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Abstract
Drop freezing experiments with ammonium sulfate water solutions have shown the existence of the temperature maxima that are a function of the salt concentration.The maxima were:-12℃ for 10-4 M solution on filter,-9℃ for 10-4 to 10-3M solution in contact with particles of continental origin,and-4℃ for 10-4 M solution in contact with particles of marine origin.It was speculated that the presence of ice-forming nuclei active at high temperature(-4℃) should extend the formation of ice in clouds toward lower latitudes,increase their albedos,and provide additional cooling during daytime for the earth.The microphysics of clouds must be included in studying climate.
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Citation
J. Rosinski, C. T. Nagamoto. 1994: ON THE ROLE OF SULFATE ION IN THE ATMOSPHERE. Journal of Meteorological Research, 8(4): 498-504.
J. Rosinski, C. T. Nagamoto. 1994: ON THE ROLE OF SULFATE ION IN THE ATMOSPHERE. Journal of Meteorological Research, 8(4): 498-504.
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J. Rosinski, C. T. Nagamoto. 1994: ON THE ROLE OF SULFATE ION IN THE ATMOSPHERE. Journal of Meteorological Research, 8(4): 498-504.
J. Rosinski, C. T. Nagamoto. 1994: ON THE ROLE OF SULFATE ION IN THE ATMOSPHERE. Journal of Meteorological Research, 8(4): 498-504.
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