F17: Remote Sensing of Land and Sea at L band (1)

Friday, August 22  13:40-15:40,  Room #4

Session Chairs: Y. Kerr, Mahta Moghaddam

L-band is important for remote sensing of soil moisture and ocean salinity, two variables important for understanding the global water cycle and ocean dynamics. There are soon to be three satellite missions with L-band sensors devoted to measuring these variables: The ESA Soil Moisture and Ocean Salinity (SMOS) mission and the NASA Aquarius/SAC-D mission, which are already in orbit and NASA’s Soil Moisture Active Passive (SMAP) mission scheduled for launch in the Fall of 2014. The latter two missions employ both passive (radiometer) and active (radar) sensors at L-band. This session will focus on results and status of these three missions but will also entertain new applications (e.g. application to the cryosphere such as L-band monitoring of sea ice) and active/passive synergy at L-band. Suggested topics are: 1) Results from Aquarius: Sea Surface Salinity; Soil Moisture, Remote Sensing Algorithm. 2) Results from SMOS: Ocean Salinity; Soil Moisture, Remote Sensing Algorithm. 3) Status of SMAP: Instrument Algorithm and plans, Active/Passive Synergy: Disaggregation using radar, Enhanced products. 4) New Applications: Sea Ice extent; Sea Ice Thickness, Drought indices, Root zone soil moisture.

13:40  F17.1   SMOS RESULTS AFTER 4 YEARS IN SPACE

Y. Kerr1, P. Richaume1, A. Mialon1, A. Albitar1, F. Cabot1, J. -P. Wigneron2, P. Ferrazzoli3, T. Pellarin4, A. Mahmoodi5, J. Grant6, S. Delwart7

1CESBIO, Toulouse, France
2INRA EPHYSE, Bordeaux, France
3Tor Vergata University, Rome, Italy
4LTHE, Genoble, France
5Arrays Systems, Toronto, Canada
6Lund University, Lund, Sweden
7ESA ESRIN, Rome, Italy


14:00  F17.2   SMOS OCEAN SALINITY: RECENT IMPROVEMENTS AND APPLICATIONS

X. Yin1,2, J. Boutin1, J. Font3, N. Reul4, P. Spurgeon2, J. -L. Vergely5, N. Martin2

1LOCEAN, Paris, France
2ARGANS, Plymouth, UK
3ICM-CSIC, Barcelona, Spain
4IFREMER, La Seyne-sur-Mer, France
5ACRI-ST, Sophia Antipolis, France


14:20  F17.3   AQUARIUS OVERVIEW AND UPDATE

D. M. Le Vine1, G. S. E. Lagerloef2, P. de Matthaeis1, E. P. Dinnat1, S. Abraham1

1Code 615, Goddard Space Flight Center, MD, United States
2Earth and Space Research, WA, United States


14:40  F17.4   AQUARIUS’ COMBINED ACTIVE PASSIVE ALGORITHM FOR OCEAN SURFACE SALINITY AND WIND RETRIEVAL

W. Tang, S. Yueh, A. Fore, A. Hayashi

Jet Propulsion Laboratory, Pasadena, CA, United States


15:00  F17.5   COMPARISON OF SMOS AND AQUARIUS SEA SURFACE SALINITY AND ANALYSIS OF POSSIBLE CAUSES FOR THE DIFFERENCES

E. P. Dinnat1, J. Boutin2, X. Yin2, D. M. Le Vine3, P. Waldteufel4, J. -L. Vergely5

1Cryospheric Sciences Laboratory, NASA-GSFC and Chapman University, Greenbelt, MD, United States
2Laboratoire d’Océanographie et du Climat: Expérimentations et Approches Numériques, CNRS/IRD/UPMC/MN, Paris, France
3Cryospheric Sciences Laboratory, NASA-GSFC, Greenbelt, MD, United States
4Laboratoire Atmosphères, Milieux, Observations Spatiales, CNRS/UVSQ/UPMC, Paris, France
5ACRI-ST, Sophia Antipolis, France


15:20  F17.6   A POTENTIAL SOIL MOISTURE PRODUCT FROM THE HY-2 SCANNING MICROWAVE RADIOMETER

T. Zhao1, J. Shi1, M. Lin2

1Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing, China
2National Satellite Ocean Application Service, State Oceanic Administration of China, Beijing, China