Loading…
Loading grant details…
| Funder | Science and Technology Facilities Council |
|---|---|
| Recipient Organization | University College London |
| Country | United Kingdom |
| Start Date | Sep 30, 2024 |
| End Date | Mar 30, 2028 |
| Duration | 1,277 days |
| Number of Grantees | 2 |
| Roles | Student; Supervisor |
| Data Source | UKRI Gateway to Research |
| Grant ID | 2920868 |
The surface of Mars is a harsh environment for robotic and human exploration, with strong temperature differences (0 to 20 C during the day and -100 to -120 C at night), ultraviolet radiation which penetrates the thin atmosphere, and a significant radiation environment from galactic and solar energetic particle sources.
Mars also has a network of crustal magnetic fields, which are evidence of a past global protective magnetic field.
Since the Mars global magnetic field was lost 3.8-4 billion years ago, the atmosphere was gradually lost via solar wind scavenging.
The current Mars atmosphere is dominated by CO2, and the atmospheric pressure varies with time of day and year, but the pressure is overall less than 1% of Earth's. Also, seasonal dust storms occur at Mars offering some protection.
In this project we will study the protection provided by crustal fields, dust and clouds in the atmosphere for potential future exploration, by modelling plasma and radiation effects and comparing with data from Mars Express, Maven and Curiosity.
We will also model subsurface effects, relevant for future missions including Mars sample return, Rosalind Franklin and future exploration, building on techniques used by Dartnell...Coates et al., GRL 2007, Regan, Coates et al PSJ 2023, Patel...Coates et al PSJ 2023.
University College London
Complete our application form to express your interest and we'll guide you through the process.
Apply for This Grant