, 2013; Jin et al., 2014). Having said that, mainly because of the exceptional ambiguity expression for each observational arc, L4 time sequence were commonly presented individually for specific satellite. This function demonstrates the algorithm of combined processing of these types of observations collected by a network of everlasting GNSS receivers, which may be regarded as the primary novelty.
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Nevertheless, resulting from the intense good results associated with, e.g. the polar cap patches, the fitting is applied in numerous way determined by detected TEC variants. The process is done for every arc by means of 3-action course of action:
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Throughout the two durations an average TEC fluctuation arrived at nearly 1.5 TECU/min. The significant ROTI values while in the polar cap are linked to patch propagation depicted in Determine 10a. Determine 13a supplies also more specific perspective of conditions amongst these periods. It demonstrates the mitigation of TEC fluctuation to the nightside, While within the sunlit element it is basically unchanged. In the second circumstance a person can also notice the poleward displacement of sturdy ionospheric variations to seventy five°–78° of latitude. This seems to be a consequence of northward IMF, partly shown in OMNI info, and particle precipitation controlled by a lobe reconnection (Østgaard et al., 2003). Such conditions explain The dearth of patches between durations #one and #two depicted in Determine 10a.
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With the boundaries of such intervals the information from different arcs overlap each other. Be sure to also Notice the dawn-dusk extension of sector may end in pretty much undisturbed details for a few satellites. In this kind of case the used range automatically excludes the arcs without any signatures. Being an indicator we used maximal relative STEC worth at each epoch.
Regardless of the inhomogeneous distribution of receivers, which can be connected to their reduced variety for picked areas and land mass configuration, this coverage makes it possible for the detection of unique ionospheric buildings as well as their convection.
Throughout S2 storm the values of AE index were being maximal in the whole analysed time period and exceeded 2500 nT. The third geomagnetic storm was preceded by two IP shocks. The very first of these caused only the average modifications of magnetic discipline and was followed by slow reduce of SYM-H values around −40 nT, whereas the 2nd one initiated the key section of S3 party. The correction of SYM-H index for solar wind ram strain introduced by Tsurutani et al. (2014) uncovered that the height of SYM-H (−seventy five nT) occurred at ~12:00 UT and so these types of epoch was adopted in Determine one. Taking this into consideration the powerful auroral action is detected only in the course of the main stage of S3. Very similar problem you can notice through the previous storm. After the IP shock, IMF Bz progressively dipped to −15 nT, what resulted in a very rapid lower of SYM-H. The height with the storm was characterized by SYM-H equivalent to −seventy nine nT. This celebration was afflicted by high velocity stream, which caused the prolonged recovery period with enhanced auroral activity (Verkhoglyadova et al., 2014).
For the alternative IMF polarity the polar structures were being noticeably less frequent and did not exceed ten TECU. Furthermore, We have now seen that STEC enhancement of detected patches diversified according to the dayside VTEC derived from world wide ionosphere maps. Because of this The mixing of each parameters may be beneficial to clarify the strength of patch exercise for different geomagnetic ailments.
However, the maximal growth of STEC is incredibly shut to those detected for GPS 1 and eleven. Figure three also depicts that algorithm operates the right way for reduced-elevated facts. The similar Evaluation for other constructions confirms the independence of relative STEC values on elevation angle and so you can think that the application of STEC-VTEC conversion would result in the distortion of effects. To be a consequence we decided to use the relative STEC values in the following analyses.