Condensation nuclei counts

This is a graph of looking at condensation nuclei counts. This is looking at the vertical scale as a log of the number. The log of the number meaning a two would be on the order of what we’re talking about as a hundred. So during the summertime, we have the high levels. The summertime, remember, is...

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Online Access:http://cdm16786.contentdm.oclc.org:80/cdm/ref/collection/antartica/id/37
id ftuwashingtonlib:oai:cdm16786.contentdm.oclc.org:antartica/37
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spelling ftuwashingtonlib:oai:cdm16786.contentdm.oclc.org:antartica/37 2023-05-15T13:45:54+02:00 Condensation nuclei counts http://cdm16786.contentdm.oclc.org:80/cdm/ref/collection/antartica/id/37 unknown zolantarc30 http://cdm16786.contentdm.oclc.org:80/cdm/ref/collection/antartica/id/37 ftuwashingtonlib 2017-12-31T16:12:15Z This is a graph of looking at condensation nuclei counts. This is looking at the vertical scale as a log of the number. The log of the number meaning a two would be on the order of what we’re talking about as a hundred. So during the summertime, we have the high levels. The summertime, remember, is January, February, March, October, November, December. We usually would go down in late October and spend November, December, January, and February down there and then return in late February, early March. But during the summertime, the condensation nuclei counts are approximately a hundred per cubic meter. When we go to the wintertime, they drop down well below ten and sometimes down in less than two or three particles per cubic centimeter. So they get extremely low levels during the Antarctic wintertime, higher levels during the summertime; and this is all due to transport, mainly of sea salt, from the oceans surrounding Antarctica and some from continents around Antarctica. Other/Unknown Material Antarc* Antarctic Antarctica University of Washington, Seattle: Digital Collections Antarctic The Antarctic
institution Open Polar
collection University of Washington, Seattle: Digital Collections
op_collection_id ftuwashingtonlib
language unknown
description This is a graph of looking at condensation nuclei counts. This is looking at the vertical scale as a log of the number. The log of the number meaning a two would be on the order of what we’re talking about as a hundred. So during the summertime, we have the high levels. The summertime, remember, is January, February, March, October, November, December. We usually would go down in late October and spend November, December, January, and February down there and then return in late February, early March. But during the summertime, the condensation nuclei counts are approximately a hundred per cubic meter. When we go to the wintertime, they drop down well below ten and sometimes down in less than two or three particles per cubic centimeter. So they get extremely low levels during the Antarctic wintertime, higher levels during the summertime; and this is all due to transport, mainly of sea salt, from the oceans surrounding Antarctica and some from continents around Antarctica.
title Condensation nuclei counts
spellingShingle Condensation nuclei counts
title_short Condensation nuclei counts
title_full Condensation nuclei counts
title_fullStr Condensation nuclei counts
title_full_unstemmed Condensation nuclei counts
title_sort condensation nuclei counts
url http://cdm16786.contentdm.oclc.org:80/cdm/ref/collection/antartica/id/37
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation zolantarc30
http://cdm16786.contentdm.oclc.org:80/cdm/ref/collection/antartica/id/37
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