Which of the following best explains why Mars' and Venus' surface temperatures vary, despite both planets having atmospheres that contain mostly carbon dioxide? (1 point)

Mars and Venus have different surface temperatures due to variations in their atmospheres and their distance from the Sun. While both planets have atmospheres that contain carbon dioxide, Venus has a much denser atmosphere than Mars. The thick atmosphere of Venus traps heat from the Sun, leading to a runaway greenhouse effect and extremely high temperatures on its surface. In contrast, Mars has a much thinner atmosphere, which cannot effectively trap heat, resulting in much colder temperatures.

The surface temperature variation between Mars and Venus can be attributed to several factors despite both planets having atmospheres with mostly carbon dioxide.

1. Distance from the Sun: One of the main factors is the distance of each planet from the Sun. Venus is closer to the Sun than Mars, resulting in higher solar radiation and consequently higher surface temperatures.

2. Atmospheric Pressure: Another important factor is the atmospheric pressure. Venus has an extremely dense atmosphere with a pressure over 90 times that of Earth's, while Mars has a very thin atmosphere with a pressure less than 1% of Earth's. The high atmospheric pressure on Venus acts as a greenhouse effect, trapping heat and leading to extremely high temperatures.

3. Greenhouse Effect: The greenhouse effect is the process by which certain gases in an atmosphere trap heat. Although both Mars and Venus have atmospheres composed mainly of carbon dioxide, the greenhouse effect on Venus is much more pronounced due to its dense atmosphere and high pressure. This causes a dramatic trapping of heat, leading to Venus' extremely hot temperatures.

In summary, the distance from the Sun, atmospheric pressure, and the intensity of the greenhouse effect are the main reasons why Mars and Venus have such different surface temperatures despite both having atmospheres dominated by carbon dioxide.

To determine why the surface temperatures of Mars and Venus vary despite having primarily carbon dioxide in their atmospheres, we need to consider a few key factors.

First, let's understand the greenhouse effect. Greenhouse gases, such as carbon dioxide, trap heat from the sun in a planet's atmosphere, raising the temperature at the surface. However, the greenhouse effect alone cannot account for the temperature differences between Mars and Venus.

One major factor to consider is the distance of each planet from the sun. Venus is closer to the sun compared to Mars, receiving significantly more solar radiation. This increased proximity to the sun means that Venus receives more energy and heat from sunlight, causing its surface temperature to rise significantly.

Second, we should examine the atmospheres of both planets. While both Mars and Venus have atmospheres predominantly composed of carbon dioxide, there are significant differences in their atmospheric conditions.

Venus has a very dense atmosphere, consisting mainly of carbon dioxide with traces of other gases. This dense atmosphere creates a strong greenhouse effect, trapping a substantial amount of heat and causing the surface temperature to soar. Venus has one of the hottest planetary surfaces in our solar system, with an average temperature of about 900 degrees Fahrenheit (475 degrees Celsius).

On the other hand, Mars has a much thinner atmosphere compared to Venus. While it also contains carbon dioxide, its atmospheric pressure is significantly lower. As a result, the greenhouse effect on Mars is much weaker, and less heat is trapped in its atmosphere. Therefore, Mars has much colder surface temperatures compared to Venus, with an average temperature of around -80 degrees Fahrenheit (-62 degrees Celsius).

In conclusion, the difference in surface temperatures between Mars and Venus despite having similar carbon dioxide-rich atmospheres can primarily be attributed to their distance from the sun and the varying compositions and densities of their atmospheres.