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In this review ROTI values have been computed on the basis of preprocessed relative STEC time sequence in lieu of raw observations. Therefore, the outliers, remaining an result of cycle-slips, ended up taken out.

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The effects for the 2nd working day of S2 function (9 March) depict the dependence of TEC fluctuation depth on auroral electrojet (#six). As a result, analysing nightside ionosphere one can notice the improvement of ROTI values (approximately ~2.0 TECU/min) equivalent to the versions of AE index. In addition, Every single of these kinds of phases was followed by poleward change of robust TEC fluctuations linked to substorm improvement. The dayside TEC fluctuation was slightly weaker and smoothed in time area. In this instance we detected the gradual poleward shift of maximal ROTI values from sixty° to 72°.

At this point the drawing you’re importing need to be placed someplace during the Energetic Inventor undertaking area.

In the situation of northwardly oriented IMF, we observed the poleward shift of maximal ROTI values. For these situations the nightside ionosphere was relatively tranquil, Whilst the sunlit component was characterized by reasonable TEC fluctuation observed at 75°–eighty° of AACGM latitude. The outcomes of TEC fluctuation confirmed that ROTI can be employed for patch detection, but its efficiency strongly depends on signature of distinct composition.

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I’ll scale the drawing based upon the origin (0,0) place and another point I will do is shift your entire drawing so on the list of connector finishes is location at the drawing origin issue.

This difference was due to a little spatial extent of sectors close to the geomagnetic pole and resulted in a bigger quantity of samples offered there. In this latter situation (previously mentioned eighty°) the factors were being preliminarily projected on midday-midnight axis and after that the latitudes of these kinds of facts were being utilized to organize Figure 6c and d. The ROTI and relative STEC were being computed for all stations supplied in Determine four with the applying of your elevation mask equivalent to thirty°. Subsequently, they were being transformed to MLT-AACGM latitude reference frame using ionosphere single layer product with top adopted at 350 km. AACGM coordinates were being computed according to methodology proposed by Shepherd (2014).