|
Detailed Reference Information |
Murcray, F.J., Goldman, A., Landry, J.C. and Stephen, T.M. (1997). O2 continuum: A possible explanation for the discrepancies between measured and modeled shortwave surface irradiances. Geophysical Research Letters 24: doi: 10.1029/97GL02220. issn: 0094-8276. |
|
Ground based solar spectra between 1 and 5 &mgr;m (10,000 and 2000 cm-1) have been obtained with a new, absolutely calibrated spectrometer. These spectra have sufficient spectral resolution (2 cm-1) to allow atmospheric absorption lines to be distinguished from underlying continuum absorption. Continuum absorption due to O2 has been identified around 1.06 &mgr;m (9366 cm-1), 1.27 &mgr;m (7882 cm-1), and 1.6 &mgr;m (6326 cm-1). These continuum absorptions are not included in the HITRAN database. Similar continuum absorption should be present around the 0.762 &mgr;m (13121 cm-1) and 0.688 &mgr;m (14525 cm-1) bands of O2.¿ 1997 American Geophysical Union |
|
|
|
BACKGROUND DATA FILES |
|
|
Abstract |
|
|
|
|
|
Keywords
Atmospheric Composition and Structure, Transmission and scattering of radiation, Atmospheric Composition and Structure, Instruments and techniques |
|
Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
|
|
|