Sampling of noctilucent cloud particles
Sampling of noctilucent cloud particles by means of sounding rockets has been successfully carried out from northern Sweden in the Summer of 1962. Two successful flights were achieved, one in the presence of noctilucent clouds and one when no such clouds could be visually observed from the ground or...
Published in: | Tellus A: Dynamic Meteorology and Oceanography |
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Format: | Article in Journal/Newspaper |
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Stockholm University Press
1964
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Online Access: | http://dx.doi.org/10.3402/tellusa.v16i1.8883 https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/download/3274/6413 |
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crstockholmup:10.3402/tellusa.v16i1.8883 2024-06-02T08:12:12+00:00 Sampling of noctilucent cloud particles Hemenway, C. L. Soberman, R. K. Witt, G. 1964 http://dx.doi.org/10.3402/tellusa.v16i1.8883 https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/download/3274/6413 unknown Stockholm University Press https://creativecommons.org/licenses/by/4.0 Tellus A: Dynamic Meteorology and Oceanography volume 16, issue 1, page 84-88 ISSN 1600-0870 journal-article 1964 crstockholmup https://doi.org/10.3402/tellusa.v16i1.8883 2024-05-07T14:17:30Z Sampling of noctilucent cloud particles by means of sounding rockets has been successfully carried out from northern Sweden in the Summer of 1962. Two successful flights were achieved, one in the presence of noctilucent clouds and one when no such clouds could be visually observed from the ground or from aircraft. The collecting surfaces were exposed between the altitudes of approximately 75 and 98 kilometers during ascent only. The particle concentration in a vertical column through the noctilucent cloud display is found to be greater than 8 × 1010 particles per square meter which is at least one thousand times greater than in the case when no clouds were observed. The integral size distribution of the cloud particles is of the form N = Ad-p where 3 < p < 4. A significant fraction of the collected cloud particles had a volatile coating prior to collection. The particles were analyzed by electron diffraction, neutron activation, and electron beam microprobe techniques. Electron-beam microprobe analysis has given evidence for iron particles with high nickel content. Calcium films were used as indicators of moisture associated with the collected particles. Study of the exposed and unexposed films flown in the sampling experiments has revealed evidence for moisture. Laboratory simulation of a ring- or halo-patterns found in the electron microscopic examination of the noctilucent cloud particles has been attempted. This was done by impacting ice-coated nickel particles on collecting surfaces similar to those used in the sampling experiment. Ring patterns similar to those observed on the rocket sampling surfaces have been produced. The primary conclusions are that the cloud particles are probably of extraterrestrial origin and that a significant fraction appears to have been coated with terrestrial ice. Plans for future experiments are briefly outlined. Article in Journal/Newspaper Northern Sweden Stockholm University Press Tellus A: Dynamic Meteorology and Oceanography 16 1 84 88 |
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Open Polar |
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Stockholm University Press |
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crstockholmup |
language |
unknown |
description |
Sampling of noctilucent cloud particles by means of sounding rockets has been successfully carried out from northern Sweden in the Summer of 1962. Two successful flights were achieved, one in the presence of noctilucent clouds and one when no such clouds could be visually observed from the ground or from aircraft. The collecting surfaces were exposed between the altitudes of approximately 75 and 98 kilometers during ascent only. The particle concentration in a vertical column through the noctilucent cloud display is found to be greater than 8 × 1010 particles per square meter which is at least one thousand times greater than in the case when no clouds were observed. The integral size distribution of the cloud particles is of the form N = Ad-p where 3 < p < 4. A significant fraction of the collected cloud particles had a volatile coating prior to collection. The particles were analyzed by electron diffraction, neutron activation, and electron beam microprobe techniques. Electron-beam microprobe analysis has given evidence for iron particles with high nickel content. Calcium films were used as indicators of moisture associated with the collected particles. Study of the exposed and unexposed films flown in the sampling experiments has revealed evidence for moisture. Laboratory simulation of a ring- or halo-patterns found in the electron microscopic examination of the noctilucent cloud particles has been attempted. This was done by impacting ice-coated nickel particles on collecting surfaces similar to those used in the sampling experiment. Ring patterns similar to those observed on the rocket sampling surfaces have been produced. The primary conclusions are that the cloud particles are probably of extraterrestrial origin and that a significant fraction appears to have been coated with terrestrial ice. Plans for future experiments are briefly outlined. |
format |
Article in Journal/Newspaper |
author |
Hemenway, C. L. Soberman, R. K. Witt, G. |
spellingShingle |
Hemenway, C. L. Soberman, R. K. Witt, G. Sampling of noctilucent cloud particles |
author_facet |
Hemenway, C. L. Soberman, R. K. Witt, G. |
author_sort |
Hemenway, C. L. |
title |
Sampling of noctilucent cloud particles |
title_short |
Sampling of noctilucent cloud particles |
title_full |
Sampling of noctilucent cloud particles |
title_fullStr |
Sampling of noctilucent cloud particles |
title_full_unstemmed |
Sampling of noctilucent cloud particles |
title_sort |
sampling of noctilucent cloud particles |
publisher |
Stockholm University Press |
publishDate |
1964 |
url |
http://dx.doi.org/10.3402/tellusa.v16i1.8883 https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/download/3274/6413 |
genre |
Northern Sweden |
genre_facet |
Northern Sweden |
op_source |
Tellus A: Dynamic Meteorology and Oceanography volume 16, issue 1, page 84-88 ISSN 1600-0870 |
op_rights |
https://creativecommons.org/licenses/by/4.0 |
op_doi |
https://doi.org/10.3402/tellusa.v16i1.8883 |
container_title |
Tellus A: Dynamic Meteorology and Oceanography |
container_volume |
16 |
container_issue |
1 |
container_start_page |
84 |
op_container_end_page |
88 |
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1800758576707272704 |