2013
DOI: 10.1029/2012ja018177
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A novel technique for rapid L* calculation using UBK coordinates

Abstract: [1] The magnetic drift invariant (L * ) is an important quantity used for tracking and organizing particle dynamics in the radiation belts, but its accurate calculation has been computationally expensive in the past, thus making it difficult to employ this quantity in real-time space weather applications. In this paper, we propose a new, efficient method to calculate L * using the principle of energy conservation. This method uses Whipple's (U, B, K) coordinates to quickly and accurately determine trajectories… Show more

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Cited by 8 publications
(13 citation statements)
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“…To examine possible magnetopause shadowing, we investigate drift shells using CIMI with the TS04 model. Drift shells are calculated finding the iso‐contours of the Hamiltonian H at a given time as done by Min et al (, ) using H=E0()E0+2MBm+qnormalΦ, where Φ is the electrostatic potential that we omit as done in Kang et al (). This approximation is valid because convective potentials are much less than 226 keV for this particular event and therefore do not change drift shells significantly; this results in drift shells that are simply a function of B m only.…”
Section: Cimi Simulation Of the Dropoutmentioning
confidence: 99%
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“…To examine possible magnetopause shadowing, we investigate drift shells using CIMI with the TS04 model. Drift shells are calculated finding the iso‐contours of the Hamiltonian H at a given time as done by Min et al (, ) using H=E0()E0+2MBm+qnormalΦ, where Φ is the electrostatic potential that we omit as done in Kang et al (). This approximation is valid because convective potentials are much less than 226 keV for this particular event and therefore do not change drift shells significantly; this results in drift shells that are simply a function of B m only.…”
Section: Cimi Simulation Of the Dropoutmentioning
confidence: 99%
“…To examine possible magnetopause shadowing, we investigate drift shells using CIMI with the TS04 model. Drift shells are calculated finding the iso-contours of the Hamiltonian H at a given time as done by Min et al (2013aMin et al ( , 2013b using…”
Section: Drift Shell Variations With Timementioning
confidence: 99%
“…Second, the functional relationship between B m and K is approximated before the L ∗ calculation (Sheldon and Gaffey [] used a polynomial expression and Min et al . [] used spline interpolation), where B m is the magnitude of the magnetic field at a mirror point s m and K is the modified invariant [ Roederer , ] K=snormalmsnormalmBnormalmB(s)normalds.In this expression, s m′ denotes the conjugate mirror point to s m so that B ( s m′)= B ( s m )≡ B m , and the integration is made along the guiding field line s . Once the model coefficients are known, B m ( K ) or K ( B m ) is approximated from the functional form whenever they are needed, avoiding the repeated expensive field line tracing.…”
Section: Introductionmentioning
confidence: 99%
“…This approach ensures that the calculated trajectory is closed if the particle's drift shell is so, regardless of the grid resolution. Second, the functional relationship between B m and K is approximated before the L calculation (Sheldon and Gaffey [1993] used a polynomial expression and Min et al [2013] used spline interpolation), where B m is the magnitude of the magnetic field at a mirror point s m and K is the modified invariant [Roederer, 1970]…”
Section: Introductionmentioning
confidence: 99%
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