Deciphering the Pre-solar-storm Features of the 2017 September Storm From Global and Local Dynamics

被引:6
作者
Raphaldini, Breno [1 ]
Dikpati, Mausumi [1 ]
Norton, Aimee A. [2 ]
Teruya, Andre S. W. [3 ]
McIntosh, Scott W. [1 ]
Prior, Christopher B. [4 ]
MacTaggart, David [5 ]
机构
[1] NCAR, High Altitude Observ, 3080 Ctr Green Dr, Boulder, CO 80301 USA
[2] Hansen Expt Phys Lab, 452 Lomita Mall, Stanford, CA 94305 USA
[3] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Sao Paulo, Brazil
[4] Univ Durham, Dept Math Sci, Stockton Rd, Durham DH1 3LE, England
[5] Univ Glasgow, Sch Math & Stat, Glasgow G12 8QQ, Scotland
基金
美国国家科学基金会; 巴西圣保罗研究基金会;
关键词
MAGNETIC HELICITY INJECTION; ROSSBY WAVES; ACTIVE REGIONS; DIFFERENTIAL ROTATION; ERUPTIVE ACTIVITY; FLARE ACTIVITY; FREE-ENERGY; RIEGER-TYPE; FIELD; FLUX;
D O I
10.3847/1538-4357/acfef0
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We investigate whether global toroid patterns and the local magnetic field topology of solar active region (AR) 12673 together can hindcast the occurrence of the biggest X-flares of solar cycle (SC)-24. Magnetic toroid patterns (narrow latitude belts warped in longitude, in which ARs are tightly bound) derived from the surface distributions of ARs, prior and during AR 12673 emergence, reveal that the portions of the south toroid containing AR 12673 was not tipped away from its north-toroid counterpart at that longitude, unlike the 2003 Halloween storms scenario. During the minimum phase there were too few emergences to determine multimode longitudinal toroid patterns. A new emergence within AR 12673 produced a complex nonpotential structure, which led to the rapid buildup of helicity and winding that triggered the biggest X-flare of SC-24, suggesting that this minimum-phase storm can be anticipated several hours before its occurrence. However, global patterns and local dynamics for a peak-phase storm, such as that from AR 11263, behaved like the 2003 Halloween storms, producing the third biggest X-flare of SC-24. AR 11263 was present at the longitude where the north and south toroids tipped away from each other. While global toroid patterns indicate that prestorm features can be forecast with a lead time of a few months, their application to observational data can be complicated by complex interactions with turbulent flows. Complex nonpotential field structure development hours before the storm are necessary for short-term prediction. We infer that minimum-phase storms cannot be forecast accurately more than a few hours ahead, while flare-prone ARs in the peak phase may be anticipated much earlier, possibly months ahead from global toroid patterns.
引用
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页数:19
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