• Keine Ergebnisse gefunden

Problem sheet IV

N/A
N/A
Protected

Academic year: 2021

Aktie "Problem sheet IV"

Copied!
2
0
0

Wird geladen.... (Jetzt Volltext ansehen)

Volltext

(1)

Problem sheet IV

Fluid Dynamics

1. Laminar Flow in a water channel

• A sluice gate controls the discharge of water down a channel. If the discharge is increased by 20%, what will be the percentage change in the depth of the water? Compare lecture notes on page 53.

• Is the percentage in the depth dependent upon the viscosity of the water? Is it dependent upon the temperature?

2. Water Flow

If the velocityw in the flow system considered on page 54 in the lecture notes is 102ms1, how deep is the boundary layer of water at normale temperature? How deep would it be for air with the same specifications?

3. 2D flow field

A two dimensional flow field occupying the domain y>0 is specified in terms of the streamfunction ψ, such that

ψ=A·sin(kx)·e−ly

(a) Sketch the streamfunctionψand the corresponding streamlines.

(b) Derive expressions for the horizontal velocity components (u, v) (c) Derive expressions for the vertical component of the vorticityζ

(d) Under what relative values ’k’ and ’l’ will the streamfunctionψbe a solution of:

D

Dtζ =ν∇2ζ whereζ= ∂v∂x∂u

∂y is the vorticity.

Hint: Use a software package such as Maple, Mathematica, Matlab, ... if you have access.

4. Shallow water system

Consider the one-spare dimension shallow water system:

∂u

∂t +u∂u

∂x−f v = −g∂h

∂x

∂v

∂t +u∂v

∂x+f u = 0

∂h

∂t +u∂h

∂x+h∂u

∂x = 0

or written as:

uz+uux−f v = −ghx

vz+uvx+f v = 0 hz+vhx+hux = 0 Non-dimensionalise this set to the form:

1

(2)

R0[˜uz˜+ ˜u˜ux˜]−v˜ = (∃R0)˜hx˜

R0[˜vz˜+ ˜vv˜x˜] + ˜u = 0 h˜z˜+ ˜u˜h˜x+ ˜h˜ux˜ = 0 where

˜ u= u

U v˜= v

V x˜= x

L y˜= y

L ˜h= h

H ˜t=

U

L

t R0 U f L (a) What is the dimensionless parameter∃?

(b) Consider some observed motions such that U ∼1cms1,L∼10km and H∼10m

What are the characteristic values ofR0 and∃?

(c) To build a laboratory analogue of the lake flow, what should be the depthH of the model, and how quickly must the laboratory model be rotated? Assume model is such that U ∼ 1/10cms1 andL∼1m.

2

Referenzen

ÄHNLICHE DOKUMENTE

Vertical lines around the probability at a = 0.85 and d = 0.45 display the range of probabilities obtained when considering, instead of 17 years, the last 10 to 20 years in the

The Gas Target Model is not binding, it is just an idea, a bold vision of how a truly integrated single gas market can be organised and operated in the

The analysis of moorings placed in the Deep Western Boundary Current (DWBC) at 44øW for three years resulted in a definite seasonal cycle, ranging from less than 7 Sv

To the south of this line are the major water mass formation areas where warm and salty water masses coming from the north are transformed into cold Weddell Sea Bottom Water

To summarize, below the surface water, the Tyrrhe- nian Sea receives LIW and a colder, fresher component from the eastern Mediterranean through the Strait of Sicily, and from

Zemba [1991] investigated the water mass distributions at higher latitudes in the western South Atlantic and estimated a poleward flow of 10 Sv of NADW within the deep western

Pamtars (1971) and GAg~TT and MUNK (1971) have shown that the fine-structure contamination of internal gravity wave spectra can be written as a function of some statistical

As already seen, the sampling window plays an important role in correctly forecast- ing losses during crisis times. A further important role is played by the degree of