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of 150
pro vyhledávání: '"O. H. Gish"'
Publikováno v:
Bulletin of the American Meteorological Society, 1938 Nov 01. 19(9), 404-404.
Externí odkaz:
https://www.jstor.org/stable/26256530
Publikováno v:
The Quarterly Review of Biology, 1947 Mar 01. 22(1), 66-66.
Externí odkaz:
https://www.jstor.org/stable/2813350
Akademický článek
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Autor:
O. H. Gish, G. R. Wait
Publikováno v:
Journal of Geophysical Research. 55:473-484
In a joint project of the Department of Terrestrial Magnetism, Carnegie Institution of Washington, and the United States Air Force, acceptable electric surveys were made over the tops of 21 thunderstorms in the central United States during July to Oc
Autor:
O. H. Gish
Publikováno v:
Physical Review. 3:353-363
Autor:
O. H. Gish
Publikováno v:
AAPG Bulletin. 16
Factors which have adversely influenced opinions and general impressions regarding the value of geoelectric methods as aids in the search for oil are thought by the author to be in considerable part of subjective rather than objective origin. However
Autor:
O. H. Gish
Publikováno v:
Journal of Geophysical Research. 47:323
That potential-gradient is less in low than in high latitudes was determined by Mauchly from data obtained on Cruises IV, V, and VI of the Carnegie. The evidence for this effect is better than was suspected by Mauchly, who based his comparison on the
Autor:
O. H. Gish
Publikováno v:
Transactions, American Geophysical Union. 16:189
Owing to the absence of the author from May to July while engaged in potential-gradient and conductivity observations at a base-station near “Strato-Camp” and in preparations for recording of atmospheric conductivity during the proposed 1935 stra
Autor:
O. H. Gish
Publikováno v:
Journal of Geophysical Research. 28:89
Autor:
O. H. Gish, Marcella Lindeman Phillips
Publikováno v:
Transactions, American Geophysical Union. 22:432
One may be interested in measurements of the concentration of the nuclei of condensation in the atmosphere for one or more of the following reasons: (a) Because of the fundamental role of these nuclei in the formation of fag and clouds; (b) because o