Perigee & Apogee: How Earth's Orbit Impacts Summer Temperatures

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Discussion Overview

The discussion explores the relationship between the Earth's orbital characteristics, specifically perihelion and aphelion, and their potential impact on summer temperatures in the northern and southern hemispheres. It includes considerations of seasonal temperature variations, the influence of Earth's axial tilt, and the distribution of land and ocean.

Discussion Character

  • Exploratory
  • Debate/contested
  • Technical explanation
  • Mathematical reasoning

Main Points Raised

  • Some participants question whether the perigee and apogee of Earth's orbit affect summer temperatures, suggesting that perihelion and aphelion are the correct terms to use.
  • One participant notes that Earth's axial tilt is the primary reason for seasonal temperature differences, with the orbit's eccentricity playing a minor role.
  • Another participant calculates that, without tilt or atmosphere, temperature variation due to orbital distance would be approximately 4.5°C (8°F), but acknowledges that other factors complicate this analysis.
  • Some participants highlight the difference in land and ocean distribution between the hemispheres as a significant factor influencing temperature, with the northern hemisphere experiencing warmer summers and colder winters compared to the southern hemisphere.
  • One participant challenges the assertion that southern hemisphere winters are milder, arguing that data shows significant differences in winter conditions between the hemispheres.
  • Another participant emphasizes that while solar irradiance varies between perihelion and aphelion, the Earth's climate system has a more substantial impact on surface temperatures than orbital distance alone.
  • Oceanic heat sinks and variations in ocean currents are mentioned as additional variables that may influence temperature differences.

Areas of Agreement / Disagreement

Participants express differing views on the impact of Earth's orbital characteristics on temperature, with no consensus reached. Some argue that axial tilt and land-ocean distribution are more significant, while others emphasize the role of orbital distance.

Contextual Notes

Participants acknowledge that the discussion is complicated by various factors, including the distribution of land and ocean, regional climate conditions, and the simplifications made in comparisons of temperatures at different latitudes.

Who May Find This Useful

This discussion may be of interest to those studying climate science, astronomy, or anyone curious about the factors influencing seasonal temperature variations on Earth.

philip porhammer
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does the Perigee and Apogee of the Earth's orbit relative to the seasons affect the temperature of our summers?
 
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philip porhammer said:
does the Perigee and Apogee of the Earth's orbit relative to the seasons affect the temperature of our summers?
What's your conclusion, given that the sun is approximately constant in its radiation output? Have you considered northern and southern hemispheres?
 
You probably mean perihelion and aphelion instead of perigee and apogee when we talk about Earth orbiting Sun.
The reason why we have seasons on Earth is due to the fact that axis of Earth's rotation is not perpendicular to the orbital plane, it is tilted by about 23 degrees. As Earth orbits Sun, one of the hemispheres is getting more sunlight than the other, except equinoxes, of course.
However, the orbit is slightly eccentric, and indeed it plays some role. Perihelion occurs at beginning of January, and as Earth is slightly closer to Sun than a mean distance, the winters on northern hemisphere are bit warmer than winters on southern hemisphere (aphelion occurs in July). Similarly, the summers are bit colder on northern hemisphere.
 
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Interesting question. From my calculations, if the Earth were not tilted, and had no atmosphere, the variation in temperature would be ≈4.5°C (≈8°F).

Wiki lists:
a. Earth's tilt
b. Higher concentration of land masses in the northern vs southern hemispheres​
as two reasons this is hard to figure out.

"...summers are 2.3 °C (4 °F) warmer in the northern hemisphere than in the southern hemisphere under similar conditions."

Which is backwards, if temperature were based on apsides.
 
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You are right! I made it too simple in my previous post, I didn't consider the difference in surface of the hemispheres. What I wrote would be the case if the Earth's surface is homogeneous.
The surface of the southern hemisphere is covered by more ocean and less land comparing to northern hemisphere. That influences how is the heat absorbed and transported over the surface. I found this link interesting.

One can learn something new every day!
 
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lomidrevo said:
Perihelion occurs at beginning of January, and as Earth is slightly closer to Sun than a mean distance, the winters on northern hemisphere are bit warmer than winters on southern hemisphere (aphelion occurs in July).
No, that is very incorrect and you only need to look at the data to see that.
The southern hemispheres have VERY mild winters compared to the northern hemisphere.
We don't get the massive snowfalls, ice storms, rivers freezing over etc etc

OmCheeto said:
"...summers are 2.3 °C (4 °F) warmer in the northern hemisphere than in the southern hemisphere under similar conditions."

yeah ... under similar conditions, which of course they are not :wink:

Dave
 
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davenn said:
No, that is very incorrect and you only need to look at the data to see that.
Yes, I thought I made it clear in my post #5, that I admit I was wrong in my first post. Although the difference of solar irradiance between perihelion and aphelion is almost 7%, the Earth's climate system (including distribution of land and ocean) has a more significant influence on the surface temperatures.

davenn said:
The southern hemispheres have VERY mild winters compared to the northern hemisphere.
We don't get the massive snowfalls, ice storms, rivers freezing over etc etc
If you compare the mean temperatures at comparable (opposite) latitudes (e.g Sydney and Los Angeles), the difference is not very big. Daily mean in Sydney 13 °C (in July) vs. 14.4 °C in LA (January) could even suggest colder winter in Sydney. Of course, this is very simplified comparison, as we do not take into account any effects due to regional climate conditions (we could also try to compare Europe and Patagonia). I just want to point out that differences might not be so big as you suggest.
 
Another variable is the oceanic heat sinc and its variation of currents.
 

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