
Validating the BERMS in situ Soil Water Content Data Record with a Large Scale Temporary Network
Author(s) -
Cosh Michael H.,
Jackson Thomas J.,
Smith Craig,
Toth Brenda,
Berg Aaron A.
Publication year - 2013
Publication title -
vadose zone journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.036
H-Index - 81
ISSN - 1539-1663
DOI - 10.2136/vzj2012.0151
Subject(s) - berm , environmental science , water content , soil water , hydrology (agriculture) , quadrat , remote sensing , soil science , geography , engineering , geology , geotechnical engineering , archaeology , oceanography , transect
Calibration and validation of soil moisture satellite products requires data records of large spatial and temporal extent and for diverse land cover types. Obtaining these data, especially for forests, can be challenging. These challenges can include the remoteness of the locations and expense of equipment. The Boreal Ecosystem Research and Monitoring Sites (BERMS) network in Saskatchewan, Canada, is a long‐term ecosystem network which includes five soil water content profile stations. These stations provide a critical but incomplete view of the soil water content patterns across a study domain of 10,000 square km; however, the representativeness of these observations for this purpose has not yet been evaluated. In coordination with the Canadian Experiment‐Soil Moisture 2010 (CANEX‐SM10), a temporary network of surface soil water content sensors was installed during the summer of 2010 to enhance the data resources of the BERMS network. This short term data record was then used as a basis for up‐scaling and validating the BERMS network. This large domain is approximately 1200 square km and provides a higher confidence because of the increased number of sampling sites. Using temporal stability analysis, this network verified that the BERMS network could be scaled to a satellite scale footprint with a root mean square error (RMSE) of 0.025 m 3 m −3 , and applied to the entire period of record.