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https://hdl.handle.net/2440/90466
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Type: | Journal article |
Title: | The soil moisture active passive experiments (SMAPEx): toward soil moisture retrieval from the SMAP mission |
Author: | Panciera, R. Walker, J. Jackson, T. Gray, D. Tanase, M. Ryu, D. Monerris, A. Yardley, H. Rudiger, C. Wu, X. Gao, Y. Hacker, J. |
Citation: | IEEE Transactions on Geoscience and Remote Sensing, 2014; 52(1):490-507 |
Publisher: | Institute of Electrical and Electronics Engineers |
Issue Date: | 2014 |
ISSN: | 0196-2892 1558-0644 |
Statement of Responsibility: | Rocco Panciera, Jeffrey P. Walker, Thomas J. Jackson, Douglas A. Gray, Mihai A. Tanase, Dongryeol Ryu, Alessandra Monerris, Heath Yardley, Christoph Rüdiger, Xiaoling Wu, Ying Gao, and Jörg M. Hacker |
Abstract: | NASA’s Soil Moisture Active Passive (SMAP) mission will carry the first combined spaceborne L-band radiometer and Synthetic Aperture Radar (SAR) system with the objective of mapping near-surface soil moisture and freeze/thaw state globally every 2–3 days. SMAP will provide three soil moisture products: i) high-resolution from radar (∼3 km), ii) low-resolution from radiometer (∼36 km), and iii) intermediate-resolution from the fusion of radar and radiometer (∼9 km). The Soil Moisture Active Passive Experiments (SMAPEx) are a series of three airborne field experiments designed to provide prototype SMAP data for the development and validation of soil moisture retrieval algo- rithms applicable to the SMAP mission. This paper describes the SMAPEx sampling strategy and presents an overview of the data collected during the three experiments: SMAPEx-1 (July 5–10, 2010), SMAPEx-2 (December 4–8, 2010) and SMAPEx-3 (September 5–23, 2011). The SMAPEx experiments were con- ducted in a semi-arid agricultural and grazing area located in southeastern Australia, timed so as to acquire data over a seasonal cycle at various stages of the crop growth. Airborne L-band brightness temperature (∼1 km) and radar backscatter (∼10 m) observations were collected over an area the size of a single SMAP footprint (38 km×36 km at 35◦latitude) with a 2–3 days revisit time, providing SMAP-like data for testing of radiometer-only, radar-only and combined radiometer-radar soil moisture retrieval and downscaling algorithms. Airborne observations were sup- ported by continuous monitoring of near-surface (0–5 cm) soil moisture along with intensive ground monitoring of soil moisture, soil temperature, vegetation biomass and structure, and surface roughness. |
Rights: | © 2013 IEEE. Personal use is permitted, but republication/redistribution requires IEEE permission. |
DOI: | 10.1109/TGRS.2013.2241774 |
Grant ID: | http://purl.org/au-research/grants/arc/DP0984586 |
Published version: | http://dx.doi.org/10.1109/tgrs.2013.2241774 |
Appears in Collections: | Aurora harvest 2 Electrical and Electronic Engineering publications |
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