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A single energetic correlation for all types of studied parallelepipedal particles is proposed for a large range of Reynolds numbers, including creeping flow and intertial regime: where Xe is an energetic dimensionless criterion: E is the mechanical power dissipated by unit volume of fluid.
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In the last line of Table 2, E/I represents good correlation with energetic electron/ion acceleration, respectively.
We found that E M, Δ B 2, R, X GSM, and Y GSM can be categorized into good correlation with energetic ion acceleration efficoency.
We find that the reconnection electric field, total amount of reduced magnetic energy, reconnection rate, satellite location in the Earth's magnetosphere (both X GSM and Y GSM) show high correlation with energetic ion acceleration efficiency.
On the other hand, only energetic electrons show good correlation with ion temperature, electron temperature, ion/electron temperature ratio, current sheet thickness, and electric field normal to the neutral sheet.
Only energetic ions show good correlation with total amount of reduced magnetic energy, reconnection rate, and satellite location in the Earth's magnetosphere (both X GSM and Y GSM).
We found that reconnection electric field, total amount of reduced magnetic energy, reconnection rate, satellite location in the Earth's magnetosphere (both X GSM and Y GSM) can be categorized into good correlation with energetic ion acceleration efficiency.
We have studied the relationship between dynamical correlations and energetic contributions in an attempt to model the transmission of information inside protein-protein complexes.
Table 2 shows the correlation coefficients between energetic electron/ion and reconnection parameters.
In (72), ( Gamma _{k k^{prime }}^{E|S} =Gamma _{k k^{prime }}^{E|S}(boldsymbol {r},boldsymbol {r}^{prime }) ) represent energetic and entropic two-point correlation kernels.
We also found a clear correlation of the energetic electron flux at geosynchronous orbit with the Pc5 power in the magnetosphere and at high and low latitude, at a time delay of approximately 2 days, in agreement with previous studies at auroral and middle latitudes (Rostoker et al. 1998; Baker et al. 1998; Mathie and Mann 2001; Mann et al. 2004).
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