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地球科学 1941

《日射准则与冰期问题》

米卢廷·米兰科维奇

地球轨道的缓慢摆动调暗了高纬度的夏日阳光——并为冰期定下节拍。

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In depth · the introduction

冰期的来去并非随机——它们与地球在轨道上的缓慢摇摆同步而行。

核心思想

地球绕日的方式并非一成不变。它的轨道时而拉长、时而复圆;它的地轴时而更直立些、时而更倾斜些;而那倾斜的地轴又像陀螺般缓缓打转,改变着「地球离太阳最近时正逢哪个季节」。每一种摆动都很轻微,又各以漫长的节律重复——动辄数万年。

米卢廷·米兰科维奇证明:它们合在一起,会改变到达遥远北方的夏季阳光有多少。而要紧的,正是那里的夏季太阳:当北方的夏天变凉,前一个冬天的积雪便无法完全融尽。年复一年,雪越积越厚,冰期于是开始。暖夏把雪融退,冰川便后撤。

它如何形成

这一想法有位苏格兰先驱——自学成才、当过门房的科学家詹姆斯·克罗尔(James Croll)。他在 1860 年代把冰期与轨道联系起来——却错猜成因是寒冷的冬天。米兰科维奇,一位转任贝尔格莱德教授的塞尔维亚工程师,约从 1911 年起立志把整件事化为精确的数学,地球、火星、金星一并算来。

那是一生的手算。第一次世界大战期间,他甚至以战俘之身,在布达佩斯的一座图书馆里继续演算。关键的指点来自气候学家弗拉迪米尔·柯本(Wladimir Köppen)——他与女婿、以「大陆漂移」闻名的阿尔弗雷德·魏格纳一道,劝米兰科维奇聚焦于高纬度的夏季。他们 1924 年的著作刊出了米兰科维奇的曲线,而它与已知的四次阿尔卑斯冰期一一吻合。

它为何重要

冰期第一次有了一座钟。不再是「过去比较冷」这样含糊的故事,而是写在太阳系几何里的、对冰川何时进退的精确预言。它把我们这颗行星的气候史,系到了诸天的运动之上,也给了地质学家一份可与岩石——并最终与海底的泥芯——对照检验的历法。

一个类比

想象有三个调光开关,接在照向遥远北方的夏季太阳上。一个是地球的倾角,一个是轨道的形状,一个是季节的时机。每个都按自己缓慢的时间表上下滑动。多数时候,它们的设置彼此部分抵消。但每隔一阵,三者会一齐调暗——北方的夏天变得黯淡而凉爽,雪不再融化,冰便向南爬行。米兰科维奇的成就,正是把这三个旋钮的确切位置,一读就读了几十万年。

一个倾斜的地球、一个太阳位于焦点的小轨道,以及一个北纬 65° 夏季阳光的竖直量表。三个滑块设定倾角、轨道形状与夏季落点;移动它们,量表随之变亮或变暗。

它的位置

米兰科维奇纠正并补全了一个比他更古老的想法(阿德马尔、克罗尔),又把它交给了未来。它在整个 1950 年代被否定,却在 1976 年获得证实——人们发现深海岩芯恰恰以他那些轨道周期脉动。如今,它支撑着我们为地球史最近这几百万年的定年。它属于本馆其他几把气候之钥——阿伦尼乌斯论温室效应(arrhenius-1896)、基林所测上升的二氧化碳(keeling-1960)——也与魏格纳漂移的大陆(wegener-1912)为伴:正是魏格纳的合作者柯本,帮米兰科维奇指对了方向。

The original document
Original source text
Milutin Milanković (1879–1958) · Kanon der Erdbestrahlung und seine Anwendung auf das Eiszeitenproblem · Royal Serbian Academy, Belgrade, 1941 (in German)
The cosmic problem
Milanković opens by setting himself a single, audacious problem: to compute, from celestial mechanics alone, exactly how much solar radiation each latitude of a planet receives in each season — and how that has changed over geological time. He solves it for the Earth and sketches it for Mars and Venus. The whole edifice rests on Newtonian gravitation and spherical astronomy; nothing is fitted to the geological record in advance.
The three orbital elements
Three slow changes in the Earth's motion govern the answer. The eccentricity of the orbit — how far from a circle the ellipse is — breathes in and out over roughly 100,000 and 413,000 years. The obliquity, the tilt of the spin axis, nods between about 22.1° and 24.5° over roughly 41,000 years. And the precession of the equinoxes — the slow swivel of the tilted axis, combined with the turning of the orbit's own long axis — shifts the season at which the Earth is nearest the Sun, with periods near 23,000 and 19,000 years.
The insolation integral
From these elements Milanković integrates the radiation arriving over a day and over a 'caloric' half-year. With Köppen's advice he fixes attention on the summer half-year at high northern latitudes, expressing each result as the latitude that would receive the same summer radiation today — the 65°N equivalent latitude. The governing quantity is the high-latitude summer insolation, not the annual total.
The curves of the past 600,000 years
He computes the summer-insolation curve back through six hundred millennia, entirely by hand. The criterion, again Köppen's: ice ages are born of cool summers that fail to melt the winter snow, not of cold winters. The dips in the curve are read as glacial epochs — and they line up with the four Alpine glaciations (Günz, Mindel, Riss, Würm) that Penck and Brückner had mapped from the field.
What lies beyond the astronomy
Milanković is candid that the orbital forcing is only the trigger. The amplification — growing ice that reflects more sunlight, shifting oceans and carbon — belongs to a physics he does not claim to have solved. The Canon supplies the metronome; the orchestra of feedbacks is left to others.
[ … ]
Belgrade, 1941