Simulations of spatial variability in particle-size emissions during wind erosion events
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作者:
Butler, Harry J.
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Univ So Queensland, Australian Ctr Sustainable Catchments, Toowoomba, Qld 4350, AustraliaUniv So Queensland, Australian Ctr Sustainable Catchments, Toowoomba, Qld 4350, Australia
Butler, Harry J.
[1
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McTainsh, Grant H.
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Griffith Univ, Griffith Sch Environm, Atmospher Environm Res Ctr, Brisbane, Qld 4111, AustraliaUniv So Queensland, Australian Ctr Sustainable Catchments, Toowoomba, Qld 4350, Australia
McTainsh, Grant H.
[2
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Hogarth, William L.
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Univ Newcastle, Fac Sci & Informat Technol, Callaghan, NSW 2308, AustraliaUniv So Queensland, Australian Ctr Sustainable Catchments, Toowoomba, Qld 4350, Australia
Hogarth, William L.
[3
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机构:
[1] Univ So Queensland, Australian Ctr Sustainable Catchments, Toowoomba, Qld 4350, Australia
[2] Griffith Univ, Griffith Sch Environm, Atmospher Environm Res Ctr, Brisbane, Qld 4111, Australia
[3] Univ Newcastle, Fac Sci & Informat Technol, Callaghan, NSW 2308, Australia
This study simulates how spatial variations in particle-size emissions from a playa affect bulk and size-resolved dust concentration profiles during two contrasting wind erosion events (a small local and a large regional event) in the Channel Country, Lake Eyre Basin, Australia. The regional event had higher dust concentration as a result of stronger frontal winds and higher erodibility across the playa. For each event, two emission scenarios are simulated to determine if measured size-resolved dust concentration profiles can be explained by spatial variability in source area emissions. The first scenario assumes that particle-size emissions from source areas occur at a uniform rate, while the second scenario assumes that particle-size emissions vary between and within source areas. The uniform emission scenario, reproduced measured bulk dust concentration profiles (R2?=?0.93 regional and R2?=?0.81 local), however simulated size-resolved dust concentration profiles had poor statistical fits to measured size-resolved profiles for each size class (the highest were R2?=?0.5 regional and R2?=?0.3 local). For the differential particle-size emission scenario, the fit to the measured bulk dust concentration profiles is improved (R2?=?0.97 regional and R2?=?0.83 local). However, the fit to the size-resolved profiles improved dramatically, with the lowest being R2?=?0.89 (regional) and R2?=?0.80 (local). Particle-size emission models should therefore be tested against both bulk and size-resolved dust concentration profiles, since if only bulk dust concentration profiles are used model performance may be over-stated. As the source areas in the first 90?m upwind of the tower were similar for both events, the percentage contributions of each particle-size class to total emissions can be compared. The contribution of each particle-size class was similar even though the wind speed, turbulence and dust concentrations were significantly different; suggesting that the contribution of each particle-size to the total emitted dusts is not related to wind speed and turbulence. Copyright (C) 2012 John Wiley & Sons, Ltd.