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Published byJanice Norton Modified over 8 years ago
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Land-surface model (cover art from Daniel Hillel, Environmental Soil Physics ) COMPONENTS OF PBL LAND SURFACE COUPLING ATMOSPHERIC LES NOAH LAND SURFACE MODEL SURFACE ENERGY BALANCE LES SURFACE FLUXES ARE NOT PRESCRIBED BUT RESULT FROM THE COUPLING 4-3
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TM image of El Reno Track, Oklahoma Southern Great Plains Experiment 1997 Soil Moisture Variability Irrigated farm (wet) Undeveloped land (dry) 4-4
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wet soil dry soil 0 0 5 3015 x (km) y (km) λ = 15 km 4-5
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λ / z i ≈ 9 LES OF PBL WITH SURFACE HETEROGENEITY 4-6
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λ / z i ≈ 4 INSTANTANEOUS FIELDS 4-7
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VELOCITY VARIANCES WITH HETEROGENEITY Total u-variance depends on heterogeneity Total w-variance nearly constant 4-8
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Phase Averaged Velocity Fields λ / z i ≈ 4 λ / z i ≈ 18 λ / z i ≈ 1 u w wetdry x/λ z/z i Patch boundary 4-10
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“VIRTUAL” MEASUREMENTS Tall towers for single- point flux measurements “Boundary-layer circulations” 4-11
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IMPACT OF HETEROGENEITY ON FLUX MEASUREMENTS AT FIXED X 4-12
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u w p x z Vertically staggered scheme Co-located scheme 4-15
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Grid for isolated hill Grid for water waves 4-17
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TIME EVOLUTION OF TURBULENT FLOW OVER A HILL 4-18
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Averaged in y and t 4-19
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Turbulence 4-20
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OCEAN MIXED LAYERS HOW DO THEY DIFFER FROM THEIR ATMOSPHERIC COUNTERPARTS? SURFACE WAVES, DO THEY ALTER THE TURBULENT PBL DYNAMICS? LIMITED OBSERVATIONAL DATABASES COMPARED TO THE ATMOSPHERE 4-21
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BREAKING WAVES IN THE GULF OF TEHUANTEPEC COURTESY KEN MEVILLE SCRIPPS INSTITUTE OF OCEANOGRAPHY 4-22
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LANGMUIR CIRCULATIONS GREAT SALT LAKE COURTESY S. MONISMITH 4-23
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+ wave field (fast) currents (slow) 4-24
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(.. ) - Stokes terms (.. ) - Breaker terms Momentum SGS e Density Most important term generated by the waves 4-25
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PARTICLE PATHS OVERLAYING VORTICITY CONTOURS NO BREAKING U 10 = 5m/s 4-29
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HOW DOES LATERAL CONVERGENCE HAPPEN? Stokes drift from waves Vortex forces u st x 3 4-30
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COHERENT STRUCTURES IN LES WITH WAVE EFFECTS IDENTIFIED USING STOCHASTIC ESTIMATION (Adrian, 1989) Top view Side view x y x yz 4-31
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