The SHAllow RADar (SHARAD) Onboard the NASA MRO Mission

This paper describes the mission concepts, design, and achievements of the Italian Space Agency (ASI)-provided Mars SHAllow RADar (SHARAD) sounder high-frequency (HF) sounding radar, used onboard the National Aeronautics and Space Administration (NASA) Mars Reconnaissance Orbiter (MRO) Spacecraft. Its goals are the detection of liquid or solid water below the surface, and the mapping of subsurface geologic structures. Following a brief overview of the MRO mission and of its main science objectives, the paper introduces the basic principles of operation of the radar sounder, and addresses the major design issues faced by such a system. The greatest challenges faced in the design are the control of the interference from off-nadir echoes and the need for a high signal fidelity over a very large fractional bandwidth. The core of the paper is devoted to describing how the above problems have been tackled in the design of the SHARAD instrument, and the main characteristics of its architecture. The two key features of the instrument system design are 1) generation of the transmitted signal directly at the transmitted frequency; and 2) sampling performed directly at the radio frequency (by means of a subsampling technique). The careful design of these features, intended to keep the analog signal path very simple, minimizes distortions and stability problems. An overview of the calibration approach of both the system impulse response and the antenna gain at nadir versus solar array position, an assessment of the in-flight performance of the instrument, and a short summary of the achieved science results are also provided.

[1]  Roberto Orosei,et al.  Shallow radar (SHARAD) sounding observations of the Medusae Fossae Formation, Mars , 2009 .

[2]  R. Keith Raney,et al.  Pathfinder Advanced Radar Ice Sounder: PARIS , 2008, IGARSS 2008 - 2008 IEEE International Geoscience and Remote Sensing Symposium.

[3]  Ali Safaeinili,et al.  Radar Sounding Evidence for Buried Glaciers in the Southern Mid-Latitudes of Mars , 2008, Science.

[4]  J. Webster,et al.  Wiley Encyclopedia of Electrical and Electronics Engineering , 2010 .

[5]  R. Phillips,et al.  SHARAD sounding radar on the Mars Reconnaissance Orbiter , 2007 .

[6]  R. Phillips,et al.  SHARAD: The MRO 2005 shallow radar , 2004 .

[7]  Roberto Orosei,et al.  SHARAD radar sounding of the Vastitas Borealis Formation in Amazonis Planitia , 2008 .

[8]  Bruce A. Campbell,et al.  Subsurface structure of Planum Boreum from Mars Reconnaissance Orbiter Shallow Radar soundings , 2009 .

[9]  Charles V. Jakowatz,et al.  Phase gradient autofocus-a robust tool for high resolution SAR phase correction , 1994 .

[10]  Diego Calabrese,et al.  SHARAD design and operation , 2007, 2007 IEEE International Geoscience and Remote Sensing Symposium.

[11]  Paolo Noschese,et al.  Calibration of the SHARAD Instrument , 2007, 2007 IEEE International Geoscience and Remote Sensing Symposium.

[12]  L. Wood,et al.  From the Authors , 2003, European Respiratory Journal.

[13]  R. Phillips,et al.  Stratigraphy of Promethei Lingula, south polar layered deposits, Mars, in radar and imaging data sets , 2009 .

[14]  John C. Curlander,et al.  Synthetic Aperture Radar: Systems and Signal Processing , 1991 .

[15]  R. Jordan,et al.  The Apollo lunar sounder radar system , 1974 .

[16]  Chris H. Okubo,et al.  Dielectric properties of lava flows west of Ascraeus Mons, Mars , 2009 .

[17]  Alessandro Frigeri,et al.  Radar evidence for ice in lobate debris aprons in the mid‐northern latitudes of Mars , 2009 .

[18]  Giovanni Picardi,et al.  Performance results of the SHARAD instrument , 2007, 2007 IEEE International Geoscience and Remote Sensing Symposium.

[19]  Wlodek Kofman,et al.  North polar deposits of Mars: Extreme purity of the water ice , 2009 .

[20]  P. P. del Marmo,et al.  Accumulation and Erosion of Mars' South Polar Layered Deposits , 2007, Science.

[21]  E. Flamini,et al.  Calibration report of the SHARAD instrument , 2007, 2007 4th International Workshop on, Advanced Ground Penetrating Radar.

[22]  Roberto Orosei,et al.  Mars North Polar Deposits: Stratigraphy, Age, and Geodynamical Response , 2008, Science.