Zobrazeno 1 - 10
of 81
pro vyhledávání: '"Elmer Robinson"'
Publikováno v:
History of Geophysics ISBN: 9781118665213
In 1967 and 1968, ice samples were taken from various depths in the ice caps of Greenland and Antarctica and transported to the Stanford Research Institute laboratories in the frozen state. These samples ranged in age from 100 to 2500 years. After th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88b96537c76e9e6307342d6edf2001a1
https://doi.org/10.1029/hg001p0120
https://doi.org/10.1029/hg001p0120
Autor:
F.L. Ludwig, Elmer Robinson
Publikováno v:
Tellus A; Vol 22, No 1 (1970)
A program of aerosol and cloud droplet measurements in stratus clouds was carried out during the summer of 1968 in the hills south of San Francisco. Size distributions were determined with a Royco light-scattering particle counter, a condensation nuc
Publikováno v:
Water, Air, and Soil Pollution. 66:389-394
Publikováno v:
Geophysical Research Letters. 19:187-190
The June 1991 eruption of the Philippine volcano Pinatubo introduced a massive plume of volcanic ash and other aerosol material into a stratosphere containing only near-background concentrations of aerosol material. At Mauna Loa Observatory, Hawaii,
Autor:
Juan Carlos S�nchez, Luis E. Herrera, Elmer Robinson, Michel Benarie, D. P. Ormrod, Arthur C. Stern, Zev Gerstl
Publikováno v:
Water, Air, and Soil Pollution. 35:423-430
Publikováno v:
Environmental Science & Technology. 15:1493-1498
Publikováno v:
Water, Air, and Soil Pollution. 28:199-209
Publikováno v:
Water, Air, and Soil Pollution. 33:443-450
Autor:
Dagmar R. Cronn, Elmer Robinson
Publikováno v:
Geophysical Research Letters. 6:641-644
The first known vertical distributions of ethane and acetylene which extend into the lower stratosphere are reported. The average upper tropospheric concentrations, between 20,000 ft and 35,000 ft, near 37 deg N-123 deg W were 1.2 micrograms/cu m (1.
Publikováno v:
Journal of Atmospheric Chemistry. 2:65-81
In early 1982 a station capable of sampling atmospheric trace gas constituents on a continuous basis was established at Palmer Station, Anvers Island, adjacent to the Antarctic Peninsula (64° 46′S 64° 04′W). Sampling operations began about 1 Fe