SOLAR UV IRRADIANCE VARIABILITY DURING THE DECLINING PHASE OF THE SOLAR-CYCLE-22

Citation
S. Chandra et al., SOLAR UV IRRADIANCE VARIABILITY DURING THE DECLINING PHASE OF THE SOLAR-CYCLE-22, Geophysical research letters, 22(18), 1995, pp. 2481-2484
Citations number
13
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
00948276
Volume
22
Issue
18
Year of publication
1995
Pages
2481 - 2484
Database
ISI
SICI code
0094-8276(1995)22:18<2481:SUIVDT>2.0.ZU;2-L
Abstract
The SUSIM (Solar Ultraviolet Spectral Irradiance Monitor) and the SOLS TICE (Solar Stellar Irradiance Comparison Experiment) instruments on t he UARS (Upper Atmosphere Research Satellite) have been making continu ous measurements of the solar UV flux in the spectral range 115-420 nm since October 1991. This period, characterized as the declining phase of solar cycle 22, shows a transition from near maximum to near minim um solar activity levels. During this period, the solar UV flux at Lym an alpha decreased by about 45% from a mean solar maximum value of abo ut 9 mW/m(2), and the integrated solar flux between 200-205 nm decreas ed by about 5 % from a mean value of about 47 mW/m(2). Using the MgII index as a proxy of solar UV irradiance variability, it is shown that the temporal relationship of the UARS solar Lyman alpha irradiance and the MgII index during solar cycle 22 is significantly different than during solar cycle 21, inferred from the SME (Solar Mesosphere Explore r) Lyman alpha measurements. Moreover, during solar cycle 22, the scal e factor for solar Lyman alpha irradiance (% change for 1% change in M gII index) is about 1.5 times larger for long term changes than for ch anges over the time scale of a solar rotation. Unlike Lyman alpha, the scale factor for the UV flux in the 200-205 nm wavelength range, is c lose to unity both for the rotational and longer time scales. The spec tral dependence of the two scale factors in the 120-200 nm range is de rived from the SOLSTICE data which may be used with the MgII index to estimate the UV irradiance variability in this spectral range for both short and long time scales.