KaydedilenlerDerginizi ekleyin

Dergiler / Atmospheric Pollution Research / 2019 / Cilt: 10 - Sayı: 4

Aerosol vertical distribution, optical properties and dust transport in the Western Mediterranean basin (case study: Summer, 2012)

Jamel BENKHALİFA
Mabrouk CHAABANE
Jean François LEON
Sayfa
1291–1298
DOI
—
🏛️Bu makalenin bibliyografik verileri ve tam metin bağlantısı DergiPark üzerinden sağlanmıştır.
DergiPark Kaydı ↗
✨

Yapay Zeka Hızlı Bakış & Çıkarımlar

AI Insight
⚡ TL;DR(1 Cümlede Hızlı Çıkarım)

The vertical distribution of theaerosol extinction coefficient reveals a complex structure with a large dust layer between 1.8 and 4.8 km AMSLhaving a rather constant extinction coefficient between 0.12 and 0.15 km−1.

📌 3 Maddede Bu Makale

🎯
Amaç & Hipotez:In this paper, we have analyzed an intense dust event at the end of June 2012 crossing the westernMediterranean basin and reaching southern Europe.
📊
Temel Bulgular & Veri:On average for the summer 2012, all satelliteAOD derived from MODIS, MISR, SEVIRI and OMI are consistent, while OMI tends to overestimate the AOD.During late June and early July 2012, a major dust outbreak occurred over the North Atlantic and has movedtoward East to cross the Mediterranean up to Northern Italy.
💡
Sonuç & Katkı:The vertical distribution of theaerosol extinction coefficient reveals a complex structure with a large dust layer between 1.8 and 4.8 km AMSLhaving a rather constant extinction coefficient between 0.12 and 0.15 km−1.
🔬Tür:Araştırma Makalesi
📍Kapsam:2012 Verileri
⚙️Değişkenler:Alan Parametreleri

Özet

In this paper, we have analyzed an intense dust event at the end of June 2012 crossing the westernMediterranean basin and reaching southern Europe. The geographical distribution of the dust event, its origins,microphysical and optical properties as well as its vertical distribution have been investigated using satellitedata, AERONET sun photometer retrievals and lidar soundings. On average for the summer 2012, all satelliteAOD derived from MODIS, MISR, SEVIRI and OMI are consistent, while OMI tends to overestimate the AOD.During late June and early July 2012, a major dust outbreak occurred over the North Atlantic and has movedtoward East to cross the Mediterranean up to Northern Italy. Satellite and Sun photometer AOD time series havecaptured this event. Dust event is clearly identified in the AERONET observations using a classification of thecoarse mode AOD and the total AOD. The size distributions of this event observed at the different AERONETstations from Northern Africa to Europe don't show a significant change due to sedimentation and the opticalproperties correspond to an aged dust event, as confirmed by the backtrajectories. The vertical distribution of theaerosol extinction coefficient reveals a complex structure with a large dust layer between 1.8 and 4.8 km AMSLhaving a rather constant extinction coefficient between 0.12 and 0.15 km−1.

🔖

Bu Makaleye Atıf Yap

BENKHALİFA, J., CHAABANE, M., LEON, J. F. (2019). Aerosol vertical distribution, optical properties and dust transport in the Western Mediterranean basin (case study: Summer, 2012). Atmospheric Pollution Research, Cilt: 10 - Sayı: 4, 1291–1298. https://ajindex.com/articles/351307

Kaynakça (7)

  1. Amiridis, V., Balis, D., Kazadzis, S., Bais, A., Giannakaki, E., Papayannis, A., Zerefos, C., 2005. Four-year aerosol observations with a Raman lidar at Thessaloniki, Greece, in the framework of European aerosol research lidar network (EARLINET). J. Geophys. Res. Atmos. 110. Ansmann, A., Müller, D., 2005. Lidar and atmospheric aerosol particles. Lidar 105–141.
  2. Antoine, D., Nobileau, D., 2006. Recent increase of Saharan dust transport over the Mediterranean Sea, as revealed from ocean color satellite (SeaWiFS) observations. J. Geophys. Res. Atmos. 111. Balis, D., Amiridis, V., Zerefos, C., Gerasopoulos, E., Andreae, M., Zanis, P., Kazantzidis, A., Kazadzis, S., Papayannis, A., 2003. Raman lidar and sunphotometric measurements of aerosol optical properties over Thessaloniki, Greece during a biomass burning episode. Atmos. Environ. 37, 4529–4538.
  3. Barnaba, F., Gobbi, G., 2004. Aerosol seasonal variability over the Mediterranean region and relative impact of maritime, continental and Saharan dust particles over the basin from MODIS data in the year 2001. Atmos. Chem. Phys. 4, 2367–2391.
  4. Benkhalifa, J., Léon, J.F., Chaabane, M., 2017. Aerosol optical properties of western mediterranean basin from multi-year aeronet data. J. Atmos. Sol. Terr. Phys. 164, 222–228. https://doi.org/10.1016/j.jastp.2017.08.029.
  5. Berthier, S., Chazette, P., Couvert, P., Pelon, J., Dulac, F., Thieuleux, F., Moulin, C., Pain, T., 2006. Desert dust aerosol columnar properties over ocean and continental Africa from Lidar in-Space Technology Experiment (LITE) and Meteosat synergy. J. Geophys. Res. Atmos. 1984–2012 111. D'Almeida, G.A., Koepke, P., Shettle, E.P., 1991. Atmospheric Aerosols: Global Climatology and Radiative Characteristics. A Deepak Pub. De Tomasi, F., Blanco, A., Perrone, M.R., 2003. Raman lidar monitoring of extinction and backscattering of African dust layers and dust characterization. Appl. Opt. 42, 1699–1709.
  6. Di Iorio, T., Di Sarra, A., Sferlazzo, D., Cacciani, M., Meloni, D., Monteleone, F., Fuà, D., Fiocco, G., 2009. Seasonal evolution of the tropospheric aerosol vertical profile in the central Mediterranean and role of desert dust. J. Geophys. Res. Atmos. 114. Di Sarra, A., Di Iorio, T., Cacciani, M., Fiocco, G., Fua, D., 2001. Saharan dust profiles measured by lidar at Lampedusa. J. Geophys. Res. Atmos. 106, 10335–10347 1984–2012.
  7. Dubovik, O., Holben, B., Eck, T.F., Smirnov, A., Kaufman, Y.J., King, M.D., Tanré, D., Slutsker, I., 2002. Variability of absorption and op