JP2.26 CLIMATOLOGY OF THE WINTER SURFACE TEMPERATURE INVERSION IN
The surface temperature inversion in the subarctic setting of Fairbanks, Alaska has been investigated. In winter the inversion is strong and semi-permanent; it separates the boundary layer from the air aloft and has great importance for pollution levels in town. We analyzed the changes that have occ...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.496.8195 2023-05-15T18:28:16+02:00 JP2.26 CLIMATOLOGY OF THE WINTER SURFACE TEMPERATURE INVERSION IN Brian Hartmann Gerd Wendler The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.496.8195 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.496.8195 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://ams.confex.com/ams/pdfpapers/84504.pdf text ftciteseerx 2016-01-08T08:49:18Z The surface temperature inversion in the subarctic setting of Fairbanks, Alaska has been investigated. In winter the inversion is strong and semi-permanent; it separates the boundary layer from the air aloft and has great importance for pollution levels in town. We analyzed the changes that have occurred since radiosonde measurements began in 1957. For the time period from 1957 to 2004 a strong warming trend was observed in Fairbanks; the winter mean surface temperatures have increased by 3.3°C, more than for any other season. The climatology of the surface-based temperature inversion is examined by analyzing the twice-daily radiosondes for Text Subarctic Alaska Unknown Fairbanks |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
description |
The surface temperature inversion in the subarctic setting of Fairbanks, Alaska has been investigated. In winter the inversion is strong and semi-permanent; it separates the boundary layer from the air aloft and has great importance for pollution levels in town. We analyzed the changes that have occurred since radiosonde measurements began in 1957. For the time period from 1957 to 2004 a strong warming trend was observed in Fairbanks; the winter mean surface temperatures have increased by 3.3°C, more than for any other season. The climatology of the surface-based temperature inversion is examined by analyzing the twice-daily radiosondes for |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Brian Hartmann Gerd Wendler |
spellingShingle |
Brian Hartmann Gerd Wendler JP2.26 CLIMATOLOGY OF THE WINTER SURFACE TEMPERATURE INVERSION IN |
author_facet |
Brian Hartmann Gerd Wendler |
author_sort |
Brian Hartmann |
title |
JP2.26 CLIMATOLOGY OF THE WINTER SURFACE TEMPERATURE INVERSION IN |
title_short |
JP2.26 CLIMATOLOGY OF THE WINTER SURFACE TEMPERATURE INVERSION IN |
title_full |
JP2.26 CLIMATOLOGY OF THE WINTER SURFACE TEMPERATURE INVERSION IN |
title_fullStr |
JP2.26 CLIMATOLOGY OF THE WINTER SURFACE TEMPERATURE INVERSION IN |
title_full_unstemmed |
JP2.26 CLIMATOLOGY OF THE WINTER SURFACE TEMPERATURE INVERSION IN |
title_sort |
jp2.26 climatology of the winter surface temperature inversion in |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.496.8195 |
geographic |
Fairbanks |
geographic_facet |
Fairbanks |
genre |
Subarctic Alaska |
genre_facet |
Subarctic Alaska |
op_source |
https://ams.confex.com/ams/pdfpapers/84504.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.496.8195 |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766210663491829760 |