Abstract
A method for determination of the difference in parameters of the Earth's tidal waves 0 1 and K 1 , which is generated by the Earth's liquid core and reveals itself in the dynamics of its surface, has been improved. The testing on the base of the experimental findings gathered on six tiltmeter stations indicates the improved accuracy in determination of the diurnal tidal waves parameters that can be used for modeling of the internal fine structures of the Earth.
Highlights
Âíóòð3øíþ áóäîâó Çåìë3 äîñë3äæóþòü ìåòîäîì ìîäåëþâàííÿ 3 ç3ñòàâëåííÿ ïàðàìåòð3â ìàòåìàòè÷íî¿ ìîäåë3 3ç ðåàëüíèìè äàíèìè ãåîëîã3÷íèõ, ñåéñì3÷íèõ òà çåìíîïðèïëèâíèõ ñïîñòåðåæåíü
A method for determination of the difference in parameters of the Earths tidal waves Î1 and Ê1, which is generated by the Earths liquid core and reveals itself in the dynamics of its surface, has been improved
Çåìíîïðèïëèâí3 ñïîñòåðåæåííÿ 3íôîðìóþòü ïðî ðåàêö3þ âñ3o¿ Çåìë3 íà âïëèâ êîñì3÷íèõ ñèë, ùî äîáðå â3äîì3
Summary
Âíóòð3øíþ áóäîâó Çåìë3 äîñë3äæóþòü ìåòîäîì ìîäåëþâàííÿ 3 ç3ñòàâëåííÿ ïàðàìåòð3â ìàòåìàòè÷íî¿ ìîäåë3 3ç ðåàëüíèìè äàíèìè ãåîëîã3÷íèõ, ñåéñì3÷íèõ òà çåìíîïðèïëèâíèõ ñïîñòåðåæåíü. A method for determination of the difference in parameters of the Earths tidal waves Î1 and Ê1, which is generated by the Earths liquid core and reveals itself in the dynamics of its surface, has been improved. The testing on the base of the experimental findings gathered on six tiltmeter stations indicates the improved accuracy in determination of the diurnal tidal waves parameters that can be used for modeling of the internal fine structures of the Earth. Çà ðîçðàõóíêàìè [Melhior,1983], ð3çíèöÿ àìïë3òóäíèõ ôàêòîð3â J ïðèïëèâíèõ õâèëü Î1 3 Ê1 ( JO1 J K1 ) ìào ñòàíîâèòè â3ä 0,040 äî 0,046 (ìîäåë3 I, II) ç3 çíàêîì «ì3íóñ».
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
