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    Aging of Accreted Ice 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 006:;page 1375
    Author(s): Prodi, F.; Levi, L.
    Publisher: American Meteorological Society
    Abstract: The effect of annealing in accreted ice has been investigated for artificially grown ice deposits after ?100 days of storage in a deep freeze unit. Cross sections of the cylindrical deposits have been cut and replicated ...
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    Crystal Size in Ice Grown by Droplet Accretion 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 011:;page 2181
    Author(s): Levi, L.; Prodi, F.
    Publisher: American Meteorological Society
    Abstract: The size of crystal grains in ice formed by accretion of supercooled droplets has been determined for a wide range of air (?11 to ?25°C) and deposit (0 to ?16°C) temperatures. At air temperatures of ?14°C and below, the ...
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    A Study of the Effect of Size on Ice Nucleation in the Aerodynamic Range of Particles 

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 007:;page 945
    Author(s): Prodi, F.; Santachiara, G.; Prodi, V.
    Publisher: American Meteorological Society
    Abstract: The effect of size on ice nucleation has been experimentally investigated for aerosol particles in the aerodynamic range. Aerosol particles are separated according to their aerodynamic diameter while airborne and deposited ...
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    A Preliminary Study of Ice Grown by Droplet Accretion Using Water-Insoluble Particles as Tracer 

    Source: Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 003:;page 284
    Author(s): Prodi, F.; Nagamoto, C. T.; Rosinski, J.
    Publisher: American Meteorological Society
    Abstract: The migration of water-insoluble particles during freezing was used to study the structure of ice grown by droplet accretion. Experiments were performed in a cold tunnel under different growth conditions using nickel powder ...
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    Natural Tracer Distribution in Hailstones 

    Source: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 001:;page 148
    Author(s): Vittori, O.; Prodi, F.; Morgan, G.; Cesari, G.
    Publisher: American Meteorological Society
    Abstract: Preliminary results of a chemical analysis of hailstone slice residues are reported. The radial pattern of Fe particles shows a marked outer ring of relatively high concentration. The possible causes are discussed and it ...
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    Crystal Size and Orientation in Ice Grown by Droplet Accretion in Wet and Spongy Regimes 

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 010:;page 2301
    Author(s): Prodi, F.; Levi, L.; Franzini, A.; Scarani, C.
    Publisher: American Meteorological Society
    Abstract: The size and orientation of crystal grains in wet and spongy ice formed by accretion of supercooled droplets has been determined in a wide range of air temperatures (?8 to ?25°C). Particular care has been taken in reducing ...
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    An Experimental Technique to Study the Effect of Size on Ice Nucleation 

    Source: Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 012:;page 1448
    Author(s): Prodi, F.; Santachiara, G.; Prodi, V.; Zaiacomo, T. De
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Natural Ice-Forming Nuclei in Severe Convective Storms 

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 003:;page 391
    Author(s): Rosinski, J.; Langer, G.; Nagamoto, C. T.; Kerrigan, T. C.; Prodi, F.
    Publisher: American Meteorological Society
    Abstract: There are two populations of aerosol particles in severe storms: normal background aerosol and aerosolized soil particles. Concentration of the latter, which depends on local wind speed and soil conditions, may be orders ...
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