Status of Aquarius and Salinity Continuity

Aquarius is an L-band radar/radiometer instrument combination that has been designed to measure ocean salinity. It was launched on 10 June 2011 as part of the Aquarius/SAC-D observatory. The observatory is a partnership between the United States National Aeronautics and Space Agency (NASA), which provided Aquarius, and the Argentinian space agency, Comisión Nacional de Actividades Espaciales (CONAE), which provided the spacecraft bus, Satelite de Aplicaciones Cientificas (SAC-D). The observatory was lost four years later on 7 June 2015 when a failure in the power distribution network resulted in the loss of control of the spacecraft. The Aquarius Mission formally ended on 31 December 2017. The last major milestone was the release of the final version of the salinity retrieval (Version 5). Version 5 meets the mission requirements for accuracy, and reflects the continuing progress and understanding developed by the science team over the lifetime of the mission. Further progress is possible, and several issues remained unresolved at the end of the mission that are relevant to future salinity retrievals. The understanding developed with Aquarius is being transferred to radiometer observations over the ocean from NASA’s Soil Moisture Active Passive (SMAP) satellite, and salinity from SMAP with accuracy approaching that of Aquarius are already being produced.

[1]  Simon Yueh,et al.  Estimates of Faraday rotation with passive microwave polarimetry for microwave remote sensing of Earth surfaces , 2000, IEEE Trans. Geosci. Remote. Sens..

[2]  R. Lang,et al.  Accurate measurements of the dielectric constant of seawater at L band , 2016 .

[3]  David M. Le Vine,et al.  Aquarius and Remote Sensing of Sea Surface Salinity from Space , 2010, Proceedings of the IEEE.

[4]  Thomas Meissner,et al.  The complex dielectric constant of pure and sea water from microwave satellite observations , 2004, IEEE Transactions on Geoscience and Remote Sensing.

[5]  D. M. Le Vine Aquarius: The Instrument and Initial Results , 2012 .

[6]  David M. Le Vine,et al.  Aquarius L-band Radiometers Calibration Using Cold Sky Observations , 2015, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.

[7]  David M. Le Vine,et al.  The Salinity Retrieval Algorithms for the NASA Aquarius Version 5 and SMAP Version 3 Releases , 2018, Remote. Sens..

[8]  Tong Lee,et al.  Satellite and In Situ Salinity: Understanding Near-Surface Stratification and Subfootprint Variability , 2016 .

[9]  Remy Baraille,et al.  The HYCOM (HYbrid Coordinate Ocean Model) data assimilative system , 2007 .

[10]  Thomas Meissner,et al.  The Emissivity of the Ocean Surface Between 6 and 90 GHz Over a Large Range of Wind Speeds and Earth Incidence Angles , 2012, IEEE Transactions on Geoscience and Remote Sensing.

[11]  Sidharth Misra,et al.  L-Band RFI as Experienced During Airborne Campaigns in Preparation for SMOS , 2010, IEEE Transactions on Geoscience and Remote Sensing.

[12]  Thomas Meissner,et al.  Sensitivity of Ocean Surface Salinity Measurements From Spaceborne L-Band Radiometers to Ancillary Sea Surface Temperature , 2016, IEEE Transactions on Geoscience and Remote Sensing.

[13]  Thomas Meissner,et al.  The emission and scattering of L‐band microwave radiation from rough ocean surfaces and wind speed measurements from the Aquarius sensor , 2014 .

[14]  S. Riser,et al.  The Argo Program : observing the global ocean with profiling floats , 2009 .

[15]  Emmanuel P. Dinnat,et al.  Aquarius whole range calibration: Celestial Sky, ocean, and land targets , 2014, 2014 13th Specialist Meeting on Microwave Radiometry and Remote Sensing of the Environment (MicroRad).

[16]  Hao Liu,et al.  Prelminary design of water cycle observation mission (WCOM) , 2016, 2016 IEEE International Geoscience and Remote Sensing Symposium (IGARSS).

[17]  David M. Le Vine,et al.  A Theoretical Algorithm for the Retrieval of Sea Surface Salinity from Smap Observations , 2019, IGARSS 2019 - 2019 IEEE International Geoscience and Remote Sensing Symposium.

[18]  David M. Le Vine,et al.  Impact of Sun Glint on Salinity Remote Sensing: An Example With the Aquarius Radiometer , 2008, IEEE Transactions on Geoscience and Remote Sensing.

[19]  D. L. Le Vine ESTAR experience with RFI at L-band and implications for future passive microwave remote sensing from space , 2002, IEEE International Geoscience and Remote Sensing Symposium.

[20]  Liang Hong,et al.  Aquarius L-Band Microwave Radiometer: 3 Years of Radiometric Performance and Systematic Effects , 2015, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.

[21]  Simon Yueh,et al.  Error sources and feasibility for microwave remote sensing of ocean surface salinity , 2001, IEEE Trans. Geosci. Remote. Sens..

[22]  Philip W. Rosenkranz,et al.  Atmospheric 60-GHz oxygen spectrum : new laboratory measurements and line parameters , 1992 .

[23]  David M. Le Vine,et al.  The dielectric constant model function and implications for remote sensing of salinity , 2017, 2017 IEEE International Geoscience and Remote Sensing Symposium (IGARSS).

[24]  David M. Le Vine,et al.  Status of Aquarius/SAC-D and Aquarius Salinity Retrievals , 2015, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.

[25]  David M. Le Vine,et al.  The effect of the ionosphere on remote sensing of sea surface salinity from space: absorption and emission at L band , 2002, IEEE Trans. Geosci. Remote. Sens..

[26]  Alan Tanner,et al.  Ultra Stable Microwave Radiometers for Future Sea Surface Salinity Missions , 2002 .

[27]  David M. Le Vine,et al.  Aquarius Third Stokes Parameter Measurements: Initial Results , 2012, IEEE Geoscience and Remote Sensing Letters.

[28]  Simon Yueh,et al.  High-stability L-band radiometer measurements of saltwater , 2004, IEEE Transactions on Geoscience and Remote Sensing.

[29]  J. Boutin,et al.  Comparison of SMOS and Aquarius Sea Surface Salinity and analysis of possible causes for the differences , 2014, 2014 XXXIth URSI General Assembly and Scientific Symposium (URSI GASS).

[30]  David M. Le Vine,et al.  Aquarius Final Release Product and Full Range Calibration of L-Band Radiometers , 2018, IGARSS 2018 - 2018 IEEE International Geoscience and Remote Sensing Symposium.

[31]  David M. Le Vine,et al.  Aquarius: An Instrument to Monitor Sea Surface Salinity From Space , 2007, IEEE Transactions on Geoscience and Remote Sensing.

[32]  Tong Lee Consistency of Aquarius sea surface salinity with Argo products on various spatial and temporal scales , 2016 .

[33]  Hao Liu,et al.  The water cycle observation mission (WCOM): Overview , 2016, 2016 IEEE International Geoscience and Remote Sensing Symposium (IGARSS).

[34]  Hao Liu,et al.  Data pre-processing of MICAP (microwave imager combined active and passive) scatterometer , 2016, 2016 IEEE International Geoscience and Remote Sensing Symposium (IGARSS).

[36]  Simon Yueh,et al.  The Aquarius Ocean Salinity Mission High Stability L-band Radiometer , 2006, 2006 IEEE International Symposium on Geoscience and Remote Sensing.

[37]  C. Swift,et al.  An improved model for the dielectric constant of sea water at microwave frequencies , 1977, IEEE Journal of Oceanic Engineering.

[38]  Emmanuel P. Dinnat,et al.  L-Band Model Function of the Dielectric Constant of Seawater , 2017, IEEE Transactions on Geoscience and Remote Sensing.