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The Maunder minimum: An extreme space climate event. The Maunder minimum: An extreme space climate event?. Mathew Owens, Mike Lockwood, Luke Barnard, Chris Scott and Ken McCracken. Overview. Direct observations Sunspots Aurora Cosmogenic isotope abundance Climate observations
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The Maunder minimum: An extreme space climate event The Maunder minimum: An extreme space climate event? Mathew Owens, Mike Lockwood, Luke Barnard, Chris Scott and Ken McCracken
Overview • Direct observations • Sunspots • Aurora • Cosmogenic isotope abundance • Climate observations • Reconstructions • Geomagnetic • Sunspot • Solar wind speed • Space weather implications
The Maunder minimumEddy, Science, 1976 • A period 1645-1715 with: • An absence of sunspots • An (apparent) reduction in auroral activity • An (apparent) reduction in coronal structure during eclipses • A reduction in 14C, suggesting increased cosmic ray flux • (10Be is now known to have increased, though still cycled)
Sunspot numberHoyt and Schatten, Sol Phys, 1998; Lessu et al, A&A, 2013;Svalgaard, IAU, 2011; Lockwood et al, JGR, 2014 Post 1750
Sunspot number: 11-year running means Post 1750
Heliospheric modulation potentialSteinhilber et al., PNAS, 2011
Climate records Manley, QJRMS, 1974, Lockwood et al., ERL, 2011 • No “little ice age.”
“closed” field line Open Solar Flux, FS Flux threading the coronal source surface UnsignedFlux, FU= |BR| r2cos() dd r = heliocentric distance BR = radial field = solar latitude = solar longitude +/2 2 -/2 0 “open” field lines
|BR| ecliptic d R |BRE| Earth Ulysses Balogh et al., 1995; Smith et al., 2001; Lockwood et al., 2000 Ulysses showed that everywhere |BR|(d/R)2 = |BRE| Thus total unsigned magnetic flux leaving the sun = 4R2 |BRE|
Geomagnetic reconstructionsLockwood et al., JGR, 2014. See also Svalgaard & Cliver, JGR, 2010
Relation of FS and VSW Lockwood & Owens, ApJ, 2014; Cliver & Ling, Sol Phys, 2011
Before 1845: FS from RSolanki et al., Nature, 2000; Owens & Crooker, JGR, 2006 • FScan be modelled as a continuity equation • dFS/dt = S – L FS • S ~ fCME ~ R
Loss of FSSheeley & Wang, ApJ, 2001; Owens et al., JGR, 2011
FS reconstructionOwens and Lockwood, JGR, 2012 FS source FS loss
FS reconstructionOwens & Lockwood, JGR, 2012; Lockwood & Owens, JGR, 2014 Post 1750
FS reconstruction (11-year)Owens & Lockwood, JGR, 2012; Lockwood & Owens, JGR, 2014 Post 1750
Modelling streamer belt widthSchwadron et al., ApJ, 2010; Lockwood et al., JGR 2014 • Separate streamer belt and coronal hole fluxes: • FS = FSB + FCHL = LSB + LCH • Assume: • New flux is injected into the streamer belt • Streamer belt flux eventually becomes coronal hole flux • Two coupled equations: • dFSB/dt= S - LSBFSB - SCH • dFCH/dt= SCH- LCHFCH • Streamer belt half width = sin-1 [1-FCH/FS]
Streamer belt widthOwens et al., JGR 2014. See also Manoharan, JGR, 2010 M. Druckmuller
Space weather“Great” geomagnetic storms, Greenwich observatory
Maunder minimum summary • “Extremely” low (long term) solar magnetic field, compared to sunspot era and the last 10,000 years • Increased occurrence of cold winters, but no “little ice age” • Reduced auroralfrequency, • Difficult to quantify if this was “extreme” • Polarity of the solar field continued to cycle • Coronal holes were “extremely” small and the streamer belt was “extremely” broad • Slow solar wind at Earth. • No/weak CIRs? • Continued CME activity?
PFSS solutionsMagnetic field polarity at coronal source surface
Three-dimensional structure of interplanetary magnetic fieldOwens et al., JGR, 2011
14C & 10Be: spallation products from O, N & Ar 10Be • 1/2 = 1.5×106 yr • < qG > = 0.018 atoms cm-2s-1 14C • 1/2 = 5370 yr • < qG> = 2 atoms cm-2s-1 GALACTIC COSMIC RAYS STRATOSPHERE (2/3) TROPOSPHERE (1/3) 14C+014C0 ; 14C0+0H14C02+ H ( ~1 year) ( ~1 week) OCEANS 10Be + AEROSOL BIOMASS ICE SHEETS
ERA-40 Analysis of DJF temperatures & circulation (difference of high and low tercile subsets) (Woollings et al, GRL.,2010; see also Barriopedro et al., JGR, 2008) ► sorted using open solar flux FS Low solar activity gives lower surface temperatures in central England Effect much stronger in central Europe Analysis shows a distinct system to NAO
Central England Temperature (CET) Winter Means (DJF) show upward drift (linear) rate of rise dTann/dt = 0.37 C c-1
Frost Fairs on the Thames e.g. Winter 1683/4. Painted by Dutch artist Thomas Wijk (1616-1677) N.B. notice how warm the next year was!
Frost Fairs on the Thames The last one was 1813/14. Painted by Luke Clenell(1781 – 1840 )
Thames Freezing Over N.B. in 1825 London Bridge demolished – acted as a salt water barrage plus embankment increased flow rate
Thames Freezing Over 1963 Thames at Windsor