Long-term trends in aerosol optical characteristics in the Po Valley, Italy

Abstract. Aerosol properties have been monitored by ground-based in situ and remote sensing measurements at the station for atmospheric research located in Ispra, on the edge of the Po Valley, for almost one decade. In situ measurements are performed according to Global Atmosphere Watch recommendations, and quality is assured through the participation in regular inter-laboratory comparisons. Sun-photometer data are produced by the Aerosol Robotic Network (AERONET). Data show significant decreasing trends over the 2004–2010 period for a number of variables, including particulate matter (PM) mass concentration, aerosol scattering, backscattering and absorption coefficients, and aerosol optical thickness (AOT). In situ measurement data show no significant trends in the aerosol backscatter ratio, but they do show a significant decreasing trend of about −0.7 ± 0.3% yr−1 in the aerosol single scattering albedo (SSA) in the visible light range. Similar trends are observed in the SSA retrieved from sun-photometer measurements. Correlations appear between in situ PM mass concentration and aerosol scattering coefficient, on the one hand, and elemental carbon (EC) concentration and aerosol absorption coefficient, on the other hand. However, no increase in the EC / PM ratio was observed, which could have explained the decrease in SSA. The application of a simple approximation to calculate the direct radiative forcing by aerosols suggests a significant diminution in their cooling effect, mainly due to the decrease in AOT. Applying the methodology we present to those sites, where the necessary suite of measurements is available, would provide important information to inform future policies for air-quality enhancement and fast climate change mitigation.

[1]  A. Dell'Acqua,et al.  Annual cycle in co-located in situ, total-column, and height- resolved aerosol observations in the Po Valley (Italy): Implications for ground-level particulate matter mass concentration estimation from remote sensing , 2010 .

[2]  J. Ogren,et al.  Determining Aerosol Radiative Properties Using the TSI 3563 Integrating Nephelometer , 1998 .

[3]  P. Chylek,et al.  Effect of absorbing aerosols on global radiation budget , 1995 .

[4]  Oleg Dubovik,et al.  Angstrom exponent and bimodal aerosol size distributions , 2006 .

[5]  Suzanne L. Reinman Intergovernmental Panel on Climate Change (IPCC) , 2012 .

[6]  T. Eck,et al.  Accuracy assessments of aerosol optical properties retrieved from AERONET Sun and sky-radiance measurements , 1999 .

[7]  T. Eck,et al.  Accuracy assessments of aerosol optical properties retrieved from Aerosol Robotic Network (AERONET) Sun and sky radiance measurements , 2000 .

[8]  Harald Flentje,et al.  Aerosol decadal trends - Part 1: In-situ optical measurements at GAW and IMPROVE stations , 2012 .

[9]  P. Hopke,et al.  Assessment of trends and present ambient concentrations of PM2.2 and PM10 in Dhaka, Bangladesh , 2008 .

[10]  J. Putaud,et al.  Aerosol hygroscopicity at Ispra EMEP-GAW station , 2012 .

[11]  J. Pichon,et al.  Characterization and intercomparison of aerosol absorption photometers: result of two intercomparison workshops , 2010 .

[12]  Comments on “direct radiative forcing of anthropogenic aerosols over oceans from satellite observation” , 2013, Advances in Atmospheric Sciences.

[13]  Wenche Aas,et al.  Introduction to the European Monitoring and Evaluation Programme (EMEP) and observed atmospheric composition change during 1972–2009 , 2012 .

[14]  A. J. Miller,et al.  Factors affecting the detection of trends: Statistical considerations and applications to environmental data , 1998 .

[15]  M. Brauer,et al.  Global Estimates of Ambient Fine Particulate Matter Concentrations from Satellite-Based Aerosol Optical Depth: Development and Application , 2010, Environmental health perspectives.

[16]  J. Haywood,et al.  The effect of anthropogenic sulfate and soot aerosol on the clear sky planetary radiation budget , 1995 .

[17]  Ulrike Lohmann,et al.  A GCM study of future climate response to aerosol pollution reductions , 2010 .

[18]  Peng Zhang,et al.  Direct radiative forcing of anthropogenic aerosols over oceans from satellite observations , 2011 .

[19]  W. Malm,et al.  Decreases in elemental carbon and fine particle mass in the United States , 2011 .

[20]  A. Dell'Acqua,et al.  Aerosol hygroscopicity at a regional background site (Ispra) in Northern Italy , 2012 .

[21]  J. Etterson,et al.  Rapid climate change and the rate of adaptation: insight from experimental quantitative genetics. , 2012, The New phytologist.

[22]  M. Schnaiter,et al.  Absorption of light by soot particles: determination of the absorption coefficient by means of aethalometers , 2003 .

[23]  Mar Viana,et al.  Toward a standardised thermal-optical protocol for measuring atmospheric organic and elemental carbon: the EUSAAR protocol , 2009 .