P033-0007
Emirates Mars Mission 2020: Emirates Mars Ultraviolet Spectrometer (EMUS) Overview

Thursday, 10 December 2020
Poster
Fatma Hussain Lootah1, Hessa Rashid Almatroushi2, Ahmed Alshehhi2, Suhail AlMheiri3, Greg Holsclaw4, Justin Deigan4, Michael Chaffin4, Heather Reed5, Robert J Lillis6, Kush Tyagi5, Matthew O. Fillingim7, Scott England8 and the EMUS team, (1)Mohammed Bin Rashid Space Centre (MBRSC), Dubai, United Arab Emirates, (2)Mohammed Bin Rashid Space Center, Al Khawaneej, United Arab Emirates, (3)Mohammed Bin Rashid Space Centre, Dubai, United Arab Emirates, (4)Laboratory for Atmospheric and Space Physics, Boulder, CO, United States, (5)Laboratory for Atmospheric and Space Physics, Boulder, United States, (6)Space Sciences Laboratory, University of California Berkeley, Berkeley, CA, United States, (7)University of California, Berkeley, CA, United States, (8)Virginia Polytechnic Institute and State University, Aerospace and Ocean Engineering, Virginia, VA, United States
Abstract:
The Emirates Mars Ultraviolet Spectrometer (EMUS) instrument is one of three science instruments on board the “Hope Probe” of the Emirates Mars Mission (EMM). EMM is a United Arab Emirates’ (UAE) mission to Mars, launching in the summer of 2020 and arriving in February 2021, to explore the global dynamics of the Martian atmosphere, sampling in time both diurnally and seasonally. The EMUS instrument is a far-ultraviolet imaging spectrograph that measures emissions in the spectral range 100-170 nm, with selectable spectral resolution (1.3 nm, 1.8 nm), and a photon-counting and -locating detector (provided by the Space Sciences Laboratory at the University of California, Berkeley). Using a combination of its one-dimensional imaging and spacecraft motion, it will build up two-dimensional far-ultraviolet images of the Martian disk and near-space environment at several important wavelengths: the Lyman beta atomic hydrogen emission (102.6 nm), the Lyman alpha atomic hydrogen emission (121.6 nm), two atomic oxygen emissions (130.4 nm and 135.6 nm), and the carbon monoxide fourth positive group band emission (140-170 nm). Radiances at these wavelengths will be used to derive the column abundance of atomic oxygen and carbon monoxide in the Martian thermosphere, and the density of atomic oxygen and atomic hydrogen in the Martian exosphere both with spatial and sub-seasonal variability. The EMUS spatial resolution of less than 300 km on the disk is sufficient to characterize spatial variability in the Martian thermosphere (100-200 km altitude) and exosphere (>200 km altitude). The instrument is jointly developed by the Mohammed Bin Rashid Space Centre (MBRSC) in Dubai, UAE and the Laboratory for Atmospheric and Space Physics (LASP) at the University of Colorado Boulder. In this presentation the status and performance of the EMUS instrument post-launch will also be discussed.