51. Erosion rates as a potential bottom‐up control of forest structural characteristics in the Sierra Nevada Mountains
- Author
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Simon M. Mudd, David T. Milodowski, and Edward T. A. Mitchard
- Subjects
landscape evolution ,LiDAR ,Soil production function ,CALIFORNIA ,UNITED-STATES ,Weathering ,ecological succession ,Ecological succession ,Forests ,Structural basin ,mixed-conifer forest ,SOIL PRODUCTION ,California ,CARBON ,Soil ,topography ,Ecosystem ,Sierra Nevada ,Ecology, Evolution, Behavior and Systematics ,WEATHERED BEDROCK ,geography ,Biogeomorphology ,geography.geographical_feature_category ,biomass ,LANDSCAPE ,Ecology ,Bedrock ,biogeomorphology ,erosion ,EVOLUTION ,Deciduous ,AIRBORNE LIDAR ,Remote Sensing Technology ,Environmental science ,SEDIMENT TRANSPORT - Abstract
The physical characteristics of landscapes place fundamental constraints on vegetation growth and ecosystem function. In actively eroding landscapes, many of these characteristics are controlled by long-term erosion rates: increased erosion rates generate steeper topography and reduce the depth and extent of weathering, limiting moisture storage capacity and impacting nutrient availability. Despite the potentially important bottom-up control that erosion rates place on substrate characteristics, the relationship between the two is largely unexplored. We investigate spatial variations in aboveground biomass (AGB) across a structurally diverse mixed coniferous/deciduous forest with an order of magnitude erosion-rate gradient in the Northern Californian Sierra Nevada, USA, using high resolution LiDAR data and field plots. Mean basin slope, a proxy for erosion rate, accounts for 32% of variance in AGB within our field area (P
- Published
- 2015
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