藏书架 登录注册
死在火星上 > 死在火星上最新目录

对火星轨道变化问题的最后解释

上一章      返回目录      下一章

不可抗御的原因,域名改为dsyq.org/感谢收藏^_^

tively,.

notethatdifferentoperatingsysternungularmomentum,whichshouldberigorouslypreserveduptomachine-eprecision.

sincethesyparethetestintegrationwiththetedtothevalue~8700°,about25rotationsofearthafter5gyr,,thelongitudeerrorofplutocanbeestimatedas~12°.thisvalueforplutoismuchbetterthantheresultinkinoshitaamp;amp;nakai(1996)wherethedifferenceisestimatedas~60°.

3numericalresults–

:noorbitalcrossingsnorcloseencountersbetweenanypairofplanetstookplace.

first,,orbitalpositionsoftheterrestrialplanetsdifferlittlebetweentheinitialandfinalpartofeachnuaryorbitalmotionremainnearlythesameastheyareatpresent.

verticalviewofthefourinnerplanetaryorbits(frondfinalpartsoftheintegrationsn±.(a)theinitialpartofn+1(t=x109yr).(b)thefinalpartofn+1(t=xx109yr).(c)theinitialpartofn?1(t=0to?x109yr).(d)thefinalpartofn?1(t=?x109to?x109yr).ineachpanel,x(takenfromde245).

thevariationofeccentricitiesandorbitalinclinationsfortheinnerfourplanetsintheinitialandfinalpartoftheintegrationn+,thecharacterofthevariationofplanetaryorbitaleles;s(1994,1996),.

theorbitalsseeroverthistime-span(seealsosection5).

–frequencymaps

althoughtheplanetaryrlyinthecaseofearth,canpotentiallyhaveasignificanteffectonitssurfaceclirinsolationvariation().

togiveanoverviewofthelong-teraryorbitalskars(1990,1993)frequencyanalysis.

.

eachfragrgeoverlappingpart:forexample,whentheithdatabeginsfromt=tiandendsatt=ti+t,thenextdatasegmentrangesfromti+δt≤ti+δt+t,whereδt?+treachesthetotalintegrationlenh.

weapplyanffttoeachofthedatafragments,andobtainnfrequencydiagrams.

ineachfrequencydiagracedbyagrey-scale(orcolour)chart.

weperforcexisrepresentstheperiod(orfrequency)oftheoscillationoforbitalelements.

wehaveadoptedanfftbecauseofitsoverwhelposedintofrequencyponentsisterriblyhuge(severaltensofgbytes).

atypicalexabyplanetandelementbyelement.

wecalculateverylong-periodicvariationandexchangeofplanetaryorbitalenergyandangularunayelementsl,g,=?,,suchasymptomofinstabilityisnotprominentinourlong-termintegrations.

,thetotalorbitalenergyandangularponent(h-h0),g0,,.

cosandallnineplanets,itisapparentthattheasares::,,wecannotneglectthecontributionfros,aswewillseeinsubsequentsections.

+1andn?,,,wecanseethatarysubsystem.

itisnotclearatthearyorbitalenergy(whichisdirectlyrelatedtothesesthanistheangulartestoe).hence,theeccentricitiesofvenusandearthcanbedisturbedeasilybyjupiterandsaturn,,–earthp

本章 共3页 / 第2页 ,请点击下一章继续阅读!

上一章      返回目录      下一章