Numerical weather prediction

Courses tagged with "Numerical weather prediction"

Understanding Uncertainty in Weather Forecasts

Learn about the main sources of uncertainty in weather forecasting and how they are addressed in early warning systems.

Level: Others
Certification course: No
What you'll learn:

In this eLearning module, we explain the basics of weather forecast uncertainty and how it can be accounted for when communicating forecasts through a forecast ‘value chain’. In this module, your learning level will be assessed through a set of quiz questions.

Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: Yes
Machine learning: No
Numerical weather prediction: Yes
Category: Forecasting

Ensemble Forecasting: Sources of forecast uncertainty (introduction)

Learn about sources of error in NWP, how they are quantified, and how ensembles are evaluated.

Level: Fundamentals
Certification course: No
What you'll learn:

  • Sources of forecast uncertainty
  • How ensembles quantify forecast uncertainty
  • How to extract information from the ensemble and evaluate performance
  • Communicating uncertainty
Full description:

Ensembles are run to account for uncertainties in initial conditions. This lesson explores the sources of error in NWP, how they are quantified, and how ensembles are evaluated.

Estimated duration: 40 minutes
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: Yes
Category: Forecasting

Forecast Jumpiness: An introduction

Learn about the ways in which forecast jumpiness can appear and how it can be mitigated.


Level: Fundamentals
Certification course: No
What you'll learn:

  • What is forecast jumpiness?
  • Examples of jumpiness
  • Jumpiness in the context of ensembles
  • How dynamic sensitivities relate to jumpiness
Full description:

There are times when consecutive forecasts can 'jump' significantly. This lesson will discuss the ways in which forecast jumpiness can appear and how it can be mitigated.

Estimated duration: 30 minutes
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: Yes
Category: Forecasting

Cloud and precipitation parametrization 2: ice and mixed-phase microphysics

This lesson covers key processes in ice and mixed-phase clouds and precipitation, and parametrization uncertainties.

Level: Others
Certification course: No
What you'll learn:

  • An overview of key microphysical processes for ice and mixed-phase cloud and precipitation in the atmosphere.
  • How to recognise the important ice and mixed-phase microphysical processes that need to be parameterised in a numerical weather prediction model.
  • The complexities of ice and mixed-phase microphysical processes, and uncertainties in their parameterisation.
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Cloud and precipitation parametrization 1: overview and warm-phase microphysics

Explore the key microphysical and warm-phase processes of cloud and precipitation parametrisation and their use in NWP.

Level: Others
Certification course: No
What you'll learn:

  • Basic concepts for the design of a cloud and precipitation microphysics parameterisation.
  • Key microphysical processes for warm phase cloud and precipitation in the atmosphere.
  • Which warm phase microphysical processes need to be parameterised in a numerical weather prediction model.
Estimated duration: 30 minutes
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Land surface: introduction to cold processes

Learn about the unique role of snow in forecasting, from short-range to seasonal time scales.

Level: Fundamentals
Certification course: No
What you'll learn:

  • The main physical properties of snow
  • The role of snow in the climate system at different time scales
  • Seasonal regimes in high latitude (cold) regions
  • How snow models are integrated into NWP and climate models
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Parametrisation of diabatic processes - case studies (convection)

Four case studies exploring the conditions that cause deep convection, considering predictability and forecast errors.

Level: Others
Certification course: No
What you'll learn:

  • The upper and lower-level flow conditions that favour deep convection
  • Translating weather maps in situations of deep convection
  • How to identify convective features and areas with potential predictability and forecast errors
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Introduction to the parametrization of sub-grid processes

Learn how sub-grid-scale processes (not explicitly simulated in NWP), are parameterised and how challenges are overcome.

Level: Fundamentals
Certification course: No
What you'll learn:

  • What parameterisation is and why it is needed
  • Methods and strategies for parameterisation
  • The role of parameterisation schemes in forecasting products
  • Examples of parameterisation, and sources of uncertainty
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

An introduction to Data Assimilation

Learn about data assimilation and how it is used to define ‘optimal' initial conditions for NWP at ECMWF.

Level: Fundamentals
Certification course: No
What you'll learn:

  • What is data assimilation and how it fits into numerical weather prediction
  • Which sources of observations are used by ECMWF in its data assimilation process
  • How data assimilation methods work, including 4D- VAR
  • Recent improvements in data assimilation, and future challenges
Estimated duration: 40 minutes
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Satellite observations and their role in NWP

Learn about the role of satellite observations and measurements, and how these are assimilated and monitored for NWP.

Level: Fundamentals
Certification course: No
What you'll learn:

  • Different data sources and the role of satellite observations in NWP
  • Types of satellites, what they measure, and how measurements are taken
  • How satellite observations are monitored and assimilated
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Representing model uncertainty with stochastic physics

Explore sources of uncertainty in NWP and how this is represented in the IFS using stochastic physics.

Level: Others
Certification course: No
What you'll learn:

  • Sources of model uncertainty
  • How model uncertainty is represented in ensemble forecasts, and in particular in the IFS
  • How process-level model uncertainty is accounted for, including the Stochastically Perturbed Parameterisation Tendencies scheme

Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

An introduction to single-column modelling

How SCM is used to investigate the physical processes of a global model in isolation, its applications and limitations.

Level: Others
Certification course: No
What you'll learn:

  • What single column models are and how they are applied
  • How to run a single column model, including data requirements
  • Practical examples of SCMs
  • Advantages and disadvantages of SCMs
Estimated duration: 30 minutes
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Sources of Uncertainty

Learn about uncertainties and chaotic behaviour in NWP, why ensembles are needed and how they are used at ECMWF.

Level: Fundamentals
Certification course: No
What you'll learn:

  • Sources of forecast uncertainty and chaotic behaviour
  • Ensembles as a tool for capturing uncertainty and probabilistic prediction
  • ECMWF model setup, initial conditions
Estimated duration: 40 minutes
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Parametrisation of diabatic processes - Convection in the context of large-scale circulation

This lesson will take you through what convection is and the phenomena it causes.

Level: Others
Certification course: No
What you'll learn:

  • The importance of convection in global energy and water balance.
  • Meteorological phenomena generated by convection.
  • About buoyancy and the parcel or plume method
  • About large scale effects of convection
  • About convectively coupled waves
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Parametrization of diabatic processes - The mass-flux approach and the IFS scheme

This lesson looks at the three classes of parametrization schemes and the main characteristics of the IFS scheme.

Level: Others
Certification course: No
What you'll learn:

  • What parameterisation schemes for convection are, and the main aims.
  • The three main parameterisation schemes used for convection:
    • Those based on moisture budgets
    • Adjustment schemes
    • Mass-flux schemes
  • The convection scheme used in ECMWF's Integrated Forecasting System (IFS)
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No

Introduction to Cloud Parametrisation

An introduction to the basic concepts for the design of a cloud and precipitation microphysics parametrisation.

Certification course: No
What you'll learn:

  • Aspects of a cloud and precipitation parameterisation
  • Processes affecting clouds
  • Components and examples of microphysics parameterisation schemes
Estimated duration: 15 minutes
Hide last updated info: No
Hide number of enrollments: No
Hide full description label: No
Atmospheric composition: No
Climate: No
Computing services and tools: No
Data applications: No
Forecasting: No
Machine learning: No
Numerical weather prediction: No