- Title
- Spatio-temporal distribution of near-surface and root zone soil moisture at the catchment scale
- Creator
- Martinez, C.; Hancock, G. R.; Kalma, J. D.; Wells, T.
- Relation
- Hydrological Processes Vol. 22, Issue 4, p. 2699-2714
- Publisher Link
- http://dx.doi.org/10.1002/hyp.6869
- Publisher
- John Wiley and Sons
- Resource Type
- journal article
- Date
- 2008
- Description
- Soil moisture is highly variable both spatially and temporally. It is widely recognized that improving the knowledge and understanding of soil moisture and the processes underpinning its spatial and temporal distribution is critical. This paper addresses the relationship between near-surface and root zone soil moisture, the way in which they vary spatially and temporally, and the effect of sampling design for determining catchment scale soil moisture dynamics. In this study, catchment scale nearsurface (0–50 mm) and root zone (0–300 mm) soil moisture were monitored over a four-week period. Measurements of near-surface soil moisture were recorded at various resolutions, and near-surface and root zone soil moisture data were also monitored continuously within a network of recording sensors. Catchment average near-surface soil moisture derived from detailed spatial measurements and continuous observations at fixed points were found to be significantly correlated (r² = 0.96; P = 0.0063; n = 4). Root zone soil moisture was also found to be highly correlated with catchment average near-surface, continuously monitored (r² = 0.81; P < 0.0001; n = 26) and with detailed spatial measurements of near-surface soil moisture (r² = 0.84). The weaker relationship observed between near-surface and root zone soil moisture is considered to be caused by the different responses to rainfall and the different factors controlling soil moisture for the soil depths of 0–50 mm and 0–300 mm. Aspect is considered to be the main factor influencing the spatial and temporal distribution of near-surface soil moisture, while topography and soil type are considered important for root zone soil moisture. The ability of a limited number of monitoring stations to provide accurate estimates of catchment scale average soil moisture for both near-surface and root zone is thus demonstrated, as opposed to high resolution spatial measurements. Similarly, the use of near-surface soil moisture measurements to obtain a reliable estimate of deeper soil moisture levels at the small catchment scale was demonstrated.
- Subject
- soil moisture; near-surface; root zone; catchment scale; NAFE’05; SASMAS
- Identifier
- http://hdl.handle.net/1959.13/43131
- Identifier
- uon:5258
- Identifier
- ISSN:0885-6087
- Language
- eng
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