Impact of dust events on aerosol optical properties over Iraq

Arabian Journal of Geosciences - Tập 10 - Trang 1-18 - 2017
Saadiyah H. Halos1, Osama T. Al-Taai2, Monim H. Al-Jiboori2
1Atmosphere and Space Sciences Center, Directorate of Space Technology and Communication, Ministry of Sciences and Technology, Baghdad, Iraq
2Department of Atmospheric Sciences, College of Science, Al-Mustansiriyah University, Ministry of Higher Education and Scientific Research, Baghdad, Iraq

Tóm tắt

The spatial and temporal characteristics of aerosol optical properties (AOP) were analyzed in order to find out the hotspot aerosol sources over Iraq and surrounding regions. The correlation of AOP with the frequency of dust events (dust storm (DS), rising dust (RD), suspended dust (SD)) over 12 Iraqi stations is evaluated during the study period (January 2005–December 2014). The AOP: aerosol absorption optical depth (AAOD), aerosol extinction optical depth (AOD), and aerosol single scattering albedo (SSA) at 388 and 500 nm and aerosol index (AI), are derived from the Ozone Monitoring Instrument (OMI) on board the Aura satellite. Three well-known spatial interpolation techniques: inverse distance weighting, radial basis function with three sub-types, and kriging with three sub-types, are examined in ArcGIS software. Statistical analysis is applied to compute the station probability of dust events and its correlation with AOP. Results showed that the spline with the lowest RMSE and MPE near zero is the optimum method for estimating AOP. The spatial mean of AAOD, AOD, and AI (SSA) have the same pattern with high (low) mean values over the south and northwest of Iraq, Kuwait, and the northeast of Saudi Arabia. The seasonal variability of AAOD and AOD over the Iraqi stations showed that high (low) values occurred during spring and summer (winter) and concluded that AAOD is a responsible component for variation in AOD. DS and RD probability is higher over stations in the middle and south of Iraq than the stations in the north. High SD probability is over Mosul, Baghdad, and Nasiriya stations. The correlation of AOP with dust events suggests that the AAOD component is more important in the study of DS than SSA and AI while AI is a good index for the study of RD and SD in the study region.

Tài liệu tham khảo

Ahmad SP, Torres O, Bhartia PK, Leptoukh G, Kempler SJ (2006) Aerosol index from TOMS and OMI measurements. Proc. of the 86th AMS annual meeting Alomari MI, Adnan T, Rasoul L, Khayri G, Sahib A, Nouri N (2009) Generalized soil map of Iraq. Ministry of Science and Technology publication Anderson RS, Haff PK (1991) Wind modification and bed response during saltation of sand in air. In: Aeolian grain transport 1, pp 21–51, Springer, Vienna Anderson TL, Masonis SJ, Covert DS, Ahlquist NC, Howell SG, Clarke AD, McNaughton CS (2003) Variability of aerosol optical properties derived from in situ aircraft measurements during ACE-Asia. J Geophys Res Atmos 108 ArcGIS (2008) Desktop Help ESRI, Redlands, CA. ArcGIS 9 Bagnold RA (1941) The physics of blown sand and desert dunes. Methuen, New York Bergstrom RW, Pilewskie P, Russell P, Redemann J, Bond T, Quinn P, Sierau B (2007) Spectral absorption properties of atmospheric aerosols. Atmos Chem Phys 7(23):5937–5943 Blitzstein JK, Hwang J (2014) Introduction to probability. CRC Press, US Corr CA (2008) Retrieval of aerosol single scattering albedo at UV wavelengths for two urban field campaigns. Dissertation, Colorado State University Denby B, Horálek J, Walker S E, Eben K, Fiala J (2005) Interpolation and assimilation methods for European scale air quality assessment and mapping. Part I: review and recommendations. European Topic Centre on Air and Climate Change Technical Paper 7 Eck T F, Holben B N, Sinyuk A, Pinker R T, Goloub P, Chen H, Chatenet B, Li Z, Singh R P, Tripathi S N, Reid J S (2010) Climatological aspects of the optical properties of fine/coarse mode aerosol mixtures. J Geophys Res Atmos 115 (D19) Flores JM (2011) Laboratory study on the optical properties of absorbing atmospheric aerosols and field applications. Dissertation, der Johannes Gutenberg Universität Mainz, Germany Generoso S, Bey I, Labonne M, Breon FM (2008) Aerosol vertical distribution in dust outflow over the Atlantic: comparisons between GEOS-Chem and Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO). J Geophys Res 113:D24209. doi:10.1029/2008JD010154 Gillette DA, Walker TR (1977) Characteristics of airborne particles produced by wind erosion of sandy soil, high plains of west Texas. Soil Sci 123:97–110 Goudie A, Middleton NJ (2006) Desert dust in the global system. Springer Science and Business Media Greeley R, Viersen JD (1985) Wind as a geological process on Earth, Mars, Venus and Titan. Cambridge Univ. Press, New York Hammer E (2011) Calculation and interpretation of cloud peak super saturations at the Jungfraujoch. Dissertation, University of Bern Hinkle DE, Wiersma W, Jurs SG (2003) Applied statistics for the behavioral sciences. Mass. Houghton Mifflin, London Johnston K, Ver Hoef JM, Krivoruchko K, Lucas N (2001) Using ArcGIS Geostatistical Analyst, 380. ESRI Press, Redlands, California Kaskaoutis D, Kambezidis H (2006) Investigation into the wavelength dependence of the aerosol optical depth in the Athens area. Q J R Meteorol Soc 132:2217–2234 Kedia S, Ramachandran S, Holben BN, Tripathi S (2014) Quantitation of aerosol type, and sources of aerosols over the Indo-Gangetic Plain. Atmos Environ 98:607–619 Kok JF, Renno NO (2009a) A comprehensive numerical model of steady state saltation (COMSALT). J Geophys Res 114:D17204 Kok JF, Renno NO (2006) Enhancement of emission of mineral dust aerosol by electric forces. Geophys Res Lett 33:L19S10 Levelt PF, Hilsenrath E, Leppelmeier GW, Van den Oord GH, Bhartia PK, Tamminen J, De Haan JF, Veefkind JP (2006) Science objectives of the Ozone Monitoring Instrument. IEEE Trans Geosci Remote Sens 44:1199–1120 Li J (2011) Improving our understanding of atmospheric aerosols and their climate effects: implications for satellite retrievals and GCM simulations. Ph.D. Dissertation, Columbia University Liu H (2005) Global scale aerosol properties: implications for surface shortwave radiation budget. Dissertation, University of Maryland, College Park Marticorena B, Bergametti G (1995) Modeling the atmospheric dust cycle: 1. Design of a soil-derived dust emission scheme. Journal of Geophysical Research: Atmospheres 100:16415–16430 Masoumi A, Bayat A, Khalesifard HR (2010) Columnar aerosol size distribution function obtained by inversion of spectral optical depth measurements for the Zanjan, Iran. Atmospheric Measurement Techniques Discussions 3:2367–2387 McCoy J, Johnston K (2001) Using ArcGIS Spatial Analyst. ESRI Press, Redlands, California Müller D, Weinzierl B, Petzold A, Kandler K, Ansmann A, Müller T, Tesche M, Freudenthaler V, Esselborn M, Heese B et al (2010) Mineral dust observed with AERONET Sun photometer, Raman lidar, and in situ instruments during SAMUM 2006: shape-independent particle properties. J Geophys Res Atmos 115(D7) NASA DISC G (2016) Giovanni online user’s manual. URL: http://disc.sci.gsfc.nasa.gov/giovanni/additional/users-manual/G3_manual_Chapter_19_AOT_comparison/. Accessed 21 July 2016 OMI (2016) Ozone Monitoring Instrument. http://projects.knmi.nl/omi/research/product/. Accessed 21 July 2016 Prospero JM, Ginoux P, Torres O, Nicholson SE, Gill TE (2002) Environmental characterization of global sources of atmospheric soil dust identified with the Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product. Reviews of Geophysics 40(1) Publishing BE (2011) Iraq (Middle East: region in transition). Britannica Educational Publishing, US Renno NO, Abreu VJ, Koch J et al (2004) A pilot field experiment on convective plumes and dust devil. J Geophys Res 109:E07001. doi:10.1029/2003JE002219 Satheesh S, Moorthy KK (2005) Radiative effects of natural aerosols: a review. Atmos Environ 39:2089–2110 Schmidt DS, Schmidt RA (1998) Electrostatic force on a saltating sand. J Geophys Res 103:8997–9001 Seinfeld JH, Pandis SN (2006) Atmospheric chemistry and physics: from air pollution to climate change. John Wiley and Sons, New York Shao Y, Dong C (2006) A review on East Asian dust storm climate, modeling and monitoring. Glob Planet Chang 52:1–22 Shao YP (2008) Physics and modeling of wind erosion. Springer, Heidelberg Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt K, Tignor M, Miller H (2007) Climate change 2007: the physical science basis: Working Group I contribution to the fourth assessment report of the IPCC (vol. 4). Cambridge University Press Stier P, Seinfeld JH, Kinne S, Boucher O (2007) Aerosol absorption and radiative forcing. Atmos Chem Phys 7:5237–5261 Stow CD (1969) Dust and sand storm electrification. Weather 24:134–137 Tegen I, Lacis AA, Fung I (1996) The influence on climate forcing of mineral aerosols from disturbed soils. Nature 380:419–422 Thalen DCP (1979) Ecology and utilization of desert shrub rangelands in Iraq. Springer Science and Business Media Thomas DS (2011) Arid zone geomorphology: process, form and change in dry lands. Wiley, University of Bern Wallace JM, Hobbs PV (2006) Atmospheric science: an introductory survey, volume 92. Academic Press Weiss NA (2011) Elementary statistics. Addison Wesley Zhao TL, Gong SL, Zhang XY, McKendry IG (2003) Modeled size-segregated wet and dry deposition budgets of soil dust aerosol during ACE-Asia 2001: implications for trans-pacific transport. J Geophys Res Atmos 108(D23) Zou KH, Tuncali K, Silverman SG (2003) Correlation and simple linear regression. Radiology 227:617–628