Parameterisation & Resolution Flashcards

1
Q

To resolve smaller weather phenomena, we need

A

More grid points

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2
Q

To improve initial conditions, we need

A

More data and better data assimilation

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3
Q

To improve the model, we need

A

Better resolution & better representation of physical processes

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4
Q

To embrace the chaos theory, we can use

A

Stochastic parameterisation and ensembles

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5
Q

Parameterisations show only the ___ aspects of the physical processes

A

Essential

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6
Q

Parameterised quantities can reflect

A

Clouds, precipitation, temperature, near-surface wind

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7
Q

If the phenomenon can be directly represented, we

A

Detect and present

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8
Q

If the phenomenon cannot be directly represented, we use

A

Diagnostic parameterisation

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9
Q

Four examples of parameterisations

A

Convection, orographic drag, cloud microphysics, surface-atmosphere fluxes

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10
Q

How to produce a parameterisation

A

Find relationships between small scale processes and grid-scale variables

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11
Q

Parameterisation is reductionist - what does this mean?

A

We assume we can explain the whole as a sum of its parts

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12
Q

The problem with using observations to test parameterisations

A

Processes parameterised are usually difficult to measure

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13
Q

2 examples of quantities needed to initialise parameterisations

A

Surface fluxes, aerosol concentrations

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14
Q

Special observations are used to produce paramaterisation relationships to

A

Relate them to model variables

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15
Q

Parameterisation relationships are assumed to be

A

Universal

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16
Q

Parameterisations act on a

A

Single profile

17
Q

3 ways in which convection is parameterised

A

Dry convection, deep moist convection, shallow moist convection

18
Q

Dry convection

A

Absolutely unstable

19
Q

Deep moist convective

A

Conditionally unstable

20
Q

Shallow, moist convection

A

Occurs in the boundary layer

21
Q

3 factors that convection redistributes

A

Heat, moisture and momentum (wind speed)

22
Q

Momentum is not redistributed in the parameterisation of

A

Deep,moist convection

23
Q

3 things a convective parameterisation must decide

A

Activation, intensity and vertical distribution

24
Q

Single biggest challenge in representing tropical rainfall

A

Convection parameterisation

25
Q

How to explicitly represent unresolved processes

A

Increase resolution

26
Q

Resolution of Met Office model

A

1.5 km

27
Q

Global model resolution

A

10 km

28
Q

Met Office transition resolution

A

4 km

29
Q

Even at scales of 1-4 km, ___ is not truly resolved

A

Convection

30
Q

Double the resolution leads to how much more computer power?

A

8x

31
Q

Convective parameterisations are

A

Idealisations