Table 3 Similar Table 2 but for positive Q-disturbances.
From: Daytime mid-latitude F2-layer Q-disturbances: A formation mechanism
Date | δNmF2 | EUVobs ×10-3 Wm−2 | EUV×1010 ph cm−2s-1 | W m s−1 | hmF2 km | Tex K | [O]300×108 cm−3 | [O]300×108 cm−3 (MSISE00) | ρobs g cm−3 |
|---|---|---|---|---|---|---|---|---|---|
23/08/2002 08/08/2002 | 1.85 | 7.74 5.82 (1.33) | 12.76 9.97 (1.28) | −7.5 −9.3 | 316 293 | 1280 1154 | 10.36 7.94 (1.30) | 10.10 8.01 (1.26) | — — |
17/06/2004 28/06/2004 | 1.42 | 4.32 4.19 (1.03) | 7.60 7.71 (0.99) | −0.1 −9.8 | 301 264 | 1071 994 | 6.96 5.30 (1.31) | 4.83 4.35 (1.11) | — — |
26/10/2004 23/10/2004 | 1.55 | 4.93 5.02 (0.98) | 9.43 9.12 (1.03) | −8.9 −14.3 | 252 246 | 938 927 | 6.11 4.84 (1.26) | 6.93 6.43 (1.08) | — — |
10/06/2007 06/06/2007 | 1.45 | 3.51 3.60 (0.97) | 6.32 6.75 (0.94) | −6.7 −11.1 | 246 229 | 878 868 | 3.99 2.70 (1.48) | 3.27 3.16 (1.03) | 4.83×10−15 3.37×10−15 (1.43) |
22/10/2009 13/10/2009 | 1.22 | 3.20 3.16 (1.01) | 6.06 5.93 (1.02) | −15.8 −20.0 | 227 219 | 780 753 | 4.36 3.56 (1.22) | 4.02 3.60 (1.12) | — — |
15/02/2010 11/02/2010 | 1.71 | 3.86 3.83 (1.01) | 7.42 7.70 (0.96) | −14.3 −20.6 | 235 217 | 818 788 | 4.51 2.83 (1.59) | 4.08 3.91 (1.04) | — — |
20/10/2010 03/10/2010 | 1.48 | 3.86 3.64 (1.06) | 7.07 6.85 (1.03) | −14.8 −16.2 | 226 222 | 792 803 | 4.45 3.57 (1.25) | 4.61 4.16 (1.11) | — — |
11/06/2012 27/06/2012 | 1.76 | 5.30 4.57 (1.16) | 10.26 9.02 (1.13) | −6.6 −12.8 | 284 250 | 1089 1004 | 6.87 4.46 (1.54) | 6.02 5.03 (1.20) | — — |
30/09/2012 12/09/2012 | 1.99 | 5.61 4.85 (1.16) | 10.49 8.61 (1.22) | −7.4 −8.6 | 278 256 | 1012 943 | 8.10 5.02 (1.61) | 7.38 6.08 (1.21) | 7.76×10−14 5.33×10−14 (1.46) |
25/08/2013 01/08/2013 | 1.59 | 5.21 4.97 (1.05) | 9.19 9.24 (0.99) | −6.1 −10.0 | 267 250 | 974 961 | 5.81 4.06 (1.43) | 5.30 4.63 (1.14) | — — |
04/07/2014 27/07/2014 | 1.47 | 6.32 5.10 (1.24) | 11.76 9.81 (1.20) | −9.1 −10.3 | 273 252 | 1111 997 | 5.77 4.42 (1.30) | 6.17 5.25 (1.17) | 12.53×10−16 7.21×10−16 (1.74) |
30/09/2015 16/09/2015 | 1.71 | 5.04 4.40 (1.14) | 9.53 8.54 (1.12) | −11.5 −7.2 | 249 251 | 943 907 | 5.76 3.58 (1.61) | 6.23 5.57 (1.12) | 8.70×10−16 5.95×10−16 (1.46) |
10/04/2016 27/04/2016 | 1.96 | 4.04 4.10 (0.98) | 8.51 7.88 (1.08) | −1.3 −18.8 | 287 229 | 1036 937 | 6.93 4.05 (1.71) | 5.65 4.99 (1.13) | — — |
11/04/2016 27/04/2016 | 2.19 | 3.98 4.10 (0.97) | 8.62 7.88 (1.09) | −3.0 −18.8 | 275 229 | 994 937 | 6.62 4.05 (1.63) | 5.50 4.99 (1.10) | — — |
15/10/2016 21/10/2016 | 1.72 | 3.80 3.53 (1.08) | 7.33 6.69 (1.09) | −10.3 −13.7 | 244 227 | 851 789 | 4.91 2.90 (1.69) | 5.15 4.08 (1.26) | — — |
11/04/2017 12/04/2017 | 1.79 | 3.04 3.07 (0.99) | 6.48 6.08 (1.06) | −8.1 −10.0 | 247 235 | 856 831 | 4.57 2.81 (1.62) | 4.33 4.23 (1.02) | — — |
16/04/2017 12/04/2017 | 1.63 | 3.29 3.07 (1.07) | 6.28 6.08 (1.03) | −10.2 −10.0 | 237 235 | 824 831 | 3.93 2.81 (1.40) | 4.07 4.23 (0.96) | — — |
29/04/2017 12/04/2017 | 1.49 | 3.47 3.07 (1.13) | 6.51 6.08 (1.07) | −10.6 −10.0 | 236 235 | 842 831 | 3.51 2.81 (1.25) | 4.15 4.23 (0.98) | — — |
