Výsledky vyhledávání - "Gordon Miller Bourne Dobson"

Observations of the height of the ozone in the upper atmosphere

Autor: Gordon Miller Bourne Dobson, F. W. P. Götz

Publikováno v: Proceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character. 120:251-259

It has been shown that there is a close connection between the amount of ozone in the upper atmosphere and the pressure conditions in the upper part of the troposphere and the lower part of the stratosphere. MM. Cabannes and Dufay, and also MM. Lambe

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::db77014535f923252305bf7f08b3c7c9
https://doi.org/10.1098/rspa.1928.0147

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The vertical distribution of ozone in the atmosphere

Autor: Gordon Miller Bourne Dobson, A. R. Meetham, F. W. Paul Götz

Publikováno v: Proceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character. 145:416-446

List of Symbols used in the Paper . I = the intensity of radiation of wave-length 3110 A. received by instrument. I´ = the intensity of radiation of wave-length 3290 A. received by instrument.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::992a048da4935d0af40bc23e52bb1ec1
https://doi.org/10.1098/rspa.1934.0109

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A flicker type of photo-electric photometer giving high precision

Autor: Gordon Miller Bourne Dobson

Publikováno v: Proceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character. 104:248-251

There are numerous types of photometer, designed either to measure the relative intensities of two light sources or the “densities” of filters or photographic plates. In the bulk of these, an estimate has to be made by eye when two illuminated ar

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3e78edba80d90588423562ad6c887d61
https://doi.org/10.1098/rspa.1923.0106

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A theory of meteors, and the density and temperature of the outer atmosphere to which it leads

Autor: Frederick Alexander Lindemann, Gordon Miller Bourne Dobson

Publikováno v: Proceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character. 102:411-437

Some thirty years ago Teisserenc de Bort announced the discovery that the temperature gradient in the atmosphere, which amounts to some 6.5 . 10 -5 degree/cm. for the first 10 km., becomes negligibly small at greater heights. Since this time it has b

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d1d8de7e558ee0825c73c20d18b7cb92
https://doi.org/10.1098/rspa.1923.0003

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Bakerian Lecture: Meteorology of the lower stratosphere

Autor: A. W. Brewer, B. M. Cwilong, Gordon Miller Bourne Dobson

Publikováno v: Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences. 185:144-175

Ever since its discovery at the end of the last century, the stratosphere has aroused much interest, not only among meteorologists, but among other men of science also. While at first its cause seemed so mysterious that many doubted the reality of it

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6b4deb919247b2e5b051f689b303f97d
https://doi.org/10.1098/rspa.1946.0010

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A note on the temperature of the air at great heights

Autor: Gordon Miller Bourne Dobson, Frederick Alexander Lindemann

Publikováno v: Proceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character. 103:339-342

In a previous paper it has been shown that the temperature of the air above 60 km., as calculated from meteor observations, is much higher than that between, say, 10 and 50 km., and is probably about 300° A. It appears that the only explanation of t

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3ea80eb66aa5ad770bcebd8af51d67f7
https://doi.org/10.1098/rspa.1923.0061

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Origin and distribution of the polyatomic molecules in the atmosphere

Autor: Gordon Miller Bourne Dobson

Publikováno v: Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences. 236:187-193

Of those gases which occur in the upper atmosphere and have strong absorption bands in the infra-red part of the spectrum and which must, therefore, be considered when calculating the absorption and radiation of heat in the atmosphere, only carbon

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::cebddf6a378abea640775bf005d64a59
https://doi.org/10.1098/rspa.1956.0127

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