Please help assign due 2marrow effective radiative temperature

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SUMMARY

The discussion revolves around calculating the effective radiative temperature of the Earth during the Archeaneon, when the sun's radiative output was 30% less than today. The initial calculations provided the sun's temperature as approximately 5488.14K using the Boltzmann equation. The peak emission wavelength was calculated to be 0.527 micrometers using Wien's Law. To find the Earth's effective radiative temperature, one must apply the Stefan-Boltzmann law, considering the reduced solar radiation received by the Earth.

PREREQUISITES
  • Understanding of the Boltzmann equation
  • Familiarity with Wien's Law
  • Knowledge of the Stefan-Boltzmann law
  • Basic concepts of solar radiation and albedo
NEXT STEPS
  • Research the application of the Stefan-Boltzmann law in thermal radiation calculations
  • Study the effects of solar output variations on planetary temperatures
  • Explore the historical context of solar radiation changes over geological time
  • Learn about the implications of Earth's albedo on temperature calculations
USEFUL FOR

Students in astrophysics, climate science researchers, and anyone interested in the historical climate conditions of Earth and solar radiation effects.

Sunshin3
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. Homework Statement

It is believed that in the Archeaneon (2.5-4 billion years ago) the sun’s radiative output was 30% less than it is today.

(i) What would the temperature of the sun have been at that time?

(ii) At what wavelength would the peak emission from the sun have been?

(iii) Ignoring the effects of the atmosphere, what would the temperature of the Earth have been at this time (i.e. the effective radiative temperature)? Assume that the Earth’s albedo was 0.3, the same as today.


2. Homework Equations
Boltzmann equation
wiens law

3. The Attempt at a Solution

a)T= 4th root[5143824/(5.67*10^-8)]
t=5488.14K

b)detlamax=2897/5488.147
=0.527

I DONT GET PART 3 PLEASE HELP MEE! MY ASSIGNMENT IS DUE TOMARROW! PLEASE
 
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You will have to do a better job of explaining your work in parts 1 and 2.

To do part 3, you have to determine what amount of radiation the Earth currently receives / unit time and then reduce it by 30%. You know that the Earth must radiate that same amount of energy /unit time (on average). From that, apply the Stefan-Boltzmann law to determine its temperature.

AM
 

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