Updated
Updated · Livescience.com · Sep 12
Venus Tops 900 F, Outheating Mercury by 100 F on Dense CO2 Blanket
Updated
Updated · Livescience.com · Sep 12

Venus Tops 900 F, Outheating Mercury by 100 F on Dense CO2 Blanket

3 articles · Updated · Livescience.com · Sep 12

Summary

  • Venus reaches about 900 F, roughly 100 F hotter than Mercury’s peak 800 F, even though it sits 31 million miles farther from the sun.
  • A carbon-dioxide atmosphere about 90 times denser than Earth’s traps infrared heat on Venus, while Mercury’s near-airless surface sheds warmth quickly after sunset.
  • Mercury’s temperatures swing from 800 F by day to minus 290 F at night, but Venus stays nearly uniformly hot because its thick atmosphere keeps reabsorbing and reradiating heat.
  • Venus reflects about three-quarters of incoming sunlight, and only around 3% reaches the surface; stripped of its clouds and atmosphere, bare-rock Venus would be cooler than Mercury.
  • Scientists say volcanic and tectonic activity likely built that greenhouse blanket, leaving Venus in a post-runaway greenhouse state that shows distance from the sun alone does not determine planetary climate.

Insights

Could the terrifying runaway greenhouse effect that turned Venus into a scorching wasteland eventually happen to Earth?
What hidden volcanic secrets are still fueling the thick, heat-trapping clouds of our solar system's hottest planet today?
Why is the second planet from the sun actually a hotter, more hellish world than the one closest to our star?