2002
DOI: 10.1023/a:1022400324489
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Cited by 15 publications
(7 citation statements)
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“…They found excellent agreement and showed that predictions of polar field reversals and the polar field strength at cycle minimum could be made years in advance. McCloughan and Durrant (2002) and Durrant and McCloughan (2004) noted that flux transport produces and requires synchronic maps rather than traditional synoptic maps and care must therefore be taken when estimating transport parameters from synoptic maps. Yeates et al (2007) used synoptic magnetogram data as the initial condition and assimilated the emergence of new active regions into the model throughout the course of the simulation to maintain the accuracy of the simulated photospheric magnetic field over many months.…”
Section: Assimilations Of Observed Magnetogramsmentioning
confidence: 99%
“…They found excellent agreement and showed that predictions of polar field reversals and the polar field strength at cycle minimum could be made years in advance. McCloughan and Durrant (2002) and Durrant and McCloughan (2004) noted that flux transport produces and requires synchronic maps rather than traditional synoptic maps and care must therefore be taken when estimating transport parameters from synoptic maps. Yeates et al (2007) used synoptic magnetogram data as the initial condition and assimilated the emergence of new active regions into the model throughout the course of the simulation to maintain the accuracy of the simulated photospheric magnetic field over many months.…”
Section: Assimilations Of Observed Magnetogramsmentioning
confidence: 99%
“…On the Sun the timescale for differential rotation to act is τ dr = 2π/(Ω(0) − Ω( 90)) ∼ 1/4 year. Within magnetic flux transport simulations the profile ( 2) is either applied directly, simulating the actual rotation of the Sun, or with the Carrington rotation rate (13.2 deg/day) subtracted (van Ballegooijen et al, 1998;McCloughan and Durrant, 2002).…”
Section: Standard Modelmentioning
confidence: 99%
“…This creates a problem when a simultaneous map is needed at all longitudes, as is required for the initial condition in the global simulation. McCloughan and Durrant (2002) deal with the problem by using a synoptic evolution equation, rather than the flux transport equation itself. We take an alternative approach and produce an initial configuration directly from the magnetogram.…”
Section: Magnetogram Data and Initial Surface Distributionmentioning
confidence: 99%