The ocean current system, flowing northward with a coast on its left side, indicates its presence by sloping density surfaces upwards towards the coast in both the Atlantic and Caribbean regions.
Using satellite imagery and relevant field data, eight thematic layers (rainfall, land slope, drainage density, soil, lineament density, geology, proximity to surface water bodies and elevation) of the factors having significant influence on groundwater occurrence were prepared.
This work is based on the integration of multi-criteria data including slope, drainage density, type of soil, Isohyet, population density, land use and sewer system density within ArcGIS interface.
The origin, movement and existence of groundwater depends on several factors such as slope, drainage density, land use, geology, lineament density and geomorphology.
Conducive areas for groundwater occurrence and storage were identified based on slope, drainage density, land use, geology, lineament density and geomorphological features of this area.
Depending on the availability of data and resources, this study is limited to and concentrates on the use of slope, drainage density, land use, geology, lineament density and geomorphological characteristics.
Other environmental variables that contributed towards the floristic variation include drainage, slope, rockiness, shrub density, herb density, climber density and canopy density.
On the steeper part of the slope, the density current reaches its maximum velocity of 1.2 metres (about 4 feet) per second.
We describe a spatially variable DEM error model that combines the influence of slope, point density, and vegetation in a fuzzy inference system.
