Beyond triple collocation: Applications to soil moisture monitoring

Triple collocation (TC) is routinely used to resolve approximated linear relationships between different measurements (or representations) of a geophysical variable that are subject to errors. It has been utilized in the context of calibration, validation, bias correction, and error characterization...

Full description

Saved in:
Bibliographic Details
Published in:Journal of geophysical research. Atmospheres Vol. 119; no. 11; pp. 6419 - 6439
Main Authors: Su, Chun-Hsu, Ryu, Dongryeol, Crow, Wade T, Western, Andrew W
Format: Journal Article
Language:English
Published: Washington Blackwell Publishing Ltd 16-06-2014
Subjects:
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Triple collocation (TC) is routinely used to resolve approximated linear relationships between different measurements (or representations) of a geophysical variable that are subject to errors. It has been utilized in the context of calibration, validation, bias correction, and error characterization to allow comparisons of diverse data records from various direct and indirect measurement techniques including in situ remote sensing and model-based approaches. However, successful applications of TC require sufficiently large numbers of coincident data points from three independent time series and, within the analysis period, homogeneity of their linear relationships and error structures. These conditions are difficult to realize in practice due to infrequent spatiotemporal sampling of satellite and ground-based sensors. TC can, however, be generalized within the framework of instrumental variable (IV) regression theory to address some of the conceptual constraints of TC. We review the theoretics of IV and consider one possible strategy to circumvent the three-data constraint by use of lagged variables (LV) as instruments. This particular implementation of IV is suitable for circumstances where multiple data records are limited and the geophysical variable of interest is sampled at time intervals shorter than its temporal correlation length. As a demonstration of utility, the LV method is applied to microwave satellite soil moisture data sets to recover their errors over Australia and to estimate temporal properties of their relationships with in situ and model data. These results are compared against standard two-data linear estimators and the TC estimator as benchmark.
Bibliography:http://handle.nal.usda.gov/10113/60043
http://dx.doi.org/10.1002/2013JD021043
ArticleID:JGRD51428
istex:A563230CBAF98C3784B4A393DCFD4A9EBCF03E90
Australian Research Council - No. LP110200520
ark:/67375/WNG-0TPPRZX9-8
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:2169-897X
2169-8996
DOI:10.1002/2013JD021043