Impact Factor (IF) - Thomson Reuters Web of KnowledgeSM)

2020: 1.500 - 5 years IF: 1.659

2019: 1.258 - 5 years IF: 1.610

2018: 1.152 - 5 years IF: 1.315

2017: 1.000 - 5 years IF: 1.000

2016: 0.938 - 5 years IF: 1.010

2015: 0.641 - 5 years IF: 0.673

2014: 0.628 - 5 years IF: 0.652

2013: 0.390 - 5 years IF: 0.504

2012: 0.605

2011: 0.468

2010: 0.309

2009: 0.136

An international Journal published under the auspices of:

Recognized by:

Volume 22 (1) - 1999


Hierarchical analysis of relief features in a small watershed in a tropical deciduous forest ecosystem in Mexico

Pages 33-40


A hierarchical analysis of relief features in a small watershed (Watershed No.1, extent area of 16 ha) was analyzed based on frequencies of slope-angle and slope-morphology parameters in different functional scales (spatial or thematic units), using a geographic information system (GIS) as an essential analyzing information tool. The hierarchical arrangement of watershed’s relief is strongly influenced by geologic structure. The following four scale non-nested hierarchical levels were analyzed: 1.The total experimental watershed (shaped by its hydrologic division), 2. Two generalized orientation facing slopes (North and South, formed by hydrologic division and generalized aspect), 3. Three altitudinal segments (Bottom, Middle and Top, caused by geologic structure and altitudinal division) and 4. Hillslope units (sub-hydrologic division and geometric form). Fourteen hillslope units were delineated, which were grouped in four types according to their configuration (straight or curved along both length and width). Two main fractures divide the watershed into three altitudinal sectors. The top sector has flat homogeneous hillslope units, the middle sector has steeper convex hililslope units and the bottom sector has steeper convex and steeper homogeneous hillslope units. Southfacing slope have a longer length slope than northfacing slopes. Longer slopes have greater numbers of changes in the degree of inclination and, as a result, south-facing hillslope units are heterogeneous. Stream-channel network arrangement are not explained at the watershed level and, slope grade have not correlation with the first-order subcatchments area. However, the fluvial network is strongly influenced by the hillslope-unit morphology. Finally, the results suggest that exist three different environments where their both, processes of channel initiation and water movement are different.

→ Download Abstract PDF

→ Download Full Text PDF