Skip to content
  • Home
  • Categories
    • Geology
    • Geography
    • Space and Astronomy
  • About
    • Privacy Policy
  • About
  • Privacy Policy
Our Planet TodayAnswers for geologist, scientists, spacecraft operators
  • Home
  • Categories
    • Geology
    • Geography
    • Space and Astronomy
  • About
    • Privacy Policy
on June 2, 2023

The Temperature Extremes of a Snowball Moon: Without an Atmosphere, How Cold and How Hot Could It Get?

Moon

The Snowball Earth hypothesis proposes that the Earth was completely covered by ice during at least two periods in its history. The first Snowball Earth event is thought to have occurred about 2.4 billion years ago, while the second occurred about 700 million years ago. During these periods, the Earth’s surface temperature is thought to have dropped drastically, leading to the formation of a global ice sheet. The question is, what would the approximate minimum and maximum temperatures be for a Snowball Earth without an atmosphere?

Contents:

  • Minimum temperature
  • Maximum temperature
  • Conclusion
  • FAQs

Minimum temperature

Without an atmosphere, the Earth’s surface would be unable to retain heat, leading to a rapid cooling of the planet. The minimum temperature that the Earth’s surface could reach without an atmosphere is about -430°F (-257°C). This temperature is based on the assumption that the Earth’s surface is completely covered in ice and that the planet has no internal heat source. At this temperature, the oceans would freeze solid and the atmosphere would become a thin layer of carbon dioxide.

The actual minimum temperature of a Snowball Earth without an atmosphere is difficult to determine. However, scientists believe it would be significantly colder than the estimated -430°F. This is because the Earth’s surface would reflect a significant amount of incoming solar radiation, further cooling the planet.

Maximum temperature

The maximum temperature the Earth’s surface could reach without an atmosphere depends largely on the amount of solar radiation the planet receives. Without an atmosphere, the Earth’s surface would be directly exposed to the Sun’s radiation, causing the planet to heat up rapidly. However, the amount of incoming solar radiation would depend on the distance between the Earth and the Sun, as well as the tilt of the Earth’s axis.

Assuming that the Earth’s distance from the Sun remains constant, the maximum temperature that the Earth’s surface could reach without an atmosphere is about 295°F (146°C). This temperature is based on the assumption that the Earth’s surface is completely free of ice and that the planet has no internal heat source. However, if the Earth’s distance from the Sun were to change, the maximum temperature could vary significantly.

Conclusion

In summary, the minimum and maximum temperatures for a Snowball Earth without an atmosphere depend on several factors, including the amount of solar radiation the planet receives, the distance between the Earth and the Sun, and the tilt of the Earth’s axis. Without an atmosphere, Earth’s surface would be unable to retain heat, leading to rapid cooling of the planet. The minimum temperature that the Earth’s surface could reach without an atmosphere is estimated to be about -430°F, while the maximum temperature could be as high as 295°F. More research is needed to determine the exact temperatures the Earth’s surface could reach under these conditions.

FAQs

1. What is the Snowball Earth hypothesis?

The Snowball Earth hypothesis proposes that Earth was completely covered in ice during at least two periods in its history. It is believed that the first Snowball Earth event occurred approximately 2.4 billion years ago, while the second occurred approximately 700 million years ago.

2. What is the minimum temperature that Earth’s surface could reach without an atmosphere?

The minimum temperature that Earth’s surface could reach without an atmosphere is approximately -430°F (-257°C). This temperature is based on the assumption that Earth’s surface is completely covered in ice and that the planet has no internal heat source.

3. Why is the actual minimum temperature of a Snowball Earth with no atmosphere difficult to determine?

The actual minimum temperature of a Snowball Earth with no atmosphere is difficult to determine precisely because Earth’s surface would reflect a significant amount of incoming solar radiation, further cooling the planet.

4. What is the maximum temperature that Earth’s surface could reach without an atmosphere?

The maximum temperature that Earth’s surface could reach without an atmosphere is approximately 295°F (146°C). This temperature is based on the assumption that Earth’s surface is entirely devoid of ice and that the planet has no internal heat source.

5. What factors determine the minimum and maximum temperatures for a Snowball Earth with no atmosphere?

The minimum and maximum temperatures for a Snowball Earth with no atmosphere are dependent on several factors, including the amount of solar radiation the planet receives, the distance between Earth and the Sun, and the tilt of Earth’s axis.

6. Would the actual minimum temperature of a Snowball Earth with no atmosphere be colder than -430°F?

Yes, scientists believe that the actual minimum temperature of a Snowball Earth with no atmosphere would be significantly colder than the estimated -430°F due to Earth’s surface reflecting a significant amount of incoming solar radiation, further cooling the planet.



7. Could the maximum temperature that Earth’s surface could reach without an atmosphere vary?

Yes, assuming that Earth’s distance from the Sun remains constant, the maximum temperature that Earth’s surface could reach without an atmosphere is approximately 295°F. However, if Earth’s distance from the Sun were to change, the maximum temperature could vary significantly.

Recent

  • Exploring the Geological Features of Caves: A Comprehensive Guide
  • What Factors Contribute to Stronger Winds?
  • The Scarcity of Minerals: Unraveling the Mysteries of the Earth’s Crust
  • How Faster-Moving Hurricanes May Intensify More Rapidly
  • Adiabatic lapse rate
  • Exploring the Feasibility of Controlled Fractional Crystallization on the Lunar Surface
  • The Greenhouse Effect: How Rising Atmospheric CO2 Drives Global Warming
  • Examining the Feasibility of a Water-Covered Terrestrial Surface
  • What is an aurora called when viewed from space?
  • Measuring the Greenhouse Effect: A Systematic Approach to Quantifying Back Radiation from Atmospheric Carbon Dioxide
  • Asymmetric Solar Activity Patterns Across Hemispheres
  • Unraveling the Distinction: GFS Analysis vs. GFS Forecast Data
  • The Role of Longwave Radiation in Ocean Warming under Climate Change
  • Esker vs. Kame vs. Drumlin – what’s the difference?

Categories

  • English
  • Deutsch
  • Français
  • Home
  • About
  • Privacy Policy

Copyright Our Planet Today 2025

We use cookies on our website to give you the most relevant experience by remembering your preferences and repeat visits. By clicking “Accept”, you consent to the use of ALL the cookies.
Do not sell my personal information.
Cookie SettingsAccept
Manage consent

Privacy Overview

This website uses cookies to improve your experience while you navigate through the website. Out of these, the cookies that are categorized as necessary are stored on your browser as they are essential for the working of basic functionalities of the website. We also use third-party cookies that help us analyze and understand how you use this website. These cookies will be stored in your browser only with your consent. You also have the option to opt-out of these cookies. But opting out of some of these cookies may affect your browsing experience.
Necessary
Always Enabled
Necessary cookies are absolutely essential for the website to function properly. These cookies ensure basic functionalities and security features of the website, anonymously.
CookieDurationDescription
cookielawinfo-checkbox-analytics11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookie is used to store the user consent for the cookies in the category "Analytics".
cookielawinfo-checkbox-functional11 monthsThe cookie is set by GDPR cookie consent to record the user consent for the cookies in the category "Functional".
cookielawinfo-checkbox-necessary11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookies is used to store the user consent for the cookies in the category "Necessary".
cookielawinfo-checkbox-others11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookie is used to store the user consent for the cookies in the category "Other.
cookielawinfo-checkbox-performance11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookie is used to store the user consent for the cookies in the category "Performance".
viewed_cookie_policy11 monthsThe cookie is set by the GDPR Cookie Consent plugin and is used to store whether or not user has consented to the use of cookies. It does not store any personal data.
Functional
Functional cookies help to perform certain functionalities like sharing the content of the website on social media platforms, collect feedbacks, and other third-party features.
Performance
Performance cookies are used to understand and analyze the key performance indexes of the website which helps in delivering a better user experience for the visitors.
Analytics
Analytical cookies are used to understand how visitors interact with the website. These cookies help provide information on metrics the number of visitors, bounce rate, traffic source, etc.
Advertisement
Advertisement cookies are used to provide visitors with relevant ads and marketing campaigns. These cookies track visitors across websites and collect information to provide customized ads.
Others
Other uncategorized cookies are those that are being analyzed and have not been classified into a category as yet.
SAVE & ACCEPT