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4-1. 4-2 Land-surface model (cover art from Daniel Hillel, Environmental Soil Physics ) COMPONENTS OF PBL LAND SURFACE COUPLING ATMOSPHERIC LES NOAH.

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Presentation on theme: "4-1. 4-2 Land-surface model (cover art from Daniel Hillel, Environmental Soil Physics ) COMPONENTS OF PBL LAND SURFACE COUPLING ATMOSPHERIC LES NOAH."— Presentation transcript:

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3 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

4 TM image of El Reno Track, Oklahoma Southern Great Plains Experiment 1997 Soil Moisture Variability Irrigated farm (wet) Undeveloped land (dry) 4-4

5 wet soil dry soil 0 0 5 3015 x (km) y (km) λ = 15 km 4-5

6 λ / z i ≈ 9 LES OF PBL WITH SURFACE HETEROGENEITY 4-6

7 λ / z i ≈ 4 INSTANTANEOUS FIELDS 4-7

8 VELOCITY VARIANCES WITH HETEROGENEITY Total u-variance depends on heterogeneity Total w-variance nearly constant 4-8

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10 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

11 “VIRTUAL” MEASUREMENTS Tall towers for single- point flux measurements “Boundary-layer circulations” 4-11

12 IMPACT OF HETEROGENEITY ON FLUX MEASUREMENTS AT FIXED X 4-12

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15 u w p x z Vertically staggered scheme Co-located scheme 4-15

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17 Grid for isolated hill Grid for water waves 4-17

18 TIME EVOLUTION OF TURBULENT FLOW OVER A HILL 4-18

19 Averaged in y and t 4-19

20 Turbulence 4-20

21 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

22 BREAKING WAVES IN THE GULF OF TEHUANTEPEC COURTESY KEN MEVILLE SCRIPPS INSTITUTE OF OCEANOGRAPHY 4-22

23 LANGMUIR CIRCULATIONS GREAT SALT LAKE COURTESY S. MONISMITH 4-23

24 + wave field (fast) currents (slow) 4-24

25 (.. ) - Stokes terms (.. ) - Breaker terms Momentum SGS e Density Most important term generated by the waves 4-25

26 z 4-26

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29 PARTICLE PATHS OVERLAYING VORTICITY CONTOURS NO BREAKING U 10 = 5m/s 4-29

30 HOW DOES LATERAL CONVERGENCE HAPPEN? Stokes drift from waves Vortex forces u st x  3 4-30

31 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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