Misc Flashcards
Members of an ensemble use slightly different…
Initial conditions
Two different ensemble methods
- Perturbed parameter ensembles
2. Multi-model ensembles
Deterministic forecasts always choose the most ____ outcome
Likely
Resolution of Met Office deterministic forecast
1.5 km
Resolution of Met Office ensemble forecast
2.2 km, 18 members
Postage stamp plots are used for…
Ensemble forecasts
How forecasts can be improved
- Better use of observational data
- Better model physics
- Increased resolution
- More ensembles
- Better communication
How is the knowledge of the atmosphere imperfect?
- Data voids
- Weather in between observing locations
- Instrument sensitivity/error
- No observation of important quantities
How is the computer model imperfect?
- Resolution
2. Physical understanding
How has use of initial conditions improved?
- More data
2. Better data assimilation
How has the model improved over time?
- Better resolution
2. Better preresentation of physical processes
How is chaos embraced?
- Stochastic parameterisations
2. Ensembles
Parameterisations deal with a lack of ____ and ___ of unresolved physical processes
Knowledge
Observations
What is parameterised at the scale of 10-100km?
- Cumulus
- Two stream radiation
- Planetary boundary layer
Sensible weather reflected by parameterised quantities
Clouds
Precipitation
Surface temperature
Near surface winds
Measurements available for convection
- Hydrometeors
2. Winds
Example of quanities needed to verify paramaterisations
- Turbulent kinetic energy
- Boundary layer depth
- Aerosol concentrations
- Convective heating profiles
Challenges of parameterisation
- Reductionist
- Observations needed
- Relationships assumed to be universal
- Act on a single profile
Most simple form of convection to parameterise
Dry convection
Soundings with large CAPE tend to be ____ at low levels
Warm and moist
Soundings with large CAPE tend to be ___ at upper levels
Cold and dry
What is not redistributed in convection parameterisations?
Momentum
Why may the cloud base be lower than predicted?
Dry air entrainment
Why may the cloud base be higher than predicted?
The parcel still has momentum at the EL
A critical issue for convective parameterisations
Timing and momentum
How to address convective and stratiform areas
- Diagnose convective/explicit precipitation separately
- Interaction with microphysics
- Model grid spacing
How to improve parameterisations
- Increase resolution
2. Explicitly represent convection
Key problem with tropical rainfall forecasts
Convection parameterisation
In the Atlantic & Eastern Pacific, instabilities form in the troughs of the…
African Easterly Jet
Which direction do the monsoon winds flow?
Southwest
Vertical wind shear has a ___ effect on tropical cyclone intensification
Negative
Tropical cyclones decay with landfall due to
- Less latent & sensible heating
2. Increased friction
Less latent and sensible heating leads to
Weaker convection
Weaker convection leads to less intense ___ gradients
Pressure
4 defining qualities of a tropical cyclone
- Non-frontal, synoptic-scale
- Originates over tropical waters
- Organised deep convection
- Closed circulation with well-defined centre
Maximum vertical motion measures the strength of convection, related to the potential for…
Precipitation production
In convection, too little moisture aloft will result in…
Evaporation of towering cumulus
To produce a sustained convective system, you need
Mesoscale organisation
In a mesoscale convective system, vertical wind shear
Separates the updrafts and downdrafts
Separating the updrafts and downdrafts allows
Sustained convection
Stratiform precipitation and systems are…
Frontal
In a supercell, vertical wind shear is important for…
Vorticity and updraft/downdraft separation
What makes the jet stream baroclinically unstable?
Strong temperature gradient
Uneven heating and mountains can cause
Rossby waves
Before ETC occlusion, rainband is
In front of the warm front
After ETC occlusion, rainband is
Focused at the occlusion
Occlusion of the cold front isn’t needed if the…
Isotherms wrap around the low
Wind which is warmed and dried by descent on the lee side of a mountain
Foehn winds