Midterm: UNIT ONE Flashcards

(35 cards)

1
Q

Which is Material view?
Which is Field view?

A

Lagrangian –> Material
Eulerian –> Field

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2
Q

What is the interest of material view

A

obeys Newton’s law and thermodynamics –> construct laws for the atmosphere and ocean

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3
Q

What is Rossby number and what does it imply?

A

scaling of acceleration versus coriolis force, if small –> can neglect acceleration
eg: geostrophic balance

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4
Q

What is the material derivative and what is each term contribution?

A

Eulerian: rate of change of a particular fluid element versus rate of change at a fixed point in space

advection: ability of the fluid to carry its properties as it moves/ contribution from spatial variation of the property experienced as the parcel moves.

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5
Q

What is the circulation equation?

A

int_c ( u dot dl ) = dint_surf ( curl of u )dot n dS –> Stokes theorem

Line integral along a closed curve C of the tangential velocity equals the surface integral over any surface bounded by C of the curl of the velocity normal to the surface

-Circulation to vorticity

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6
Q

Physical meaning of divergence

A

For the velocity field:
Measures how fast the flow is expanding at a given point

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7
Q

Parcel Volume may expand/contract as the parcel moves around in the atm/ocean. How does the volume change?

A

Changes through net inward/outward motion through the surface that encloses the cube

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8
Q

What is the fractional rate of change with time of the parcel’s volume?

A

1/delV d(delV)/dt

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9
Q

Derive Divergence

A

∇ ∙ u

-Expansion/contraction of the cube and the difference in advection speed on opposing faces of the cube

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10
Q

Divergence theorem

A

d_int_S [ u dot N ] dS = t_int_V [ ∇ ∙ u ] dV

the integral over the closed surface that contains V of the velocity normal to this surface = integral within volume V enclosed by the surface of the divergence of the velocity

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11
Q

What is Helmotz decomposition?

and express the horizontal flow through the gradients of the two potentials

A

Two components of the flow:

-divergence free: Stream function
-curl-free: Velocity Potential

–> flow can be resolved as a sum of the two potentials

𝑢 = − 𝜕Ψ/𝜕𝑦 + 𝜕χ/𝜕𝑥
𝑣 = 𝜕Ψ/𝜕𝑥 + 𝜕χ/𝜕𝑦

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12
Q

With what is the vertical vorticity associated with?

A

Entirely associated with potential Ψ, streamfunction

∇ℎ^2 Ψ

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13
Q

With what is the divergence associated with?

A

Entirely associated with χ, velocity potential

∇ℎ ∙ 𝒖 = ∇ℎ^2 χ

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14
Q

How do you get a non-divergent flow?

A

∇ℎ ∙ 𝒖 = ∇ℎ^2 χ = 0

𝑢 = − 𝜕Ψ/𝜕𝑦
𝑣 = 𝜕Ψ/𝜕𝑥

-streamfunction parallel with u, magnitude of u = ∇ℎ Ψ

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15
Q

How do you get irrotational flow?

A

vort_z = k(curl u) = ∇ℎ^2 Ψ = 0
𝑢 = 𝜕χ/𝜕𝑥
𝑣 = 𝜕χ/𝜕𝑦

-divergence velocity potential perpendicular to u , ||u|| = ||∇ℎχ||

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16
Q

Derive pressure gradient force

A

p = F/dS

F = (p1 - p2)dS = (p1=p2)delydelz

p1 = p(x_0 - delx/2,y_0,z_0) –> Taylor expansion in x
–> F1p - F2p = − 𝜕𝑝/𝜕𝑥 𝛿𝑥 𝛿𝑦 𝛿𝑧

In 3D –> F_p = −∇𝑝 𝛿𝑥𝛿𝑦𝛿𝑧
divide by mass – > F_p/unit mass = − 1/𝜌 ∇𝑝

17
Q

What are the 3 forces acting on a parcel (in inertial frame of reference)?

A

Gravity : -g k
PGF: − 1/𝜌 ∇𝑝
Friction: F

Ftot/m = Du/Dt –> get momemtum equation

18
Q

Derive principle of mass conservation
–> Continuity equation

A

1/𝛿𝑀 𝐷(𝛿𝑀)/𝐷𝑡 = 0
–> D𝑝/Dt + 𝑝∇ ∙ 𝒖 = 0 : Divergence form

19
Q

Implication of incompressible flow in terms of continuity equation?

A

∇ ∙ 𝒖 = 0 –> non-divergent flow

So, can get information on vertical acceleration
∇h u = - 𝜕𝑤/𝜕𝑧 (unless all gradients are 0)

20
Q

From divergence form of continuity equation, what is the mass flux form?

A

Express material derivative
–>
𝜕𝜌/𝜕𝑡 + 𝜵 ∙ 𝜌 ∙ 𝒖 = 0

21
Q

What is the mass flux?

A

The rate at which mass enters the cube through the surface

Net mass flux through a surface is
(𝜌1𝑢1 − 𝜌2𝑢2)𝛿𝑦𝛿𝑧 –> Taylor expand to get that the net mass flux per unit volume is
-∇ ∙ 𝜌𝒖

22
Q

Write the momentum equation in rotating frame

A

(𝑑𝒖_𝑅/𝑑𝑡)_𝑅 = (𝑑𝒖_𝐼/𝑑𝑡)_𝐼− 2Ω × 𝒖𝑅 − Ω × (Ω × 𝒓)

23
Q

How can centrifugal force be rewritten?

A

Ω × (Ω × 𝒓) = Ω^𝟐𝒓¬
Given the dependence on r, the centrifugal acceleration may also be expressed as gradient of a potential:

∇Φ𝑐𝑒= (∇ 1/2 Ω^2𝑟¬^2)
Φ𝑐𝑒 = 1/2 Ω^2𝑟¬^2

24
Q

Rewrite the momentum equation in rotating frame by replacing what the inertial acceleration is

A

(𝑑𝒖_𝑅/𝑑𝑡)_𝑅 = 1/𝜌 ∇𝑝 -gk − 2Ω × 𝒖_𝑅 + ∇Φ𝑐𝑒

25
How do you express gravity as a gradient of potential?
𝑑𝜑/𝑑𝑧 = 𝑔 such that gk = ∇𝜑 so -gk = - ∇(gz) = -∇𝜑
26
What is the Coriolis acceleration due to?
Acceleration due to the effect of rotating background on the moving particle
27
What is the combination of centrifugal force and gravity?
Consider the sum: -CEN --> direction at right angles to the Earth's rotation axis -GRAV --> in radial direction from the center Gravity is dominant over CEN such that the resulting/apparent gravity points in a direction close to that of g --> as a result, the Earth obtained over the geological times an ellipsoidal (rather than a spherical) shape.
28
What is the modified geopotential?
𝜑∗ = 𝜑 − Ω^2𝑟^2/2 acting along g* radius --> local vertical z --> effective gravity g* that varies slightly with position on Earth's surface since 𝑟¬ = 𝛼 𝑐𝑜𝑠𝜑
29
What are the 3 characteristics of the Coriolis force
1. No coriolis force if parcels are not moving on the rotating planet 2. Coriolis acts to deflect the parcel at right angles to the direction it moves 3. Does no work on the parcel because at right angles to the direction it moves.
30
Write the momentum equation in the compact format for a rotating planet
𝐷𝒖/𝐷𝑡 + 2𝜴 × 𝒖 = − 1/𝜌 ∇𝑝 − 𝒈∗
31
Write the angular velocity components Name Ω𝑧
Ω𝑥 = 0 Ω𝑦 = Ωcos(lat) Ω𝑧 = Ωsin(lat) components of Ω that are related to w may be ignored because too small compared to the other terms So Ω𝑧 = 2 Ωsin(lat) = f_0
32
What is the horizontal momentum equation in rotating frame, vector format
𝐷𝒖/𝐷𝑡 + 𝒇𝒐 × 𝒖 = − 1/𝜌 ∇ℎ𝑝
33
What is the continuity equation on rotating planet?
- equation is unchanged because (𝜌∇ ∙ 𝒖𝐼 = 𝜌 ∙ ∇𝒖𝑅) (to show) and (𝐷𝜌/𝐷𝑡 )_I = (𝐷𝜌/𝐷𝑡 )_R but the individual terms of the material derivative are not equal
34
How does the thermodynamic equation change in inertial vs rotating frame?
They remain the same in rotating frame of reference
35
Consider vertical momentum equation in rotating frame, scale each terms and draw conclusions
W/T + UW/L + W^2/H + ΩU << − (1/𝜌)𝜕𝑝/𝜕𝑧 − 𝑔 such that we get hydrostatic balance