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- W1601825445 abstract "The changes in the ionospheric composition and temperature profiles, in the altitude range of 120 to 1000 km, due to different mechanisms currently considered important during storms, are estimated quantitatively for Delhi for moderate solar activity conditions using the method of Stubbe. These results are discussed in the light of our observational results reported earlier. It is thought that during day the neutral temperature changes and thus the neutral composition changes along with the change in equatorward winds are responsible for the observed effect. However, at night, if eastward electric fields and neutral winds are thought to be operative for 3 hrs. with a very slight change in Tn, the observed results can be explained." @default.
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- W1601825445 date "1980-01-01" @default.
- W1601825445 modified "2023-10-02" @default.
- W1601825445 title "ON EXPLAINING THE IONOSPHERIC COMPOSITION AND TEMPERATURE CHANGES DURING STORMS AT LOW LATITUDES" @default.
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- W1601825445 doi "https://doi.org/10.1016/b978-0-08-024439-6.50028-4" @default.
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