Mass accumulation of earth from interplanetary dust, meteoroids, asteroids and comets. (1st September 2017)
- Record Type:
- Journal Article
- Title:
- Mass accumulation of earth from interplanetary dust, meteoroids, asteroids and comets. (1st September 2017)
- Main Title:
- Mass accumulation of earth from interplanetary dust, meteoroids, asteroids and comets
- Authors:
- Drolshagen, Gerhard
Koschny, Detlef
Drolshagen, Sandra
Kretschmer, Jana
Poppe, Björn - Abstract:
- Abstract: Using new data and recent models this paper derives a total combined flux model of the mass reaching Earth as interplanetary material. For the small sizes the interplanetary flux model by Grün et al. (1985) was used which describes the mass flux at 1 AU for meteoroids in the mass range 10 –21 kg to about 10 −1 kg. For the large objects the flux models by Brown et al. (2002) were used which were derived for bodies greater than 1 m and are based on sensor data of fireballs that entered the Earth atmosphere. For the intermediate size range interpolations and alternative models based on meteor and fireball data were used. All flux models were converted to an altitude of 100 km above the Earth surface to make them comparable. The total combined flux model covers more than 34 orders of magnitude in mass. Using recent measurements and alternative flux models the uncertainties of the obtained model were estimated. Recent measurements include in-situ impact data on retrieved space hardware and optical meteor and fireball data. Depending on the models and interpolation used the interplanetary material that enters the Earth atmosphere per day is in the range of 30−180 t with a best guess value of 54 t per day for an upper cut-off size of 1 km. If the upper size limit is placed at 0.5 m which is the largest size where statistically a daily impact is expected, the expected mass influx is slightly more than 32 t per day. The combined models with interpolations suggestAbstract: Using new data and recent models this paper derives a total combined flux model of the mass reaching Earth as interplanetary material. For the small sizes the interplanetary flux model by Grün et al. (1985) was used which describes the mass flux at 1 AU for meteoroids in the mass range 10 –21 kg to about 10 −1 kg. For the large objects the flux models by Brown et al. (2002) were used which were derived for bodies greater than 1 m and are based on sensor data of fireballs that entered the Earth atmosphere. For the intermediate size range interpolations and alternative models based on meteor and fireball data were used. All flux models were converted to an altitude of 100 km above the Earth surface to make them comparable. The total combined flux model covers more than 34 orders of magnitude in mass. Using recent measurements and alternative flux models the uncertainties of the obtained model were estimated. Recent measurements include in-situ impact data on retrieved space hardware and optical meteor and fireball data. Depending on the models and interpolation used the interplanetary material that enters the Earth atmosphere per day is in the range of 30−180 t with a best guess value of 54 t per day for an upper cut-off size of 1 km. If the upper size limit is placed at 0.5 m which is the largest size where statistically a daily impact is expected, the expected mass influx is slightly more than 32 t per day. The combined models with interpolations suggest deviations from a simple power law. The flux in the diameter range of 0.01–0.1 m appears not as large as suggested by a simple power law interpolation. Highlights: This paper derives a total combined flux model of the mass reaching Earth as interplanetary material. The total combined flux model covers more than 34 orders of magnitude in mass. The interplanetary material that enters the Earth atmosphere per day is in the range of 30 - 180 tons with a best guess value of 54 tons per day. If the upper size limit is placed at 0.5 m, the expected mass influx is slightly more than 32 tons per day. The flux in the diameter range of 0.01 m – 0.1 m appears not as large as suggested by a simple power law interpolation. … (more)
- Is Part Of:
- Planetary and space science. Volume 143(2017)
- Journal:
- Planetary and space science
- Issue:
- Volume 143(2017)
- Issue Display:
- Volume 143, Issue 2017 (2017)
- Year:
- 2017
- Volume:
- 143
- Issue:
- 2017
- Issue Sort Value:
- 2017-0143-2017-0000
- Page Start:
- 21
- Page End:
- 27
- Publication Date:
- 2017-09-01
- Subjects:
- Meteoroids -- Asteroids -- Mass accumulation -- Impacts -- Meteoroid fluxes
Space sciences -- Periodicals
Atmosphere, Upper -- Periodicals
Sciences spatiales -- Périodiques
Haute atmosphère -- Périodiques
523 - Journal URLs:
- http://www.sciencedirect.com/science/journal/00320633 ↗
http://www.elsevier.com/journals ↗ - DOI:
- 10.1016/j.pss.2016.12.010 ↗
- Languages:
- English
- ISSNs:
- 0032-0633
- Deposit Type:
- Legaldeposit
- View Content:
- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library DSC - 6508.320000
British Library DSC - BLDSS-3PM
British Library HMNTS - ELD Digital store - Ingest File:
- 1378.xml