Полярные геомагнитные возмущения и связанные с ними явления : материалы международного симпозиума «Полярные геомагнитные явления», 25-31 мая 1986 г., Суздаль / Междунар. геодез. и геофиз. союз, междунар. ассоциация геомагнетизма и аэрономии, АН СССР, КНЦ, ПГИ. – Апатиты : [б. и.], 1989.

Pig.7. a - before an d b - af t e r r e aching the nec e s s a r y accuracy i n the numerical procedure. w o r k of Roble et al.(197B). For determining the n onstationary picture of the ionization d ensity the problem (1), (3) is solved by nonexplicit differential scheme f o r a (Danov and Kartalev,1986). In such a n a p p r o a c h the step along t, i.e. A t , m a y be of the order of 10 в, and the step along z- i z - a b o u t 2 km. C o n v e r g ence of the iterative process seoures smoothness of the profile of N within the whole interval (120,170 km) a n d we can speak about truetworthy results w h e n z < 200 k m as distinguished f r o m similar situations i n many i n v estiga tions. R e s u l t s . In the numerical s olving of the considered problem the models are chosen for d i s t r ibution of temperature of the neutral component (model MSIS) and the mass of the neutral component (Clark et al.,1970). Using these data one determines p Q and p0 fr o m equatio n (5) of the Appendix. The value of T 120 is taken 355°K.. I n M i llstone Hill a n d A recibo their, corresponding magnet i c indices A p are accounted for. The n u m e r i c a l l y received normalized amplitude fun c t i o n of the vertical component of the n eutral v elocity fo r Millstone Hill a n d its c orresponding a m p litude funotions for d isturb ances i n density, pressure, h o r izontal velocity, and temperature are given i n P i g . 1-5. P i g . 6 gives the shape of the solitone go i n g through Millstone Pig. 1. N o r malized amplitude Pig. 2. Nor m a l i z e d amplitude fu n c t i o n of the vertical component f u n c t i o n of the horizontal velocity, of the neutral v e l o c i t y for Millstone Num e r i c a l results. Hill. Numerical results. 97