'Entrainment' presentation slideshows

Chapter 6 Cloud Development and Forms

Chapter 6 Cloud Development and Forms. Four mechanisms lift air so that condensation and cloud formation can occur:. Orographic lifting, the forcing of air above a mountain barrier Localized convective lifting due to buoyancy

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The ASTEX Lagrangian model intercomparison case

The ASTEX Lagrangian model intercomparison case. Stephan de Roode and Johan van der Dussen TU Delft, Netherlands. The ASTEX First Lagrangian (June 1992). Flight 1. Flight 2. Flight 3. Flight 4. Flight 5. ? Lagrangian evolution of cloudy boundary layer observed

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Deep Moist Convection (DMC)

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Parameterization in large-scale atmospheric modelling

Parameterization in large-scale atmospheric modelling. General parameterization problem :

589 views • 45 slides

Measuring Entrainment: Some Methods and Issues

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EFFECTS OF OCEAN MIXING ON HURRICANE HEAT CONTENT ESTIMATES: A NUMERICAL STUDY

EFFECTS OF OCEAN MIXING ON HURRICANE HEAT CONTENT ESTIMATES: A NUMERICAL STUDY. S. DANIEL JACOB and LYNN K. SHAY Meteorology and Physical Oceanography Rosenstiel School of Marine and Atmospheric Science University of Miami, Miami, FL 33149. Drs. Peter Black, Rainer Bleck and Arthur Mariano

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Plumes, hotspots and the CMB

503 views • 27 slides

Garde

534 views • 22 slides

Garde

374 views • 22 slides

Plant Responses to Signals IV

Plant Responses to Signals IV . Photomorphogenesis Circadian Rhythms Gravitropism. http://sunflower.bio.indiana.edu/~rhangart/plantsinmotion.html. Germination. Stem elongation (inhibition). Action Spectra. Action Spectrum , graph of the magnitude of a biological response to light,

351 views • 21 slides

Evidence for jet-driven outflows : 3C293 in 3D

Evidence for jet-driven outflows : 3C293 in 3D. Elizabeth Mahony (ASTRON, the Netherlands Institute for Radio Astronomy)

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310 views • 18 slides

DECOMPOSING COHESIVE SEDIMENT ENTRAINMENT

DECOMPOSING COHESIVE SEDIMENT ENTRAINMENT. Timothy Keen Naval Research Laboratory, Stennis Space Center, Mississippi 39529. Factors in Cohesive Sediment Consolidation and Entrainment. Sedimentological: Grain characteristics

297 views • 16 slides

Ch-3. There are several equations useful in understanding hydraulics and sediments deposits.

Ch-3. There are several equations useful in understanding hydraulics and sediments deposits. Reynolds Number Froude Number

314 views • 15 slides

Dworshak Dam Resident Fish Mitigation Project

Dworshak Dam Resident Fish Mitigation Project. Andy Dux and Sean Wilson Idaho Department of Fish and Game Project #2007-003-00. Dworshak Reservoir. Created in 1972 54 miles long 17k surface acres >600 ft deep No fish passage. Background.

396 views • 15 slides

Biological Responses

Biological Responses. Response of Organisms to the Abiotic World. Biological Timing Responses All organisms, except those living in deep caves or in the depths of the ocean, respond to night and day, the seasons, the tides and even the phases of the moon. These organisms can have:

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Convection plans

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Large Eddy Simulations of Entrainment and Inversion Structure

Large Eddy Simulations of Entrainment and Inversion Structure. Alison Fowler Supervisor: Ian Brooks. Convectively driven entrainment. Example of LES. The IMPORTANCE of the EZ. The EZ is responsible for the growth of the ML.

217 views • 11 slides

Sc to Cu transition

Randall 1980. Sc to Cu transition. A fundamental feature of the Hadley circulation. Important to global radiation balance A challenge for climate models, because it involves cloud-turbulence interaction that must be parameterized. Net cloud radiative effect. Sc. Cu.

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Large Eddy Simulations of Entrainment and Inversion Structure

Large Eddy Simulations of Entrainment and Inversion Structure. Alison Fowler (MRes Physics of Earth and Atmosphere) Supervisor: Ian Brooks. Statistics of the Entrainment Zone.

114 views • 1 slides