VO5 - Parameterization 3

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Last updated 5:13 AM on 7/8/26
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35 Terms

1
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What are the main tasks of microphysics?

  • description of formation/growth/sedimentation of hydrometeors

  • phase transitions with accompanying release of latent heat (Thermodynamics)

  • Determine quantitity and nature of hydrometeors for electromagnetic calculations (radiation, radar, satellite comparisons)

  • Type and amount of precipiation (rain, snow, hail,..)

2
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What are the theoretical foundations for the description of hydrometeors in parameterizations?

  • no universally valid theory

  • scales mostly well below 1cm

  • difficult to gain insight from high-resolution simulations

3
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What are important approaches to describe hydrometeors in parameterizations?

  • one and two-bulk schemes

  • bin-schemes

4
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Regarding the phases of water, what must be decided in the model?

how a total amount of H2O is divided into water vapor, water and ice

5
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What is the simplest assumption for thermodynamics in the model?

  • Saturation water vapor depends only on T and p (Clausius Clapeyron)

  • T>0 water

  • T<0 ice

  • T=0 water and ice

6
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Why do simple assumptions regarding thermodynamics in models not hold?

  • In reality saturation water vapor depends on droplet radius, ice crystal shape and CCN/IN

  • mixed-phase clouds exist for T<0, no thermal equilibrium

7
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What does the Kessler parameterization consider?

only:

  • cloud water

  • rain

processes:

  • condensation

  • evaporation

  • autoconversion - cloud droplets collide → raindrops

  • accretion - falling raindrops collect cloud droplets while falling

  • evaporation

<p>only:</p><ul><li><p>cloud water</p></li><li><p>rain</p></li></ul><p>processes:</p><ul><li><p>condensation</p></li><li><p>evaporation</p></li><li><p>autoconversion - cloud droplets collide → raindrops</p></li><li><p>accretion - falling raindrops collect cloud droplets while falling</p></li><li><p>evaporation</p></li></ul><p></p>
8
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<p>Explain Autoconversion.</p>

Explain Autoconversion.

as a function, with M rain and m cloud water,

  • has 2 tuning parameters

    • a… at what amount of cloud water autoconversion begins, m<a term turned of

    • k1… how quickly cloud water is converted into rain

<p>as a function, with M rain and m cloud water,</p><ul><li><p>has 2 tuning parameters</p><ul><li><p>a… at what amount of cloud water autoconversion begins, m&lt;a term turned of</p></li><li><p>k<sub>1</sub>… how quickly cloud water is converted into rain</p></li></ul></li></ul><p></p>
9
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<p>Explain Accretion.</p>

Explain Accretion.

another therm added to autoconversion function,

adds another tuning parameter:

  • k2… collection efficiency, how efficiently raindrops collect cloud droplets

<p>another therm added to autoconversion function,</p><p>adds another tuning parameter:</p><ul><li><p>k<sub>2</sub>… collection efficiency, how efficiently raindrops collect cloud droplets</p></li></ul><p></p>
10
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Explain 2 properties of bulk schemes.

  • more often used

  • assume an analytical distribution

11
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Explain properties of a One-moment bulk scheme.

  • assume a fixed distribution

  • only the mass of each hydrometeor category is calculated, e.g. 1kg cloud water

  • essentially the Kessler parameterization

<ul><li><p>assume a fixed distribution</p></li><li><p>only the mass of each hydrometeor category is calculated, e.g. 1kg cloud water</p></li><li><p>essentially the Kessler parameterization</p></li></ul><p></p>
12
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Explain properties of a Two-moment bulk scheme.

  • distribution not assumed fixed, shape the same but stretch possible

  • mass and number of hydrometeors are determined, e.g. 1kg cloud water, 10^6 droplets

  • adds self collection as well

<ul><li><p>distribution not assumed fixed, shape the same but stretch possible</p></li><li><p>mass and number of hydrometeors are determined, e.g. 1kg cloud water, 10^6 droplets</p></li><li><p>adds self collection as well</p></li></ul><p></p>
13
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Explain properties of Bin microphysics schemes.

  • not that often used

  • approximate the distribution through several discrete “bins”

  • are also called “spectral”

  • usually, 30-45 bins → expensive

14
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How do microphysics parameterization depend on other parameterizations?

  • vertical updrafts critical, they determine how long and quickly precipitation objects can grow in the cloud before they fall → often from convection parameterizations

  • turbulent mixing leads to evaporation at cloud edges

  • aerosols from BL act as CCN/IN

15
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<p>What does this plot show?</p>

What does this plot show?

bulk-two-moment scheme with 6 hydrometeors

  • 12 prognostic variables

  • many processes that need to be formulated with help of tuning parameters and various closures

  • many coupled PDEs need to be solved

  • all hydrometeors always > 0

<p>bulk-two-moment scheme with 6 hydrometeors</p><ul><li><p>12 prognostic variables</p></li><li><p>many processes that need to be formulated with help of tuning parameters and various closures</p></li><li><p>many coupled PDEs need to be solved</p></li><li><p>all hydrometeors always &gt; 0</p></li></ul><p></p>
16
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To which other parameterizations are microphysics closely linked?

  • radiation

  • convection

  • aerosols

17
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How do microphysics directly influence the dynamics of the model?

through latent heat (e.g. moist adiabatic processes)

18
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Define radiation in general.

  • driving force of our atmosphere, controls daily and annual cycles

  • 1% more outgoing radiation → -3°C

19
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What aspects of radiation are particularly interesting in NWP models?

  • warming / cooling of surface (driver daily cycle)

  • waming / cooling of the air layers directly (O3, Clouds in LW, etc…)

  • forecasts in PV performance

20
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On what does scattering and absorption in gases depend on?

  • wavelength

  • angle

<ul><li><p>wavelength</p></li><li><p>angle</p></li></ul><p></p>
21
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On what does the interaction of radiation and hydrometeors depend?

  • geometry

  • properties of the microscopic objects

<ul><li><p>geometry</p></li><li><p>properties of the microscopic objects</p></li></ul><p></p>
22
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Which geometric property has a strong influence on interaction between radiation and hydrometeors?

radius of cloud droplet → has enormous effect (RADAR)
same amount of water will have different effects if there are many small or few large objects

23
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<p>What does this plot show?</p>

What does this plot show?

Example of mie scattering on a sphere

Extent of surface corresponds to intensity of scattering in that direction

<p>Example of mie scattering on a sphere</p><p>Extent of surface corresponds to intensity of scattering in that direction</p>
24
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How does cloud geometry influence radiation?

  • in 1D column, different overlap with same cloud fraction lead to different cloud cover

<ul><li><p>in 1D column, different overlap with same cloud fraction lead to different cloud cover</p></li></ul><p></p>
25
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Name the challenges of parameterizing radiation.

  • wavelength dependent

  • 3D

  • angle dependent

  • sensitive to number, size, type of hydrometeors

  • affected by aerosols

  • cloud geometry plays important role

  • non-trivial interactions with earths surface

26
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Name important approaches to parameterize radiation.

  • Spectral bands

  • 2-stream approach

  • Effective radius of cloud droplets

  • cloud generators

  • stochastic cloud generators

27
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Explain the sprectral bands approach.

  • instead of calculating each wavelength individually, closely correlated wavelengths are calculated together

  • number of groups is conceptually closely related to grid resolution

  • individual groups can be calculated independent of each other

28
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Explain the 2-stream approach.

  • no horizontal processes

  • for each band/group, only one upward and one downward calculation is performed

  • each direction represents an integral over all angles in a hemisphere

  • each column can be calculated separately as no horizontal exchange occurs

<ul><li><p>no horizontal processes</p></li><li><p>for each band/group, only one upward and one downward calculation is performed</p></li><li><p>each direction represents an integral over all angles in a hemisphere</p></li><li><p>each column can be calculated separately as no horizontal exchange occurs</p></li></ul><p></p>
29
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Explain the approach of Effective radius of cloud droplets.

  • instead of considering the full droplet distribution, a single radius is used that is supposed to achieve the same result

30
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How much of the total ECMWF computation time is taken by radiation?

~5%, so very expensive → rest parameterizations ~25%

31
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Explain how Cloud generators work.

  • despite 1D simplifications there are still many different cloud profiles in a column due to varying overlaps

  • There are 10 cloud sub profiles and on clear sky sub profile, each has a different radiation profile (in the example plot)

<ul><li><p>despite 1D simplifications there are still many different cloud profiles in a column due to varying overlaps</p></li><li><p>There are 10 cloud sub profiles and on clear sky sub profile, each has a different radiation profile (in the example plot)</p></li></ul><p></p>
32
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Explain how stochastic cloud generators work.

  • randomly generates several subprofiles from average profiles of cloud cover, cloud water, ice

  • distinguishes not only between cloudy and clear but also varies the amount of moisture

  • assumptions about overlap probability and assumed distributions of water and ice in each layer are take into account

  • in expl. 25 cloud profiles generated, 5 with no clouds at all, some other identical

<ul><li><p>randomly generates several subprofiles from average profiles of cloud cover, cloud water, ice</p></li><li><p>distinguishes not only between cloudy and clear but also varies the amount of moisture</p></li><li><p>assumptions about overlap probability and assumed distributions of water and ice in each layer are take into account</p></li><li><p>in expl. 25 cloud profiles generated, 5 with no clouds at all, some other identical</p></li></ul><p></p>
33
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How can computing time be reduced for radiation parameterizations?

  • calculate solutions for limited number of spectral bands

  • for each band, only 1 up/down flux calculated, no horizontal communication between columns (2-stream)

  • calculate radiation on coarser grid and longer time step

  • determine average radiation properties for all hydrometeors (effective radius, spherical)

34
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What are important input variables for radiation parameterizations?

  • Temperature

  • Gas composition

  • aerosols

  • hydrometeors

  • cloud fraction

35
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What are important uncertainties in radiation parameterizations?

  • geometric arrangement of clouds and distribution

  • characteristics of hydrometeors