'Atmospheric boundary layer' presentation slideshows

Dimensional Analysis and Similitude

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Micrometeorology Boundary Layer Meteorology Surface Energy Budget

Micrometeorology Boundary Layer Meteorology Surface Energy Budget.

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Basic bluff-body aerodynamics II

Basic bluff-body aerodynamics II. Wind loading and structural response Lecture 9 Dr. J.D. Holmes. -0.20. -0.10. -0.20. x. x. x. leeward wall. roof. -0 . 23. -0.18. -0.23. x. x. x. -0.20. -0.20. x. x. -0.2. side wall. -0.5. -0.5. Sym.about C L. -0.7. -0.8. -0.8.

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Hurtling Over Regional Observations of Extreme Weather Events while Forming Partnerships

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Longitudinally Oriented Cloud Systems Associated With The Gulf Stream Off The Florida East Coast

Longitudinally Oriented Cloud Systems Associated With The Gulf Stream Off The Florida East Coast Wanda Reeves Department of Marine Environmental Systems Florida Institute of Technology Melbourne, Fl 32901. Weather.msfc.nasa.gov. Theories for Longitudinally Oriented Cloud Systems.

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Assimilation of Cabauw observations in a single-column model using an ensemble-kalman filter

Assimilation of Cabauw observations in a single-column model using an ensemble-kalman filter. Peter Baas. Summary status. 1D RACMO physics with dynamics from 3D RACMO available for Cabauw point; Prototype for ensemble Kalman filtering System for Cabauw column available.

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Gustiness parameterization in the atmospheric boundary layer

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SENSITIVITY ANALYSIS ON TURBULENCE MODELS FOR THE ABL IN COMPLEX TERRAIN

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REACTIVITY SCALES AS COMPARATIVE TOOLS FOR CHEMICAL MECHANISMS: SAPRC-07 vs MCM

REACTIVITY SCALES AS COMPARATIVE TOOLS FOR CHEMICAL MECHANISMS: SAPRC-07 vs MCM. Dick Derwent rdscientific, Newbury, United Kingdom Presentation to Reactivity Scientific Advisory Committee Air Resources Board, Sacramento March 2009. COMPARISON OF SAPRC-07 AND MCM v3.1.

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Chapter 4 The Energy Balance of The Surface

Chapter 4 The Energy Balance of The Surface. Why The SEB? What and How? SEB components (Rn, SH, LE, G, B, Tskin, ? , ? , examples) ABL (neutral, stable, unstable, Ri, z/L, entrainment, LCL, eddy covariance, bulk formulations, examples) SEB measurements SEB remote sensing

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Wind Over Hills

Wind Over Hills. Ryan Wallace MAE 741 4/26/06. Outline. Flow Structure Momentum and Continuity Equations Scales of the Flow Turbulent Stress and its Model Momentum Scaling Interaction between Regions Vorticity Distortion and Turbulence Structure Separation Effect of Froude Number

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Boundary Layer Meteorology

Boundary Layer Meteorology. Prof. Daniel Kirk-Davidoff Rm. 3423 CSS (301)-270-3704 dankd@atmos.umd.edu. Lecture 1 8/31/04. Course Syllabus: discuss requirements, schedule, readings. Starting Point Exam Introduction to the Boundary Layer Hand out readings.

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Importance of the atmospheric boundary layer (2)

Importance of the atmospheric boundary layer (2). Review of last lecture. The mission of meteorology is to understand and predict weather- and climate-related disasters (e.g. tornados, hurricanes, El Nino and global warming).

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Observed Structure of the Atmospheric Boundary Layer (2)

Observed Structure of the Atmospheric Boundary Layer (2). Review of last lecture. Vertical structure of the atmosphere and definition of the boundary layer Vertical structure of the boundary layer Definition of turbulence and forcings generating turbulence

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The Vasco-Cirene experiment

The Vasco-Cirene experiment. J.Ph. Duvel J. Vialard and R. Molcard LMD-ENS Paris, France LODYC, UPMC, Paris, France Support from CNES, CNRS/INSU, CORIOLIS. Intraseasonal Variation SST-OLR. OLR/NOAA. SST/TMI. Coherent variations of the TMI-SST and the NOAA-OLR

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PARAMETERIZATION OF URBAN COVERS IN MESOSCALE MODELS

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N. Maximenko : Satellite ocean surface currents and winds

Ocean Vector Wind Working Group meeting, October 7, 2013, Boulder. N. Maximenko : Satellite ocean surface currents and winds. Surface currents are not well measured. 3659 active Argo floats (3659 / 10 days * 10 hours ? 152 continuous sites).

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