403-2 SMAP L2/L3 Soil Moisture Product Validation Using in Situ Based Core Validation Sites.

See more from this Division: SSSA Division: Soil Physics and Hydrology
See more from this Session: Remote Sensing of Soil Water: Soil Moisture Active Passive and Beyond

Wednesday, November 18, 2015: 2:05 PM
Minneapolis Convention Center, L100 F

Andreas Colliander1, Thomas Jackson2, Narendra Das1, Seungbum Kim1, Rajat Bindlish3, Michael H. Cosh4, Todd G. Caldwell5, Aaron Berg6, Tracy Rowlandson6, Kelly Caylor7, Hala K AlJassar8, Ernesto Lopez-Baeza9, Jose Martinez Fernandez10, Ángel González-Zamora10, Heather McNairn11, Anna Pacheco11, Mahta Moghaddam12, Carsten Montzka13, Claudia Notarnicola14, Georg Niedrist15, Thierry Pellarin16, Jouni Pulliainen17, Kimmo Rautiainen17, Judith Ramos18, Mark S Seyfried19, Zhongbo Su20, Yijian Zeng21, Rogier van der Velde20, Marouane Temimi22, Marc Thibeault23, Mariette Vreugdenhil24, Wouter Dorigo24, Jeff Walker25, Xiaoling Wu25, Michael Spencer1, Peggy O'Neill26, Dara Entekhabi27, Simon H Yueh1 and Eni Njoku1, (1)Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA
(2)Hydrology and Remote Sensing Lab, USDA-ARS, Beltsville, MD
(3)USDA-ARS, Beltsville, MD
(4)10300 Baltimore Ave, USDA-ARS, Beltsville, MD
(5)University Station, Box X, University of Texas-Austin, Austin, TX
(6)Dept. of Geography, University of Guelph, Guelph, ON, Canada
(7)Department of Civil and Environmental Engineering, Princeton University, Princeton, NJ
(8)Physics Department, Kuwait University, Kuwait, Kuwait
(9)University of Valencia, Valencia, Spain
(10)Universidad de Salamanca, Villamayor, Spain
(11)Agriculture and Agri-Food Canada, Ottawa, ON, Canada
(12)Department of Electrical Engineering, University of Southern California, Los Angeles, CA
(13)Forschungszentrum Juelich, Juelich, Germany
(14)Institute for Applied Remote Sensing, EURAC, Bolzano, Italy
(15)Institute for Alpine Environment, EURAC, Bolzano, Italy
(16)University of Grenoble Alpes, Domaine universitaire, BP 53, Grenoble, France
(17)Finnish Meteorological Institute, Helsinki, Finland
(18)Department of Hydrology, Universidad Nacional Autónoma de México, Mexico City, Mexico
(19)Northwest Watershed Research Center, USDA-ARS, Boise, ID
(20)ITC Faculty, University of Twente, Enschede, Netherlands
(21)ITC Faculty, Univeristy of Twente, Enschede, Netherlands
(22)NOAA CREST, New York, NY
(23)Comisión Nacional de Actividades Espaciales, Buenos Aires, Argentina
(24)Vienna University of Technology, Vienna, Austria
(25)Monash University, Clayton, Australia
(26)NASA Goddard Space Flight Center, Greenbelt, MD
(27)Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA
Abstract:
NASA’s Soil Moisture Active Passive (SMAP) Mission was launched in January 2015. The objective of the mission is global mapping of soil moisture and landscape freeze/thaw state. SMAP utilizes L-band radar and radiometer instruments sharing a rotating 6-meter mesh reflector antenna. Merging of active and passive L-band observations enables an unprecedented combination of accuracy, resolution, global coverage and revisit-time for soil moisture and freeze/thaw retrievals. The primary validation reference of the data products will be ground-based measurements. Well characterized sites with calibrated in situ measurements will be used to determine the quality of the data products; these sites are designated as core validation sites. The mission success criteria will be evaluated with respect to these core site comparisons. Other remote sensing and model-based products will be used as additional resources to expand the spatial and temporal scope of the evaluation. In an effort to ensure the geographic distribution and diversity of conditions of the core validation sites, SMAP has partnered with investigators across the globe. Because different SMAP Level 2 soil moisture products have different spatial scales, the suitability of the various sites for validation of the different products must be done for each site while considering several factors. The main factors are gravimetric calibration of the sensors within a site and determination of a spatial scaling function of the sensor measurements up to the SMAP resolution scales. The mission has been able to utilize the core site measurements since the launch of the satellite because the infrastructure for data transmission and processing was established well before the launch. The validated soil moisture products will be released by May 2016. In this presentation we will show the performance of the beta version of the soil moisture products (released by November 2015) and discuss the status of the validation process.

See more from this Division: SSSA Division: Soil Physics and Hydrology
See more from this Session: Remote Sensing of Soil Water: Soil Moisture Active Passive and Beyond