Abstract
WHEN ‘dry-ice’ pellets, or other suitable nucleation agents, are introduced into a cloud of supercooled water droplets, large numbers of ice crystals are formed1. These ice crystals grow at the expense of the water droplets and are generally precipitated.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
See, for example, Schaefer, Science, 104, No. 2707 (1946).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
FRITH, R. Details of Wind Structure Revealed by Artificial Nucleation of Supercooled Clouds. Nature 165, 899–900 (1950). https://doi.org/10.1038/165899b0
Issue Date:
DOI: https://doi.org/10.1038/165899b0
Comments
By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.