The Sun 73
10-3A10-2A10-1A1 A 10 A 102 A
103 A
1∝m
10∝m
102
∝m1 mm 1 cm 10 cm 1 m 10 m1021Hz1020Hz1019Hz1018Hz1017Hz1016Hz1015Hz1014Hz1013Hz103 GHz
102 GHz
10 GHz1 GHz100 MHz10 -2010 -1910 -1810 -1710 -1610 -1510 -1410 -1310 -1210 -1110 -1010 -910 -810 -710 -610 -510 -610 -510 -410 -310 -210 -1110100103104105106107SPECTRAL IRRADIANCE (erg cm-2s-1∝m-1)WAVELENGTHFREQUENCYGAMMA RAY X RAY
ULTRA
VIOLETVISIBLE
INFRARED
RADIOLARGE BURST
(3B FLARE, 8/4/72)
(NONTHERMAL)NON-FLARE
CONDITIONS1B FLAREPOSTFLARE2B FLAREQUIET SUNQUIET SUN
(THERMAL)LARGE STORM
(NONTHERMAL)SLOWLY-VARYING
S-COMPONENT
ACTIVE REGIONS
(THERMAL)GRADUAL
BURST
(NONTHERMAL)LARGE BURST
3B FLARE, 8/1/72
(NONTHERMAL)LARGEST BURST
REPORTED
(NONTHERMAL)FIGURE 2 The solar irradiance spectrum from gamma rays to radio waves. The spectrum is
shifted by 12 orders of magnitude in the vertical axis atλ=1 mm to accommodate for the large
dynamic range in spectral irradiance. (Courtesy of H. Malitson and NASA/NSSDC.)
by ionized plasma in the coronal temperature range of
∼1–2 million K. Emissions in shorter wavelengths require
higher plasma temperatures and thus occur duringflares
only. Flares also accelerate particles to nonthermal ener-
gies, which cause emission in hard X-rays, gamma rays, and
radio wavelengths, but to a highly variable degree.
2. The Solar Interior
The physical structure of the solar interior is mostly based
on theoretical models that are constrained (1) by global
quantities (age, radius, luminosity, total energy output; see
Table 1); (2) by the measurement of global oscillations