W. Curdt
Hot emission lines (Te > 3 x
106 K) are normally not observed on the disk. However, during a flare
the plama temperatures can easily reach
3 x 107 K. In spectra
obtained during the May 9, 1999 flare of size M8 more than 80 lines were
observed, which include lines from
Fe XVIII - Fe XXIII that provide evidence
of 107 K plasmas. These are the hottest high-resolution astrophysical
spectral recordings ever made in the 500 Å - 1600 Å range.
The line list is taken from Feldman et al. (ApJ 544, 508;
2000); the references in the last column that point to the most accurate
previous measurements are also given therein.
Table: Flare lines in the SUMER spectral range.
Ion
0) |
Transition | Measured l / Å | Previously known l / Å | Log Te
1) |
References | |
Cr XVIII | 2s22p3 2D3/2 | - 2s22p34S3/2 | 793.160 ± 0.021 | 793.3±0.3 | 6.6 | Hinnov et al. (1982) |
Ni XIX | 2s22p53s 3P0 | - 2s22p53s3P1 | 794.605 ± 0.025 | ~6.6 | ||
Si XIII | 1s2p 3P2 | - 1s2s 3S1 | 814.715 ± 0.025 | 814.71±0.02; 814.729±0.024 | 6.952) | Howie et al. (1994); Curdt et al. (2000) |
Co XIX | 2s22p5 2P1/2 | - 2s22p52P3/2 | 820.019 ± 0.025 | 6.65 | ||
Fe XX | 2s22p3 2P1/2 | - 2s22p32D3/2 | 821.706 ± 0.030 | 821.74±0.05 | 6.9 | Kucera et al. (2000) |
Fe XXII | 2s22p 2P3/2 | - 2s22p 3P1/2 | 845.570 ± 0.020 | 845.55±0.1 | 7.05 | Hinnov & Suckewer (1980) |
Ti XVI | 2s22p3 2D3/2 | - 2s22p34S3/2 | 861.799 ± 0.020 | 861.8±0.1 | 6.6 | Hinnov (private communication) |
Si XIII | 1s2p 3P0 | - 1s2s 3S1 | 878.690 ± 0.040 | 878.85; 878.684±0.029 | 6.952) | Howie et al. (1994); Curdt et al. (2000) |
Ca XIV | 2s22p3 2D5/2 | - 2s22p34S3/2 | 880.401 ± 0.015 | 880.43±0.02 | 6.45 | Feldman et al. (1998a) |
Ni XXIII | 2s22p2 3P1 | - 2s22p23P0 | 910.855 ± 0.028 | 911.0 | 7.05 | Hinnov et al. (1982) |
Ti XV | 2s22p4 1D2 | - 2s22p43P2 | 919.730 ± 0.019 | 919.73±0.08 | 6.5 | Peacock et al. (1984) |
Ca XIV | 2s22p3 2D3/2 | - 2s22p34S3/2 | 943.585 ± 0.020 | 943.61±0.02 | 6.45 | Feldman et al. (1998a) |
K XIII | 2s22p3 2D5/2 | - 2s22p34S3/2 | 945.880 ± 0.020 | 6.35 | ||
S X | 2s22p23p 4D7/2 | - 2s22p23s3P5/2 | 946.307 ± 0.020 | 946.29±0.02 | 6.2 | Kink & Engsröm (1999) |
Ti XVI | 2s22p32P3/2 | - 2s22p32D3/2 | 968.868 ± 0.015 | 968.8±0.3 | 6.6 | Hinnov (private communication) |
Fe XVIII | 2s22p5 2P1/2 | - 2s22p52P3/2 | 974.850 ± 0.020 | -; 974.86±0.02 | 6.7 | Peacock et al (1984); Feldman et al. (1998a) |
K XIII | 2s22p3 2D3/2 | - 2s22p34S3/2 | 994.442 ± 0.020 | 6.35 | ||
Mg XI | 1s2p 3P2 | - 1s2s 3S1 | 997.456 ± 0.015 | 997.38±0.08; 997.451±0.019 | 6.81) | Klein et al. (1985); Curdt et al. (2000) |
Mn XXI | 2s22p 2P§/2 | - 2s22p 2P!/2 | 1005.862 ± 0.020 | 6.95 | ||
Ar XII | 2s22p3 2D5/2 | - 2s22p34S3/2 | 1018.790 ± 0.020 | 1018.87±0.02 | 6.3 | Feldman et al. (1998a) |
Ni XV | 3s23p2 1S0 | - 3s23p23P1 | 1033.041 ± 0.015 | 1033.04±0.02 | 6.35 | Feldman et al. (1998a) |
Ni XIV | 3s23p3 2P3/2 | - 3s23p34S3/2 | 1034.485 ± 0.020 | 1034.48±0.02 | 6.3 | Feldman et al. (1998a) |
Mg XI | 1s2p 3P0 | - 1s2s 3S1 | 1043.282 ± 0.020 | 1043.29±0.08; 1043±0.008 | 6.82) | Klein et al. (1985); Curdt et al. (2000) |
Ar XII | 2s22p3 2D3/2 | - 2s22p34S3/2 | 1054.585 ± 0.015 | 1054.62±0.02 | 6.3 | Feldman et al. (1998a) |
? | 1062.450 ± 0.040 | >6.2 | ||||
? | 1077.172. ± 0.025 | >6.2 | ||||
Fe XXIII | 2s2p 3P2 | - 2s2p 3P1 | 1079.415 ± 0.025 | 1079.3±0.3 | 7.1 | Hinnov et al. (1982) |
Ca XIV /2 | 2s22p3 2P3/2 | - 2s22p34S3/2 | 1090.450 ± 0.030 /2 | 545.26±0.02 | 6.45 | Feldman et al. (1982) |
Ca XV | 2s22p2 1D2 | - 2s22p23P1 | 1098.484 ± 0.040 | 1098.44±0.02 | 6.55 | Feldman et al. (1998a) |
Ca XV /2 | 2s22p2 1S0 | - 2s22p23P1 | 1110.764 ± 0.040 /2 | 6.55 | ||
Na X | 1s2p 3P2 | - 1s2s 3S1 | 1111.754 ± 0.030 | 1111.759±0.017 | 6.72) | Curdt et al. (2000) |
Fe XIX | 2s22p4 3P1 | - 2s22p43P2 | 1118.078 ± 0.015 | 1118.060±0.01 | 6.8 | Peacock et al. (1984) |
Ca XIII | 2s22p4 1D2 | - 2s22p23P2 | 1133.756 ± 0.020 | 1133.79±0.02 | 6.35 | Feldman et al. (1998a) |
Fe XX /2 | 2s22p3 2D5/2 | - 2s22p34S3/2 | 1135.650 ± 0.025 /2 | 567.76; 567.84 | 6.9 | Widing (1978); Kucera et al. (2000) |
Fe XVII | 2s22p53s 3P0 | - 2s22p53s3P1 | 1153.151 ± 0.025 | -; 1153.16 ± 0.02 | 6.45 | Feldman et al. (1985); Feldman et al. (1998a) |
Ca XIV /2 | 2s22p3 2P1/2 | - 2s22p34S3/2 | 1159.706 ± 0.030 /2 | 579.85±0.02 | 6.45 | Feldman et al. (1998a) |
? | 1164.813 ± 0.040 | >6.2 | ||||
Mn XVII | 2s22p5 2P1/2 | - 2s22p52P3/2 | 1167.760 ± 0.015 | 6.55 | ||
Fe XXI /2 | 2s22p2 1D2 | - 2s22p23P1 | 1171.531 ± 0.030 /2 | 585.8±0.3 | 6.95 | Hinnov et al. (1982) |
Ni XIV | 3s23p3 2P1/2 | - 3s23p34S3/2 | 1174.656 ± 0.020 | -; 1174.65 ± 0.02 | 6.3 | Sandlin et al. (1977); Feldman et al. (1998a) |
Fe XIX /2 | 2s22p4 1D2 | - 2s22p43P2 | 1184.467 ± 0.030 /2 | 592.234±0.006 | 6.8 | Peacock et al. (1984) |
? | 1188.108 ± 0.025 | >6.2 | ||||
? | 1192.978 ± 0.040 | >6.2 | ||||
? | 1201.192 ± 0.035 | >6.2 | ||||
Cr XX | 2s22p 2P3/2 | - 2s22p 2P1/2 | 1205.728 ± 0.025 | 1205.9±0.3 | 6.9 | Hinnov et al. (1982) |
Ne IX | 1s2p 3P2 | - 1s2s 3S1 | 1248.088 ± 0.015 | 1248.07±0.02; 1248.097±0.014 | 6.52) | Beyer et al. (1986); Curdt et al. (2000) |
K XII | 2s22p4 1D2 | - 2s22p43P2 | 1256.484 ± 0.025 | 6.3 | ||
Ni XIII | 3s23p4 1S0 | - 3s23p43P1 | 1277.204 ± 0.025 | -; 1277.22 ± 0.02 | 6.25 | Sandlin et al. (1977); Feldman et al. (1998a) |
Ne IX | 1s2p 3P0 | - 1s2s 3S1 | 1277.790 ± 0.050 | 1277.71±0.02 | 6.52 | Brown et al. (1985) |
Ca XIV | 2s22p3 2P3/2 | - 2s22p32D3/2 | 1291.607 ± 0.030 | 1291.61±0.02 | 6.45 | Feldman et al. (1998a) |
Ca XIII /2 | 2s22p4 1S0 | - 2s22p43P1 | 1297.398 ± 0.030 /2 | 648.68±0.02 | 6.35 | Feldman et al. (1998a) |
Ar XII | 2s22p3 2P3/2 | - 2s22p34S3/2 | 1298.186 ± 0.040 | 6.3 | ||
? / 2 | 1308.146 ± 0.030 /2 | >6.2 | ||||
? / 2 | 1309.752 ± 0.030 /2 | >6.2 | ||||
Ar XIII /2 | 2s22p2 1S0 | - 2s22p23P1 | 1313.344 ± 0.020 /2 | 656.69±0.020 | 6.4 | Feldman et al. (1998a) |
? /2 | 1314.650 ± 0.040 /2 | >6.2 | ||||
? /2 | 1320.402 ± 0.025 /2 | >6.2 | ||||
Cr XVIII /2 | 2s22p3 2D5/2 | - 2s22p34S3/2 | 1325.901 ± 0.030 /2 | 663.1±0.3 | 6.75 | Denne & Hinnov (1984) |
Fe XIX | 2s22p4 3P0 | - 2s22p43P2 | 1328.791 ± 0.030 | 6.8 | ||
Ar XIII | 2s22p2 1D2 | - 2s22p23P1 | 1330.532 ± 0.030 | 1330.54±0.02 | 6.4 | Feldman et al. (1998a) |
(f) | 1331.503 ± 0.021 | 1331.48±0.02 | >6.2 | Feldman et al. (1998b) | ||
Ar XII /2 | 2s22p3 2P1/2 | - 2s22p34S3/2 | 1340.603 ± 0.020 /2 | 670.34±0.02 | 6.3 | Feldman et al. (1998a) |
Fe XXI | 2s22p2 3P1 | - 2s22p23P0 | 1354.064 ± 0.020 | 1354.1±0.1 | 6.95 | Doschek et al. (1975) |
Mn XVIII | 2s22p4 3P1 | - 2s22p43P2 | 1354.892 ± 0.025 | 6.75 | ||
Fe XX /2 | 2s22p3 2P3/2 | - 2s22p32D5/2 | 1358.537 ± 0.029 /2 | 679.29 | 6.9 | Kucera et al. (2000) |
Ca XV | 2s22p2 1D2 | - 2s22p23P2 | 1375.959 ± 0.035 | 6.55 | Feldman & Doschek (1977), Sandlin et al. (1977) | |
Ar XI | 2s22p4 1D2 | - 2s22p43P2 | 1392.095 ± 0.017 | 1392.12 | 6.2 | Feldman & Doschek (1977), Sandlin et al. (1977) |
Cr XVI | 2s22p5 2P1/2 | - 2s22p53P3/2 | 1410.584 ± 0.025 | 1410.62±0.02 | 6.45 | Peacock et al. (1984) |
Ca XIV | 2s22p3 2P3/2 | - 2s22p32D5/2 | 1432.228 ± 0.050 | 6.45 | ||
Ar XI /2 | 2s22p3 3p5P3 | - 2s22p3 3s5S2 | 1435.705 ± 0.040 /2 | 717.88±0.02 | 6.2 | Kink (1999) |
Fe XX /2 | 2s22p3 2D3/2 | - 2s22p34S3/2 | 1443.107 ± 0.025 /2 | 721.55±0.02 | 6.9 | Kucera et al. (2000) |
? | 1452.655 ± 0.040 | >6.2 | ||||
Ar XI /2 | 2s22p3 3p5P2 | - 2s22p3 3s5S2 | 1460.877 ± 0.030 /2 | 730.41 | 6.2 | Kink (1999) |
Ar XI /2 | 2s22p3 3p5P1 | - 2s22p3 3s5S2 | 1472.980 ± 0.040 /2 | 736.55 | 6.2 | Kink (1999) |
Cr XVII /2 | 2s22p4 1D2 | - 2s22p43P2 | 1481.479 ± 0.020 /2 | 740.75±0.03 | 6.6 | Peacock et al. (1984) |
Ar XI | 2s22p4 1S0 | - 2s22p43P1 | 1491.605 ± 0.020 | 6.2 | ||
Ca XIV | 2s22p3 2P1/2 | - 2s22p32D3/2 | 1504.275 ± 0.032 | 6.45 | ||
? | 1515.190 ± 0.060 | >6.2 | ||||
Mn XIX /2 | 2s22p3 2D3/2 | - 2s22p34S3/2 | 1517.180 ± 0.040 /2 | 6.9 | ||
Ni XXI /2 | 2s22p4 3P1 | - 2s22p43P2 | 1558.901 ± 0.030 /2 | 779.5±0.3 | 6.9 | Hinnov et al. (1982) |
Fe XXI /2 | 2s22p2 1D2 | - 2s22p23P2 | 1572.061 ± 0.030 /2 | 786.1±0.3 | 6.95 | Hinnov et al. (1982) |
Fe XX+
Cr XVIII /2 |
2s22p3
2P3/2
2s22p3 2D3/2 |
-
2s22p32P1/2
- 2s22p3 4S3/2 |
1586.309 ± 0.030
& 1586.309 /2 |
1586.29 ± 0.03
793.3±0.3 |
6.9
6.75 |
Kucera et al. (2000)
Hinnov et al. (1982) |
Ni XIX /2 | 2s22p53s 3P0 | - 2s22p53s3P1 | 1589.256 ± 0.035 | ~6.6 |
0 Unidentified lines are noted by question mark or by the temperature classification of Feldman et al. (1998b), if available. Second order lines are noted by /2.
I In all other than the He-like ions the temperature of maximum fractional abundance is given.
2For all He-like lines the given values represents the temperature at which the contribution function reaches maximum.