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Drainage pattern of watershed refers to geospatial relationship among the streams or rivers and is associated with slope, soil type, rock resistance, structural and geological status of the basin.
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Based on the SPI pattern of each watershed, the SPI of −0.1 for the Foyle and Xarrama watersheds and +0.1 for the Shazand Watershed was selected as the drought threshold.
As shown in Fig. 4, the drainage pattern of Agula watershed can be described as dominantly dendritic; however, in some sub-watersheds trellis and parallel patterns also co-exist.
Therefore, the extent and spatial pattern of the watershed's soil erosion needs to be assessed.
The general drainage pattern of Sarabanga watershed is dendritic (Fig. 4).
Hence, the drainage pattern of a watershed helps understand the topographic and structural/lithologic controls on the water flow.
Hence, the information of geomorphology, hydrology, geology and land use pattern is highly informative for reliable study of drainage pattern of the watershed (Astras and Soulankellis 1992).
Whereas trellis type drainage pattern suggests down-turned folds called synclines form valleys. Open image in new window Fig. 2 Drainage pattern of Chakrar watershed.
Using GIS tools, the landscape pattern index method was proposed to compare the landscape patterns of Baiyangdian Watershed in 2002 and 2007, determine the transformation rules of landscape essential factors, and analyze the correlation between the changes of landscape patterns and water quality in Baiyangdian Watershed.
The drainage pattern of the Makhawan watershed is dendritic to sub-dendritic due to homogenous lithology; however, parallel-to-sub-parallel pattern has also developed locally confirming some structural control over drainage development.
Toward this end, we quantified the land use and land cover pattern of the Dongjiang River watershed, China between 1990 and 2006 based on remote sensing data and field measurements.
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