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Aerial photography can be conducted at an altitude designed to produce maps that show drainage configuration, roads, buildings, lakes, streams, timber, power lines, railroads, and fences or other features that may be missed by a ground survey.
All peer-reviewed models lack the ability to simultaneously perform both of the following functions: (1) model an internal water storage (IWS) zone drainage configuration and (2) account for soil water content using the soil water characteristic curve.
Previous field studies have shown that the hydrologic performance of bioretention cells varies greatly because of factors such as underlying soil type, physiographic region, drainage configuration, surface storage volume, drainage area to bioretention surface area ratio, and media depth.
The depth and lateral extent of incision was partly conditioned by underlying geology (rock type and tectonic structure), climatic conditions and changes in water and sediment discharge coupled to ice sheet dynamics and the drainage configuration of major rivers in Northwest Europe.
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Each field site had two sets of bioretention cells with varying media depths, media types, drainage configurations, underlying soil types, and surface storage volumes.
Bioretention areas with varied media depths, in situ soil types, drainage configurations, and surface infiltration capabilities have previously been monitored, modelled, and calibrated using the continuous simulation model, DRAINMOD.
To map the large-scale modern and palaeo-drainage configuration of the region, we analysed the geomorphology using remotely sensed optical imagery and a Synthetic Aperture Radar (SAR -derived digital elevation model (DEM) focuSAR -derivedticular on the Ghaggar–Hakra palaeochannel.
Thirty-metre DEMs are smoother and less detailed, but the AW3D shows the closest fit to the real drainage network configuration.
To investigate the relationship between drainage angle configuration with untreated intraocular pressure (IOP) and optic disc cupping in subjects with chronic angle-closure glaucoma (CACG).
When these rules are applied at small scales, the resulting landscape has large-scale properties which are apparent in its morphological attributes, e.g., drainage network configuration, and in its functional attributes, e.g., sediment dynamics.
However, the amount of information that proglacial hydrographs contain about drainage system configurations depends critically on the degree to which the drainage systems modify recharge hydrographs.
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