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Table 1.

Comparison of predicted and observed quiet-Sun UV and EUV radiances.

Ion λobs Iobs Tmax Teff R1 R2
S II 1253.80 15.9 4.50 4.41 1.05
S II 1102.30 4.4 4.55 4.44 1.08
N II 1085.70 36.7a 4.65 4.49 1.34
N II 915.60 5.0 4.70 4.53 0.77
Si III 1206.50 694.6 4.80 4.57 0.82
S III 1200.96 8.0b 4.80 4.64 1.09
N III 991.60 47.2 4.95 4.88 0.73
N III 685.70 23.7 4.95 4.95 1.13
O III 702.70 56.6 5.00 4.98 0.76
O III 525.90 23.2 5.05 5.03 0.78
S IV 753.70 1.4 5.05 5.05 0.99
S IV 661.40 6.9 5.05 5.06 1.10
O IV 554.00 159.5 5.20 5.20 1.10
Ne IV 544.00 9.1 5.25 5.25 0.72
O V 630.00 335.0 5.40 5.38 1.00
Ne V 572.10 8.8 5.45 5.48 1.01

C II 1335.70 1205.0 4.60 4.45 0.92 0.71
C II 1036.30 35.9a 4.65 4.49 1.92 1.29
C III 977.00 702.0a 4.95 4.82 0.67 1.07
C III 1176.37 36.2a 4.95 4.82 0.67 1.01
C III 1175.74 104.0a 4.95 4.82 0.70 1.06
C III 1174.88 37.4a 4.95 4.82 0.65 0.98
C IV 1548.20 361.0a 5.05 5.07 0.30 0.68

Notes. Ion – principal ion emitting at observed wavelength; λobs (Å) – the observed wavelength; Iobs – the measured radiance (ergs cm−2 s−1 sr−1) using Vernazza & Reeves (1978), except those marked by superscript: (a) using Wilhelm et al. (1998), (b) using Parenti et al. (2005); Tmax and Teff – the maximum and effective temperature using Chianti ionisation equilibria (log values, in K – see text); R1 – the ratio between the predicted and observed intensities using populations from Chianti for all elements; R2 – the same ratio using carbon populations from this work.

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