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pro vyhledávání: '"George C. Simpson"'
Autor:
George C. Simpson
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 67:163-169
Autor:
George C. Simpson
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 31:295-306
Autor:
George C. Simpson, W. N. Shaw
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 32:249-257
Autor:
George C. Simpson B.Sc.
Publikováno v:
The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science. 6:589-598
(1903). LXXV. On charging through ion absorption and its bearing on the earth's permanent negative charge. The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science: Vol. 6, No. 35, pp. 589-598.
Autor:
George C. Simpson
Publikováno v:
Proceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character. 83:394-404
In connection with a theory of the electricity of thunderstorms published in the ‘Philosophical Transactions,’ measurements of the charges of rain were made in 1908, and it appeared advisable that these should be continued for a second year. 1. T
Autor:
George C. Simpson
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 38:291-302
Autor:
George C. Simpson
Publikováno v:
Weather. 4:104-108
Autor:
George C. Simpson, C. S. Wright
Publikováno v:
Proceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character. 85:175-199
Although the different phenomena of atmospheric electricity have been thoroughly investigated over land, very little work has yet been done over the ocean, and on the few occasions on which experiments have been made, the observations have been too f
Autor:
George C. Simpson
Publikováno v:
Monthly Weather Review. 44:115-122
Autor:
George C. Simpson, F. J. Scrase
Publikováno v:
Proceedings of the Royal Society of London. Series A - Mathematical and Physical Sciences. 161:309-352
The mechanism of thunderstorms has been the subject of much controversy in recent years, and at the present time there are at least two theories which find considerable support. To arrive at a theory which would satisfy all criticism would be a great