The new Sunspot Number A full recalibration Frédéric Clette World Data Center SILSO, Royal Observatory of Belgium L. Svalgaard Stanford University J.M.

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Presentation transcript:

The new Sunspot Number A full recalibration Frédéric Clette World Data Center SILSO, Royal Observatory of Belgium L. Svalgaard Stanford University J.M. Vaquero Universidad de Extremadura E.W. Cliver National Solar Observatory, Sunspot ROB STCE

Sunspot Number: definition Wolf Number (Wolf 1851) : W= 10 Ng + Ns ≠ Sunspot number: – Multiple stations – Statistical k personal scaling factors 18/11/201411th European Space Weather Week, Liège2 Wide range of applications: Constraint for solar dynamo models Quantitative reference for solar irradiance and solar wind reconstructions, cosmogenic isotopes, as timebase for Sun-driven processes Tracer of the long-term solar influences on Earth (climate change, atmospheric drag, cumulative GIC effects). Fröhlich & Lean 2004

Sunspot Number: a composite series Historical reconstruction ( ): Scale adjusted to Wolf’s observations Primary Wolf observations ( ): Standard 83mm refractor Small 37 and 43 mm travel telescopes Zürich period ( ): New counting method: 0.6 factor 1955: Zürich + Specola (Locarno) stations 18/11/201411th European Space Weather Week, Liège3

Sunspot Number: a composite series Historical reconstruction ( ): Scale adjusted to Wolf’s observations Primary Wolf observations ( ): Standard 83mm refractor Small 37 and 43 mm travel telescopes Zürich period ( ): New counting method: 0.6 factor 1955: Zürich + Specola (Locarno) stations Brussels period (1981-now): Statistics over worldwide network New pilot station: Specola (Locarno) 18/11/201411th European Space Weather Week, Liège4

Group sunspot number: a recent construction New larger data set back to 1610 (Hoyt & Schatten 1998) : Group counts only: – lower dependency on evolution of optical quality of telescopes (mainly before 19 th century) Built as a single series Commonly used for long-term reconstructions of solar irradiance and cosmogenic isotopes (e.g. Hathaway et al. 2002, Solanki and Krivova 2004, Wang et al. 2005, Krivova et al. 2007, Vieira et al. 2011, Shapiro et al and Owens and Lockwood 2012) Single non-visual scaling reference: RGO photographic catalogue 18/11/201411th European Space Weather Week, Liège5 Visual RGOSOON

SN and GN: major discrepancies 18/11/201411th European Space Weather Week, Liège6

Metrological approach SN treated like any absolute index (e.g. TSI): – Accuracy: based on a model of the measuring process Base data: – Exclusively direct sunspot counts (tables, drawings) – Original documents (metadata): Instrument and method descriptions Indications of changes – Re-counting (statistical tests, effect of a change of method) No use of any external calibration reference: – geomagnetic indices, cosmogenic isotopes: only indirect indices – Subject to additional disturbing factors (Earth magnetism, deposition processes) – Parallel data series are used only for final validation 18/11/201411th European Space Weather Week, Liège7

The « Greenwich » trend (GN) All values before 1880 are about 40% lower than the SN 18/11/201411th European Space Weather Week, Liège8 ~40%

The « Greenwich » trend (GN) Ratio of the RGO group count relative to parallel visual observers (Svalgaard 2012,Vaquero 2013) Ratio increases by ~40% from 1880 to 1915 Indications of changes in the early RGO data set (Willis et al, 2013) : – Photographic plate type – Measuring method 18/11/201411th European Space Weather Week, Liège9 Vaquero, SSN Workshop, 2013 Svalgaard, 2012 the R Z -R g discrepancy is due to an underestimate of R g before 1880

Group Number: a full reconstruction Same base visual data as Hoyt&Schatten before 20 th century Visual group counts for the 20 th century, instead of the RGO GN 18/11/201411th European Space Weather Week, Liège10 Backbone observerTime interval Staudach Schwabe Wolfer Koyama New cross-calibration strategy: long-duration “backbone” observers (Svalgaard 2013) – 4 sequences of simultaneous observers with mutual overlap

The 1947 « Waldmeier » jump (SN) Sharp jump around 1947 : ratio R g /R Z decreases by ~15-20% 18/11/201411th European Space Weather Week, Liège11 ~20%

The 1947 « Waldmeier » jump (SN) Jump in SSN confirmed by different cross-comparisons: – long-duration stations (e.g. Madrid) (Vaquero 2012) – Sunspot area (RGO) (Svalgaard 2012) No indications of changes in the RGO data around Change in the SSN scale typical amplitude 20% 18/11/201411th European Space Weather Week, Liège12 Vaquero, SSN Workshop, 2012 Svalgaard, SSN Workshop, 2012 Madrid SSN SSN - N G RGO sunspot area Svalgaard, 2012

The 1947 « Waldmeier » jump (SN) Sunspot weighting (introduced by M. Waldmeier around 1947): – Large spots with penumbrae counted as 2, 3, 4 or 5 according to size. Specola station (Locarno) trained to the method (1955): Still in use ! 18/11/201411th European Space Weather Week, Liège13 Blind test (2003 – 2014) : double counting by Marco Cagnotti – Mean ratio W w / W u = ~1.16 Lower proposed value of 1.11 (Lockwood et al. 2014) WwWw WuWu Svalgaard, = 3x3 6 =3x1+3

The 1947 « Waldmeier » jump (SN) The inflation factor depends on the activity level: – Locarno data – Range: w= 1.09 (minimum) to 1.20 (maximum SN=115) – Linear fit : w= R i / 1150 The time averaged ratio will depends on the amplitude of the cycles included in the average (for , w=1.20) 18/11/201411th European Space Weather Week, Liège14

The « Specola » drifts (SN) 18/11/201411th European Space Weather Week, Liège15 All raw observations are preserved in the SILSO database : – values Full recalculation in progress – Broad choice of possible alternate scaling references Drift of the main Specola observer versus the average of all long-duration stations in the SIDC- SILSO network: – Amplitude: 20% – Two reversals – Starts only in 1981 (end of the Zürich reference)

Boulder SN comparison: same trends 18/11/201411th European Space Weather Week, Liège16 D. Biesecker, 1 st SSN Workshop, 2011

SN : full recalculation 18/11/201411th European Space Weather Week, Liège17 First run: only single pilot stations with long duration > 25 years No more trend for all series: Only the orginal R i and the new Locarno-based SN deviate systematically in the same way All alternate station show temporary inhomogeneities Need to implement a multi-station reference (subset of core pilots stations) Powerful new tool to study and improve the SN calculation method For more details see poster 1 of this session

The GN scale is less reliable over : mixture of Wolf and rescaled Schwabe values (Wolf, 1861, 1862, 1863) used as Wolf’s data with k=1 (Hoyt & Schatten 1994) – Amplitude of the 1849 jump is uncertain Correction possibly valid for , but the Schwabe scale increased over (Lenssu et al. 2013) – The correction for SN data before 1826 is lower than the 20% jump in 1849 The 1849 Schwabe-Wolf transition The Wolf correction (Lenssu et al. 2013) : SN should be reduced by 20% before /11/201411th European Space Weather Week, Liège18 Lenssu et al Misconception: Wolf’s 1.25 scale correction is not based on geomagnetic data !

Other investigated corrections Uncertainties in the early sunspot data: – The gap: « missing cycle 4» ? (Usoskin et al. 2001, 2009, Zolotova & Ponyavin 2011) – The gap (Usoskin 2003, Vaquero 2007, Vaquero & Trigo 2014) – Maunder Minimum: overestimated data coverage by H&S (Clette et al. 2014) Work still in progress 18/11/201411th European Space Weather Week, Liège19 Schwabe - Wolf RGO - SOON

Combining all main corrections: early preview aa 18/11/201411th European Space Weather Week, Liège20

Combining all main corrections: early preview aa 18/11/201411th European Space Weather Week, Liège21 Clette, Svalgaard, Vaquero, Cliver, 2014 Space Science Reviews, Aug. 2014, Springer Online First, 69 pages DOI /s Arxiv: Clette, Svalgaard, Vaquero, Cliver, 2014 Space Science Reviews, Aug. 2014, Springer Online First, 69 pages DOI /s Arxiv:

Combining all main corrections: early preview aa 18/11/201411th European Space Weather Week, Liège22 RGO trend SN weighting RGO/ SOON Specola drift Clette, Svalgaard, Vaquero, Cliver, 2014 Space Science Reviews, Aug. 2014, Springer Online First, 69 pages DOI /s Arxiv: Clette, Svalgaard, Vaquero, Cliver, 2014 Space Science Reviews, Aug. 2014, Springer Online First, 69 pages DOI /s Arxiv:

A variable number of spots/group Reconstructed GN series (SILSO, SONNE): Both indices R i and R g calculated from the same data set 18/11/201411th European Space Weather Week, Liège23 SONNE SN/GN Locarno SN/GN CycleNs/NgNorthSouthR i /R G NorthSouth Changing R i /R G ratio : – Stable over cycles 19 to 22 – Decline in cycle 23 and 24 Decrease of the average number of spots per group by ~30%

N S /N G increase for stronger cycles ? A full agreement between SN and GN cannot be expected SN and GN carry a different information about the solar dynamo A variable number of spots/group Apparent secular variations of the ratio SN/GN (Tlatov 2013) : Higher uncertainties in early data: – group and sunspot numbers based on different sets of observations. 18/11/201411th European Space Weather Week, Liège24 Tlatov 2013

Implications: long-term (preview) Corrected SN & GN series agree Secular trend is largely eliminated < 5% / century 18/11/201411th European Space Weather Week, Liège25 Trend +15%/centuryTrend +40%/century SN correction: SN /1.20 after 1947 GN correction: GN * 1.37 before 1880 Soon after the Maunder Minimum, solar activity was similar to present levels

Long-term integration: a moderate Modern Maximum ? Time-integrated responses to the solar input: – Cosmogenic isotopes: deposition processes (ice, sediments) – Earth climate: thermal inertia of oceans Gaussian running mean over 22 years (2 solar cycles): 18/11/201411th European Space Weather Week, Liège26 Original series Ratio Max cycles 3-19 = 1.27 Ratio 22-yr envelope = 1.30 Corrected series Ratio Max cycles 3-19 = 1.08 Ratio 22-yr envelope = 1.17 The clustering of high solar cycles reduces the time-integrated effects of the corrections by 50%

Conclusions and prospects Release of new SN and GN series in spring 2015: In preparation: – Uncertainties (error bars) – Implementation of a versioning system – New conventions: Removing the 0.6 Zürich factor Continuous mean SN values between 0 and 11 (no more 0-11 jump) Implications: – Variable number of spots per group (scale-dependant mechanism) – Limited rise of average solar activity since the Maunder minimum: – Reconstructions of the solar output need revision: e.g. concept of a Grand Maximum in the 20 th century is questioned (Solanki et al. 2004, Abreu et al. 2008, Usoskin et al. 2012, 2014) Full recalculation of the modern SN now started: – Improved method: composite multi-station reference (to be identified) – Powerful tool for assessing the role of various factors on the SN (statistics of k coefficients, group splitting, visual observer practices) 18/11/201411th European Space Weather Week, Liège27

For the latest information, please visit … 18/11/201411th European Space Weather Week, Liège28 Sunspot Number Workshops Historical Archive of Sunspot Observations

18/11/201411th European Space Weather Week, Liège29

Open solar flux from geomagnetic indices: latest update Similar conclusions: recent open magnetic field reconstructions show no clear trend over last 180 years (Lockwood, Living Reviews SP, 9/2013) 18/11/201411th European Space Weather Week, Liège30

Wolf’s different telescopes K coefficient for 37mm “Pariser” travel telescope = 1.5 (confirmed by current observations by Thomas Friedli, Wolf Gezelschaft, Zürich) 18/11/201411th European Space Weather Week, Liège31

The 1893 Wolf-Wolfer transition (SN) Simultaneous Wolf & Wolfer observations (17 years) Origin of the 0.6 = 1/1.667 Zürich factor applied to SN after 1892 Our determination (ratios of yearly means): / (agreement to better than 1%) Very robust scaling of the SN over the 1876 visual-to- photography transition in the H&S Group Number 18/11/201411th European Space Weather Week, Liège32

The RGO-SOON jump Reconstruction and extension of the Group Number R g up to 2012 (WDC – Sunspot database) Good overall match with R g from Hoyt & Schatten: ratio near 1.0 and constant except for Scale jump at the RGO- SOON transition in 1976 SOON GN 10% higher than the RGO GN (cf. Lockwood et al. 2014) 18/11/201411th European Space Weather Week, Liège33 Wauters & Clette, SSN Workshop 2013 R g Hoyt & Schatten Rg SILSO reconstruction Ratio R g (HS)/R g (SILSO)

The « Specola » drifts (SN) All k coefficients vs time before correction 18/11/201411th European Space Weather Week, Liège34

The « Specola » drifts (SN) After correction based on a multi-station average reference 18/11/201411th European Space Weather Week, Liège35

Implications: recent cycles 18/11/201411th European Space Weather Week, Liège36 Cycle 22 Slightly decreased (- 5 to10%) Maximum 22 second peak is higher, almost equal to first peak

Implications: recent cycles 18/11/201411th European Space Weather Week, Liège37 Cycle 23 Slightly increased (+ 5 to 10%) Maximum 23 second peak becomes higher than the first peak. Cycle 23 decline raised by about 20% New maximum in 2002 instead of 2000

Implications: recent cycles 18/11/201411th European Space Weather Week, Liège38 Better overall agreement Still significant disagreement during the decline of cycle 23 Return to a better match in cycle 24

Implications: recent cycles 18/11/201411th European Space Weather Week, Liège39 Cycle 24 Only slight increase (+ 3%)

Global scale-dependent decline True global change in sunspot properties Supported by parallel studies: – Scale-dependant small- spot deficit in cycle 23 (Lefèvre & Clette , Kilcik et al. 2011, Nagovitsyn 2012) – Global decline of core magnetic fields in sunspot umbrae (Livingston & Penn 2009, 2012; Penn & Livingston 2006): Stabilisation since /11/201411th European Space Weather Week, Liège40 Lefèvre & Clette 2011 F. Watson, NSO, 2014