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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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The abundance of freezing nuclei in water samples is routinely determined by experiments involving the cooling of sample drops and observing the temperatures at which the drops freeze. This is used for characterizing the nucleating abilities of materials in laboratory preparations or to determine the numbers of nucleating particles in rain, snow, river water or other natural waters. The evaluation of drop-freezing experiments in terms of differential nucleus spectra is advocated in the paper.
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AMT | Articles | Volume 12, issue 2
AMT | Articles | Volume 12, issue 2
Atmos. Meas. Tech., 12, 1219–1231, 2019
https://doi.org/10.5194/amt-12-1219-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Meas. Tech., 12, 1219–1231, 2019
https://doi.org/10.5194/amt-12-1219-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
AMT | Articles | Volume 12, issue 2

Research article 26 Feb 2019

Research article | 26 Feb 2019

Revisiting the differential freezing nucleus spectra derived from drop-freezing experiments: methods of calculation, applications, and confidence limits

Gabor Vali

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Short summary
The abundance of freezing nuclei in water samples is routinely determined by experiments involving the cooling of sample drops and observing the temperatures at which the drops freeze. This is used for characterizing the nucleating abilities of materials in laboratory preparations or to determine the numbers of nucleating particles in rain, snow, river water or other natural waters. The evaluation of drop-freezing experiments in terms of differential nucleus spectra is advocated in the paper.
Read more
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Atmospheric Measurement Techniques

An interactive open-access journal of the European Geosciences Union

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