1997
DOI: 10.1590/s0102-261x1997000300009
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Aeroluminescência da região equatorial: estudo via experimento do foguete

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“…Estimated errors in the absolute intensities for the two emissions are approximately AE15%. In order to calculate the radiation energy loss as a function of the height, the OH(8,3) and O 2 atmospheric (0,0) band volume emission pro®les observed at equatorial location (Melo, 1994;Takahashi et al, 1995) were used in the calculations. These simultaneous pro®les were obtained during an airglow rocket photometer campaign called MULTIFOT and are the only measured vertical pro®les in the Brazilian sector.…”
Section: Observationsmentioning
confidence: 99%
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“…Estimated errors in the absolute intensities for the two emissions are approximately AE15%. In order to calculate the radiation energy loss as a function of the height, the OH(8,3) and O 2 atmospheric (0,0) band volume emission pro®les observed at equatorial location (Melo, 1994;Takahashi et al, 1995) were used in the calculations. These simultaneous pro®les were obtained during an airglow rocket photometer campaign called MULTIFOT and are the only measured vertical pro®les in the Brazilian sector.…”
Section: Observationsmentioning
confidence: 99%
“…To obtain this, a weighting function was calculated from the volume emission pro®le observed by rocket photometer (Melo, 1994), as az szas where sz is the volume emission rate for 1 km interval in the vertical pro®le and s is the total column volume emission rate of the vertical pro®le. Notice that az is in step of 1 km and the ground intensity in photons s À1 cm À2 acolumnY so a conversion factor, b 10, is necessary to get photons s À1 m À3 units.…”
Section: Equivalent Energy Loss Rate By Airglowmentioning
confidence: 99%
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