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Cosmic dust in the earth's atmosphere
1School of Chemistry, University of Leeds, Woodhouse Lane, Leeds LS2 9JT, UK. j.m.c.plane@leeds.ac.uk
Chemical Society Reviews
|June 9, 2012
Summary
Cosmic dust enters Earth's atmosphere daily, with estimates ranging from 5 to 300 tonnes. This interplanetary dust impacts atmospheric processes, climate change indicators, and ocean fertilization.
Area of Science:
- Earth Science
- Atmospheric Science
- Planetary Science
Background:
- Interplanetary dust continuously enters Earth's atmosphere.
- Discrepancies exist between estimates of cosmic dust input.
- Cosmic dust influences atmospheric chemistry and climate.
Purpose of the Study:
- To review the magnitude of cosmic dust input into Earth's atmosphere.
- To discuss the impacts of cosmic dust from 100 km to the surface.
- To highlight the implications of differing dust input estimates.
Main Methods:
- Zodiacal cloud observations and spaceborne dust detector measurements.
- Analysis of cosmic-enriched elements (Ir, Pt, Os, Fe) in polar ice and deep-sea sediments.
- Middle atmosphere measurements using radar, lidar, aircraft, and satellite remote sensing.
Main Results:
- Interplanetary dust input estimates range from 100-300 tonnes/day (remote sensing) to 5-50 tonnes/day (middle atmosphere).
- Discrepancies suggest either faster-than-expected atmospheric transport or a need to revise solar system dust evolution models.
- Ablated metals from cosmic dust form atmospheric layers, influence noctilucent clouds, stratospheric aerosols, and ocean fertilization.
Conclusions:
- The significant discrepancy in cosmic dust input estimates necessitates further research into atmospheric transport mechanisms.
- Understanding cosmic dust's role is crucial for accurately modeling atmospheric chemistry, climate change, and potential geo-engineering impacts.
- Cosmic dust deposition influences atmospheric phenomena from noctilucent cloud formation to ocean biogeochemistry.
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