Physical Layer Communications Technologies

被引:2
|
作者
Romanofsky, Robert [1 ]
Scardelletti, Maximilian [1 ]
Jordan, Jennifer [1 ]
机构
[1] NASA, Glenn Res Ctr, Cleveland, OH 44135 USA
关键词
GATE;
D O I
10.1109/MMM.2021.3110157
中图分类号
TM [电工技术]; TN [电子技术、通信技术];
学科分类号
0808 ; 0809 ;
摘要
Although terrestrial wireless communications often must function under harsh environmental conditions, there are peculiar demands on communications systems for planetary exploration. For example, the mil-spec electronics temperature range is generally regarded as -55-+125 °C. A probe on the surface of Venus will experience a nearly constant operational temperature of +460 °C. Conversely, the temperature of Europa at the equator never exceeds ≈-140 °C, and the temperature at the poles never exceeds ≈-220 °C. The (physical layer) communications channel for each represents unique challenges, which are described. For example, RF opacity of the toxic Venus atmosphere is inversely proportional to wavelength ${(}mathit{lambda}{)}$ squared, imposing an upper limit to a viable lander-to-orbiter link frequency. Similarly, communicating from Europa's presumed deeply buried liquid ocean through a thick, briny (electrically conductive) ice layer renders a conventional RF link useless. Plus, Europa receives approximately 5.4 Sv of radiation per day, roughly 1,000 times the average annual dose experienced by humans on Earth (only a fraction of that comes from outer space). © 2000-2012 IEEE.
引用
收藏
页码:73 / 85
页数:13
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