Longest day of year in the tropics

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Discussion Overview

The discussion revolves around the concept of the longest day of the year in the tropics, particularly focusing on the relationship between the sun's declination, latitude, and the length of daylight. Participants explore the implications of these factors for locations such as Hawaii and the equator, examining both theoretical and practical aspects of solar positioning and its effects on day length.

Discussion Character

  • Exploratory
  • Technical explanation
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • One participant claims that the longest day of the year in the tropics does not coincide with the summer solstice but occurs when the angle of declination equals the latitude of the location.
  • Another participant challenges this claim, suggesting that the main assertion is incorrect.
  • A participant expresses confusion about the relationship between the sun's position on specific dates and the length of the day, particularly questioning the validity of their earlier statement.
  • One participant provides a formula for calculating the length of the day based on declination and latitude.
  • There is a discussion about whether all days along the equator are always 12 hours long, with some participants asserting this is true while others contest it.
  • A participant presents data showing that days at the equator vary slightly in length, contradicting the notion of a constant 12-hour day.
  • Another participant mentions atmospheric refraction as a factor contributing to the average day length exceeding 12 hours.
  • Further elaboration is provided on how sunrise and sunset definitions impact the perceived length of the day.
  • One participant introduces the concept of "Lahaina Noon," noting that there are two longest days of the year in Hawaii, occurring around May 18th and July 25th.

Areas of Agreement / Disagreement

Participants do not reach a consensus on the relationship between the longest day of the year and the summer solstice, with multiple competing views and ongoing confusion about specific claims and calculations.

Contextual Notes

Some discussions involve unresolved assumptions regarding the definitions of sunrise and sunset, as well as the impact of atmospheric conditions on day length. The calculations and observations presented may depend on specific geographic locations and conditions.

bigislander72
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It is not the summer solstice(june 21) but when the angle of declination(angle sun makes with equitorial plane at solar noon) equals the degree of latitude for that particular location. I calculated that today, may 25 is that for honolulu,hi and will again repeat sometime in july. These are the days the sun appears directly overhead at solar noon. For locations north of 23.5 degrees latitude the longest day of the year coincides with the summer solstice.

Are these statements correct?
 
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Well I have confirmed that my statement was incorrect via this handy website www.srrb.noaa.gov/highlights/sunrise/sunrise.html

I am still confused as to why. It seems that on that day ( approx. may 25) the sun is directley over the latitude for which Hawaii lies and on the summer solstice, the sun makes an arc that is slightly to the north(shadow points due south at solar noon). So I don't understand why the day would be longer. Is this true anywhere in the norther hemisphere?Please explain.
 
Calculate the length-of-day ( LD ) by

cos(LD/2) = - tan(declination) tan(latitude)

LD is in degrees that can be converted to hours, min, sec

For locations north of EQUATOR the longest day of the year coincides with the summer solstice.
 
Helios said:
For locations north of EQUATOR the longest day of the year coincides with the summer solstice.

If this is true and if it is also true that the longest day of the year south of the equator is the summer solstice, then it must be that all days along the equator are always 12 hours long. Is this true?
 
Yes, this is true
 
Helios -

Not strictly true.

For an arbitrary position on Earth at the Equator given as:
0 0 N 106 35 W - for 2009
May 29 2009 sunrise 06:00:11 sunset 18:07:21 12hrs 7min 10sec
Solstice Jun 20 sunrise 06:04:37 sunset 18:11:53 12hrs 7min 16sec
Solstice Dec 21 sunrise 06:01:21 sunset 18:08:36 12hrs 7min 15sec

The days are very slighty varying in length but the mean time between official sunrise and official sunset are clearly 12 hours 7 minutes and few seconds. Due to the arc subtended by the disc of the sun it is not 12 hours even - sunset occurs when the top of the disc appears, sunset at the time when the "other side" top of solar the disc disappears. The difference is the transit time for the angle of solar disc.
Works out to circa 7 minutes.
 
Interesting. I remember from my astronomy class that days average longer than 12 hours because of the refraction of the atmosphere, the sun still appears above the horizon even after it has set. Is that the reason for the extra 7 minutes?
 
partly - it also has to do with how we define sunrise and sunset, too - any part of the sun's disc is visible == we are in daytime.
 
  • #10
bigislander72 said:
Well I have confirmed that my statement was incorrect via this handy website www.srrb.noaa.gov/highlights/sunrise/sunrise.html

I am still confused as to why. It seems that on that day ( approx. may 25) the sun is directley over the latitude for which Hawaii lies and on the summer solstice, the sun makes an arc that is slightly to the north(shadow points due south at solar noon). So I don't understand why the day would be longer. Is this true anywhere in the norther hemisphere?Please explain.
This is an interesting question - I've had to think about it for a while myself. Here's a suggestion for another way to look at it, which might help:

Instead of thinking about the arc traversed by the Sun as it "moves" across the sky (I admit that I haven't yet found a way to explain the answer in those terms), try thinking about the arc you traverse as your location on the Earth's surface moves throughout the day. If you look at portion of this path that is in the sunlit half of the Earth's sphere, it's clearly half at equinox, and pretty clearly its longest at Summer Solstice, when the path extends the farthest distance past the noon +/- 6 hour angle points to the terminator line. It's a little harder to see what's going on at the days you reference in your OP, but maybe you can convince yourself that it must be shorter than on Solstice.
 
  • #11
jim mcnamara said:
partly - it also has to do with how we define sunrise and sunset, too - any part of the sun's disc is visible == we are in daytime.

Well, that would account for two of the seven minutes - one in the morning and one in the evening.
 
  • #12
skeptic2 said:
Well, that would account for two of the seven minutes - one in the morning and one in the evening.
Or slightly longer than 2 if the sun is setting at an angle. I think the remainder of the difference is refraction. Although this varies from day to day, it is not predictable long-term. So the predicted sunset / sunrise times probably use an average which is about 3-4 extra minutes before sunrise and after sunset.
 
  • #13
It's called "Lahaina Noon" here in Hawai'i. Lahaina means 'cruel sun', and the name was chosen in a competition sponsored by the Bishop Museum. And YES, we have TWO longest days of the year in the tropics. Here in Hilo, on the Big Island of Hawai'i, those days are approximately May 18th and July 25th.
 

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