA RAS), the concentrations of reactive gases NO, NO 2 , CO, and O 3 exceeded both the average daily and the general maximum permissi� ble concentration (MPC). The concentrations of greenhouse gases CO2, CH4, and other hydrocarbons were also excessive. Analysis of variation in gas content in the nearsurface air and in the atmospheric bound� ary layer has shown a close dependence on vertical stratification of the atmosphere. The blocking anticyclone above the European part of Russia recorded in summer 2010 significantly exceeded all the previously recorded ones in its dura� tion. According to (1), the duration of summer block� ing anticyclones in the Northern and Southern Hemi� spheres has not exceeded three weeks for the last forty years, while the longest periods of anticyclonic weather in winter have not lasted more than a month. Anomalies in the frequency and intensity of atmo� spheric blockings were recorded most often in the years of El Nino/La Nina phenomenon, including 2010 (see, for instance, (2)). The formed hot weather lead to the outbreak of numerous forest and peat wildfires. In total, 29 000 wild� fires were recorded in summer 2010 with a total burned area of 1.2 million ha (3). And though the wildfire intensity in 2010 was weaker than in some other years (e.g., 40 000 wildfires with a total burned area of about 1.5 million ha were recorded in 1972; 28 000 wildfires of 4.2 million ha, in 1998; 29 000 wildfires of 2.4 mil� lion ha, in 2009), the economic, ecological, and social consequences were more significant. The most important consequence of the emer� gency situation that appeared in summer 2010 was change in the chemical composition of the atmo� sphere above the European territory of Russia and West Siberia. Cities and settlements were covered with a dense haze when they happened to be in smoke trails of forest and peat wildfires. The presence of obviously extreme quantities of aerosols in the nearsurface air caused extreme concern and a demand for introduc� tion of required protective activities (3). No less nega� tive an effect on people's health and ecosystems was made by a significant change in gas composition of the atmosphere.