2011
DOI: 10.1007/s11214-011-9783-y
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Can Surface Flux Transport Account for the Weak Polar Field in Cycle 23?

Abstract: To reproduce the weak magnetic field on the polar caps of the Sun observed during the declining phase of cycle 23 poses a challenge to surface flux transport models since this cycle has not been particularly weak. We use a well-calibrated model to evaluate the parameter changes required to obtain simulated polar fields and open flux that are consistent with the observations. We find that the low polar field of cycle 23 could be reproduced by an increase of the meridional flow by 55% in the last cycle. Alternat… Show more

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Cited by 30 publications
(27 citation statements)
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“…Please note that different definitions of the polar field were used between the observation (left panel, line-of-sight component and averaged over 35 • wide polar caps) and the reconstruction (right panel, radial component and averaged over the 15 • wide polar caps). Jiang et al (2011c) show that they are consistent when the same definitions are used. The good correlation provides the evidence for the polar field to be the solar cycle precursor.…”
Section: Solar Polar Field Precursorsupporting
confidence: 55%
“…Please note that different definitions of the polar field were used between the observation (left panel, line-of-sight component and averaged over 35 • wide polar caps) and the reconstruction (right panel, radial component and averaged over the 15 • wide polar caps). Jiang et al (2011c) show that they are consistent when the same definitions are used. The good correlation provides the evidence for the polar field to be the solar cycle precursor.…”
Section: Solar Polar Field Precursorsupporting
confidence: 55%
“…The converging motion of the meridional flow in the activity band or the active region inflow (e.g., Haber et al 2002;Zhao & Kosovichev 2004;Hathaway & Rightmire 2010) in the low latitude will prevent the cross-equatorial transport of the magnetic flux (e.g., De Rosa & Schrijver 2006;Cameron & Schüssler 2012;Martin-Belda & Cameron 2017). The high gradient of the meridional flow near the equator is also a possible origin of the small cross-equatorial flux transport (Schrijver & Liu 2008;Jiang et al 2013). Although the meridional flow variation at the Cycle 23/24 minimum is not suitable to explain the observed axial dipole moment (Upton & Hathaway 2014a), the effect on the flux transport should be considered to explain the plateau.…”
Section: Discussionmentioning
confidence: 99%
“…We use the MUDPACK package here to solve Equation (3) in its nonseparable form in spherical coordinates, subject to the boundary conditions described above. Jiang & Feng (2012) have recently presented a high-speed combined spectral/finite-difference PFSS solution method using the related NCAR FISHPACK package.…”
Section: Finite-difference Potential-field Source-surface Models For mentioning
confidence: 99%
“…One explanation is that the meridional flows are so fast that the leading polarities in the two hemispheres do not have time to interconnect and interact with each other before being swept poleward (e.g., Schrijver & Liu 2008;Wang et al 2009;Nandy et al 2011). To affect the polar fields significantly, these fast meridional flows would have to occur at active latitudes, as Dikpati (2011) An alternative explanation is that the active region Joy's law tilts lost their hemispheric bias during cycle 23 (e.g., Jiang et al 2011;Petrie 2012). In this scenario approximately equal quantities of each polarity would be sent poleward with approximately zero net effect on the polar fields even for slow meridional flow speeds.…”
Section: Multipolar Fieldsmentioning
confidence: 99%