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I have found 2 definitions of Eclipse Magnitude in total eclipse:

Solar eclipse for example, below we define $r_1$ as the radius of the Sun, $r_2$ as the radius of the Moon's Shadow, $d$ as the distance of Sun's center and Moon's center

if it is a partial eclipse, the Eclipse Magnitude have no objection:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} $$

Definition 1:

After the Sun is totally blocked, the Eclipse Magnitude jumps from $1$ to $r_2/r_1$, which is the ratio of Moon and Sun's diameter

http://www.jgiesen.de/eclipse/

https://www.oxfordreference.com/display/10.1093/oi/authority.20110803100126148

Definition 2:

After the Sun is totally blocked, the Eclipse Magnitude is still:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} > 1,\quad 0 \leq d \leq r_2 - r_1 $$

only if the Sun and Moon's center overlap, will $d = 0$, and $\epsilon = \epsilon_{max} = \dfrac{r_1 + r_2}{2r_1}$, but this will still be less than $r_2/r_1$

This provide a continuous definition of eclipse magnitude, on the other hand, in an annular solar eclipse, the Eclipse Magnitude is always $r_2/r_1$, having nothing to do with $d$, but this is continuous

https://www.geogebra.org/m/SnZ7QGTJ

Which one is right? I didn't find any books or professional articles defines the calculation of Eclipse Magnitude, Thanks!


I found this in The Explanatory Supplement to the Astronomical Almanac 3rd edition

but it do not give thecore question I think is: a total eclipse part that I want, especially lunar total eclipse, while the earth's umbra is much larger than the moon.

It said ambiguously $OA = -L_2$, but it did not say I should useThen the magnitude will be larger if the center of the Moon and the center of the Earth's umbra are closer together inSee BBottom Figure $(L_1 - m)/(L_1 + L_2)$ or

(comparing if the moon is close to the edge of the umbra inSee ETop Figure $(L_1 - L_2)/(L_1 + L_2)$) if using Definition II.

enter image description here In Definition I, the magnitude will have nothing to do with center distance, as long as the moon is all in the earth's shadow.

enter image description here

enter image description here

I have found 2 definitions of Eclipse Magnitude in total eclipse:

Solar eclipse for example, below we define $r_1$ as the radius of the Sun, $r_2$ as the radius of the Moon's Shadow, $d$ as the distance of Sun's center and Moon's center

if it is a partial eclipse, the Eclipse Magnitude have no objection:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} $$

Definition 1:

After the Sun is totally blocked, the Eclipse Magnitude jumps from $1$ to $r_2/r_1$, which is the ratio of Moon and Sun's diameter

http://www.jgiesen.de/eclipse/

https://www.oxfordreference.com/display/10.1093/oi/authority.20110803100126148

Definition 2:

After the Sun is totally blocked, the Eclipse Magnitude is still:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} > 1,\quad 0 \leq d \leq r_2 - r_1 $$

only if the Sun and Moon's center overlap, will $d = 0$, and $\epsilon = \epsilon_{max} = \dfrac{r_1 + r_2}{2r_1}$, but this will still be less than $r_2/r_1$

This provide a continuous definition of eclipse magnitude, on the other hand, in an annular solar eclipse, the Eclipse Magnitude is always $r_2/r_1$, having nothing to do with $d$, but this is continuous

https://www.geogebra.org/m/SnZ7QGTJ

Which one is right? I didn't find any books or professional articles defines the calculation of Eclipse Magnitude, Thanks!


I found this in The Explanatory Supplement to the Astronomical Almanac 3rd edition

but it do not give the total eclipse part that I want

It said ambiguously $OA = -L_2$, but it did not say I should use the in B $(L_1 - m)/(L_1 + L_2)$ or in E $(L_1 - L_2)/(L_1 + L_2)$

enter image description here

I have found 2 definitions of Eclipse Magnitude in total eclipse:

Solar eclipse for example, below we define $r_1$ as the radius of the Sun, $r_2$ as the radius of the Moon's Shadow, $d$ as the distance of Sun's center and Moon's center

if it is a partial eclipse, the Eclipse Magnitude have no objection:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} $$

Definition 1:

After the Sun is totally blocked, the Eclipse Magnitude jumps from $1$ to $r_2/r_1$, which is the ratio of Moon and Sun's diameter

http://www.jgiesen.de/eclipse/

https://www.oxfordreference.com/display/10.1093/oi/authority.20110803100126148

Definition 2:

After the Sun is totally blocked, the Eclipse Magnitude is still:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} > 1,\quad 0 \leq d \leq r_2 - r_1 $$

only if the Sun and Moon's center overlap, will $d = 0$, and $\epsilon = \epsilon_{max} = \dfrac{r_1 + r_2}{2r_1}$, but this will still be less than $r_2/r_1$

This provide a continuous definition of eclipse magnitude, on the other hand, in an annular solar eclipse, the Eclipse Magnitude is always $r_2/r_1$, having nothing to do with $d$, but this is continuous

https://www.geogebra.org/m/SnZ7QGTJ

Which one is right? I didn't find any books or professional articles defines the calculation of Eclipse Magnitude, Thanks!


The core question I think is: a total eclipse, especially lunar total eclipse, while the earth's umbra is much larger than the moon.

Then the magnitude will be larger if the center of the Moon and the center of the Earth's umbra are closer together See Bottom Figure

(comparing if the moon is close to the edge of the umbra See Top Figure) if using Definition II.

In Definition I, the magnitude will have nothing to do with center distance, as long as the moon is all in the earth's shadow.

enter image description here

enter image description here

added 379 characters in body
Source Link

I have found 2 definitions of Eclipse Magnitude in total eclipse:

Solar eclipse for example, below we define $r_1$ as the radius of the Sun, $r_2$ as the radius of the Moon's Shadow, $d$ as the distance of Sun's center and Moon's center

if it is a partial eclipse, the Eclipse Magnitude have no objection:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} $$

Definition 1:

After the Sun is totally blocked, the Eclipse Magnitude jumps from $1$ to $r_2/r_1$, which is the ratio of Moon and Sun's diameter

http://www.jgiesen.de/eclipse/

https://www.oxfordreference.com/display/10.1093/oi/authority.20110803100126148

Definition 2:

After the Sun is totally blocked, the Eclipse Magnitude is still:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} > 1,\quad 0 \leq d \leq r_2 - r_1 $$

only if the Sun and Moon's center overlap, will $d = 0$, and $\epsilon = \epsilon_{max} = \dfrac{r_1 + r_2}{2r_1}$, but this will still be less than $r_2/r_1$

This provide a continuous definition of eclipse magnitude, on the other hand, in an annular solar eclipse, the Eclipse Magnitude is always $r_2/r_1$, having nothing to do with $d$, but this is continuous

https://www.geogebra.org/m/SnZ7QGTJ

Which one is right? I didn't find any books or professional articles defines the calculation of Eclipse Magnitude, Thanks!


I found this in The Explanatory Supplement to the Astronomical Almanac 3rd edition

but it do not give the total eclipse part that I want

It said ambiguously $OA = -L_2$, but it did not say I should use the in B $(L_1 - m)/(L_1 + L_2)$ or in E $(L_1 - L_2)/(L_1 + L_2)$

enter image description here

I have found 2 definitions of Eclipse Magnitude in total eclipse:

Solar eclipse for example, below we define $r_1$ as the radius of the Sun, $r_2$ as the radius of the Moon's Shadow, $d$ as the distance of Sun's center and Moon's center

if it is a partial eclipse, the Eclipse Magnitude have no objection:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} $$

Definition 1:

After the Sun is totally blocked, the Eclipse Magnitude jumps from $1$ to $r_2/r_1$, which is the ratio of Moon and Sun's diameter

http://www.jgiesen.de/eclipse/

https://www.oxfordreference.com/display/10.1093/oi/authority.20110803100126148

Definition 2:

After the Sun is totally blocked, the Eclipse Magnitude is still:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} > 1,\quad 0 \leq d \leq r_2 - r_1 $$

only if the Sun and Moon's center overlap, will $d = 0$, and $\epsilon = \epsilon_{max} = \dfrac{r_1 + r_2}{2r_1}$, but this will still be less than $r_2/r_1$

This provide a continuous definition of eclipse magnitude, on the other hand, in an annular solar eclipse, the Eclipse Magnitude is always $r_2/r_1$, having nothing to do with $d$, but this is continuous

https://www.geogebra.org/m/SnZ7QGTJ

Which one is right? I didn't find any books or professional articles defines the calculation of Eclipse Magnitude, Thanks!

I have found 2 definitions of Eclipse Magnitude in total eclipse:

Solar eclipse for example, below we define $r_1$ as the radius of the Sun, $r_2$ as the radius of the Moon's Shadow, $d$ as the distance of Sun's center and Moon's center

if it is a partial eclipse, the Eclipse Magnitude have no objection:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} $$

Definition 1:

After the Sun is totally blocked, the Eclipse Magnitude jumps from $1$ to $r_2/r_1$, which is the ratio of Moon and Sun's diameter

http://www.jgiesen.de/eclipse/

https://www.oxfordreference.com/display/10.1093/oi/authority.20110803100126148

Definition 2:

After the Sun is totally blocked, the Eclipse Magnitude is still:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} > 1,\quad 0 \leq d \leq r_2 - r_1 $$

only if the Sun and Moon's center overlap, will $d = 0$, and $\epsilon = \epsilon_{max} = \dfrac{r_1 + r_2}{2r_1}$, but this will still be less than $r_2/r_1$

This provide a continuous definition of eclipse magnitude, on the other hand, in an annular solar eclipse, the Eclipse Magnitude is always $r_2/r_1$, having nothing to do with $d$, but this is continuous

https://www.geogebra.org/m/SnZ7QGTJ

Which one is right? I didn't find any books or professional articles defines the calculation of Eclipse Magnitude, Thanks!


I found this in The Explanatory Supplement to the Astronomical Almanac 3rd edition

but it do not give the total eclipse part that I want

It said ambiguously $OA = -L_2$, but it did not say I should use the in B $(L_1 - m)/(L_1 + L_2)$ or in E $(L_1 - L_2)/(L_1 + L_2)$

enter image description here

added 207 characters in body
Source Link

I have found 2 definitions of Eclipse Magnitude in total eclipse:

Solar eclipse for example, below we define $r_1$ as the radius of the Sun, $r_2$ as the radius of the Moon's Shadow, $d$ as the distance of Sun's center and Moon's center

if it is a partial eclipse, the Eclipse Magnitude have no objection:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} $$

Definition 1:

After the Sun is totally blocked, the Eclipse Magnitude jumps from $1$ to $r_2/r_1$, which is the ratio of Moon and Sun's diameter

http://www.jgiesen.de/eclipse/

https://www.oxfordreference.com/display/10.1093/oi/authority.20110803100126148

Definition 2:

After the Sun is totally blocked, the Eclipse Magnitude is still:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} > 1,\quad 0 \leq d \leq r_2 - r_1 $$

only if the Sun and Moon's center overlap, will $d = 0$, and $\epsilon = \epsilon_{max} = \dfrac{r_1 + r_2}{2r_1}$, but this will still be less than $r_2/r_1$

This provide a continuous definition of eclipse magnitude, on the other hand, in an annular solar eclipse, the Eclipse Magnitude is always $r_2/r_1$, having nothing to do with $d$, but this is continuous

https://www.geogebra.org/m/SnZ7QGTJ

Which one is right? I didn't find any books or professional articles defines the calculation of Eclipse Magnitude, Thanks!

I have found 2 definitions of Eclipse Magnitude in total eclipse:

Solar eclipse for example, below we define $r_1$ as the radius of the Sun, $r_2$ as the radius of the Moon's Shadow, $d$ as the distance of Sun's center and Moon's center

if it is a partial eclipse, the Eclipse Magnitude have no objection:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} $$

Definition 1:

After the Sun is totally blocked, the Eclipse Magnitude jumps from $1$ to $r_2/r_1$, which is the ratio of Moon and Sun's diameter

http://www.jgiesen.de/eclipse/

https://www.oxfordreference.com/display/10.1093/oi/authority.20110803100126148

Definition 2:

After the Sun is totally blocked, the Eclipse Magnitude is still:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} > 1,\quad 0 \leq d \leq r_2 - r_1 $$

only if the Sun and Moon's center overlap, will $d = 0$, and $\epsilon = \epsilon_{max} = \dfrac{r_1 + r_2}{2r_1}$, but this will still be less than $r_2/r_1$

https://www.geogebra.org/m/SnZ7QGTJ

Which one is right? I didn't find any books or professional articles defines the calculation of Eclipse Magnitude, Thanks!

I have found 2 definitions of Eclipse Magnitude in total eclipse:

Solar eclipse for example, below we define $r_1$ as the radius of the Sun, $r_2$ as the radius of the Moon's Shadow, $d$ as the distance of Sun's center and Moon's center

if it is a partial eclipse, the Eclipse Magnitude have no objection:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} $$

Definition 1:

After the Sun is totally blocked, the Eclipse Magnitude jumps from $1$ to $r_2/r_1$, which is the ratio of Moon and Sun's diameter

http://www.jgiesen.de/eclipse/

https://www.oxfordreference.com/display/10.1093/oi/authority.20110803100126148

Definition 2:

After the Sun is totally blocked, the Eclipse Magnitude is still:

$$ \epsilon = \frac{r_1 + r_2 - d}{2r_1} > 1,\quad 0 \leq d \leq r_2 - r_1 $$

only if the Sun and Moon's center overlap, will $d = 0$, and $\epsilon = \epsilon_{max} = \dfrac{r_1 + r_2}{2r_1}$, but this will still be less than $r_2/r_1$

This provide a continuous definition of eclipse magnitude, on the other hand, in an annular solar eclipse, the Eclipse Magnitude is always $r_2/r_1$, having nothing to do with $d$, but this is continuous

https://www.geogebra.org/m/SnZ7QGTJ

Which one is right? I didn't find any books or professional articles defines the calculation of Eclipse Magnitude, Thanks!

Source Link
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