Investigations of potassium, lithium, and sodium emission in the nightglowand OH cross calibration

Citation
Tg. Slanger et De. Osterbrock, Investigations of potassium, lithium, and sodium emission in the nightglowand OH cross calibration, J GEO RES-A, 105(D1), 2000, pp. 1425-1429
Citations number
28
Categorie Soggetti
Earth Sciences
Volume
105
Issue
D1
Year of publication
2000
Pages
1425 - 1429
Database
ISI
SICI code
Abstract
Sky spectra from the high-resolution echelle spectrometer (HIRES) on the Ke ck I telescope have been analyzed to obtain information on the potassium, l ithium, and sodium resonance line emission in the nightglow. Relative inten sity calibration is carried out against OH band intensities, and absolute v alues are obtained by utilizing new averaged intensities of the OH 9-4 band . The D-1 line of potassium, at 7699 A, is shown to be present, as previous ly speculated by Swider [1987]. Its average intensity is 1.0 R, twice as la rge as predicted. Any lithium line emission at the resonance wavelengths ne ar 6708 Angstrom is obscured by the P-P(3) line of the 12-9 emission band o f the O-2 (b(1)Sigma(g)(+)-X(3)Sigma(g)(-)) Atmospheric Band system. Howeve r, as that line has an intensity of similar to 60 mR, our estimated upper l imit on the Li line intensities is similar to 15 mR. The intensity that we extract for the Na(D-1) line, averaged over 4 years, is 20 R. Although ther e is no solar scattering contribution to the Na and K data, the Na D-2/D-1 line intensity ratio is substantially smaller than reported earlier for nig htglow conditions. Observing that the Na/K D-1 line intensity ratio is an o rder of magnitude smaller than the typical [Na]/[K] concentration ratio lea ds to the conclusion that the maximum efficiency for production of mesosphe ric Na(P-2) is 0.1.