对火星轨道变化问题的最后解释(第10/16页)
in each frequency diagranbsp;obtained above， the strengthperiodicity canreplaceda greyscalecolour chart.
we perfornbsp;the replacent， and connect all the greyscalecolour charts into one graph for eac horizontal axisthese new graphs shouldthe ti， i.e. the starting tiseach fragntdata ti， where i 1，…， n. the vertical axis represents the periodfrequencythe oscillationorbital elents.
we have adoptedfft becauseits overwhelng speed， since the auntnurical databe dposed into frequency&nbspponentsterribly hu several tensgbytes.
a typical exalethe ti–frequencreatedthe above proceduresshowna greyscale diagranbsp;a， which shows the variationperiodicitythe entricity and inclinationearthn fig. 5， the dark area shows thattheindicatedthe valuethe abscissa， the periodicity indicatedthe ordinatestronr thanthe lighter area around it.can recognize fronbsp;thihat the periodicitythe entricity and inclinationearth only chans slightly over the entire period coveredthearly regular trendqualitatively thein other integrations and for other pls， although typical frequencies differbyand elentelent.
4.2 longternbsp;exchanorbital energy and angular ntubr>
we calculate very longperiodic variation and exchanplary orbital energy and angular ntunbsp;using filtered delaunay elents l， g， h. g anre equivalentthe plary orbital angular ntunbsp;and its vertical&nbspponent per unit ss. lrelatedthe plary orbital enerr unita the systenbsp;is&nbsppletely linear， the orbital energy and the angular ntunbsp;in each frequency binbthe plary systenbsp;can causeex
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we perfornbsp;the replacent， and connect all the greyscalecolour charts into one graph for eac horizontal axisthese new graphs shouldthe ti， i.e. the starting tiseach fragntdata ti， where i 1，…， n. the vertical axis represents the periodfrequencythe oscillationorbital elents.
we have adoptedfft becauseits overwhelng speed， since the auntnurical databe dposed into frequency&nbspponentsterribly hu several tensgbytes.
a typical exalethe ti–frequencreatedthe above proceduresshowna greyscale diagranbsp;a， which shows the variationperiodicitythe entricity and inclinationearthn fig. 5， the dark area shows thattheindicatedthe valuethe abscissa， the periodicity indicatedthe ordinatestronr thanthe lighter area around it.can recognize fronbsp;thihat the periodicitythe entricity and inclinationearth only chans slightly over the entire period coveredthearly regular trendqualitatively thein other integrations and for other pls， although typical frequencies differbyand elentelent.
4.2 longternbsp;exchanorbital energy and angular ntubr>
we calculate very longperiodic variation and exchanplary orbital energy and angular ntunbsp;using filtered delaunay elents l， g， h. g anre equivalentthe plary orbital angular ntunbsp;and its vertical&nbspponent per unit ss. lrelatedthe plary orbital enerr unita the systenbsp;is&nbsppletely linear， the orbital energy and the angular ntunbsp;in each frequency binbthe plary systenbsp;can causeex
本章未完，请点击下一页继续阅读 》》