Possible impact of interplanetary and interstellar dust fluxes on the Earth's climate

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

1

Scientific paper

This article considers the process of entry of cosmic substance into the Earth's atmosphere and the further evolution of the formed extraterrestrial aerosol. It is shown that meteorite-derived aerosol generated in the atmosphere may affect the Earth's climate in two ways: (a) particles of meteoric haze may serve as condensation nuclei in the troposphere and stratosphere; (b) charged meteor particles residing in the mesosphere may markedly change (by a few percent) the total atmospheric resistance and, thereby, affect the global current circuit. Changes in the global electric circuit, in turn, may influence cloud formation processes. The obtained results argue for the fact that the meteoric dust in the Earth's atmosphere is potentially one of the important climate-forming agents. It is shown that the amount of interstellar dust in the Earth's atmosphere is too small to have a considerable affect on atmospheric processes.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Possible impact of interplanetary and interstellar dust fluxes on the Earth's climate does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Possible impact of interplanetary and interstellar dust fluxes on the Earth's climate, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Possible impact of interplanetary and interstellar dust fluxes on the Earth's climate will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-765009

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.