Assessment of Boreal/Arctic Biogeochemistry using Radar Derived Freeze/Thaw-State and an Ecosystem Process Model
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Engineering topics
Publications and source records attributed to Zimmermann, R..
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We hypothesize that the strong sensitivity of radar backscatter to surface dielectric properties, and hence to the phase (solid or liquid) of any water near the surface, should make space-borne radar observations a powerful tool for large-scale spatial monitoring of the freeze/thaw state of the land surface, and thus ecosystem growing season length.
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This paper reports on the first all solid-state two-diode subharmonically pumped (SHP) mixer operating at 640 GHz.
The focus of this effort is the assessment of spaceborne scatteromter observations for monitoring landscape freeze/thaw transitions in the boreal forest thereby providing a means for estimating growing season duration.
Design and implementation of a system for the automated and continous in situ monitoring of the dielectric constant of woody vegetation tissue is presented.
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Vegetation maps of inaccessible areas in the tropics tend to divide vegetation into broad types.
Two major forest types in the upper Amazonian headwater region are floodplain and upland (terra firme) forests.
Five semi-deciduous broadleaf forest types growing over tropical karst in Belize, Central America, were monitored for three years to study diurnal and seasonal changes of transpiration and micro-meteorologic conditions.
Tree canopy microclimate, xylem water flux and xylem dielectric constant have been monitored in situ since June 1993 in two adjacent natural forest stands in central Alaska. The deciduous stand represents a mature balsam poplar site on the Tanana River floodplain, while the coniferous stand consists of mature white spruce with some black spruce mixed in. During solstice in June and later in summer, diurnal changes of xylem water potential were measured to investigate the occurrence and magnitude of tree transpiration and dielectric constant changes in stems.
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