Boundar Layer Meteorology Lecture 2 - PowerPoint PPT Presentation

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Boundar Layer Meteorology Lecture 2

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Note definitions of the Kronecker delta (and distinction between it and the unit ... Reynolds number is ratio of acceleration (or 'inertial force') to friction force. ... – PowerPoint PPT presentation

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Title: Boundar Layer Meteorology Lecture 2


1
Boundar Layer Meteorology Lecture 2
  • Review chapter 1 of Garratt
  • Terminology and Notation Review
  • Some non-dimensional numbers
  • Reynolds Averaging

2
Review chapter 1 of Garratt
  • Inner and outer layers (whats with this, is the
    outer layer really part of the boundary layer?)
  • Seasonal and geographic variations of the
    boundary layers character.

3
Modeled Boundary Layer Depth
4
Modeled Boundary Layer Depth
5
Observed Boundary Layer Depth
6
Terminology
  • Boundary Layer Regions
  • Surface Layer
  • Mixed Layer
  • Residual Layer
  • Stable (Nocturnal Boundary) Layer
  • Entrainment Zone
  • Ekman Layer (Outer Layer)
  • Surface Layer

7
Boundary Layer Regions
8
Notation
  • Variables T, Tv ,?, ?v , ?, q, x, y, z,
  • Viscosity ? ???du/dy? ??????T?????????kg/(m
    s)Pa/s?
  • Kinetmatic viscosity ????????????????m2/s
  • Summation (Einstein) notation see Stull handout
    (pp. 57-74). Note definitions of the Kronecker
    delta (and distinction between it and the unit
    vector), and the alternating unit tensor
    (Levi-Civita symbol) used to express the cross
    product.

9
Some Non-Dimensional Numbers
  • Reynolds number Re VL/?
  • Reynolds number is ratio of acceleration (or
    inertial force) to friction force. It governs
    transition to turbulence (at high Reynolds
    numbers , e.g. about 2300 for pipes highly
    variable!).
  • Richardson numbers ratio of
  • Flux
  • Gradient Ri (g/???d??dz)/(du/dz)2
  • Bulk

10
Reynolds averaging and Reynolds Stresses
t1 should be enough larger than t2 so that the
average is independent of time.
11
Reynolds averaging and Reynolds Stresses
12
Understanding Reynolds Stress
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