Sentence examples for elevation difference between the from inspiring English sources

Exact(16)

Assuming the station site to have a rectangular shape with user specified length and width, the fixed cost for station facilities varies only with the construction type, i.e., at-grade, elevated, or underground, which depends on the elevation difference between the proposed station and the existing ground.

The height of simple waves means the elevation difference between the top of a crest and the bottom of a trough.

The elevation difference between the two paleoshorelines implies a decrease in ocean level of ~300 m, which could have taken place via evaporation/sublimation within several million years6.

In contrast, the shoreline accreted on nearby control beaches following a seasonal pattern common in southern California, reducing the elevation difference between the nourished and adjacent beaches.

In addition, the water flow rate due to the mean of the elevation difference between the bend of the dam and plant was used to design the HEPP.

The elevation difference between the landslide toe and top was only 60 m.

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Similar(44)

"When we looked at our original plans, the elevation difference between those plans and what was built was about three inches," he said.

Also, the simulated elevation differences between the ridges and sloughs are of the same order of those typically found in the field.

Elevation differences between the Waipaoa-1 (c.15 ka) terrace and the level of maximum channel incision (i.e. before aggradation since the turn of the 20th century) suggest about 50% of the topographic relief within headwater reaches of the Waipaoa catchment has been formed in postglacial times.

Figure 4 Elevation differences between the original DTM generated from the full-density data (D20) and the thinned DTMs (D8, D4, D2, D1) extracted from a 1-m grid along the central line of the study area.

(3) Elevation differences between the hanging wall and the footwall on the basin margin determine potential energy differences between the proximal provenance and the sink, which directly affect denudation rates, hydrodynamic conditions, sediment supply rates, and even clastic properties (Song et al. 2013).

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