Abstract:Abstract. Data from the Interagency Monitoring of Protected Visual Environments (IMPROVE) network of aerosol samplers and NOAA monitoring sites are examined for weekly cycles. At remote and rural sites, fine particle elemental carbon, crustal elements, and coarse particle mass had pronounced (up to 20%) weekly cycles with minima on Sunday or Monday. Fine particle organic carbon and mass had smaller amplitude cycles, also with Sunday or Monday minima. There was no statistically significant weekly cycle in fine … Show more
“…The weekly σ sp and σ ap cycles are likely the result of a build-up of scattering and absorbing aerosols in the PBL during the first half of the week. Sunday σ ap minima and weekly cycle amplitudes of ∼ 25-35 % during spring and fall are consistent with the timing and amplitudes of weekly EC concentration cycles reported for the rural US (Murphy et al, 2008) and with weekday-weekend EC concentration differences in the urban US (Bae et al, 2004;Blanchard et al, 2008). Smaller but significant weekly σ sp cycle amplitudes of ∼ 15-20 % during spring, summer, and fall are larger than weekly cycles in OC and sulfate reported by Murphy et al (2008).…”
Section: Temporal Variability At Appsupporting
confidence: 69%
“…Our weekly σ sp cycle amplitude for the entire year (Fig. 3c) is similar to that of Murphy et al (2008).…”
Section: Temporal Variability At Bndsupporting
confidence: 57%
“…Aerosol optical properties at the four sites vary primarily on seasonal timescales. Day of week variability in AOPs can be used as a tool for distinguishing anthropogenic from natural aerosol sources, since natural sources would not be expected to have AOPs that vary on weekly scales (Murphy et al, 2008). Diurnal variability is used along with co-located meteorological data to infer the influence of local pollution sources and mixing layer height on measured AOPs.…”
Abstract. Hourly averaged aerosol optical properties (AOPs) measured over the years 2010-2013 at four continental North American NOAA Earth System Research Laboratory (NOAA/ESRL) cooperative aerosol network sites -Southern Great Plains near Lamont, OK (SGP), Bondville, IL (BND), Appalachian State University in Boone, NC (APP), and Egbert, Ontario, Canada (EGB) are analyzed. Aerosol optical properties measured over 1996 at BND and 1997 at SGP are also presented. The aerosol sources and types in the four regions differ enough so as to collectively represent rural, anthropogenically perturbed air conditions over much of eastern continental North America. Temporal AOP variability on monthly, weekly, and diurnal timescales is presented for each site. Differences in annually averaged AOPs and those for individual months at the four sites are used to examine regional AOP variability. Temporal and regional variability are placed in the context of reported aerosol chemistry at the sites, meteorological measurements (wind direction, temperature), and reported regional mixing layer heights. Basic trend analysis is conducted for selected AOPs at the long-term sites (BND and SGP). Systematic relationships among AOPs are also presented.Seasonal variability in PM 1 (sub-1 µm particulate matter) scattering and absorption coefficients at 550 nm (σ sp and σ ap , respectively) and most of the other PM 1 AOPs is much larger than day of week and diurnal variability at all sites. All sites demonstrate summer σ sp and σ ap peaks. Scattering coefficient decreases by a factor of 2-4 in September-October and coincides with minimum single-scattering albedo (ω 0 ) and maximum hemispheric backscatter fraction (b). The covariation of ω 0 and b lead to insignificant annual cycles in top-of-atmosphere direct radiative forcing efficiency (DRFE) at APP and SGP. Much larger annual DRFE cycle amplitudes are observed at EGB (∼ 40 %) and BND (∼ 25 %), with least negative DRFE in September-October at both sites. Secondary winter peaks in σ sp are observed at all sites except APP. Amplitudes of diurnal and weekly cycles in σ ap at the sites are larger for all seasons than those of σ sp , with the largest differences occurring in summer. The weekly and diurnal cycle amplitudes of most intensive AOPs (e.g., those derived from ratios of measured σ sp and σ ap ) are minimal in most cases, especially those related to parameterizations of aerosol size distribution.Statistically significant trends in σ sp (decreasing), PM 1 scattering fraction (decreasing), and b (increasing) are found at BND from 1996 to 2013 and at SGP from 1997 to 2013. A statistically significant decreasing trend in PM 10 scattering Ångström exponent is also observed for SGP but not BND. Most systematic relationships among AOPs are similar for the four sites and are adequately described for individual seasons by annually averaged relationships, althoughPublished by Copernicus Publications on behalf of the European Geosciences Union.
“…The weekly σ sp and σ ap cycles are likely the result of a build-up of scattering and absorbing aerosols in the PBL during the first half of the week. Sunday σ ap minima and weekly cycle amplitudes of ∼ 25-35 % during spring and fall are consistent with the timing and amplitudes of weekly EC concentration cycles reported for the rural US (Murphy et al, 2008) and with weekday-weekend EC concentration differences in the urban US (Bae et al, 2004;Blanchard et al, 2008). Smaller but significant weekly σ sp cycle amplitudes of ∼ 15-20 % during spring, summer, and fall are larger than weekly cycles in OC and sulfate reported by Murphy et al (2008).…”
Section: Temporal Variability At Appsupporting
confidence: 69%
“…Our weekly σ sp cycle amplitude for the entire year (Fig. 3c) is similar to that of Murphy et al (2008).…”
Section: Temporal Variability At Bndsupporting
confidence: 57%
“…Aerosol optical properties at the four sites vary primarily on seasonal timescales. Day of week variability in AOPs can be used as a tool for distinguishing anthropogenic from natural aerosol sources, since natural sources would not be expected to have AOPs that vary on weekly scales (Murphy et al, 2008). Diurnal variability is used along with co-located meteorological data to infer the influence of local pollution sources and mixing layer height on measured AOPs.…”
Abstract. Hourly averaged aerosol optical properties (AOPs) measured over the years 2010-2013 at four continental North American NOAA Earth System Research Laboratory (NOAA/ESRL) cooperative aerosol network sites -Southern Great Plains near Lamont, OK (SGP), Bondville, IL (BND), Appalachian State University in Boone, NC (APP), and Egbert, Ontario, Canada (EGB) are analyzed. Aerosol optical properties measured over 1996 at BND and 1997 at SGP are also presented. The aerosol sources and types in the four regions differ enough so as to collectively represent rural, anthropogenically perturbed air conditions over much of eastern continental North America. Temporal AOP variability on monthly, weekly, and diurnal timescales is presented for each site. Differences in annually averaged AOPs and those for individual months at the four sites are used to examine regional AOP variability. Temporal and regional variability are placed in the context of reported aerosol chemistry at the sites, meteorological measurements (wind direction, temperature), and reported regional mixing layer heights. Basic trend analysis is conducted for selected AOPs at the long-term sites (BND and SGP). Systematic relationships among AOPs are also presented.Seasonal variability in PM 1 (sub-1 µm particulate matter) scattering and absorption coefficients at 550 nm (σ sp and σ ap , respectively) and most of the other PM 1 AOPs is much larger than day of week and diurnal variability at all sites. All sites demonstrate summer σ sp and σ ap peaks. Scattering coefficient decreases by a factor of 2-4 in September-October and coincides with minimum single-scattering albedo (ω 0 ) and maximum hemispheric backscatter fraction (b). The covariation of ω 0 and b lead to insignificant annual cycles in top-of-atmosphere direct radiative forcing efficiency (DRFE) at APP and SGP. Much larger annual DRFE cycle amplitudes are observed at EGB (∼ 40 %) and BND (∼ 25 %), with least negative DRFE in September-October at both sites. Secondary winter peaks in σ sp are observed at all sites except APP. Amplitudes of diurnal and weekly cycles in σ ap at the sites are larger for all seasons than those of σ sp , with the largest differences occurring in summer. The weekly and diurnal cycle amplitudes of most intensive AOPs (e.g., those derived from ratios of measured σ sp and σ ap ) are minimal in most cases, especially those related to parameterizations of aerosol size distribution.Statistically significant trends in σ sp (decreasing), PM 1 scattering fraction (decreasing), and b (increasing) are found at BND from 1996 to 2013 and at SGP from 1997 to 2013. A statistically significant decreasing trend in PM 10 scattering Ångström exponent is also observed for SGP but not BND. Most systematic relationships among AOPs are similar for the four sites and are adequately described for individual seasons by annually averaged relationships, althoughPublished by Copernicus Publications on behalf of the European Geosciences Union.
“…Reddy and Venkataraman [7] and Abera et al [8] note that the pollutants like CO and NO x emanate from automobile exhausts, whereas use of coal based fuels causes heavy emissions of SO 2 . Murphy (2008) et al [2] and Rosibeto et al [9] find that the levels of O 3 , NO x and particulate matter are an issue of concern in the urban environment. The variation in concentration of such pollutants strongly relates to the pattern of human activities in the city.…”
Section: Pollution Emissionmentioning
confidence: 99%
“…On the other hand, changing patterns of vehicular traffic and industrial activities also act as a factor for variation in pollution levels. Authors such as Blanchard et al [1], Murphy (2008) et al [2], Fujita et al [3], Gour et al [4], Murphy (2007) et al [5] and Kakoli et al [6] note that weekly cycle of activities of population explains divergent temporal variation in pollution levels from weekdays (Monday to Friday) to weekend (Saturday and Sunday). The paper attempts to carry out an assessment of 24 h daily average concentration of six major pollutants for a period of five years (from 2006 to 2010).…”
Air Pollution is an escalating problem worldwide fuelled by increasing anthropogenic activities, speedy development, rapid industrialization, transportation, superfluous use of fossil fuel consumption, increasing global power needs, etc. Also the diverse meteorological factors influence our environment to a great extent. Population explosion has led to remarkable increase in vehicular population. The use solely depends upon the lifestyle of the citizen. Any change in the lifestyle has a remarkable effect on the air we breathe. A comprehensive database for pollution levels from the year 2006 to 2010 was analyzed for a main traffic intersection and a non-traffic area in Delhi (India). The paper asserts that pollutant concentration levels on weekend are lower than those on weekdays (increase on Sundays with respect to weekdays is CO 2.98 times, PM2.5 1.18 times, NO 1.62 times, NO2 5.76 times, SO 2 1.27 times and O 3 1.15 times). The pollution levels have been found to attenuate on public holidays and weekends. Pollution can hence be related to the weekly cycle of human activities. Pollutions due to vehicular emissions on roads, rails, air or water all serve as major sources of pollution. Hence, viably possible solutions for pollution control can also be achieved by controlling the magnitude of traffic flow on roads.
This study identified distinct weekly cycles in thunderstorm activities and convection‐associated variables in two regions of China dominated by different types of aerosol during the summers of 1983–2005. In both regions, visibility has similar weekly cycle: lower on weekdays than on weekends. Barring any possible “natural” weekly cycles, the findings of the poorest and best visibility on Friday and Monday, respectively, point to the weekly variations in anthropogenic emissions. However, the phases of the thunderstorm cycles between the two regions were different. In central China, thunderstorms occurred more frequently from Saturday to Monday than on other days. The cycles were out of phase in southeast China. It is hypothesized that the phase difference is associated with aerosol type. In central China aerosol absorption is strong, which suppresses convection more on weekdays. In southeast China aerosols are less absorbing but more hygroscopic, which helps invigorate thunderstorms more on weekdays.
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