Sentence examples for drainage lengths from inspiring English sources

Google Earth images (2.5 m spatial resolution) were used to extract catchment characteristics such as area, drainage lengths, number of houses in the catchment and the impervious surface area.

Stream length (Lu) is a significant hydrological parameter of the any river basin as it divulges surface runoff characteristics of comparatively smaller drainage lengths and characteristics of larger gradients area and finer textures.

After a certain number of years, it decreases mainly due to the increase in the characteristic drainage length and decrease in the effective consolidation time.

It is found that thaw consolidation is controlled by several factors, including load, the effective consolidation time as well as the characteristic drainage length.

Based on field data and spatial analysis, the geomorphic design criteria of mean drainage length and mean drainage density were calculated as 124 m (408 ft) and 4.7 km−1 (61.7 ft/ac), respectively.

Immediately postoperatively in the intensive care unit (ICU), cardiac filling pressures (central venous and left atrial pressure), coagulation profile, cardiac rhythm, chest tube drainage, length of stay in the ICU, and use of atrial pacing were reviewed.

No significant differences were found between the two groups with regard to mean operative time, intraoperative blood loss, amount of closed suction drainage, length of hospital stay, and readmission rate.

This measure is an essential input for computing various other morphometric parameters such as mean stream length, drainage density, length of overland flow, etc. Estimation of total stream length for the watersheds of the study area shows that among the watersheds of the study area the total stream length varies from 28.08 km (in Valaiyur watershed) to 412.53 km (Koneri watershed).

Defined as the Natural Agricultural Suitability Analysis, the foundation of this study is a hierarchical geospatial analysis that integrates six key natural factors: slope, soil texture, soil depth, non-catastrophic overbank flooding potential, drainage flow length, and drainage proximity and flow potential.

To quantitatively measure landscape features we used several classical geomorphic indices (spacing ratio, hypsometric curves and integral, stream frequency drainage, stream length-gradient).

Compared with two nearby basins that record precessional (21-kyr) and long-eccentricity (400-kyr) forcing within sedimentary and geomorphic archives, the recorded cyclicity scales with the square of the drainage basin length.