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Significant upper thermospheric contribution to the O (1S) 557.7 nm dayglow emission: first ground based evidence

✍ Scribed by Alok Taori; R. Sridharan; D. Chakrabarty; N.K. Modi; R. Narayanan


Book ID
104407456
Publisher
Elsevier Science
Year
2003
Tongue
English
Weight
605 KB
Volume
65
Category
Article
ISSN
1364-6826

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✦ Synopsis


Out of the two source regions of O ( 1 S) green line 557:7 nm emission namely the one in the lower thermosphere and the other in the upper thermosphere, the upper thermospheric source is known to contribute only 15 -20% of the total 557:7 nm volume emission during nighttime. On the other hand, successful, simultaneous ground based measurements of daytime 557:7 nm O ( 1 S) and 630:0 nm O ( 1 D) thermospheric emissions with the multiwavelength daytime photometer (MWDPM) reveal striking similarities in their variabilities, the inference being the dominance of thermospheric contribution in 557:7 nm O ( 1 S) emission throughout the day, in conformity with the space borne measurements made else where. The ÿrst set of ground-based measurements are presented and discussed.