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The main activity concerns the development and subsequent application of numerical modeling for VIA studies, i.e. the upgrading of our ISAC-TO dispersion models (SPRAY, MicroSPRAY, MIRS and MILORD), the development of new modules, the verifies them and, finally, their application to ISAC-TO cases of interest. Considering that the sites where weak wind is prevalent (or in any case present in non-negligible percentages of time) the study of dispersion is particularly interesting, I also intend to continue the study of these situations and their dispersive capacities. This part of the study will be based on the analysis of five data sets in our possession: UTP (measured in the urban environment, Turin, in the UTP research project); Tisby (Sweden, measured in a flat area with no significant obstacles), Graz (measured in complex terrain on the outskirts of Graz, Austria), Antartica (measured at the Nancen Ice Sheet site during the 1993-94 campaign) and Amazonia (Brazil, measured in flat terrain with no significant obstacles at approximately 2 degrees south latitude ). In particular, I will continue the analysis of the power spectra, which provide the estimate of how the variance is distributed as a function of frequency, in the various stability conditions. Also in this case I will study the changes to be made to the literature reports to take into account what happens in the case of light wind. In particular, I will continue the analysis of the power spectra, which provide the estimate of how the variance is distributed as a function of frequency, in the various stability conditions. Also in this case I will study the changes to be made to the literature reports to take into account what happens in the case of light wind. In particular, I will continue the analysis of the power spectra, which provide the estimate of how the variance is distributed as a function of frequency, in the various stability conditions. Also in this case I will study the changes to be made to the literature reports to take into account what happens in the case of light wind.
The main activity concerns the development and subsequent application of numerical modeling for VIA studies, i.e. the upgrading of our ISAC-TO dispersion models (SPRAY, MicroSPRAY, MIRS and MILORD), the development of new modules, the verifies them and, finally, their application to ISAC-TO cases of interest. Considering that the sites where weak wind is prevalent (or in any case present in non-negligible percentages of time) the study of dispersion is particularly interesting, I also intend to continue the study of these situations and their dispersive capacities. This part of the study will be based on the analysis of five data sets in our possession: UTP (measured in the urban environment, Turin, in the UTP research project); Tisby (Sweden, measured in a flat area with no significant obstacles), Graz (measured in complex terrain on the outskirts of Graz, Austria), Antartica (measured at the Nancen Ice Sheet site during the 1993-94 campaign) and Amazonia (Brazil, measured in flat terrain with no significant obstacles at approximately 2 degrees south latitude ). In particular, I will continue the analysis of the power spectra, which provide the estimate of how the variance is distributed as a function of frequency, in the various stability conditions. Also in this case I will study the changes to be made to the literature reports to take into account what happens in the case of light wind. In particular, I will continue the analysis of the power spectra, which provide the estimate of how the variance is distributed as a function of frequency, in the various stability conditions. Also in this case I will study the changes to be made to the literature reports to take into account what happens in the case of light wind. In particular, I will continue the analysis of the power spectra, which provide the estimate of how the variance is distributed as a function of frequency, in the various stability conditions. Also in this case I will study the changes to be made to the literature reports to take into account what happens in the case of light wind.
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EGU General Assembly Conference Abstractspp.8497, (2017)
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