2021
DOI: 10.1186/s40623-020-01324-w
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Geomagnetic secular variation forecast using the NASA GEMS ensemble Kalman filter: A candidate SV model for IGRF-13

Abstract: We have produced a 5-year mean secular variation (SV) of the geomagnetic field for the period 2020–2025. We use the NASA Geomagnetic Ensemble Modeling System (GEMS), which consists of the NASA Goddard geodynamo model and ensemble Kalman filter (EnKF) with 400 ensemble members. Geomagnetic field models are used as observations for the assimilation, including gufm1 (1590–1960), CM4 (1961–2000) and CM6 (2001–2019). The forecast involves a bias correction scheme that assumes that the model bias changes on timescal… Show more

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Cited by 4 publications
(3 citation statements)
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“…For the predictive secular variation models covering 2020.0 to 2025.0, the candidates broadly fall into two main categories: (1) computing SV solely from the latest available satellite and ground data (Alken et al 2020a;Pavón-Carrasco et al 2020;Huder et al 2020;Petrov and Bondar 2020;Rother et al 2020), or (2) applying physics-based modeling, combined with recent satellite and ground data to forecast future field changes based on underlying core dynamics (Brown et al 2020;Fournier et al 2020;Minami et al 2020;Metman et al 2020;Sanchez et al 2020;Tangborn et al 2020 et al 2020). Accurately forecasting the temporal evolution of the main geomagnetic field is nontrivial, due to challenges such as the low resolution of the recoverable magnetic field at the core-mantle boundary, the occurrence of unpredictable geomagnetic jerks or the uncertainty associated with diffusion of the field over short timescales (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…For the predictive secular variation models covering 2020.0 to 2025.0, the candidates broadly fall into two main categories: (1) computing SV solely from the latest available satellite and ground data (Alken et al 2020a;Pavón-Carrasco et al 2020;Huder et al 2020;Petrov and Bondar 2020;Rother et al 2020), or (2) applying physics-based modeling, combined with recent satellite and ground data to forecast future field changes based on underlying core dynamics (Brown et al 2020;Fournier et al 2020;Minami et al 2020;Metman et al 2020;Sanchez et al 2020;Tangborn et al 2020 et al 2020). Accurately forecasting the temporal evolution of the main geomagnetic field is nontrivial, due to challenges such as the low resolution of the recoverable magnetic field at the core-mantle boundary, the occurrence of unpredictable geomagnetic jerks or the uncertainty associated with diffusion of the field over short timescales (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…CM6 was used to generate main field candidates for epochs 2015.0 and 2020.0. Tangborn et al (2021) present a secular variation forecast for 2020 to 2025 combining a geodynamo model with an ensemble Kalman filter. Various geomagnetic field models are used as inputs to the data assimilation scheme.…”
Section: Open Accessmentioning
confidence: 99%
“…The two families of physical models (based on core surface flows or on dynamos) are themselves uncertain; in an attempt to take, at least partly, this uncertainty into account, most groups now resort to ensemble approaches (Minami et al 2020;Sanchez et al 2020;Brown et al 2021;Fournier et al 2021;Tangborn et al 2021) for steps (2) and (3) in Fig. 4.…”
Section: Physical Modelsmentioning
confidence: 99%