Сериальное издание: Bulletin of the Russian Academy of Sciences: Physics
Страницы: 721-723
Аннотация
Temporal variations in the intensity of cosmic rays occur when effects of different natures (including atmospheric effects) coincide. The latter are primarily due to changes in the temperature and density of the atmosphere. One way of obtaining information on variations in temperature at different isobaric levels of the atmosphere using data on the continuous registration of cosmic rays is shown
