Title: Dating Quaternary alluvial fans with morphologic methods based on hillslope diffusion
1Dust-model upscaling from plot scale to global
scale
- Challenge
- To provide large-scale models with estimates for
z0, u, and dispersion that reflect small-scale
BL processes and surface characteristics.
- Two basic approaches
- Run global models in a nested, or multi-grid,
framework. - Provide global models with a database of
high-resolution boundary-layer model results to
use as lookup tables.
Paula Helm USGS
Vegetation cover changes through El Nino-La Nina
cycles, Yuma AZ
2Application Topographic shielding with analytic
solutions
u/u0
Owens Valley, CA 30m USGS DEM
0.0 2.0
Analytic solutions provided by Jackson and Hunt
(1975), wind from the south.
3A hierarchy of boundary-layer models
- Analytic solutions for flow over low hills,
augmented by separated-flow regions (Jackson and
Hunt). - Computationally fast (uses FFTs), but only
approximate. - Numerical solutions to Reynolds stress equations
(mean turbulence) with turbulent closure (e.g.
MSFD model). - Higher-order effects included.
- Large-Eddy Simulations Direct Numerical
Simulations
4Application Mom. part. over vegetated surfaces
w/ MSFD
u/u0
0.0 1.0 2.0
MSFD model run over surfaces with different
heights, densities, and spatial distributions
(regular vs clustered).
5Application Effects of vegetation on surface
roughness
Using individual-plant map, aggregate data at
coarser scale, calculate density, cluster index,
and use forward models to map effective z0
Vidal Valley, CA color DOQQ
Map of individual plants
6Application Effects of vegetation on surface
roughness
z0
u/u0
0.005 0.05
0.1 1.0
In this way, the effects of vegetation changes
can be incorporated from plant scale to basin
scale.
7Application Sub-grid scale dispersion
With Fourier-transform framework, localized and
distributed sources can be calculated with equal
ease.
8Application High-res emission and dispersion in
Phoenix, AZ
cgr,sand
Landsat-derived land cover, Phoenix, AZ
0.0 1.0
Analytic solutions for advection, dispersion, and
settling can be used to improve sub-grid
transport fate, especially for coarse particles.
9Active Interests/Projects
- Boundary-layer modeling of the effects of
small-scale topography and vegetation on dust
emissions - Water-table dynamics and their influence on dust
emissions from playas (w/ USGS Earth Surface
Processes) - Using soil AV horizons as dust-deposition
indicators over geologic time