Artificial Cloud Formation in the Atmosphere

An artificial cloud in the cloudless atmosphere at a temperature below 0°C was formed by introducing pellets of Dry Ice into air containing more water vapor than would be present at the saturation point with respect to ice. Such clouds could be utilized to establish radiative equilibrium between gro...

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Bibliographic Details
Published in:Science
Main Authors: Jayaweera, K. O. L. F., Ohtake, Takeshi
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1972
Subjects:
Arctic
Online Access:http://dx.doi.org/10.1126/science.178.4060.504
https://www.science.org/doi/pdf/10.1126/science.178.4060.504
id craaas:10.1126/science.178.4060.504
record_format openpolar
spelling craaas:10.1126/science.178.4060.504 2024-06-09T07:43:43+00:00 Artificial Cloud Formation in the Atmosphere Jayaweera, K. O. L. F. Ohtake, Takeshi 1972 http://dx.doi.org/10.1126/science.178.4060.504 https://www.science.org/doi/pdf/10.1126/science.178.4060.504 en eng American Association for the Advancement of Science (AAAS) Science volume 178, issue 4060, page 504-505 ISSN 0036-8075 1095-9203 journal-article 1972 craaas https://doi.org/10.1126/science.178.4060.504 2024-05-16T12:55:23Z An artificial cloud in the cloudless atmosphere at a temperature below 0°C was formed by introducing pellets of Dry Ice into air containing more water vapor than would be present at the saturation point with respect to ice. Such clouds could be utilized to establish radiative equilibrium between ground and air so as to inhibit the cooling of selective arctic surface regions under clear skies. Article in Journal/Newspaper Arctic AAAS Resource Center (American Association for the Advancement of Science) Arctic Science 178 4060 504 505
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description An artificial cloud in the cloudless atmosphere at a temperature below 0°C was formed by introducing pellets of Dry Ice into air containing more water vapor than would be present at the saturation point with respect to ice. Such clouds could be utilized to establish radiative equilibrium between ground and air so as to inhibit the cooling of selective arctic surface regions under clear skies.
format Article in Journal/Newspaper
author Jayaweera, K. O. L. F.
Ohtake, Takeshi
spellingShingle Jayaweera, K. O. L. F.
Ohtake, Takeshi
Artificial Cloud Formation in the Atmosphere
author_facet Jayaweera, K. O. L. F.
Ohtake, Takeshi
author_sort Jayaweera, K. O. L. F.
title Artificial Cloud Formation in the Atmosphere
title_short Artificial Cloud Formation in the Atmosphere
title_full Artificial Cloud Formation in the Atmosphere
title_fullStr Artificial Cloud Formation in the Atmosphere
title_full_unstemmed Artificial Cloud Formation in the Atmosphere
title_sort artificial cloud formation in the atmosphere
publisher American Association for the Advancement of Science (AAAS)
publishDate 1972
url http://dx.doi.org/10.1126/science.178.4060.504
https://www.science.org/doi/pdf/10.1126/science.178.4060.504
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Science
volume 178, issue 4060, page 504-505
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.178.4060.504
container_title Science
container_volume 178
container_issue 4060
container_start_page 504
op_container_end_page 505
_version_ 1801372590404534272

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