卷四·第 232–238 问 正午影、卯酉圈、晡时影、礼拜朝向与七个气候带
正午影随纬度的三种情形,卯酉圈上的高度,晡礼之影,礼拜朝向的方位,七个气候带的表,以及气候带以北直到北极的天象。
§232. Into how many kinds are the shadows of midday and its altitude divided?
The tip of the shadow at midday is always towards the north in the lands whose latitudes exceed the amount of the greatest declination, and the altitude of midday there is on the side of the south; I mean that its complement is the distance of the Sun from the zenith towards the south. There the Sun has a greatest altitude in summer, whose shadow is the shortest of the shadows, and that is at the beginning of Cancer; a least altitude in winter, whose shadow is the longest of the midday shadows, and that is in Capricorn; and a third altitude midway between them, equal to the complement of the latitude of the town, whose shadow is called the shadow of equality or the shadow of the equinox, because it and that altitude occur when the Sun enters the beginning of Aries or the beginning of Libra. In the lands whose latitude equals the greatest declination, what we have mentioned holds good, except for the greatest of the midday altitudes, which there is 90 degrees exactly, not ascribed to north or to south; and the shadow then vanishes there and comes to nothing. In the lands whose latitudes from the equator fall short of the amount of the greatest declination, the state of the winter altitude and the equinoctial altitude, and of what follows them, is also as described above; but the summer altitude is on the side of the north. That is because when the Sun, in its ascent in the north and in its descent from it, has a declination equal to the latitude of the town, it passes over its zenith, and the shadow vanishes there at midday. Then, when its declination exceeds the latitude of the town, the altitude of midday comes to be on the side of the north, and its complement is the Sun's distance from the zenith on that side; and the altitude of midday does not increase as it used to increase on the side of the south, but decreases, as far as the beginning of Cancer, and there it begins to increase. When the altitude is in the north, the tip of the midday shadow is found there once towards the north and once towards the south of the base of the gnomon; and so those lands are called the lands of two shadows, because the tip of the midday shadow is found there once towards the north and another time towards the south.
翻译点开
§232. Into how many kinds are the shadows of midday and its altitude divided?
第二百三十二问 正午的影与高度分为几种?
The tip of the shadow at midday is always towards the north in the lands whose latitudes exceed the amount of the greatest declination, and the altitude of midday there is on the side of the south; I mean that its complement is the distance of the Sun from the zenith towards the south. There the Sun has a greatest altitude in summer, whose shadow is the shortest of the shadows, and that is at the beginning of Cancer; a least altitude in winter, whose shadow is the longest of the midday shadows, and that is in Capricorn; and a third altitude midway between them, equal to the complement of the latitude of the town, whose shadow is called the shadow of equality or the shadow of the equinox, because it and that altitude occur when the Sun enters the beginning of Aries or the beginning of Libra. In the lands whose latitude equals the greatest declination, what we have mentioned holds good, except for the greatest of the midday altitudes, which there is 90 degrees exactly, not ascribed to north or to south; and the shadow then vanishes there and comes to nothing. In the lands whose latitudes from the equator fall short of the amount of the greatest declination, the state of the winter altitude and the equinoctial altitude, and of what follows them, is also as described above; but the summer altitude is on the side of the north. That is because when the Sun, in its ascent in the north and in its descent from it, has a declination equal to the latitude of the town, it passes over its zenith, and the shadow vanishes there at midday. Then, when its declination exceeds the latitude of the town, the altitude of midday comes to be on the side of the north, and its complement is the Sun's distance from the zenith on that side; and the altitude of midday does not increase as it used to increase on the side of the south, but decreases, as far as the beginning of Cancer, and there it begins to increase. When the altitude is in the north, the tip of the midday shadow is found there once towards the north and once towards the south of the base of the gnomon; and so those lands are called the lands of two shadows, because the tip of the midday shadow is found there once towards the north and another time towards the south.
在纬度超过最大赤纬的地方,正午的影端总是朝北,那里的正午高度在南方一侧;我是说,它的余弧就是太阳在天顶以南离天顶的距离。在那里,太阳有一个夏季的最大高度,其影是诸影中最短的,那是在巨蟹座起点;有一个冬季的最小高度,其影是正午诸影中最长的,那是在摩羯座;还有第三个高度,居于二者正中,等于城市纬度的余弧,其影称为均等之影或春秋分之影,因为它和那个高度出现在太阳进入白羊座起点或天秤座起点之时。在纬度等于最大赤纬的地方,我们所说的都成立,只有正午的最大高度例外:那里它恰为九十度,不属北也不属南;那时影子在那里消失,化为乌有。在离赤道的纬度不足最大赤纬的地方,冬季高度与春秋分高度以及随之而来的情形,也如上所述;但夏季高度在北方一侧。那是因为太阳在北方上升与下降的途中,当它的赤纬等于城市纬度时,它经过城市的天顶,正午时影子在那里消失。然后,当它的赤纬超过城市纬度时,正午高度就到了北方一侧,它的余弧就是太阳在那一侧离天顶的距离;而且正午高度不再像在南方一侧时那样增加,而是减小,一直到巨蟹座起点,从那里它又开始增加。当高度在北方时,正午影端在那里有时在表基之北,有时在表基之南;所以那些地方称为有两种影的地方,因为正午影端在那里一时朝北、一时朝南。
大意与图解点开
🔎 大意:纬度大于最大赤纬处,正午影恒朝北,夏至最短、冬至最长、春秋分居中;纬度等于它时夏至无影;小于它时一年中影有南北两向。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 最大赤纬 | the greatest declination | 本书取二十三度三十五分 |
| 均等之影 | the shadow of equality | 春秋分正午之影 |
| 表基 | the base of the gnomon | 表立地之处 |
| 有两种影的地方 | lands of two shadows | 正午影时南时北之地 |
🧭 图解与讲解
这一问把正午影分成三种情形,分界就是最大赤纬(本书取二十三度三十五分)。纬度大于它的地方,正午太阳终年在天顶以南,影端终年朝北:夏至(巨蟹座起点)高度最大、影最短,冬至(摩羯座)高度最小、影最长,春秋分的高度正在两者中间,等于纬度的余弧,这时的影叫“均等之影”或“春秋分之影”(图一)。
〔图〕纬度大于最大赤纬之地,正午影总朝北:夏至最短、冬至最长,春秋分之影居中
| 城市纬度 | 正午太阳 | 正午影 | 特别之处 |
|---|---|---|---|
| 大于最大赤纬 | 终年在天顶以南 | 终年朝北 | 夏至最短,冬至最长,春秋分之影居中 |
| 等于最大赤纬 | 夏至恰在天顶(九十度) | 平时朝北 | 夏至正午无影 |
| 小于最大赤纬 | 赤纬超过纬度时在天顶以北 | 时北时南 | 一年两次过天顶,两次无影;称“有两种影的地方” |
纬度恰等于最大赤纬的地方,夏至正午太阳正在天顶,高度九十度,“不属北也不属南”,影子消失。纬度更小的地方,太阳北行时会先后两次经过天顶:赤纬等于本地纬度时,正午无影;赤纬再大,太阳就到了天顶以北,正午影反朝南,而正午高度不增反减,直到夏至再回升。这些地方正午影一年中有时朝北、有时朝南,所以叫“有两种影的地方”(表二)。
比鲁尼的叙述其实就是一个公式:正午高度等于纬度余弧加上太阳的赤纬(北正南负),超过九十度时就要从北边量。这个关系反过来,就是古人测纬度的主要办法:量春秋分的正午影,便得纬度的余弧;量夏至、冬至的正午影,两者相差即两倍最大赤纬。下文气候带表里的“夏至正午影”一栏,就是这样算出来的。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 最大赤纬 | the greatest declination | 本书取二十三度三十五分 |
| 均等之影 | the shadow of equality | 春秋分正午之影 |
| 表基 | the base of the gnomon | 表立地之处 |
| 有两种影的地方 | lands of two shadows | 正午影时南时北之地 |
🧭 图解与讲解
这一问把正午影分成三种情形,分界就是最大赤纬(本书取二十三度三十五分)。纬度大于它的地方,正午太阳终年在天顶以南,影端终年朝北:夏至(巨蟹座起点)高度最大、影最短,冬至(摩羯座)高度最小、影最长,春秋分的高度正在两者中间,等于纬度的余弧,这时的影叫“均等之影”或“春秋分之影”(图一)。
| 城市纬度 | 正午太阳 | 正午影 | 特别之处 |
|---|---|---|---|
| 大于最大赤纬 | 终年在天顶以南 | 终年朝北 | 夏至最短,冬至最长,春秋分之影居中 |
| 等于最大赤纬 | 夏至恰在天顶(九十度) | 平时朝北 | 夏至正午无影 |
| 小于最大赤纬 | 赤纬超过纬度时在天顶以北 | 时北时南 | 一年两次过天顶,两次无影;称“有两种影的地方” |
纬度恰等于最大赤纬的地方,夏至正午太阳正在天顶,高度九十度,“不属北也不属南”,影子消失。纬度更小的地方,太阳北行时会先后两次经过天顶:赤纬等于本地纬度时,正午无影;赤纬再大,太阳就到了天顶以北,正午影反朝南,而正午高度不增反减,直到夏至再回升。这些地方正午影一年中有时朝北、有时朝南,所以叫“有两种影的地方”(表二)。
比鲁尼的叙述其实就是一个公式:正午高度等于纬度余弧加上太阳的赤纬(北正南负),超过九十度时就要从北边量。这个关系反过来,就是古人测纬度的主要办法:量春秋分的正午影,便得纬度的余弧;量夏至、冬至的正午影,两者相差即两倍最大赤纬。下文气候带表里的“夏至正午影”一栏,就是这样算出来的。
§233. What are the altitude and the shadow that have no azimuth?
This is a companion of the altitude of midday. The altitude circle passing through the intersection of the horizon with the equator is called the circle that has no azimuth, and it is also called the circle of the first of the azimuths (the prime vertical). When the Sun is on it, its altitude is the one that has no azimuth, and so is its shadow, because it lies in a straight line with the equinoctial line and so is not distant from it. This is not found for the Sun or anything else except when it has a declination in the north, just as it has no azimuth towards the north from the equinoctial line except together with a northern declination.
§234. What is the shadow of the afternoon (ʿaṣr)?
This belongs to the chapters of the imams on the end of the times of the noon prayer (ẓuhr) and the beginning and the end of the times of the afternoon prayer (ʿaṣr). When the shadow of midday is known, which they call the shadow at the declining (zawāl), and then the length of the gnomon is added to it once, and one watches until its shadow becomes of that amount, that is the beginning of the time of the afternoon prayer on that day according to the people of the Ḥijāz. It is called the addition of the like, and on instruments 'beginning of the ʿaṣr' is written against it. When the length of the gnomon is added twice to the shadow at the declining, and one then watches until its shadow becomes of that amount, that is the time of the afternoon prayer according to the people of Iraq. It is called the addition of the two likes, and on instruments 'end of the ʿaṣr' is written against it.
翻译点开
§233. What are the altitude and the shadow that have no azimuth?
第二百三十三问 何谓没有方位的高度与影?
This is a companion of the altitude of midday. The altitude circle passing through the intersection of the horizon with the equator is called the circle that has no azimuth, and it is also called the circle of the first of the azimuths (the prime vertical). When the Sun is on it, its altitude is the one that has no azimuth, and so is its shadow, because it lies in a straight line with the equinoctial line and so is not distant from it. This is not found for the Sun or anything else except when it has a declination in the north, just as it has no azimuth towards the north from the equinoctial line except together with a northern declination.
这是正午高度的伴侣。通过地平与天赤道交点的那个高度圈,称为没有方位之圈,也称为诸方位之首圈(即卯酉圈)。太阳在它上面时,它的高度就是没有方位的高度,它的影也是如此,因为影与春秋分线成一直线,所以不离开它。这对太阳或别的东西来说,只在它有北赤纬时才会出现,正如它不会有春秋分线以北的方位,除非同时有北赤纬。
§234. What is the shadow of the afternoon (ʿaṣr)?
第二百三十四问 何谓晡时之影?
This belongs to the chapters of the imams on the end of the times of the noon prayer (ẓuhr) and the beginning and the end of the times of the afternoon prayer (ʿaṣr). When the shadow of midday is known, which they call the shadow at the declining (zawāl), and then the length of the gnomon is added to it once, and one watches until its shadow becomes of that amount, that is the beginning of the time of the afternoon prayer on that day according to the people of the Ḥijāz. It is called the addition of the like, and on instruments 'beginning of the ʿaṣr' is written against it. When the length of the gnomon is added twice to the shadow at the declining, and one then watches until its shadow becomes of that amount, that is the time of the afternoon prayer according to the people of Iraq. It is called the addition of the two likes, and on instruments 'end of the ʿaṣr' is written against it.
这属于伊玛目们论晌礼时间之末与晡礼时间之始末的章节。当正午之影——他们称为偏转之影——已知,再把表长加上一次,然后守候到影长等于这个量,按希贾兹人的说法,那就是那一天晡礼时间的开始。这称为“加一倍”,器物上在它的对应处写着“晡时之始”。若在偏转之影上把表长加两次,再守候到影长等于这个量,按伊拉克人的说法,那就是晡礼的时间。这称为“加两倍”,器物上在它的对应处写着“晡时之末”。
大意与图解点开
🔎 大意:过正东正西的高度圈叫卯酉圈,太阳在其上时影正指东西;正午影加一倍表长为晡礼之始(希贾兹),加两倍为晡时(伊拉克)。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 卯酉圈 | the prime vertical | 过正东正西的高度圈 |
| 晡礼 | the afternoon prayer (ʿaṣr) | 午后的礼拜 |
| 晌礼 | the noon prayer (ẓuhr) | 正午后的礼拜 |
| 偏转之影 | the shadow at the declining (zawāl) | 太阳过中天时之影 |
| 加一倍 | the addition of the like | 正午影加一表长 |
🧭 图解与讲解
第二百三十三问是正午高度的“伴侣”。子午圈过正南正北,与它垂直、过正东正西(地平与天赤道的交点)的那条高度圈,阿拉伯人称“没有方位之圈”或“诸方位之首圈”,今称卯酉圈。太阳在这条圈上时,它在地平上的方向正是东或西,从春秋分线量起的方位为零,影子也正落在东西线上,所以叫“没有方位的高度”(图二)。
〔图〕晡时之影:正午之影加一倍表长是晡礼之始,加两倍是晡礼之末
〔图〕卯酉圈上的高度没有方位:太阳正在东西线上,影也正落在东西线上
比鲁尼补了一句限制:在北方有纬度的地方,太阳要有北赤纬,即在白羊到处女这半年,才会在地平以上经过卯酉圈;赤纬在南时,它升起就在东西线以南,整天不到这条圈上。这与上一章“日出方位的幅度”的道理相同。
第二百三十四问转入宗教实用。伊斯兰每日五次礼拜,晌礼在太阳偏过中天之后,晡礼在午后。教法学家(伊玛目)用表影来定时刻:先量出当天正午的影,即“偏转之影”(zawāl),再加上一个表长,影长到此即晡礼开始,这是希贾兹(Ḥijāz)人的说法,叫“加一倍”;加两个表长,是伊拉克人所定的晡礼时刻,叫“加两倍”(图一)。
当时的星盘、象限仪背面常刻有这两条线,标作“晡时之始”“晡时之末”,比鲁尼说的“器物上在它的对应处写着”就是指这个。这一问说明,测影这门学问在当时不只为占星和历法服务,也是每日礼拜的依据。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 卯酉圈 | the prime vertical | 过正东正西的高度圈 |
| 晡礼 | the afternoon prayer (ʿaṣr) | 午后的礼拜 |
| 晌礼 | the noon prayer (ẓuhr) | 正午后的礼拜 |
| 偏转之影 | the shadow at the declining (zawāl) | 太阳过中天时之影 |
| 加一倍 | the addition of the like | 正午影加一表长 |
🧭 图解与讲解
第二百三十三问是正午高度的“伴侣”。子午圈过正南正北,与它垂直、过正东正西(地平与天赤道的交点)的那条高度圈,阿拉伯人称“没有方位之圈”或“诸方位之首圈”,今称卯酉圈。太阳在这条圈上时,它在地平上的方向正是东或西,从春秋分线量起的方位为零,影子也正落在东西线上,所以叫“没有方位的高度”(图二)。
比鲁尼补了一句限制:在北方有纬度的地方,太阳要有北赤纬,即在白羊到处女这半年,才会在地平以上经过卯酉圈;赤纬在南时,它升起就在东西线以南,整天不到这条圈上。这与上一章“日出方位的幅度”的道理相同。
第二百三十四问转入宗教实用。伊斯兰每日五次礼拜,晌礼在太阳偏过中天之后,晡礼在午后。教法学家(伊玛目)用表影来定时刻:先量出当天正午的影,即“偏转之影”(zawāl),再加上一个表长,影长到此即晡礼开始,这是希贾兹(Ḥijāz)人的说法,叫“加一倍”;加两个表长,是伊拉克人所定的晡礼时刻,叫“加两倍”(图一)。
当时的星盘、象限仪背面常刻有这两条线,标作“晡时之始”“晡时之末”,比鲁尼说的“器物上在它的对应处写着”就是指这个。这一问说明,测影这门学问在当时不只为占星和历法服务,也是每日礼拜的依据。
§235. What is the azimuth of the qibla?
It is the meeting of the horizon of the town with the circle that passes through the zenith of the people of that town and of the people of Mecca [corrected: MS omits 'and of the people of Mecca']; and its distance from the equinoctial line or from the meridian line is the amount by which the one who prays must turn away from these. This is the figure of it.

翻译点开
§235. What is the azimuth of the qibla?
第二百三十五问 何谓礼拜朝向的方位?
It is the meeting of the horizon of the town with the circle that passes through the zenith of the people of that town and of the people of Mecca [corrected: MS omits 'and of the people of Mecca']; and its distance from the equinoctial line or from the meridian line is the amount by which the one who prays must turn away from these. This is the figure of it.
它是城市的地平与那个通过该城居民天顶和麦加居民天顶〔抄本脱“和麦加居民”,据文义改正〕的圆的交点;它离春秋分线或离子午线的距离,就是礼拜的人须从这两条线转开的量。这是它的图。
大意与图解点开
🔎 大意:过本城天顶与麦加天顶的大圆和本城地平的交点,就是礼拜朝向;它离东西线或南北线的度数,就是礼拜者应转的角度。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 礼拜朝向 | the qibla | 礼拜时面对麦加的方向 |
| 朝向的方位 | the azimuth of the qibla | 朝向在地平上的点 |
| 天顶 | zenith | 头顶正上方 |
🧭 图解与讲解
礼拜朝向(qibla)是礼拜时所面对的麦加方向。比鲁尼的定义是:通过本城天顶与麦加天顶作一个大圆,它与本城地平的交点,就是朝向的方位;这一点离东西线或南北线的度数,就是礼拜的人应当转身的量(图一)。
〔图〕礼拜朝向:过本地天顶与麦加天顶的大圆和本地地平的交点,从东西线或南北线量出
〔图〕朝向的求法:连两地天顶作大圆,看它在本地地平上落在哪里
抄本这里只写“通过该城居民天顶的圆”,没有提麦加。过一个天顶的大圆有无数条,这样就定不出方向,所以统稿时据文义补上“和麦加居民”(〔〕中注明)。大圆是球面上两点之间最短的路,所以朝向就是沿着地球表面最短的路朝麦加看去的方向。
这里只给定义,算法要用到前面讲过的球面三角:两地的纬度、经度之差,加上三角形的边角关系。占星书里求“两地之间的方位”,例如推算某地远行的方向,用的也是同一种计算。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 礼拜朝向 | the qibla | 礼拜时面对麦加的方向 |
| 朝向的方位 | the azimuth of the qibla | 朝向在地平上的点 |
| 天顶 | zenith | 头顶正上方 |
🧭 图解与讲解
礼拜朝向(qibla)是礼拜时所面对的麦加方向。比鲁尼的定义是:通过本城天顶与麦加天顶作一个大圆,它与本城地平的交点,就是朝向的方位;这一点离东西线或南北线的度数,就是礼拜的人应当转身的量(图一)。
抄本这里只写“通过该城居民天顶的圆”,没有提麦加。过一个天顶的大圆有无数条,这样就定不出方向,所以统稿时据文义补上“和麦加居民”(〔〕中注明)。大圆是球面上两点之间最短的路,所以朝向就是沿着地球表面最短的路朝麦加看去的方向。
这里只给定义,算法要用到前面讲过的球面三角:两地的纬度、经度之差,加上三角形的边角关系。占星书里求“两地之间的方位”,例如推算某地远行的方向,用的也是同一种计算。
§236. What are the climes?
The practitioners of this art have divided the habitable part of the inhabited quarter into seven oblong strips, which they have called climes (aqālīm), running from east to west parallel to the equinoctial line, such that the longest summer daytime in their middles differs by half an hour; for the changes come only from latitude, and from longitude there comes nothing but the difference in rising, which is known only by report. The hours of the longest daytime in the middle of the middle one of them, which is the fourth, are 14 1/2 hours; then one goes back from it until the hours of the longest daytime in the middle of the first of them are 13, and one goes beyond it to the middle of the seventh clime, where the hours of its longest daytime are 16. Since their latitudes are found in the books with differing amounts, on account of the disagreement about the amount of the greatest declination, of the different methods of dividing the sines, and of some who reckon them hitting on what is right while others deviate from it in [illegible] their reckoning [text uncertain], I have put them in this table with the utmost accuracy.
翻译点开
§236. What are the climes?
第二百三十六问 何谓气候带?
The practitioners of this art have divided the habitable part of the inhabited quarter into seven oblong strips, which they have called climes (aqālīm), running from east to west parallel to the equinoctial line, such that the longest summer daytime in their middles differs by half an hour; for the changes come only from latitude, and from longitude there comes nothing but the difference in rising, which is known only by report. The hours of the longest daytime in the middle of the middle one of them, which is the fourth, are 14 1/2 hours; then one goes back from it until the hours of the longest daytime in the middle of the first of them are 13, and one goes beyond it to the middle of the seventh clime, where the hours of its longest daytime are 16. Since their latitudes are found in the books with differing amounts, on account of the disagreement about the amount of the greatest declination, of the different methods of dividing the sines, and of some who reckon them hitting on what is right while others deviate from it in [illegible] their reckoning [text uncertain], I have put them in this table with the utmost accuracy.
本行的从业者把有人居住的四分之一中可以居住的部分分成七条长带,称为气候带,自东向西延伸,与赤道线平行,使各带中线上的夏季最长白昼相差半小时;因为变化只来自纬度,从经度来的只是升起时刻的差别,而那只能凭传闻得知。居中的一带即第四带,其中线上的最长白昼为十四个半小时;然后由它往回退,直到第一带中线上的最长白昼为十三小时;再往前,直到第七带中线,那里的最长白昼为十六小时。由于书中所载各带的纬度数值不一,原因在于对最大赤纬之数有分歧、正弦的分法不同,以及推算的人有的算对了,有的在〔抄本此处字迹难辨〕他们的推算上有偏差〔原文疑有讹误〕,我就以极其精确的方式把它们列在这张表里。
大意与图解点开
🔎 大意:有人居住之地分为七条东西向的长带,各带中线的最长白昼依次相差半小时,自第一带十三小时到第七带十六小时。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 气候带 | climes (aqālīm) | 按最长白昼分的纬度带 |
| 最长白昼 | the longest daytime | 夏至之昼 |
| 正弦 | sines | 三角计算所用之数 |
🧭 图解与讲解
“气候带”(iqlīm,复数 aqālīm)出自希腊语 klima(倾斜),原指地平对天赤道的倾斜,后来指纬度带。比鲁尼说,本行的人把有人居住之地分成七条东西向的长带,划分的标准不是距离,而是夏至最长白昼:各带中线依次相差半小时,第一带十三小时,第四带居中十四个半小时,第七带十六小时(图二)。
| 位置 | 最长白昼 | 纬度 | 夏季日出方位的幅度 | 夏至正午影(十二指表) |
|---|---|---|---|---|
| 赤道线 | 12 时 00 分 | 0°00′ | 23°35′ | 5 指 14 分⁺ |
| 第一带起点 | 12 时 45 分 | 12°39′ | 24°18′⁺ | 2 指 19 分 |
| 第一带中线 | 13 时 00 分 | 16°39′⁺ | 24°41′ | 1 指 13 分 按算约 1 指 27 分 |
| 第二带起点 | 13 时 15 分 | 20°27′ | 25°17′ | 0 指 39 分 |
| 第二带中线 | 13 时 30 分 | 24°30′ | 36°05′ 按算应作 26°05′ | 0 指 12 分⁺ |
| 第三带起点 | 13 时 45 分 | 27°33′⁺ | 26°49′ | 0 指 49 分 |
| 第三带中线 | 14 时 00 分 | 30°39′ | 27°41′ | 1 指 29 分 |
| 第四带起点 | 14 时 15 分 | 33°37′ | 28°44′ | 2 指 27 分 |
| 第四带中线 | 14 时 30 分 | 36°51′ | 29°47′ | 2 指 43 分 |
| 第五带起点 | 14 时 45 分 | 38°54′ | 30°17′ | 3 指 17 分 |
| 第五带中线 | 15 时 00 分 | 41°14′ | 32°09′ | 3 指 49 分 |
| 第六带起点 | 15 时 15 分 | 43°23′ | 33°25′ | 4 指 19 分 |
| 第六带中线 | 15 时 30 分 | 45°21′(读法未定) | 34°44′ | 4 指 43 分 |
| 第七带起点 | 15 时 45 分 | 47°11′ | 36°05′ | 5 指 05 分 |
| 第七带中线 | 16 时 00 分 | 48°12′ | 37°25′ | 5 指 47 分 |
| 第七带末尾 | 16 时 15 分 | 55°25′ 按前后应作 50°25′ | 38°05′ | 6 指 04 分 |
〔图〕七带中线的最长白昼,每带递增半小时;第四带居中,为十四个半小时
他特别说明为什么按纬度分而不按经度:同一纬度上,昼夜长短、天象都相同,经度不同只造成升起时刻的先后,而那只能靠传闻(两地的人互报月食时刻之类)才知道。所以气候带是一种“天象相同”的分区,对占星来说,同一气候带里的城市,星座的上升时间也大致相同。
表一是比鲁尼的原表,列出赤道线与七带各自起点、中线的最长白昼、纬度、夏季日出方位的幅度与夏至正午影(十二指表)。他说书中各家数值不一,因为最大赤纬取值、正弦表的分法和计算功夫各不相同,所以自己重新精算。统稿时按本书最大赤纬逐格核算:多数格吻合,少数格字迹潦草,注“读法未定”;有三格与计算不合,照抄本录出,以小字注明:第一带中线影长、第二带中线的日出幅度,以及第七带末尾的纬度(抄本作五十五度二十五分,按前后应是五十度二十五分)。
赤道线一行的影长格抄本字形认不出;按算,赤道上夏至正午影朝北,约五指十四分。第二带中线纬度二十四度半,已在回归线以北,正午影极短,抄本两格也认不出。这张表是卷四的核心数据,下一章讲各带的城市,再下一章的星座上升时间表,都以这七带的中线为准。
表中带“⁺”的格是本站据公式补回或定读的,不是抄本读出的:赤道影长按 12·tan 23°35′ 补作五指十四分;第二带中线影长按纬度二十四度半补作零指十二分;第一带起点的日出幅度、第一带中线与第三带起点的纬度分,抄本字形两读,按最长白昼与日出方位两种算法都指向同一读,才取定。可读各格与算值多在一分以内,所以这样补是可靠的;第六带中线纬度分两读相差太小,算不出取舍,仍注“读法未定”。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 气候带 | climes (aqālīm) | 按最长白昼分的纬度带 |
| 最长白昼 | the longest daytime | 夏至之昼 |
| 正弦 | sines | 三角计算所用之数 |
🧭 图解与讲解
“气候带”(iqlīm,复数 aqālīm)出自希腊语 klima(倾斜),原指地平对天赤道的倾斜,后来指纬度带。比鲁尼说,本行的人把有人居住之地分成七条东西向的长带,划分的标准不是距离,而是夏至最长白昼:各带中线依次相差半小时,第一带十三小时,第四带居中十四个半小时,第七带十六小时(图二)。
| 位置 | 最长白昼 | 纬度 | 夏季日出方位的幅度 | 夏至正午影(十二指表) |
|---|---|---|---|---|
| 赤道线 | 12 时 00 分 | 0°00′ | 23°35′ | 5 指 14 分⁺ |
| 第一带起点 | 12 时 45 分 | 12°39′ | 24°18′⁺ | 2 指 19 分 |
| 第一带中线 | 13 时 00 分 | 16°39′⁺ | 24°41′ | 1 指 13 分 按算约 1 指 27 分 |
| 第二带起点 | 13 时 15 分 | 20°27′ | 25°17′ | 0 指 39 分 |
| 第二带中线 | 13 时 30 分 | 24°30′ | 36°05′ 按算应作 26°05′ | 0 指 12 分⁺ |
| 第三带起点 | 13 时 45 分 | 27°33′⁺ | 26°49′ | 0 指 49 分 |
| 第三带中线 | 14 时 00 分 | 30°39′ | 27°41′ | 1 指 29 分 |
| 第四带起点 | 14 时 15 分 | 33°37′ | 28°44′ | 2 指 27 分 |
| 第四带中线 | 14 时 30 分 | 36°51′ | 29°47′ | 2 指 43 分 |
| 第五带起点 | 14 时 45 分 | 38°54′ | 30°17′ | 3 指 17 分 |
| 第五带中线 | 15 时 00 分 | 41°14′ | 32°09′ | 3 指 49 分 |
| 第六带起点 | 15 时 15 分 | 43°23′ | 33°25′ | 4 指 19 分 |
| 第六带中线 | 15 时 30 分 | 45°21′(读法未定) | 34°44′ | 4 指 43 分 |
| 第七带起点 | 15 时 45 分 | 47°11′ | 36°05′ | 5 指 05 分 |
| 第七带中线 | 16 时 00 分 | 48°12′ | 37°25′ | 5 指 47 分 |
| 第七带末尾 | 16 时 15 分 | 55°25′ 按前后应作 50°25′ | 38°05′ | 6 指 04 分 |
他特别说明为什么按纬度分而不按经度:同一纬度上,昼夜长短、天象都相同,经度不同只造成升起时刻的先后,而那只能靠传闻(两地的人互报月食时刻之类)才知道。所以气候带是一种“天象相同”的分区,对占星来说,同一气候带里的城市,星座的上升时间也大致相同。
表一是比鲁尼的原表,列出赤道线与七带各自起点、中线的最长白昼、纬度、夏季日出方位的幅度与夏至正午影(十二指表)。他说书中各家数值不一,因为最大赤纬取值、正弦表的分法和计算功夫各不相同,所以自己重新精算。统稿时按本书最大赤纬逐格核算:多数格吻合,少数格字迹潦草,注“读法未定”;有三格与计算不合,照抄本录出,以小字注明:第一带中线影长、第二带中线的日出幅度,以及第七带末尾的纬度(抄本作五十五度二十五分,按前后应是五十度二十五分)。
赤道线一行的影长格抄本字形认不出;按算,赤道上夏至正午影朝北,约五指十四分。第二带中线纬度二十四度半,已在回归线以北,正午影极短,抄本两格也认不出。这张表是卷四的核心数据,下一章讲各带的城市,再下一章的星座上升时间表,都以这七带的中线为准。
表中带“⁺”的格是本站据公式补回或定读的,不是抄本读出的:赤道影长按 12·tan 23°35′ 补作五指十四分;第二带中线影长按纬度二十四度半补作零指十二分;第一带起点的日出幅度、第一带中线与第三带起点的纬度分,抄本字形两读,按最长白昼与日出方位两种算法都指向同一读,才取定。可读各格与算值多在一分以内,所以这样补是可靠的;第六带中线纬度分两读相差太小,算不出取舍,仍注“读法未定”。
§237. What happens in the climes, and is there habitation beyond them?
As for habitation, Ptolemy has asserted that its farthest end is found in the island of Thule (Tūlī), whose latitude is close to the complement of the greatest declination, which is approximately 66 parts. But the nations between the end of the seventh clime and that limit are more like wild beasts than men in their way of living and their eating. With all that, the differences we have mentioned, and the difference in the ascensions of the signs, keep increasing as one goes farther into the north. The risings of the two solstices widen and come nearer to their settings, until they coincide at the latitude equal to the complement of the greatest declination. Then the whole orbit of the beginning of Cancer is visible, and the longest daytime is 24 hours, since the Sun stays visible. It happens at this place that the north pole of the zodiac passes over the zenith once each day, and the zodiac then coincides with the horizon; then six signs of it appear all at once. From this place on, the summer shadows begin to go round the gnomons on all sides.
翻译点开
§237. What happens in the climes, and is there habitation beyond them?
第二百三十七问 诸气候带中会发生什么?气候带之外还有人居住吗?
As for habitation, Ptolemy has asserted that its farthest end is found in the island of Thule (Tūlī), whose latitude is close to the complement of the greatest declination, which is approximately 66 parts. But the nations between the end of the seventh clime and that limit are more like wild beasts than men in their way of living and their eating. With all that, the differences we have mentioned, and the difference in the ascensions of the signs, keep increasing as one goes farther into the north. The risings of the two solstices widen and come nearer to their settings, until they coincide at the latitude equal to the complement of the greatest declination. Then the whole orbit of the beginning of Cancer is visible, and the longest daytime is 24 hours, since the Sun stays visible. It happens at this place that the north pole of the zodiac passes over the zenith once each day, and the zodiac then coincides with the horizon; then six signs of it appear all at once. From this place on, the summer shadows begin to go round the gnomons on all sides.
至于居住,托勒密断言它的最远之处在图勒岛,其纬度接近最大赤纬的余弧,约为六十六度。但从第七带的末尾到那个界限之间的民族,在生活方式和饮食上,更像野兽而不像人。尽管如此,我们所说的那些差别,以及星座上升时间的差别,越往北深入就越增大。两至的日出处越来越向两旁展开,越来越靠近它们的日落处,直到在纬度等于最大赤纬之余弧的地方两者重合。那时巨蟹座起点的日周圈全都可见,最长白昼为二十四小时,因为太阳一直可见。在这个地方,黄道的北极每天经过天顶一次,那时黄道与地平重合;于是它的六个星座一下子同时出现。从这个地方起,夏季的影子开始绕着表四面转。
大意与图解点开
🔎 大意:托勒密说人居最远到图勒岛,约北纬六十六度;越往北差别越大,到此夏至太阳终日不落,黄道一时与地平重合,六宫同升。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 图勒岛 | the island of Thule (Tūlī) | 托勒密所说人居极北 |
| 最大赤纬的余弧 | the complement of the greatest declination | 约六十六度 |
| 黄道的北极 | the north pole of the zodiac | 黄道之极 |
🧭 图解与讲解
第七带以北还有人吗?比鲁尼引托勒密:人居的极限在图勒岛(Thule,阿拉伯语作 Tūlī),纬度约六十六度,正是最大赤纬的余弧。第七带末尾到那里之间也住着人,但比鲁尼照当时的看法说他们“更像野兽”,这是古代以文明自居的成见,照原文译出。
| 纬度约六十六度(最大赤纬的余弧)处 | 比鲁尼所说 |
|---|---|
| 夏至日出处与日落处 | 向北展开,终于在正北重合 |
| 巨蟹座起点的日周圈 | 全在地平以上,最长白昼二十四小时 |
| 黄道的北极 | 每日经过天顶一次 |
| 那一刻的黄道 | 与地平重合,六个星座一下子同时出现 |
| 夏季的影子 | 从此开始绕着表四面转 |
〔图〕越往北,日出处越向北展开,到六十六度夏至之日太阳不落
越往北,各种差别越大:昼夜长短、日出方位、星座上升时间都更悬殊。夏至的日出处与日落处越来越向北靠拢,到纬度等于最大赤纬余弧的地方,两者在正北重合,夏至太阳整天不落,最长白昼二十四小时(表一)。今天称这条纬线为北极圈,比鲁尼的数是九十减二十三度三十五分,即六十六度二十五分。
这里还有一个奇景:黄道的北极离天极二十三度多,每天绕天极转一圈,在这个纬度上会经过天顶;那一刻黄道恰与地平重合,半个黄道(六个星座)一下子同时升到地平以上。占星上说,这时上升点在一瞬间跳过六宫,宫位制在这里失去意义;夏天的影子也开始绕着表转一整圈。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 图勒岛 | the island of Thule (Tūlī) | 托勒密所说人居极北 |
| 最大赤纬的余弧 | the complement of the greatest declination | 约六十六度 |
| 黄道的北极 | the north pole of the zodiac | 黄道之极 |
🧭 图解与讲解
第七带以北还有人吗?比鲁尼引托勒密:人居的极限在图勒岛(Thule,阿拉伯语作 Tūlī),纬度约六十六度,正是最大赤纬的余弧。第七带末尾到那里之间也住着人,但比鲁尼照当时的看法说他们“更像野兽”,这是古代以文明自居的成见,照原文译出。
| 纬度约六十六度(最大赤纬的余弧)处 | 比鲁尼所说 |
|---|---|
| 夏至日出处与日落处 | 向北展开,终于在正北重合 |
| 巨蟹座起点的日周圈 | 全在地平以上,最长白昼二十四小时 |
| 黄道的北极 | 每日经过天顶一次 |
| 那一刻的黄道 | 与地平重合,六个星座一下子同时出现 |
| 夏季的影子 | 从此开始绕着表四面转 |
越往北,各种差别越大:昼夜长短、日出方位、星座上升时间都更悬殊。夏至的日出处与日落处越来越向北靠拢,到纬度等于最大赤纬余弧的地方,两者在正北重合,夏至太阳整天不落,最长白昼二十四小时(表一)。今天称这条纬线为北极圈,比鲁尼的数是九十减二十三度三十五分,即六十六度二十五分。
这里还有一个奇景:黄道的北极离天极二十三度多,每天绕天极转一圈,在这个纬度上会经过天顶;那一刻黄道恰与地平重合,半个黄道(六个星座)一下子同时升到地平以上。占星上说,这时上升点在一瞬间跳过六宫,宫位制在这里失去意义;夏天的影子也开始绕着表转一整圈。
§238. What happens beyond this place?
Together with the orbit of the beginning of Cancer other orbits appear, on which the Sun stays visible as long as it goes round with them, so that the longest daytime grows from a single day to several days, then months. Opposite it, together with the orbit of the beginning of Capricorn, orbits are hidden on which the Sun stays hidden as long as it is on them, and the amount of the longest night goes beyond a day to days and months, according to how far one penetrates towards the north. It happens in these places at certain times that the signs rise in reverse of their order: I mean Taurus, then Aries, then Pisces, then Aquarius. Just as the daily orbits stand upright on the horizon of the equinoctial line, which is why the orb there is called the right orb and its revolution an upright one, and then incline on the horizons of the towns that have latitudes, so that the revolution of the orb there is called ḥamāʾilī ('like a sword-belt'), so at the extreme of latitude, where the north pole is at the zenith, the equator always coincides with the horizon, all the northern orbits are visible there and the southern ones hidden, and the revolution of the orb is raḥawī ('like a millstone'). As long as the Sun is north of the equator it is visible there, and as long as it is south it is hidden; so the year there becomes a single day, of which about 6 months are daytime and the rest night.

翻译点开
§238. What happens beyond this place?
第二百三十八问 过了这个地方又会怎样?
Together with the orbit of the beginning of Cancer other orbits appear, on which the Sun stays visible as long as it goes round with them, so that the longest daytime grows from a single day to several days, then months. Opposite it, together with the orbit of the beginning of Capricorn, orbits are hidden on which the Sun stays hidden as long as it is on them, and the amount of the longest night goes beyond a day to days and months, according to how far one penetrates towards the north. It happens in these places at certain times that the signs rise in reverse of their order: I mean Taurus, then Aries, then Pisces, then Aquarius. Just as the daily orbits stand upright on the horizon of the equinoctial line, which is why the orb there is called the right orb and its revolution an upright one, and then incline on the horizons of the towns that have latitudes, so that the revolution of the orb there is called ḥamāʾilī ('like a sword-belt'), so at the extreme of latitude, where the north pole is at the zenith, the equator always coincides with the horizon, all the northern orbits are visible there and the southern ones hidden, and the revolution of the orb is raḥawī ('like a millstone'). As long as the Sun is north of the equator it is visible there, and as long as it is south it is hidden; so the year there becomes a single day, of which about 6 months are daytime and the rest night.
与巨蟹座起点的日周圈一起,又有别的日周圈显现出来,太阳随它们运转期间一直可见,所以最长白昼从一日增到好几日,再到几个月。与之相对,与摩羯座起点的日周圈一起,有些日周圈隐没,太阳在它们上面时一直隐没,最长黑夜的长度超过一日,到几日、几个月,视人向北深入多远而定。在这些地方,某些时候星座会逆着次序升起:我是说,先金牛,再白羊,再双鱼,再宝瓶。正如日周圈在赤道线的地平上直立,所以那里的天球称为正球,它的运转称为直立的运转;在有纬度的城市的地平上则倾斜,所以那里天球的运转称为“佩带式”;同样,在纬度的极端,北极在天顶,天赤道总与地平重合,北方的诸日周圈在那里全都可见,南方的全都隐没,天球的运转是“磨盘式”。太阳在天赤道以北时,在那里可见;在以南时,就隐没;所以那里的一年成为一日,其中约六个月是白昼,其余是黑夜。
大意与图解点开
🔎 大意:过了六十六度,长昼长夜由几日到几月,星座有时逆序而升;天球的转法由正球、佩带式变为北极下的磨盘式,一年只一昼一夜。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 正球 | the right orb | 赤道线上的天球 |
| 佩带式 | ḥamāʾilī ('like a sword-belt') | 斜挎如佩剑之带 |
| 磨盘式 | raḥawī ('like a millstone') | 平转如磨盘 |
| 逆序而升 | rise in reverse of their order | 金牛先于白羊 |
🧭 图解与讲解
过了六十六度,夏至前后不落的日周圈不止一条,太阳连续几天、几个月都在地平以上;冬至前后则连续几天、几个月不升,越北越长(表二)。在这些地方,某些时刻星座会倒着升起:先金牛,再白羊、双鱼、宝瓶。原因是黄道这一段在那时与地平相交的方向反了过来,地平从黄道下方“扫”过去的顺序正好与星座次序相反。
〔图〕日周圈与地平:赤道上直立(正球),有纬度处倾斜(佩带式),北极下与地平平行(磨盘式)
| 纬度 | 最长白昼 | 最长黑夜 | 天球的转法 |
|---|---|---|---|
| 赤道线上 | 十二小时 | 十二小时 | 正球:日周圈直立于地平 |
| 有纬度之地 | 随纬度增长 | 随纬度增长 | 佩带式:日周圈斜交地平 |
| 约六十六度 | 一日 | 一日 | 黄道每日有一刻与地平重合 |
| 更北 | 数日至数月 | 数日至数月 | 星座有时逆序而升 |
| 北极之下 | 约六个月 | 约六个月 | 磨盘式:天赤道与地平重合 |
比鲁尼用三个形象的名字概括天球的转法(图一)。赤道线上,日周圈垂直于地平,叫“正球”,运转是直立的;有纬度之地,日周圈斜交地平,像斜挎在身上的佩剑之带,叫“佩带式”(ḥamāʾilī);到北极之下,天极在天顶,天赤道与地平重合,诸星平平地绕着转,像推磨,叫“磨盘式”(raḥawī)。
在北极之下,太阳在天赤道以北的半年一直可见,以南的半年一直不见,一年就成了一昼一夜,各约六个月。这一章从正午影一路讲到北极,把纬度对天象的影响讲完了。下一章将列出各气候带的城市,再下一章讲星座的上升时间,正是“佩带式”天球上星座升起快慢不等的计算。
📖 术语
| 术语 | 英文原词 | 意思 |
|---|---|---|
| 正球 | the right orb | 赤道线上的天球 |
| 佩带式 | ḥamāʾilī ('like a sword-belt') | 斜挎如佩剑之带 |
| 磨盘式 | raḥawī ('like a millstone') | 平转如磨盘 |
| 逆序而升 | rise in reverse of their order | 金牛先于白羊 |
🧭 图解与讲解
过了六十六度,夏至前后不落的日周圈不止一条,太阳连续几天、几个月都在地平以上;冬至前后则连续几天、几个月不升,越北越长(表二)。在这些地方,某些时刻星座会倒着升起:先金牛,再白羊、双鱼、宝瓶。原因是黄道这一段在那时与地平相交的方向反了过来,地平从黄道下方“扫”过去的顺序正好与星座次序相反。
| 纬度 | 最长白昼 | 最长黑夜 | 天球的转法 |
|---|---|---|---|
| 赤道线上 | 十二小时 | 十二小时 | 正球:日周圈直立于地平 |
| 有纬度之地 | 随纬度增长 | 随纬度增长 | 佩带式:日周圈斜交地平 |
| 约六十六度 | 一日 | 一日 | 黄道每日有一刻与地平重合 |
| 更北 | 数日至数月 | 数日至数月 | 星座有时逆序而升 |
| 北极之下 | 约六个月 | 约六个月 | 磨盘式:天赤道与地平重合 |
比鲁尼用三个形象的名字概括天球的转法(图一)。赤道线上,日周圈垂直于地平,叫“正球”,运转是直立的;有纬度之地,日周圈斜交地平,像斜挎在身上的佩剑之带,叫“佩带式”(ḥamāʾilī);到北极之下,天极在天顶,天赤道与地平重合,诸星平平地绕着转,像推磨,叫“磨盘式”(raḥawī)。
在北极之下,太阳在天赤道以北的半年一直可见,以南的半年一直不见,一年就成了一昼一夜,各约六个月。这一章从正午影一路讲到北极,把纬度对天象的影响讲完了。下一章将列出各气候带的城市,再下一章讲星座的上升时间,正是“佩带式”天球上星座升起快慢不等的计算。
原文为公有领域古籍;翻译、印象画与图文解读由 AI 辅助生成,鲲侯审校。