Publications
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Estimating stem water content with L-band tomographic radar
The study provides preliminary evidence that estimating forest VWC is feasible using tomographic L-band radar platforms. These findings suggest that future spaceborne missions may require vertical separation of canopy and ground backscatter (through tomography or interferometry) and subdaily revisit times to effectively capture diurnal water dynamics in forests.
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The Maximum Heat Ratio method
The MHR method provides a more versatile tool for researchers studying forest hydrology. It is ideal for: Fast-growing species that move water rapidly. High-latitude or high-altitude forests where freeze-thaw cycles frequently disrupt standard sensor readings. Low-power, remote monitoring, as the algorithm is easy to implement in standard data loggers without significantly increasing energy. consumption. In short, this method provides a "best of both worlds" solution for measuring tree water use across a much wider range of environmental conditions and species.
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How drought affects tree transpiration
In this study we highlight that drought response in boreal forests is not a "one-size-fits-all" phenomenon. Instead, it is driven by a complex, codependent interaction between biological traits (species and size) and the physical environment (topography). These insights are critical for predicting how northern forests will respond to the increasing frequency of extreme climate events.
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Effects of irrigation on oil palm transpiration
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Errors in heater power adjustment in heat dissipation sensors
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Can irrigation increase productivity in palm oil?
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Can irrigation mitigate drought in palm oil plantations?
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Is there an ideal method to partition ET?
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Predict winter-time sap flow with stem temperature
In this study we aimed to identify "critical wood temperatures" at which the most sap flow occurs, as this process is vital for both embolism repair and syrup production. We speculate that sap flow is strongly influenced by liquid-to-solid and solid-to-liquid phase changes. Freezing exotherms and thawing endotherms—where volume changes but temperature remains constant—likely explain why flow was highest when temperatures were not changing.
Working on or submitted
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Radar & tree water content
Monteith, et al estimate tree water content using exclusively radar attenuation and backscatter
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Sap flow and cloud cover
Talvinen et al, assess the role between tree transpiration, and cloud formation
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Tree water content from thermal properties
Gutierrez Lopez, et al, study how to estimate tree water content from thermal properties and water dielectric
Technical reports
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The heat dissipation method for sap flow measurements
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Construction of heat dissipation probes to estimate sap flow
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Manual for the construction and operation of a vacuum cryogenic distilation apparatus
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Changing address in SDI12 sensors using Campbell Scientific loggers
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