Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer]:
Gespeichert in:
1. Verfasser: | |
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Format: | Elektronisch E-Book |
Sprache: | German |
Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1967
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Schriftenreihe: | Mitteilungen aus dem Max-Planck-Institut für Aeronomie
29 |
Schlagworte: | |
Online-Zugang: | Volltext |
Beschreibung: | The apparatus consists of a coelostat and an infrared spectrometer coupled with an appropriate amplifier, mechanical rectifier and arecorder. The coelostat was constructed for use at stations of different geographical latitude. With this apparatus the emission spectra of the sun and the earth's atmosphere between 8 IJ. and 111J. wave-length were measured on clear days at different zenith angles of the sun and the percentage absorption and emission, respectively, of the atmospherical ozone layer were computed. Assuming the validity of the Lambert-Beer law the measured atmospherical transmission yielded the product of the absorption coefficient Ci and the total amount of ozone x ; ä is a mean absorption coefficient. In the infrared the absorption coefficient is a function of pressure P and hence of the height h above the ground. Imagine the atmosphere up to a height of 50 km to be divided into any given number of homogeneous layers, the absorption in each layer depends upon the respective absorption coefficient (Xi and the amount of ozone xi . A summation over all layers yields the total absorption which depends on the total amount of ozone x and on a mean absorption coefficient Ci. This mean absorption coefficient is defined by the equation It was shown that ii is sufficiently constant even in consideration of the seasonal variations of the total amount of ozone x . Therefore, it was possible to derive the total amount of ozone x from the measured products ii . x |
Beschreibung: | 1 Online-Ressource (45 S. 23 Abb) |
ISBN: | 9783642480072 9783540039297 |
DOI: | 10.1007/978-3-642-48007-2 |
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490 | 1 | |a Mitteilungen aus dem Max-Planck-Institut für Aeronomie |v 29 | |
500 | |a The apparatus consists of a coelostat and an infrared spectrometer coupled with an appropriate amplifier, mechanical rectifier and arecorder. The coelostat was constructed for use at stations of different geographical latitude. With this apparatus the emission spectra of the sun and the earth's atmosphere between 8 IJ. and 111J. wave-length were measured on clear days at different zenith angles of the sun and the percentage absorption and emission, respectively, of the atmospherical ozone layer were computed. Assuming the validity of the Lambert-Beer law the measured atmospherical transmission yielded the product of the absorption coefficient Ci and the total amount of ozone x ; ä is a mean absorption coefficient. In the infrared the absorption coefficient is a function of pressure P and hence of the height h above the ground. Imagine the atmosphere up to a height of 50 km to be divided into any given number of homogeneous layers, the absorption in each layer depends upon the respective absorption coefficient (Xi and the amount of ozone xi . A summation over all layers yields the total absorption which depends on the total amount of ozone x and on a mean absorption coefficient Ci. This mean absorption coefficient is defined by the equation It was shown that ii is sufficiently constant even in consideration of the seasonal variations of the total amount of ozone x . Therefore, it was possible to derive the total amount of ozone x from the measured products ii . x | ||
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Datensatz im Suchindex
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any_adam_object | |
author | Specht, Horst |
author_facet | Specht, Horst |
author_role | aut |
author_sort | Specht, Horst |
author_variant | h s hs |
building | Verbundindex |
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discipline | Physik Allgemeine Naturwissenschaft |
doi_str_mv | 10.1007/978-3-642-48007-2 |
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id | DE-604.BV042445289 |
illustrated | Not Illustrated |
indexdate | 2024-07-10T01:21:53Z |
institution | BVB |
isbn | 9783642480072 9783540039297 |
language | German |
oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-027880536 |
oclc_num | 1002258863 |
open_access_boolean | |
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owner_facet | DE-91 DE-BY-TUM DE-634 DE-92 DE-706 |
physical | 1 Online-Ressource (45 S. 23 Abb) |
psigel | ZDB-2-SNA ZDB-2-BAD ZDB-2-SNA_Archive |
publishDate | 1967 |
publishDateSearch | 1967 |
publishDateSort | 1967 |
publisher | Springer Berlin Heidelberg |
record_format | marc |
series | Mitteilungen aus dem Max-Planck-Institut für Aeronomie |
series2 | Mitteilungen aus dem Max-Planck-Institut für Aeronomie |
spelling | Specht, Horst Verfasser aut Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer] von Horst Specht Berlin, Heidelberg Springer Berlin Heidelberg 1967 1 Online-Ressource (45 S. 23 Abb) txt rdacontent c rdamedia cr rdacarrier Mitteilungen aus dem Max-Planck-Institut für Aeronomie 29 The apparatus consists of a coelostat and an infrared spectrometer coupled with an appropriate amplifier, mechanical rectifier and arecorder. The coelostat was constructed for use at stations of different geographical latitude. With this apparatus the emission spectra of the sun and the earth's atmosphere between 8 IJ. and 111J. wave-length were measured on clear days at different zenith angles of the sun and the percentage absorption and emission, respectively, of the atmospherical ozone layer were computed. Assuming the validity of the Lambert-Beer law the measured atmospherical transmission yielded the product of the absorption coefficient Ci and the total amount of ozone x ; ä is a mean absorption coefficient. In the infrared the absorption coefficient is a function of pressure P and hence of the height h above the ground. Imagine the atmosphere up to a height of 50 km to be divided into any given number of homogeneous layers, the absorption in each layer depends upon the respective absorption coefficient (Xi and the amount of ozone xi . A summation over all layers yields the total absorption which depends on the total amount of ozone x and on a mean absorption coefficient Ci. This mean absorption coefficient is defined by the equation It was shown that ii is sufficiently constant even in consideration of the seasonal variations of the total amount of ozone x . Therefore, it was possible to derive the total amount of ozone x from the measured products ii . x Physics Geography Physics, general Earth Sciences, general Geografie Mitteilungen aus dem Max-Planck-Institut für Aeronomie 29 (DE-604)BV002538099 29 https://doi.org/10.1007/978-3-642-48007-2 Verlag Volltext |
spellingShingle | Specht, Horst Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer] Mitteilungen aus dem Max-Planck-Institut für Aeronomie Physics Geography Physics, general Earth Sciences, general Geografie |
title | Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer] |
title_auth | Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer] |
title_exact_search | Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer] |
title_full | Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer] von Horst Specht |
title_fullStr | Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer] von Horst Specht |
title_full_unstemmed | Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer] von Horst Specht |
title_short | Über die Absorptions- und Emissionsstrahlung der Atmosphärischen Ozonschicht bei der Wellenlänge 9,6 [mü] [Mikrometer] |
title_sort | uber die absorptions und emissionsstrahlung der atmospharischen ozonschicht bei der wellenlange 9 6 mu mikrometer |
topic | Physics Geography Physics, general Earth Sciences, general Geografie |
topic_facet | Physics Geography Physics, general Earth Sciences, general Geografie |
url | https://doi.org/10.1007/978-3-642-48007-2 |
volume_link | (DE-604)BV002538099 |
work_keys_str_mv | AT spechthorst uberdieabsorptionsundemissionsstrahlungderatmospharischenozonschichtbeiderwellenlange96mumikrometer |