Abstract
Non-tidal variations of gravity are the residual part of the monitoring of the variations after subtraction from them the lunar-solar gravity variations and the drift of the zero point of the gravimeter. Non-tidal variations have a complex morphology and structure. The sources of the non-tidal variations are the intracrustal processes, flows of the charged particles in space and meteor showers. Meteor showers interacting with the Earth’s atmosphere determine the occurrence, development and movement in the atmosphere of the large-scale eddies - cyclones and anticyclones. The atmospheric fronts are distinguished in isolated cyclones. These fronts can influence the measurements of the gravimeters and seismographs.
Highlights
Ê ë þ ÷ åâûåñëîâà: àòìîñôåðíûé ôðîíò; íåïðèëèâíûå âàðèàöèè ñèëû òÿæåñòè; ëóííî-ñîëíå÷íûå âàðèàöèè ñèëû òÿæåñòè; ìåòåîðíûå ïîòîêè; ïóëüñàöèè ñåéñìè÷åñêîãî è ãðàâèòàöèîííîãî ïîëåé
Non-tidal variations of gravity are the residual part of the monitoring of the variations after subtraction from them the lunar-solar gravity variations and the drift of the zero point of the gravimeter
The atmospheric fronts are distinguished in isolated cyclones
Summary
Ê ë þ ÷ åâûåñëîâà: àòìîñôåðíûé ôðîíò; íåïðèëèâíûå âàðèàöèè ñèëû òÿæåñòè; ëóííî-ñîëíå÷íûå âàðèàöèè ñèëû òÿæåñòè; ìåòåîðíûå ïîòîêè; ïóëüñàöèè ñåéñìè÷åñêîãî è ãðàâèòàöèîííîãî ïîëåé. Íà÷íåì ðàññìîòðåíèå âîïðîñà ñ ïóëüñàöèé íåïðèëèâíûõ âàðèàöèé ñèëû òÿæåñòè è ñåéñìè÷åñêîãî ïîëÿ, êîòîðûå ðàíåå áûëè âûÿâëåíû è òàê íàçâàíû â [1, 3]. Äåëî â òîì, ÷òî ïóëüñàöèè ñèëû òÿæåñòè è ñåéñìè÷åñêèå ïóëüñàöèè ñîâïàäàþò ìåæäó ñîáîé, î ÷åì ïîäðîáíî èçëîæåíî â [4]. Ïóëüñàöèè ñèëû òÿæåñòè âî Âëàäèâîñòîêå è Áèøêåêå ñîâïàäàþò ìåæäó ñîáîé Ñëåäóåò òàêæå îòìåòèòü, ÷òî àìïëèòóäà ïóëüñàöèè ïðàêòè÷åñêè ïîâòîðÿåò àìïëèòóäó ñðåäíåêâàäðàòè÷åñêîé ïîãðåøíîñòè èçìåðåíèé, âû÷èñëåíèå êîòîðîé ïðåäóñìîòðåíî â ïðîãðàììíîì ïðîäóêòå ãðàâèìåòðà [1, 4].
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