Being an indicator of searched parameter we adopted the bottom latitude with common ROTI better than 0.three TECU/min. These types of dataset, 4 or fewer (determined by distribution of observations), was subsequently placed on find the best-fitted product of oval. Treating it because the approximation of present-day ionospheric conditions, it absolutely was doable to recalculate AACGM latitude of ROTI observations from working day- and night time-facet ionosphere to noon and midnight Instructions, respectively. Due to nevertheless feasible discrepancies among dataset and model, the conversion coated data in the modelled oval and three-diploma adjacent bands. In precise, the observations Found Within the oval were projected proportional to both its boundaries at specified MLT and target axis, Whilst in the case of outer bands, it absolutely was accomplished making use of variances between equatorward/poleward boundaries. Eventually, we computed signify ROTI values in fifteen min intervals for 2° bands of AACGM latitude (shift involving consecutive values equalled 1°).
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The main points of auroral oval progress for the next party are given in Determine 13b. As it was indicated in former portion this storm was preceded by many hours of northwardly oriented IMF, characterised by really low ionospheric activity. Analysing these outcomes you can observe the reasonable TEC fluctuation happening within the dayside only (76°–seventy nine° of AACGM latitude). In the next hours ROTI values display a speedy growth of ionospheric variability to the extent of 1.seven TECU/min (#three).
The outcomes for the second working day of S2 celebration (nine March) depict the dependence of TEC fluctuation intensity on auroral electrojet (#6). Therefore, analysing nightside ionosphere one can notice the enhancement of ROTI values (as much as ~two.0 TECU/min) similar to the versions of AE index. Additionally, Every single of such phases was accompanied by poleward change of robust TEC fluctuations linked to substorm advancement. The dayside TEC fluctuation was somewhat weaker and smoothed in time area. In cases like this we detected the gradual poleward shift of maximal ROTI values from sixty° to 72°.
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The S1 occasion was a typical geomagnetic storm with a negative IMF Bz ahead of the IP shock. The transfer of photo voltaic wind Strength for the magnetosphere by means of magnetic reconnection is considered as a reason behind storm. Once the interplanetary shock, there was noticed a quick reduce of SYM-H index towards the minimum equivalent to −98 nT. At the same time, the intensified auroral action was started to sign-up. It may be divided into two periods with destructive IMF Bz, i.e. the primary at the peak of SYM-H (with AE index ~ 1300 nT) and the next ~8 h later on (1750 nT). An additional south-to-north improve of IMF Bz (22:00 UT) terminated the auroral action, which remained at low degrees through the IP shock of the 2nd storm. S2 celebration was initiated in the course of northward IMF by the sudden favourable impulse triggering rapid expansion of SYM-H to fifty four nT. In the next the next several hours By and Bz modified their orientation various instances. Curiously, Whilst IMF problems were being dynamic, AE index elevated by degrees as many as 1200 nT. schimb cauciucuri Sector 1 The north-south change of Bz polarity (~2:20 UT, 9 March) brought about enhancement of geomagnetic storm with minimal of SYM-H at the level −148 nT.
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