The performance of gallium arsenide/germanium solar cells at the Martian surface

Abstract A theoretical model was used to predict the electrical power output by Gallium Arsenide/ Germanium solar cells at the surface of Mars. This model was validated using measurements from the Mars Pathfinder Lander. It was then used to estimate the solar power output as a function of latitude, local time, and season for airborne dust optical depths between 0.1 and 5. For this range of dust opacities, the power output varies by about a factor of three at low and mid-latitudes. This model was also used to estimate the solar cell performance degradation due to dust accumulation. Dust accumulation reduced the power output by 0.4 to 0.5% Martian day during the first 20 days of the mission, but the power loss rate fell to ∼0.1%/day after that. If these power loss rates are typical, solar power provides a viable option for long-lived stations on the Martian surface.

[1]  M. Lemmon,et al.  Opacity of the Martian atmosphere measured by the Imager for Mars Pathfinder , 1999 .

[2]  D. Crisp,et al.  Ground‐based near‐infrared observations of the Venus nightside: The thermal structure and water abundance near the surface , 1996 .

[3]  D. Crisp Infrared radiative transfer in the dust-free Martian atmosphere , 1990 .

[4]  James B. Pollack,et al.  Viking Lander image analysis of Martian atmospheric dust , 1995 .

[5]  Eugene H. Avrett,et al.  Calculation of Solar Irradiances. I. Synthesis of the Solar Spectrum , 1999 .

[6]  Ralph A. Kahn,et al.  Properties of aerosols in the Martian atmosphere, as inferred from Viking lander imaging data , 1977 .

[7]  Phillip P. Jenkins,et al.  Measurement of the settling rate of atmospheric dust on Mars by the MAE instrument on Mars Pathfinder , 2000 .

[8]  J. Hansen,et al.  Light scattering in planetary atmospheres , 1974 .

[9]  Christopher P. McKay,et al.  Atmospheric Effects on the Utility of Solar Power on Mars , 1993 .

[10]  D. Crisp Radiative forcing of the Venus mesosphere: I. Solar fluxes and heating rates , 1986 .

[11]  C. H. Acton,et al.  Ancillary data services of NASA's Navigation and Ancillary Information Facility , 1996 .

[12]  R. Todd Clancy,et al.  A new look at dust and clouds in the Mars atmosphere: analysis of emission-phase-function sequences from global viking IRTM observations , 1991 .

[13]  K. Stamnes,et al.  Numerically stable algorithm for discrete-ordinate-method radiative transfer in multiple scattering and emitting layered media. , 1988, Applied optics.

[14]  David Crisp,et al.  Absorption of sunlight by water vapor in cloudy conditions: A partial explanation for the cloud absorption anomaly , 1997 .

[15]  J. Appelbaum,et al.  Photovoltaic power system operation in the Mars environment , 1989, Proceedings of the 24th Intersociety Energy Conversion Engineering Conference.

[16]  Mark T. Lemmon,et al.  Properties of dust in the Martian atmosphere from the Imager on Mars Pathfinder , 1999 .