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scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

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STP12 Abstracts<br />

Berlin, 12 - 16 July <strong>2010</strong><br />

SCOSTEP Symposium <strong>2010</strong><br />

A partial review of current progress with our un<strong>der</strong>st<strong>an</strong>ding of small scale ionospheric<br />

irregularities <strong>an</strong>d of some of the remaining challenges.<br />

St-Maurice Je<strong>an</strong>-Pierre<br />

ISAS, University of Saskatchew<strong>an</strong><br />

The advent of increasingly high temporal <strong>an</strong>d spatial resolution instruments coupled with a<br />

growing global perspective on the subject has me<strong>an</strong>t that even some very basic properties of<br />

ionospheric irregularities have continued to challenge our un<strong>der</strong>st<strong>an</strong>ding, this in spite of<br />

impressive progress in our capability to perform sophisticated numerical simulations. A brief<br />

presentation on the subject c<strong>an</strong> only cover a limited r<strong>an</strong>ge of topics. Here we will only look at<br />

some of the challenges associated with short scale irregularities accessible to ground-based<br />

radars. Even then, there is a long list of questions to choose from such as: the age-old<br />

question of what causes the saturation of E region irregularities at something comparable to<br />

the ion-acoustic speed of the medium; how aspect <strong>an</strong>gles have to grow as individual structures<br />

evolve <strong>an</strong>d how these same aspect <strong>an</strong>gles relate to saturation <strong>an</strong>d to electron heating at high<br />

latitudes; the possible role played by <strong>an</strong>omalous diffusion; the possible origin of very low<br />

altitude E region echoes; the possible origin of up-down <strong>an</strong>d east-west asymmetries seen in E<br />

region echoes below 105 km at low latitudes; the non-local character of gradient-drift<br />

irregularities higher up; what we know we don't know about so-called 150 km echoes; `wall<br />

echoes' in the lower F region at mid-latitudes; the origin of the systematic lower Doppler<br />

shifts seen by HF radars in comparison to drifts determined from other techniques; the<br />

question of what seeds equatorial spread F <strong>an</strong>d the possible connection with the pre-reversal<br />

enh<strong>an</strong>cement in the low latitude electric field.

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