Potential effects of atmospheric collapse on Martian heat flow and application to the InSight measurements. (January 2020)
- Record Type:
- Journal Article
- Title:
- Potential effects of atmospheric collapse on Martian heat flow and application to the InSight measurements. (January 2020)
- Main Title:
- Potential effects of atmospheric collapse on Martian heat flow and application to the InSight measurements
- Authors:
- Attree, N.
Patel, N.
Hagermann, A.
Grott, M.
Spohn, T.
Siegler, M. - Abstract:
- Abstract: Heat flow is an important constraint on planetary formation and evolution. It has been suggested that Martian obliquity cycles might cause periodic collapses in atmospheric pressure, leading to corresponding decreases in regolith thermal conductivity (which is controlled by gas in the pore spaces). Geothermal heat would then build up in the subsurface, potentially affecting present–day heat flow — and thus the measurements made by a heat–flow probe such as the InSight HP 3 instrument. To gauge the order of magnitude of this effect, we model the diffusion of a putative heat pulse caused by thermal conductivity changes with a simple numerical scheme and compare it to the heat–flow perturbations caused by other effects. We find that an atmospheric collapse to 300 Pa in the last 40 kyr would lead to a present–day heat flow that is up to 2 − 8 % larger than the average geothermal background. Considering the InSight mission with expected 5 − 15 % error bars on the HP 3 measurement, this perturbation would only be significant in the best-case scenario of full instrument deployment, completed measurement campaign, and a well–modelled surface configuration. The prospects for detecting long-term climate perturbations via spacecraft heat–flow experiments remain challenging. Highlights: Mars obliquity cycles probably cause periodic collapses in atmospheric pressure. Regolith thermal conductivity decreases along with pressure. Reduced conductivity allows heat to build-up in theAbstract: Heat flow is an important constraint on planetary formation and evolution. It has been suggested that Martian obliquity cycles might cause periodic collapses in atmospheric pressure, leading to corresponding decreases in regolith thermal conductivity (which is controlled by gas in the pore spaces). Geothermal heat would then build up in the subsurface, potentially affecting present–day heat flow — and thus the measurements made by a heat–flow probe such as the InSight HP 3 instrument. To gauge the order of magnitude of this effect, we model the diffusion of a putative heat pulse caused by thermal conductivity changes with a simple numerical scheme and compare it to the heat–flow perturbations caused by other effects. We find that an atmospheric collapse to 300 Pa in the last 40 kyr would lead to a present–day heat flow that is up to 2 − 8 % larger than the average geothermal background. Considering the InSight mission with expected 5 − 15 % error bars on the HP 3 measurement, this perturbation would only be significant in the best-case scenario of full instrument deployment, completed measurement campaign, and a well–modelled surface configuration. The prospects for detecting long-term climate perturbations via spacecraft heat–flow experiments remain challenging. Highlights: Mars obliquity cycles probably cause periodic collapses in atmospheric pressure. Regolith thermal conductivity decreases along with pressure. Reduced conductivity allows heat to build-up in the subsurface. We model the excess heat flow with regards to the InSight HP 3 measurements. Atmospheric collapse effects are small compared to existing sources of error. … (more)
- Is Part Of:
- Planetary and space science. Volume 180(2020)
- Journal:
- Planetary and space science
- Issue:
- Volume 180(2020)
- Issue Display:
- Volume 180, Issue 2020 (2020)
- Year:
- 2020
- Volume:
- 180
- Issue:
- 2020
- Issue Sort Value:
- 2020-0180-2020-0000
- Page Start:
- Page End:
- Publication Date:
- 2020-01
- Subjects:
- Mars -- Mars -- Interior -- Mars -- Climate
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.2019.104778 ↗
- 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:
- 12571.xml