Supplementary material to "A comprehensive land surface vegetation model for multi-stream data assimilation, D&B v1.0"
Wolfgang KnorrMatthew WilliamsTea ThumThomas KaminskiMichael VoßbeckMarko ScholzeTristan QuaifeLuke SmallmannSusan Steele‐DunneMariëtte VreugdenhilTimothy R. GreenSönke ZähleMika AurelaAlexandre BouvetEmanuel BueechiWouter DorigoTarek S. El‐MadanyMirco MigliavaccaMarika HonkanenYann H. KerrAnna KontuJuha LemmetyinenHannakaisa LindqvistArnaud MialonTuuli MiinalainenGaétan PiqueAmanda OjasaloS. QueganP. J. RaynerPablo Reyes-MuñozNemesio Rodríguez-FernándezMike SchwankJochem VerrelstSongyan ZhuDirk SchüttemeyerMatthias Drusch
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In order to explore the influence of different assimilation indicators on the sequential data assimilation,in this paper, based on Lorenz-1963 model, we attempt to test the sensitivities of three typical assimilation methods, including En KF, DEn KF and En SRF. We have investigated the effects of different indicators on the data assimilation results. These indicators include the total assimilation time, the assimilation step, the ensemble number, the inflation factor, the observation number and the localization radius. The experimental results show that the total assimilation time, the assimilation step, the ensemble number, the inflation factor, the observation number and the localization radius directly affect the data assimilation result. The improved algorithm based on En KF is superior to the En KF under a given condition. When some preconditions are satisfied, the data assimilation results of all above methods tend to be the same. In practice, this work is of great significance in choosing the optimal sequential assimilation method.
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Data assimilation combines observational data with a numerical model. It is commonly used in numerical weather prediction, but is't also applied also in oceanography and hydrology. The integrating observations with models in a quantitative way, data assimilation allows to estimate and improve the model states, e.g. to initialize model forecasts. Also it can estimate parameters that control processes in the model or fluxes, which can be difficult and even impossible to measure. As such data assimilation can use observations to provide information about unobservable quantities if the model represents those. The combination of model and observation requires to have error estimates of both information sources. In ensemble data assimilation the error in the model state is estimated by an ensemble of model state realizations. This ensemble not only provides estimates of uncertainties, but also of cross-correlations between different model variables or parameters. The ensemble information is then used by the assimilation method, whose most widely known is the ensemble Kalman filter.
To simplify the implementation and use of ensemble data assimilation, the Parallel Data Assimilation Framework - PDAF - has been developed. PDAF is a freely-available open-source software (http://pdaf.awi.de) that provides ensemble-based data assimilation methods like the ensemble Kalman filter, but also support to perform ensemble simulations. PDAF is designed so that it can be used from small toy problems running on notebook computers up to high-dimensional Earth Systems models running on supercomputers.
This short course aims at geoscientists who have a modeling application or observations and are interested in applying data assimilation, but haven't found a starting point yet. The course will first provide an introduction to the ensemble data assimilation methodology. Then, it will explain the implementation concept of PDAF and finally provide a hands-on example of building a data assimilation system based on a numerical model. This practical introduction will prepare the participants to build a data assimiliton system by combining their numerical model with PDAF, hence providing a quick starting point for apply the ensemble data assimilation.
Ensemble forecasting
Ensemble Learning
Errors-in-Variables Models
Assimilation (phonology)
Unobservable
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Data assimilation applications with large-scale numerical models
exhibit extreme requirements on computational resources. Good
scalability of the assimilation system is necessary to make these
applications feasible. Sequential data assimilation methods based on
ensemble forecasts, like ensemble-based Kalman filters, provide such
good scalability, because the forecast of each ensemble member can be
performed independently. However, this parallelism has to be combined
with the parallelization of both the numerical model and the data
assimilation algorithm. In order to simplify the implementation of
scalable data assimilation systems based on existing numerical models,
the Parallel Data Assimilation Framework PDAF (http://pdaf.awi.de) has
been developed. PDAF provides support for implementing a data
assimilation system with parallel ensemble forecasts and parallel
numerical models. Further, it includes several optimized parallel
filter algorithms, like the Ensemble Transform Kalman Filter.
We will discuss the philosophy behind PDAF as well as features and
scalability of data assimilation systems based on PDAF on the example
of data assimilation with the finite element ocean model FEOM.
Ensemble forecasting
Ensemble Learning
Assimilation (phonology)
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Assimilation (phonology)
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Data assimilation applications with large-scale numerical models
exhibit extreme requirements on computational resources. Good
scalability of the assimilation system is necessary to make these
applications feasible. Sequential data assimilation methods based on
ensemble forecasts, like ensemble-based Kalman filters, provide such
good scalability, because the forecast of each ensemble member can be
performed independently. However, this parallelism has to be combined
with the parallelization of both the numerical model and the data
assimilation algorithm. In order to simplify the implementation of
scalable data assimilation systems based on existing numerical models,
the Parallel Data Assimilation Framework PDAF (http://pdaf.awi.de) has
been developed. PDAF provides support for implementing a data
assimilation system with parallel ensemble forecasts and parallel
numerical models. Further, it includes several optimized parallel
filter algorithms, like the Ensemble Transform Kalman Filter.
We will discuss the philosophy behind PDAF as well as features and
scalability of data assimilation systems based on PDAF on the example
of data assimilation with the finite element ocean model FEOM.
Assimilation (phonology)
Ensemble forecasting
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Data assimilation applications with high-dimensional numerical modelsshow extreme requirements on computational resources. Thus, goodscalability of the assimilation system is necessary to make theseapplications feasible. Sequential data assimilation methods based onensemble forecasts, like ensemble-based Kalman filters, provide suchgood scalability, because the forecast of each ensemble member can beperformed independently. However, this parallelism has to be combinedwith the parallelization of both the numerical model and the data assimilation algorithm. In order to simplify the implementation ofscalable data assimilation systems based on existing numerical models,the Parallel Data Assimilation Framework PDAF has been developed. Itprovides support for parallel ensemble forecasts and parallelnumerical models. Further, it includes several optimized parallel filteralgorithms, like the ensemble transform Kalman filter. We will discussthe features and scalability of data assimilation systems based onPDAF on the example of data assimilation with the finite element oceanmodel FEOM.
Assimilation (phonology)
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Abstract The Joint Effort for Data assimilation Integration (JEDI) is an international collaboration aimed at developing an open software ecosystem for model agnostic data assimilation. This paper considers implementation of the model‐agnostic family of the local volume solvers in the JEDI framework. The implemented solvers include the Local Ensemble Transform Kalman Filter (LETKF), the Gain form of the Ensemble Transform Kalman Filter (GETKF), and the optimal interpolation variant of the LETKF (LETKF‐OI). This paper documents the implementation strategy for the family of the local volume solvers within the JEDI framework. We also document an expansive set of localization approaches that includes generic distance‐based localization, localization based on modulated ensemble products, and localizations specific to ocean (based on the Rossby radius of deformation), and land (based on the terrain difference between observation and model grid point). Finally, we apply the developed solvers in a limited set of experiments, including single‐observation experiments in atmosphere and ocean, and cycling experiments for the atmosphere, ocean, land, and aerosol assimilation. We also illustrate how JEDI Ensemble Kalman Filter solvers can be used in a strongly coupled framework using the interface solver approximation, which provides increments to the ocean based on observations from the ocean and atmosphere.
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The paper gives a comprehensive and systemical description on advances in the meteorological data assimilation,and presents an introduction to the theories and application of the main methods(especially the Adjoint method and Genetic Algorithm) in Data Assimilation.The GA (Genetic Algorithm)has opened a new way in solving the data assimilation problems.
Assimilation (phonology)
Genetic data
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