期刊
EARTH SURFACE PROCESSES AND LANDFORMS
卷 46, 期 7, 页码 1257-1267出版社
WILEY
DOI: 10.1002/esp.5096
关键词
fluvial network; hyper‐ arid; hypsometric curve; monsoon precipitation; Oman; sapping
资金
- Boston University
- Sultan Qaboos University
This study investigated the relationships among precipitation, vegetation, and morphological characteristics of watersheds on both sides of the Dhofar Mountains in southeastern Oman. The research found a correlation between vegetation and cloud cover, and highlighted how hypsometric curves and statistical moments can differentiate between wet and dry watersheds. The findings suggest a significant link between hydrology and morphology, especially when watersheds are aggregated in zones, with distinct groups identified based on their hydrological and morphological characteristics.
We study the relationships among precipitation, vegetation, and morphological characteristics of watersheds draining either side of the Dhofar Mountains in southeastern Oman to understand the geomorphic signature of water availability in a semi-arid carbonate landscape. Water availability is expressed in terms of vegetation and cloud cover. The integral and the statistical moments of the hypsometric curve were used to determine whether hyper-arid, inland-draining watersheds are significantly different from seasonally wet watersheds on the coast side of the mountain range. We demonstrate that the vegetation and cloud cover are correlated, with locations with longer cloud periods also having a longer period with a vegetation canopy. The analysis shows that the hypsometric curve and its statistical moments capture the morphological difference between wet watersheds shaped by groundwater sapping and dry watersheds with fluvial morphology. Specifically, the curves exhibit two shapes: watersheds with more vegetation and cloud cover are characterized by higher convexity, and those with less vegetation and cloud cover are characterized by higher concavity. A variance analysis of cloud cover, vegetation, and hypsometric integral shows that they are significantly different between the wet and dry watersheds. The link between hydrology and morphology is not strong at the scale of a single watershed, but it is significant when the watersheds are aggregated in zones. The statistical moments of the hypsometric curve in the range of values of the integral and skewness show good separation between watersheds dominated by sapping and fluvial erosion processes. We can separate the watersheds draining the mountain range in two distinct groups on the basis of their bimodal hydrological and morphological characteristics. Our findings support other studies that hypothesize a trade-off from chemical- to mechanical-dominated denudation in carbonate terranes as precipitation decreases.
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