Although the
asteroids and
comets that impact the Earth hit with many times the explosive force of a
volcano, the mechanisms of an impact winter are similar to those that occur after a mega-
volcanic eruption-induced
volcanic winter. In this scenario massive amounts of debris injected into the
atmosphere would block some of the
Sun's radiation for an extended period of time and lower the mean global temperature by as much as 20°C after a year. This is
controversially purported to have occurred following the
Toba eruption. These pulverized rock particles would remain in the
atmosphere until
dry deposition and due to their size, they would also act as
cloud condensation nuclei and would be washed out by
wet deposition/precipitation, but even then, about 15% of the
sun's radiation might not reach the surface. After the first 20 days, the land temperature might drop quickly, by about 13°C. After about a year, the temperature could rebound by about 6°C, but by this time about one-third of the Northern Hemisphere might be covered in ice. This volcanism could alone therefore create a
volcanic winter, irrespective of the other impact effects.
Multiple firestorms In combination with the initial debris ejected into the
atmosphere, if the impactor is extremely large ( or more), like at the Cretaceous–Paleogene extinction event (estimated ), there might be the ignition of multiple
fire storms, possibly with a global reach into every dense and therefore firestorm-prone forest. These wood fires might release enough amounts of water vapor, ash, soot, tar and carbon dioxide into the atmosphere to
perturb the climate on their own and cause the pulverized rock dust cloud blocking the sun to last longer. Alternatively it could cause it to last for a much shorter time, as there would be more water vapor for the rocky aerosol particles to form
cloud condensation nuclei. If it causes the dust cloud to last longer, it would prolong the Earth's cooling time, possibly causing thicker ice sheets to form. == Past events==