1961
DOI: 10.1016/0032-0633(61)90189-1
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The observation of corpuscles by means of the third artificial earth satellite

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Cited by 5 publications
(5 citation statements)
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“…In addition to astrophysical measurements, ionospheric and atmospheric studies [10][11][12][13][14][15][16][17] and satellite data failures studies (e.g., [18,19]) also found several effects suggesting that electron impact is important factor at low and middle latitudes. That is, more importantly, the occasional electron flux increases below the radiation belt were discovered even earlier in direct satellite-borne measurements [20,21] and then corroborated in several studies [22][23][24][25].…”
Section: Introductionsupporting
confidence: 68%
“…In addition to astrophysical measurements, ionospheric and atmospheric studies [10][11][12][13][14][15][16][17] and satellite data failures studies (e.g., [18,19]) also found several effects suggesting that electron impact is important factor at low and middle latitudes. That is, more importantly, the occasional electron flux increases below the radiation belt were discovered even earlier in direct satellite-borne measurements [20,21] and then corroborated in several studies [22][23][24][25].…”
Section: Introductionsupporting
confidence: 68%
“…A quasi‐trapped population of energetic electrons was observed below the IRB at an L < 1.2 within the near‐equatorial region. While its existence has been known for a long time [e.g., Krasovskii et al ., , ; Galperin et al ., ; Hill et al ., ; Heikkila , ; Hayakawa et al ., ; Kohno , ], information for fluxes and spectra has been scarce and controversial. In general, the flux of energetic electrons at L < 1.2 is invariably weak and certainly less than those inside of the IRB, ORB, or auroral zone during quiet as well as storm times.…”
Section: Introductionmentioning
confidence: 99%
“…The quasi-trapped population of energetic electrons is observed below the IRB at L < 1.2 in the near-equatorial region. While its existence was known long time ago [9][10][11], the information about the fluxes and spectra was scarce and controversial. Traditionally it is thought that the electron fluxes below the IRB are invariably weak and certainly less than inside the IRB zone, therefore the particle impact is insufficient to produce appreciable ionization [1].…”
Section: Introductionmentioning
confidence: 99%
“…At low latitudes and heights of several hundred kilometers, i.e., under the inner ERB, sporadic intense fluxes of electrons with energies of 10 keV < E < 300 keV are also observed [13,14]. In this region, electrons drift across the geomagnetic field in longitude to the east and in less than 20 h reach the SAA, where they descend to heights below 100 km, which results in their loss in the atmosphere due to ionization.…”
Section: Introductionmentioning
confidence: 99%