Calibration of Sunspot Numbers

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Calibration of Sunspot Numbers Leif Svalgaard Stanford University leif@leif.org Eddy Symposium 22 Oct. 2010

Waldmeier s Description of What he Believed was the Counting Method Waldmeier, 1961 I believe (2) is incorrect, having read all Wolfer s [and Brunner s] papers and not found any such description. Waldmeier may have believed that the spots were weighted by size and carried that belief into his count.

Waldmeier s Own Description of his [?] Counting Method 1968 Can we see this in the Historical Record?

This is still the basis for the SSN 2010-8-27 2010-9-13 2010-4-22 2003-10-30 Group # weighted count Has been observing 50+ years Locarno is the Reference station for SIDC

Wolf s Discovery: rd = a + b R W. ry North X H Morning rd D Evening Y = H sin(d) East Y dy = H cos(d) dd For small dd A current system in the ionosphere is created and maintained by solar FUV radiation Wolf realized that this relation can be used to check the sunspot calibration

The clear solar cycle variation of ry 80 nt 70 Yearly Average Range ry PSM - VLJ - CLF 60 50 40 30 20 10 All mid-latitude stations show the same variation, responding to the same current system 0 1880 1890 1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000 2010 This was Wolf s justification for his calibration of the SSN

300 250 200 150 100 50 0 F10.7 y = 5.4187x - 129.93 R 2 = 0.9815 y = 0.043085x 2.060402 R 2 = 0.975948 30 35 40 45 50 55 60 65 70 ry Using ry from nine chains of stations we find that the correlation between F10.7 and ry is extremely good (more than 98% of the variation is accounted for) 250 200 Solar Activity From Diurnal Variation of Geomagnetic East Component F10.7 sfu Nine Station Chains F10.7 calc = 5.42 ry - 130 150 100 12 13 14 15 16 17 18 19 20 21 22 23 50 25+Residuals 0 1880 1890 1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000 2010 2020 This establishes that Wolf s procedure and calibration are physically sound

The diurnal range ry is thus an extremely good proxy for the F10.7 radio flux and [presumably] for solar activity in general 70 nt Stability of Amplitude of Diurnal Variation of East Component 60 50 40 30 20 HLS Helsinki Nine Station Chain NUR Nurmijarvi 10 0 Year 1840 1850 1860 1870 1880 1890 1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000 2010 Here is the response at Helsinki and at its replacement station Nurmijärvi Note, that activity in the 1840s-1870s was similar to that in the 1970s-2000s

The Waldmeier Discontinuity, I Waldmeier s counts are 22% higher than Wolfer and Brunner s, for the same amplitude of the Diurnal Geomagnetic Variation.

The Waldmeier Discontinuity, II

The Group Sunspot Number R G is derived from the RGO data after ~1874, so should show the same discontinuity, and it does: 2.0 1.8 1.6 1.4 1.2 1.0 0.8 0.6 0.4 0.2 0.0 Ratio RG/RZ (when RG,Z > 10) Wolf Wolfer Brunner Waldmeier SIDC 1740 1760 1780 1800 1820 1840 1860 1880 1900 1920 1940 1960 1980 2000 Note, that I plot the inverse ratio, thus R Z after 1945 is about 20% too high I ll come back to this discontinuity a bit later

The Waldmeier Discontinuity, III From ~40,000 CaK spectroheliograms from the 60-foot tower at Mount Wilson between 1915 and 1985 a daily index of the fractional area of the visible solar disk occupied by plages and active network has been constructed [Bertello et al., 2008]. Monthly averages of this index is strongly correlated with the sunspot number. The relationship is not linear, but can be represented by the following equation: R = [(CaK 0.002167)*8999] 1.29 using data from 1910-1945, i.e. the pre-waldmeier era. 300 R Calibration of Sunspot Number 250 RC = [(CaII-K - 0.002167)*8999] 1.29 200 Rz Wolfer-Brunner Rz Waldmeier Ri SIDC 150 100 50 0 1915 1920 1925 1930 1935 1940 1945 1950 1955 1960 1965 1970 1975 1980 1985 The SSN observed by Waldmeier is 20% higher than that calculated from CaK using the pre-waldmeier relation.

The Waldmeier Discontinuity, IV The value of the Ionospheric Critical Frequency fof2 depends strongly on solar activity. The slope of the correlation changed 20% between sunspot cycle 17 and 18 when Waldmeier took over.

If we accept the fidelity of the RGO sunspot observations [at least for a few decades around 1945] we must ascribe the artificial increase of Rz after 1945 to Waldmeier s inexperience [Friedli, 2005] as he struggled with learning how to construct the sunspot number [introducing the weights?]. Subsequent observers have strived to match Waldmeier, so in order to remove the 1945 discontinuity [and be consistent with modern counts] we must increase the pre-1945 Rz by ~20%: 200 180 160 140 Rz,i Rg < 1996 0.43*F Sunspot Number Series 120 100 80 60 40 20 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 1750 1770 1790 1810 1830 1850 1870 1890 1910 1930 1950 1970 1990 2010 This, of course, just makes the discrepancy with the Group Spot Number worse [<Rz> ~ 1.4 <Rg> before 1875].

Wolf himself was not afraid of such wholesale adjustments 1.8 1.6 1.4 1.2 1.0 0.8 0.6 0.4 0.2 0.0 25% Staudacher Evolution of Wolf Sunspot Numbers 2x W1857 / Rnow W1861 / Rnow W1875 / Rnow W1880 / Rnow 1740 1750 1760 1770 1780 1790 1800 1810 1820 1830 1840 1850 1860 1870 1880

Rudolf Wolf s Relative Sunspot Number values change over time Wolf started his own observations in 1849 Rudolf Wolf 1861 1837 111.0 Different! SIDC 2009 1837 138.3 25% higher

200 Sunspot Number Series 180 160 140 120 Wolf Group Eddy 100 80 60 40 20 1600 1650 1700 1750 1800 1850 1900 1950 2000 Even GSN has been adjusted 0

The Group Sunspot Number R G is derived from the RGO data after ~1874 2.0 1.8 1.6 1.4 1.2 1.0 0.8 0.6 0.4 0.2 0.0 Ratio RG/RZ (when RG,Z > 10) Wolf Wolfer Brunner Waldmeier SIDC 1740 1760 1780 1800 1820 1840 1860 1880 1900 1920 1940 1960 1980 2000 Note, that I plot the inverse ratio, thus R G before ~1880 is about 40% too low I m back at this discontinuity as promised

The Discontinuity in the 1880s between Group and Zurich Sunspot Numbers, I Adolf Schmidt [~1900] had analyzed the data for two intervals on either side of the start [1875] of the RGO sunspot observations for several stations and determined the diurnal ranges: obs name lat long interval WDC Washington D.C. 38.9 283.0 1840-1842 DUB Dublin 53.4 353.7 1840-1843 MNH Munchen 48.2 11.6 1841-1842 PGC Philadelphia 40.0 284.8 1840-1845 SPE St. Peterburg 60.0 30.3 1841-1845 GRW Greenwich 51.5 0.0 1841-1847 PRA Praha 50.1 14.4 1840-1849 HBT Hobarton -42.9 147.5 1841-1848 MAK Makerstoun 55.6 357.5 1843-1846 KRE Kremsmunster 48.1 14.1 1839-1850 TOR Toronto 43.7 280.6 1842-1848 WLH Wilhelmshaven 53.7 7.8 1883-1883 GRW Greenwich 51.5 0.0 1883-1889 WDC Washington D.C. 38.9 283.0 1891-1891 PSM Parc Saint-Maur 48.8 0.2 1883-1899 POT Potsdam 52.4 13.1 1890-1899 COP Kobenhavn 55.7 12.6 1892-1898 UTR Utrecht 52.1 5.1 1893-1898 IRT Irkutsk 52.3 104.3 1899-1899 -10 8 6 4 2 0-2 -4-6 -8-10 8 6 4 2 0-2 -4-6 -8 dd' 1957-1959 1964-1965 dd' 1840-1849 Diurnal Variation of Declination at Praha (Pruhonice) Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Diurnal Variation of Declination at Praha Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year rd

The Discontinuity in the 1880s between R G and R Z explained and resolved 80 70 60 50 40 30 20 10 80 70 60 50 40 30 20 10 0 <R > Sunspot Number as a Function of Diurnal Range Rz Rg after 1880 <ry > nt 25 30 35 40 45 50 55 <R > Sunspot Number as a Function of Diurnal Range Rz Rg after 1880 1.4*Rg before 1850 Rg before 1850 <ry > nt 25 30 35 40 45 50 55 For each station we now compute the average <Rz>, <Rg>, and diurnal range [converted to force units, nt, from arc minutes] and plot <Rz> against the range <ry> [blue diamonds, left]. You can see Wolf s linear relationship in action. For the eight stations with data after 1880, the <Rg>s are also plotted [pink dots] and they match the <Rz> points reasonably well. This is, however, not the case for the eleven stations from 1850 and before. Their <Rg> [red diamonds] lie well below the fitted line. To make them fit it suffices to multiply their values by 1.4 [giving red open diamonds]. 0

Waldmeier [1971] already noticed that the tight correlation between the solar microwave flux F10.7 and the sunspot number could be used as a calibration tool Waldmeier: As long as this relation holds, the Zürich series of sunspot-numbers may be considered to be homogeneous. If this relation should be subject to changes in the time to come, then the reduction factor used hitherto ought to be changed in such a way that the old R-F relation is reestablished

The change in relationship is perhaps clearer in monthly values 250 R 200 Sunspot Number vs. F10.7 Flux Monthly Averages y = -1.4940E-11x 6 + 1.6779E-08x 5-7.4743E-06x 4 + 1.7030E-03x 3-2.1083E-01x 2 + 1.4616E+01x - 4.1029E+02 R 2 = 0.9759 150 1951-1990 100 50 1996-2010 0 F10.7 sfu 0 50 100 150 200 250 300 We know that the F10.7 measurements themselves [which are absolute flux values] have not changed because of the agreement between Canadian [since 1947] and Japanese [since 1951] measurements.

Comparing Observed and Synthetic SSN from F10.7 2.0 1.8 1.6 1.4 1.2 1.0 0.8 0.6 0.4 0.2 0.0 Ratio Observed Sunspot Number to SSN from F10.7 Monthly Averages when SSN > 4 The growing discrepancy could be due to a drift in the SIDC calibration or to a real change in the Sun, or both! Waldmeier did not consider the possibility of a solar change 1950 1960 1970 1980 1990 2000 2010 Do we?

Some other organizations that have kept a keen eye on the Sun, making their own sunspot number series: ht t p: / / www. vds- sonne. de/ gem/ r es/ r esul t s. ht ml SIDC: Solar Influences Data Analysis Center, Brussels (International sunspot numbers) SONNE prov.: SONNE network, provisional sunspot numbers SONNE def. : SONNE network, definitive sunspot numbers AAVSO: American Association of Variable Star Observers - Solar Division AKS: Arbeitskreis Sonne des Kulturbundes e.v., Germany BAA: The British Astronomical Association - Solar Section, UK GFOES: G.F.O.E.S. Commission "Nombre de Wolf", France GSRSI: GruppoSole Ricerce Solari Italia, Italy OAA: The Oriental Astronomical Association - Solar Division, Japan RWG: Rudolf Wolf Gesellschaft - Solar Obs. Group of Swiss Astron. Society TOS: Towarzystwo Obserwatorow Slonca - Solar Observers Society, Poland VVS: Vereniging voor Sterrenkunde, Werkgroep Zon, Belgium

All these series can be successfully scaled to SIDC before ~2001 200 180 R SONNE AAVSO AKS BAA GFOES GSRSI OAA RWG TOS VVS 160 140 120 100 80 60 40 20 SIDC 0 1994 1996 1998 2000 2002 2004 2006 2008 2010 2012 But the same scaling relation yields a sunspot number after that time that is systematically 12% higher than SIDC s. Did all these organizations somehow change their procedures and/or observer cadre? Or did SIDC?

It seems that we increasingly see fewer spots for the same amount of microwave flux. We can quantify that by the ratio between observed spots and expected spots from the pre-1991 relationship: 2.0 1.8 1.6 1.4 Ratio of Observed Sunspot Number to Simulated SSN Monthly means when R>4 +12% correction 1.2 1.0 0.8? 0.6 0.4 0.2 Zurich SIDC 0.0 1945 1950 1955 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005 2010 2015 Adding 12% [assuming that SIDC has a problem from ~2001] does not materially alter this conclusion (red crosses).

Conclusions The current sunspot number is not correctly calibrated. SIDC undercounts since 2001 Waldmeier introduced an artificial upwards jump ~1945 The Group Sunspot Number is too low before ~1880. There is no long-term change in the SSN since 1700. No Modern Grand Maximum Sunspots are becoming harder to see and may become effectively invisible in a few years