Incumbent
发表于 2025-3-28 16:07:31
H. Wintz,F. Wittenbeck because the new material we wished to include was too extensive for—and far beyond the usual scope—of a second edition. More importantly, we felt that some fundamental changes regarding this topic’s scope and terminology would be desirable and timely.978-1-4419-4576-1978-0-387-76852-6Series ISSN 1574-0463 Series E-ISSN 2698-5497
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发表于 2025-3-28 21:31:36
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洞穴
发表于 2025-3-29 01:24:37
Sasi Kanumuri,Matthew Zeiernd hydrocarbon compounds. The anthropogenic aerosol commonly known as Arctic haze peaks in concentration (SO.. 1.5 to 4 μg m.) in the northern lower troposphere (0 to 5 km) from about November to May. It is a minimum in summer (~ 0.1 μg m.). Arctic aerosol composition varies with particle size. Belo
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发表于 2025-3-29 06:09:01
Scott L. Newstok,Ayanna Thompsonrom the solar corpuscular radiation and the solar wind. If an additional heat source is used, which has a maximum at about 9. local time and a flux of 1 erg cm. sec., a time-dependent model of the upper atmosphere is obtained that is in good agreement with the observed densities.