Relation Between Actual and Virtual Ionospheric Height
Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are describ...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
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| Format: |
E-Artikel |
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| Erschienen: |
1940 |
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| Umfang: |
Online-Ressource 8 |
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| Reproduktion: |
APS Digital Backfile Archive 1893-2003 |
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| Übergeordnetes Werk: |
Enthalten in: The physical review - Lancaster, Pa. [u.a.], 1893, 57(1940), 2, Seite 87-94 |
| Übergeordnetes Werk: |
volume:57 ; year:1940 ; number:2 ; pages:87-94 ; extent:8 |
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| 520 | |a Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are described and applied. The simplest measure of the actual height of maximum electron density is the virtual height at five-sixths of the penetration frequency. This measure is found to be remarkably reliable for F region at night. During the daytime it is often necessary to correct F1 observations for presence of E region, and F2 observations for presence of F1 region. A simple technique of correction is described and applied. The disadvantages of minimum virtual height for quantitative study of diurnal variation of ionospheric height are emphasized. | ||
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(DE-627)NLEJ251405060 (DE-601)aps:3b38e9b98d61d28235f9fe47eb7ea7e45067d311 DE-627 ger DE-627 rakwb Relation Between Actual and Virtual Ionospheric Height 1940 Online-Ressource 8 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are described and applied. The simplest measure of the actual height of maximum electron density is the virtual height at five-sixths of the penetration frequency. This measure is found to be remarkably reliable for F region at night. During the daytime it is often necessary to correct F1 observations for presence of E region, and F2 observations for presence of F1 region. A simple technique of correction is described and applied. The disadvantages of minimum virtual height for quantitative study of diurnal variation of ionospheric height are emphasized. APS Digital Backfile Archive 1893-2003 Booker, H. G. oth Seaton, S. L. oth Enthalten in The physical review Lancaster, Pa. [u.a.], 1893 57(1940), 2, Seite 87-94 (DE-627)NLEJ24823790X (DE-600)2177092-X 1536-6065 nnns volume:57 year:1940 number:2 pages:87-94 extent:8 https://www.tib.eu/de/suchen/id/aps%3A3b38e9b98d61d28235f9fe47eb7ea7e45067d311 Verlag Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-APS GBV_NL_ARTICLE AR 57 1940 2 87-94 8 |
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(DE-627)NLEJ251405060 (DE-601)aps:3b38e9b98d61d28235f9fe47eb7ea7e45067d311 DE-627 ger DE-627 rakwb Relation Between Actual and Virtual Ionospheric Height 1940 Online-Ressource 8 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are described and applied. The simplest measure of the actual height of maximum electron density is the virtual height at five-sixths of the penetration frequency. This measure is found to be remarkably reliable for F region at night. During the daytime it is often necessary to correct F1 observations for presence of E region, and F2 observations for presence of F1 region. A simple technique of correction is described and applied. The disadvantages of minimum virtual height for quantitative study of diurnal variation of ionospheric height are emphasized. APS Digital Backfile Archive 1893-2003 Booker, H. G. oth Seaton, S. L. oth Enthalten in The physical review Lancaster, Pa. [u.a.], 1893 57(1940), 2, Seite 87-94 (DE-627)NLEJ24823790X (DE-600)2177092-X 1536-6065 nnns volume:57 year:1940 number:2 pages:87-94 extent:8 https://www.tib.eu/de/suchen/id/aps%3A3b38e9b98d61d28235f9fe47eb7ea7e45067d311 Verlag Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-APS GBV_NL_ARTICLE AR 57 1940 2 87-94 8 |
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(DE-627)NLEJ251405060 (DE-601)aps:3b38e9b98d61d28235f9fe47eb7ea7e45067d311 DE-627 ger DE-627 rakwb Relation Between Actual and Virtual Ionospheric Height 1940 Online-Ressource 8 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are described and applied. The simplest measure of the actual height of maximum electron density is the virtual height at five-sixths of the penetration frequency. This measure is found to be remarkably reliable for F region at night. During the daytime it is often necessary to correct F1 observations for presence of E region, and F2 observations for presence of F1 region. A simple technique of correction is described and applied. The disadvantages of minimum virtual height for quantitative study of diurnal variation of ionospheric height are emphasized. APS Digital Backfile Archive 1893-2003 Booker, H. G. oth Seaton, S. L. oth Enthalten in The physical review Lancaster, Pa. [u.a.], 1893 57(1940), 2, Seite 87-94 (DE-627)NLEJ24823790X (DE-600)2177092-X 1536-6065 nnns volume:57 year:1940 number:2 pages:87-94 extent:8 https://www.tib.eu/de/suchen/id/aps%3A3b38e9b98d61d28235f9fe47eb7ea7e45067d311 Verlag Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-APS GBV_NL_ARTICLE AR 57 1940 2 87-94 8 |
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(DE-627)NLEJ251405060 (DE-601)aps:3b38e9b98d61d28235f9fe47eb7ea7e45067d311 DE-627 ger DE-627 rakwb Relation Between Actual and Virtual Ionospheric Height 1940 Online-Ressource 8 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are described and applied. The simplest measure of the actual height of maximum electron density is the virtual height at five-sixths of the penetration frequency. This measure is found to be remarkably reliable for F region at night. During the daytime it is often necessary to correct F1 observations for presence of E region, and F2 observations for presence of F1 region. A simple technique of correction is described and applied. The disadvantages of minimum virtual height for quantitative study of diurnal variation of ionospheric height are emphasized. APS Digital Backfile Archive 1893-2003 Booker, H. G. oth Seaton, S. L. oth Enthalten in The physical review Lancaster, Pa. [u.a.], 1893 57(1940), 2, Seite 87-94 (DE-627)NLEJ24823790X (DE-600)2177092-X 1536-6065 nnns volume:57 year:1940 number:2 pages:87-94 extent:8 https://www.tib.eu/de/suchen/id/aps%3A3b38e9b98d61d28235f9fe47eb7ea7e45067d311 Verlag Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-APS GBV_NL_ARTICLE AR 57 1940 2 87-94 8 |
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(DE-627)NLEJ251405060 (DE-601)aps:3b38e9b98d61d28235f9fe47eb7ea7e45067d311 DE-627 ger DE-627 rakwb Relation Between Actual and Virtual Ionospheric Height 1940 Online-Ressource 8 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are described and applied. The simplest measure of the actual height of maximum electron density is the virtual height at five-sixths of the penetration frequency. This measure is found to be remarkably reliable for F region at night. During the daytime it is often necessary to correct F1 observations for presence of E region, and F2 observations for presence of F1 region. A simple technique of correction is described and applied. The disadvantages of minimum virtual height for quantitative study of diurnal variation of ionospheric height are emphasized. APS Digital Backfile Archive 1893-2003 Booker, H. G. oth Seaton, S. L. oth Enthalten in The physical review Lancaster, Pa. [u.a.], 1893 57(1940), 2, Seite 87-94 (DE-627)NLEJ24823790X (DE-600)2177092-X 1536-6065 nnns volume:57 year:1940 number:2 pages:87-94 extent:8 https://www.tib.eu/de/suchen/id/aps%3A3b38e9b98d61d28235f9fe47eb7ea7e45067d311 Verlag Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-APS GBV_NL_ARTICLE AR 57 1940 2 87-94 8 |
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Relation Between Actual and Virtual Ionospheric Height |
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Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are described and applied. The simplest measure of the actual height of maximum electron density is the virtual height at five-sixths of the penetration frequency. This measure is found to be remarkably reliable for F region at night. During the daytime it is often necessary to correct F1 observations for presence of E region, and F2 observations for presence of F1 region. A simple technique of correction is described and applied. The disadvantages of minimum virtual height for quantitative study of diurnal variation of ionospheric height are emphasized. |
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Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are described and applied. The simplest measure of the actual height of maximum electron density is the virtual height at five-sixths of the penetration frequency. This measure is found to be remarkably reliable for F region at night. During the daytime it is often necessary to correct F1 observations for presence of E region, and F2 observations for presence of F1 region. A simple technique of correction is described and applied. The disadvantages of minimum virtual height for quantitative study of diurnal variation of ionospheric height are emphasized. |
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Translation of virtual height of the ionosphere into actual height is achieved by fitting a parabolic maximum of electron density to observations of variation of virtual height with wave frequency. Methods for measuring the thickness of a region and the height of maximum electron density are described and applied. The simplest measure of the actual height of maximum electron density is the virtual height at five-sixths of the penetration frequency. This measure is found to be remarkably reliable for F region at night. During the daytime it is often necessary to correct F1 observations for presence of E region, and F2 observations for presence of F1 region. A simple technique of correction is described and applied. The disadvantages of minimum virtual height for quantitative study of diurnal variation of ionospheric height are emphasized. |
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