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Description

A magnetic polarity inversion line (MPIL) in the photosphere of an active region (AR) separates distinct patches of positive and negative magnetic polarities. There have been several studies showing the relation between flare occurrence and MPIL characteristics (e.g., Schrijver 2007; Mason and Hoeksema 2010; Falconer et al. 2012). In particular, strong-gradient, strong-field MPILs (sMPILs) have been considered as the most likely place where flux cancellation and/or flux rope emergence can take place in relation to the triggering of flares (e.g., Fang et al. 2012). We developed an algorithm to determine and characterise sMPILs in ARs. 

Input data

Blos and Br images from SDO/HMI Space-weather HMI Active Region Patch (SHARP) cylindrical equal area (CEA) near-realtime (NRT) data

Output parameters 

MPIL_BLOS.MAX_LENGTH: Length of the longest sMPIL segment calculated from Blos of a given AR

MPIL_BLOS.TOT_LENGTH: Total length of sMPIL segments calculated from Blos of a given AR

MPIL_BLOS.TOT_USFLUX: Total unsigned magnetic flux around sMPIL segments calculated from Blos of a given AR

MPIL_BR.MAX_LENGTH: Length of the longest sMPIL segment calculated from Br of a given AR

MPIL_BR.TOT_LENGTH: Total length of sMPIL segments calculated from Br of a given AR

MPIL_BR.TOT_USFLUX: Total unsigned magnetic flux around sMPIL segments calculated from Br of a given AR

Repository

https://dev.flarecast.eu/stash/projects/FE/repos/mpil-idl/browse

References

Falconer et al. 2012, The Astrophysical Journal, 757, 32
Fang et al. 2012, The Astrophysical Journal, 754, 15
Mason and Hoeksema 2010, The Astrophysical Journal, 723, 634
Schrijver 2007, The Astrophysical Journal Letters, 655, L117
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