scholarly journals Spatio-Temporal Identification of Areas Suitable for West Nile Disease in the Mediterranean Basin and Central Europe

PLoS ONE ◽  
2015 ◽  
Vol 10 (12) ◽  
pp. e0146024 ◽  
Author(s):  
Annamaria Conte ◽  
Luca Candeloro ◽  
Carla Ippoliti ◽  
Federica Monaco ◽  
Fabrizio De Massis ◽  
...  
2006 ◽  
Vol 951 (1) ◽  
pp. 117-126 ◽  
Author(s):  
B. MURGUE ◽  
S. MURRI ◽  
H. TRIKI ◽  
V. DEUBEL ◽  
H. G. ZELLER

2010 ◽  
Vol 4 (2) ◽  
pp. 29-37 ◽  
Author(s):  
Paolo Calistri ◽  
Armando Giovannini ◽  
Zdenek Hubalek ◽  
Aurelia Ionescu ◽  
Federica Monaco ◽  
...  

2020 ◽  
Vol 13 (12) ◽  
pp. 5897-5915
Author(s):  
Laura Palacios-Peña ◽  
Jerome D. Fast ◽  
Enrique Pravia-Sarabia ◽  
Pedro Jiménez-Guerrero

Abstract. The size distribution of atmospheric aerosols plays a key role for understanding and quantifying the uncertainties related to aerosol–radiation and aerosol–cloud interactions. These interactions ultimately depend on the size distribution through optical properties (such as aerosol optical depth, AOD) or cloud microphysical properties. Hence, the main objective of this contribution is to disentangle the impact of the representation of aerosol size distribution on aerosol optical properties over central Europe, particularly over the Mediterranean Basin, during a summertime aerosol episode. To fulfill this objective, a sensitivity test has been conducted using the coupled chemistry–meteorology model WRF-Chem (Weather Research Forecast model coupled with Chemistry). The test modified the parameters defining a lognormal size distribution (geometric diameter and standard deviation) by 10 %, 20 %, and 50 %. Results reveal that the reduction in the standard deviation of the accumulation mode leads to the largest impacts on AOD due to a transfer of particles from the accumulation mode to the coarse mode. A reduction in the geometric diameter of the accumulation mode also has an influence on AOD representation since particles in this mode are assumed to be smaller. In addition, an increase in the geometric diameter of the coarse mode produces a redistribution through the total size distribution by relocating particles from the finer modes to the coarse.


2020 ◽  
Author(s):  
Laura Palacios-Peña ◽  
Jerome D. Fast ◽  
Enrique Pravia-Sarabia ◽  
Pedro Jiménez-Guerrero

Abstract. Aerosol size distribution is, among others, a key property of atmospheric aerosols when trying to establish the uncertainties related to aerosol-radiation (ARI) and aerosol-clouds (ACI) interactions. These interactions ultimately depend on the size distribution through optical properties as aerosol optical depth (AOD) or cloud microphysical properties. Hence, the main objective of this work is to study the impact of the representation of aerosol size distribution on aerosol optical properties over Central Europe, and particularly over the Mediterranean Basin during a summertime aerosol episode. To fulfill this objective, a sensitivity test has been carried out using the WRF-Chem on-line model. The test consisted on modifying the parameters which define a log-normal size distribution (the geometric diameter, from now on DG, and the standard deviation, SG) by 10, 20 and 50 %. Results reveal that the reduction in the SG of the accumulation mode leads to the largest impacts in the AOD representation due to a transfer of particles from the accumulation mode to the coarse mode. A reduction in the DG of the accumulation mode has also an influence on AOD representation since particles in this mode are assumed to be smaller. In addition, an increase in the DG of the coarse mode produces a redistribution through the total size distribution by relocating particles from the finer modes to the coarse.


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