타이틀 |
Solar UV Variations During the Decline of Cycle 23 |
저자 |
DeLand, Matthew, T.;; Cebula, Richard P. |
Keyword |
EARTH ATMOSPHERE;; IRRADIANCE;; RADIATION MEASURING INSTRUMENTS;; SOLAR ACTIVITY;; SOLAR CYCLES;; SOLAR OBSERVATORIES;; SOLAR RADIATION;; SOLAR TERRESTRIAL INTERACTIONS;; ULTRAVIOLET RADIATION |
URL |
http://hdl.handle.net/2060/20110023422 |
보고서번호 |
GSFC.JA.5420.2011 |
발행년도 |
2011 |
출처 |
NTRS (NASA Technical Report Server) |
ABSTRACT |
Characterization of temporal and spectral variations in solar ultraviolet irradiance over a solar cycle is essential for understanding the forcing of Earth''s atmosphere and climate. Satellite measurements of solar UV variability for solar cycles 21, 22, and 23 show consistent solar cycle irradiance changes at key wavelengths (e.g. 205 nm, 250 nm) within instrumental uncertainties. All historical data sets also show the same relative spectral dependence for both short-term (rotational) and long-term (solar cycle) variations. Empirical solar irradiance models also produce long-term solar UV variations that agree well with observational data. Recent UV irradiance data from the Solar Radiation and Climate Experiment (SORCE) Spectral Irradiance Monitor (SIM) and Solar Stellar Irradiance Comparison Experiment (SOLSTICE) instruments covering the declining phase of Cycle 23 present a different picture oflong-term solar variations from previous results. Time series of SIM and SOLSTICE spectral irradiance data between 2003 and 2007 show solar variations that greatly exceed both previous measurements and predicted irradiance changes over this period, and the spectral dependence of the SIM and SOLSTICE variations during these years do not show features expected from solar physics theory. The use of SORCE irradiance variations in atmospheric models yields substantially different middle atmosphere ozone responses in both magnitude and vertical structure. However, short-term solar variability derived from SIM and SOLSTICE UV irradiance data is consistent with concurrent solar UV measurements from other instruments, as well as previous results, suggesting no change in solar physics. Our analysis of short-term solar variability is much less sensitive to residual instrument response changes than the observations of long-term variations. The SORCE long-term UV results can be explained by under-correction of instrument response changes during the first few years of measurements, rather than requiring an unexpected change in the physical behavior of the Sun. |