Auroral emissions on the Mars nightside were initially observed as individual events of MUV emission by the SPICAM spectrometer on board Mars Express in 2005. These observations have shown the auroral ultraviolet emissions are highly correlated with crustal magnetic fields structures. MAVEN's Imaging Ultraviolet Spectrograph (IUVS) has measured hundreds of individual discrete MUV electron auroral events since 2014 and showed that they can also occur globally, in regions of weak or absent crustal fields. Another type of event is the ‘’diffuse’’ aurora which occurs following Solar Energetic Particle (SEP) events and covers a large fraction of the planet. It is caused by the interaction of very energetic electrons and protons with the atmosphere. Since April 2021, the EMUS EUV/FUV spectrograph on board the Emirates Mars Mission (EMM) has shown that the FUV electron auroral emission is not necessarily "discrete" but is observed in a variety of morphologies. Crustal field aurora and enigmatic "sinuous" aurora have well-defined edges, while most emission away from strong crustal fields is fainter and "patchy". Finally, on the dayside, enhancements of Lyman-a have also been observed, resulting from the interaction of solar wind protons with the hydrogen corona surrounding the planet. We will show that visible counterparts to the UV emissions would probably be detectable and visible to future Mars astronauts. This seminar will also describe the current state of Mars aurora modelling and future investigations.