What is the “runaway greenhouse effect” scientists discussed on Venus? What has it resulted in on Venus?

The "runaway greenhouse effect" is a term used to describe a hypothetical scenario where a planet's atmosphere becomes so thick with heat-trapping gases, such as carbon dioxide, that the planet's surface temperature becomes hot enough to trigger a positive feedback loop where more vaporizes and contributes to the greenhouse effect.

On Venus, the runaway greenhouse effect has resulted in an extreme greenhouse effect with its surface temperature at an average of 464°C (867°F) – which is hotter than the surface of Mercury, despite Venus being farther from the Sun. Because Venus is so close to the sun and has a thick atmosphere, the heat is trapped inside, and it has no oceans, so it cannot regulate temperature through natural processes like Earth does. The planet's surface also has a pressure that is about 90 times greater than Earth's. Overall, the runaway greenhouse effect has made Venus one of the hottest planets in the solar system.

The "runaway greenhouse effect" is a term used by scientists to describe a situation where a planet's atmosphere traps an excessive amount of heat, causing the planet's surface temperature to rise uncontrollably.

On Venus, this runaway greenhouse effect has resulted in extremely high temperatures and a hostile environment. Venus is known as Earth's "sister planet" due to its similar size and composition, but it experiences extreme conditions. The average surface temperature on Venus is about 870 degrees Fahrenheit (465 degrees Celsius), making it the hottest planet in our solar system. The atmospheric pressure is also about 92 times greater than Earth’s, which is equivalent to being submerged 3,000 feet (900 meters) below the ocean surface.

The runaway greenhouse effect on Venus is primarily caused by the presence of a thick atmosphere predominantly consisting of carbon dioxide (CO2) and clouds of sulfuric acid. The CO2 in the atmosphere absorbs the sunlight and traps the heat, preventing it from escaping back into space. This leads to a rise in temperature, which in turn increases the rate of evaporation of water on Venus. Water vapor is also a greenhouse gas, contributing to the greenhouse effect and further amplifying the heating process. This creates a positive feedback loop, where higher temperatures lead to more evaporation and more evaporation leads to higher temperatures.

The extreme conditions on Venus serve as a cautionary example for our own planet. It demonstrates the potential consequences of a planet's atmosphere trapping excess heat, highlighting the importance of understanding and mitigating the factors that can contribute to a runaway greenhouse effect.

The "runaway greenhouse effect" refers to a phenomenon where a planet's atmosphere becomes so heat-trapping that it leads to a self-reinforcing cycle, causing temperatures to escalate uncontrollably.

On Venus, the runaway greenhouse effect has resulted in extreme temperatures and a hostile environment. Venus has a thick atmosphere composed mostly of carbon dioxide, which acts as a greenhouse gas. Sunlight passes through this atmosphere, heats the planet's surface, and the surface then radiates this heat back into space. However, the high concentration of carbon dioxide causes much of this heat to be trapped and retained, leading to a significant increase in surface temperatures.

The surface of Venus now experiences an average temperature of about 900 degrees Fahrenheit (475 degrees Celsius), which is higher than the temperatures found on Mercury, the planet closest to the Sun. Additionally, Venus has a dense cloud cover composed of sulfuric acid, causing a runaway greenhouse effect that further traps heat and raises the surface temperature even more. These extreme conditions make Venus an inhospitable and uninhabitable planet.