Abstract
Differences of relations between geomagnetic field and climate for Northern and Southern hemispheres considered earlier have been shown. They are connected, first of all, with the depth of penetration of the charged particles into the Earth’s atmosphere, modulated by geomagnetic field and their impact on the ozone balance near the tropopause. In the Northern hemisphere ozone formation in the lower stratosphere occurs during ionic-molecular autocatalitic cycle of ozone production, initiated by GCR, and in the Southern one — as a result of “self-reduction” of ozone initiated by solar energetic particles. Explanation of the observed simultaneous warming in the Western Antarctica and the fall of temperature in the Central and Eastern Antarctica has also been presented.
Highlights
Ïîêàçàíî â3äì3ííîñò3 ðîçãëÿíóòèõ ðàí3øå çâÿçê3â ì3æ ãåîìàãí3òíèì ïîëåì 3 êë3ìàòîì äëÿ Ï3âí3÷íî¿ 3 Ï3âäåííî¿ ï3âêóëü
Îáíàðóæåíî òàêæå ñîâïàäåíèå ïîëîæåíèÿ ìèíèìóìîâ è ìàêñèìóìîâ èíòåãðàëüíûõ õàðàêòåðèñòèê ïîëåé ìîäóëÿ ïîëíîãî âåêòîðà íàïðÿæåííîñòè ìàãíèòíîãî ïîëÿ, òåìïåðàòóðû è äàâëåíèÿ, ñîäåðæàíèÿ îçîíà è óäåëüíîé âëàæíîñòè íà óðîâíå âåðõíåé òðîïîñôåðûíèæíåé ñòðàòîñôåðû (UTLS) çà âòîðóþ ïîëîâèíó ÕÕ â. â Ñåâåðíîì ïîëóøàðèè
Ïî àíàëîãèè ñ Ñåâåðíûì ïîëóøàðèåì [Êèëèôàðñêà è äð., 2015], ïðîàíàëèçèðîâàíû äàííûå ðåàíàëèçà ERA-40 è ERA Interim ïî ïðèçåìíîé òåìïåðàòóðå âîçäóõà T 2m, ïî ñîäåðæàíèþ îçîíà íà óðîâíå 70 ãÏà è óäåëüíîé âëàæíîñòè íà óðîâíå 150 ãÏà, à òàêæå âûïîëíåí ðàñ÷åò ìîäóëÿ ïîëíîãî âåêòîðà íàïðÿæåííîñòè ãåîìàãíèòíîãî ïîëÿ F è åãî âåêîâûõ âàðèàöèé ïî êîýôôèöèåíòàì IGRF
Summary
Ïîêàçàíî â3äì3ííîñò ðîçãëÿíóòèõ ðàí3øå çâÿçê3â ì3æ ãåîìàãí3òíèì ïîëåì 3 êë3ìàòîì äëÿ Ï3âí3÷íî¿ 3 Ï3âäåííî¿ ï3âêóëü. Âî âòîðîé ÷àñòè ñòàòüè ïðåäëîæåí ìåõàíèçì, êîòîðûé äåìîíñòðèðóåò ïðè÷èííîñëåäñòâåííóþ öåïî÷êó âçàèìîäåéñòâèé ìåæäó ðàçëè÷íûìè àòìîñôåðíûìè ïàðàìåòðàìè è ãåîìàãíèòíûì ïîëåì [Êèëèôàðñêà è äð., 2015]. Êîòîðûé îáúÿñíÿåò, êàêèì îáðàçîì ìàãíèòíîå ïîëå Çåìëè ìîæåò âëèÿòü íà ïðîñòðàíñòâåííîå ðàñïðåäåëåíèå è âàðèàöèè ïðèçåìíîé òåìïåðàòóðû âîçäóõà [Kilifarska, 2012à, á; Êèëèôàðñêà è äð., 2015]. Ïî àíàëîãèè ñ Ñåâåðíûì ïîëóøàðèåì [Êèëèôàðñêà è äð., 2015], ïðîàíàëèçèðîâàíû äàííûå ðåàíàëèçà ERA-40 è ERA Interim ïî ïðèçåìíîé òåìïåðàòóðå âîçäóõà T 2m (íà âûñîòå 2 ì íàä çåìíîé ïîâåðõíîñòüþ), ïî ñîäåðæàíèþ îçîíà íà óðîâíå 70 ãÏà è óäåëüíîé âëàæíîñòè íà óðîâíå 150 ãÏà (áûëè èñïîëüçîâàíû ñåçîííûå äàííûå äëÿ çèìíèõ ìåñÿöåâ, åñëè íå óêàçàíî äðóãîå), à òàêæå âûïîëíåí ðàñ÷åò ìîäóëÿ ïîëíîãî âåêòîðà íàïðÿæåííîñòè ãåîìàãíèòíîãî ïîëÿ F (íÒë) è åãî âåêîâûõ âàðèàöèé ïî êîýôôèöèåíòàì IGRF
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