Hooper and Arvelius (2000): Monitoring of the Arctic winter tropopause 1 Monitoring of the Arctic winter tropopause: a comparison of radiosonde, ozonesonde and MST radar observations.

VHF radar return signal strength for a vertically directed beam, PRAD, is approximately proportional to M2=r2- see, e.g., Low et al. (1998)- where M is the vertical gradient of generalised potential refractive index, and r is the range from the radar. Above the rst few km of the atmosphere, where th...

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Main Authors: D. A. Hooper, J. Arvelius
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Arctic
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9879
http://home.badc.rl.ac.uk/dahooper/PUBLICATIONS/proc-mst9_hooper-and-arvelius_tropopause.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.581.9879 2023-05-15T14:44:32+02:00 Hooper and Arvelius (2000): Monitoring of the Arctic winter tropopause 1 Monitoring of the Arctic winter tropopause: a comparison of radiosonde, ozonesonde and MST radar observations. D. A. Hooper J. Arvelius The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9879 http://home.badc.rl.ac.uk/dahooper/PUBLICATIONS/proc-mst9_hooper-and-arvelius_tropopause.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9879 http://home.badc.rl.ac.uk/dahooper/PUBLICATIONS/proc-mst9_hooper-and-arvelius_tropopause.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://home.badc.rl.ac.uk/dahooper/PUBLICATIONS/proc-mst9_hooper-and-arvelius_tropopause.pdf text ftciteseerx 2016-08-28T00:02:12Z VHF radar return signal strength for a vertically directed beam, PRAD, is approximately proportional to M2=r2- see, e.g., Low et al. (1998)- where M is the vertical gradient of generalised potential refractive index, and r is the range from the radar. Above the rst few km of the atmosphere, where the contributions Text Arctic Unknown Arctic
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description VHF radar return signal strength for a vertically directed beam, PRAD, is approximately proportional to M2=r2- see, e.g., Low et al. (1998)- where M is the vertical gradient of generalised potential refractive index, and r is the range from the radar. Above the rst few km of the atmosphere, where the contributions
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author D. A. Hooper
J. Arvelius
spellingShingle D. A. Hooper
J. Arvelius
Hooper and Arvelius (2000): Monitoring of the Arctic winter tropopause 1 Monitoring of the Arctic winter tropopause: a comparison of radiosonde, ozonesonde and MST radar observations.
author_facet D. A. Hooper
J. Arvelius
author_sort D. A. Hooper
title Hooper and Arvelius (2000): Monitoring of the Arctic winter tropopause 1 Monitoring of the Arctic winter tropopause: a comparison of radiosonde, ozonesonde and MST radar observations.
title_short Hooper and Arvelius (2000): Monitoring of the Arctic winter tropopause 1 Monitoring of the Arctic winter tropopause: a comparison of radiosonde, ozonesonde and MST radar observations.
title_full Hooper and Arvelius (2000): Monitoring of the Arctic winter tropopause 1 Monitoring of the Arctic winter tropopause: a comparison of radiosonde, ozonesonde and MST radar observations.
title_fullStr Hooper and Arvelius (2000): Monitoring of the Arctic winter tropopause 1 Monitoring of the Arctic winter tropopause: a comparison of radiosonde, ozonesonde and MST radar observations.
title_full_unstemmed Hooper and Arvelius (2000): Monitoring of the Arctic winter tropopause 1 Monitoring of the Arctic winter tropopause: a comparison of radiosonde, ozonesonde and MST radar observations.
title_sort hooper and arvelius (2000): monitoring of the arctic winter tropopause 1 monitoring of the arctic winter tropopause: a comparison of radiosonde, ozonesonde and mst radar observations.
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9879
http://home.badc.rl.ac.uk/dahooper/PUBLICATIONS/proc-mst9_hooper-and-arvelius_tropopause.pdf
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source http://home.badc.rl.ac.uk/dahooper/PUBLICATIONS/proc-mst9_hooper-and-arvelius_tropopause.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.9879
http://home.badc.rl.ac.uk/dahooper/PUBLICATIONS/proc-mst9_hooper-and-arvelius_tropopause.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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