Ana Lourenço, Gennady P. Marchenko, Manjunath Hegde, Jean-Marie Malherbe, Nuno Peixinho, Andrey Tlatov, Jan Klimeš, Yoichiro Hanaoka, Natalie A. Krivova, Viktor Korokhin, Marcel Belik, Dipankar P. K. Banerjee, Theodosios Chatzistergos, Teresa Barata, Ilaria Ermolli, R. Gafeira, Sami K. Solanki, Adriana Garcia, Takashi Sakurai, ITA, USA, GBR, FRA, DEU, European Commission, and Ministry of Education (South Korea)
Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited., Context. Studies of long-term solar activity and variability require knowledge of the past evolution of the solar surface magnetism. The archives of full-disc Ca II K observations that have been performed more or less regularly at various sites since 1892 can serve as an important source of such information. Aims. We derive the plage area evolution over the last 12 solar cycles by employing data from all Ca II K archives that are publicly available in digital form, including several as-yet-unexplored Ca II K archives. Methods. We analysed more than 290 000 full-disc Ca II K observations from 43 datasets spanning the period between 1892-2019. All images were consistently processed with an automatic procedure that performs the photometric calibration (if needed) and the limb-darkening compensation. The processing also accounts for artefacts affecting many of the images, including some very specific artefacts, such as bright arcs found in Kyoto and Yerkes data. Our employed methods have previously been tested and evaluated on synthetic data and found to be more accurate than other methods used in the literature to treat a subset of the data analysed here. Results. We produced a plage area time-series from each analysed dataset. We found that the differences between the plage areas derived from individual archives are mainly due to the differences in the central wavelength and the bandpass used to acquire the data at the various sites. We empirically cross-calibrated and combined the results obtained from each dataset to produce a composite series of plage areas. The 'backbone' approach was used to bridge the series together. We have also shown that the selection of the backbone series has little effect on the final composite of the plage area. We quantified the uncertainty of determining the plage areas with our processing due to shifts in the central wavelength and found it to be less than 0.01 in fraction of the solar disc for the average conditions found on historical data. We also found the variable seeing conditions during the observations to slightly increase the plage areas during the activity maxima. Conclusions. We provide the most complete so far time series of plage areas based on corrected and calibrated historical and modern Ca II K images. Consistent plage areas are now available on 88% of all days from 1892 onwards and on 98% from 1907 onwards. © T. Chatzistergos et al. 2020., The authors thank the observers at the Arcetri, Baikal, Big Bear, Brussels, Calern, Catania, Coimbra, Kanzelhohe, Kharkiv, Kenwood, Kislovodsk, Kodaikanal, Kyoto, Manila, Mauna Loa, McMathHulbert, Mees, Meudon, Mitaka, European Union's Horizon 2020 research and innovation program Mt Wilson, Pic du Midi, Rome, Sacramento Peak, San Fernando, Schauinsland, Teide, Upice, Valasske Mezi.ri.ci, Wendelstein, and Yerkes sites for all their work in carrying out the observing programs. We thank Isabelle Buale for all her e fforts to digitise the Meudon archive. We thank Je ff Kuhn and Cindy Maui for locating and sharing with us the Mees Ca II K data. We thank Satoru Ueno and Reizaburo Kitai for providing the Kyoto observations. We thank the anonymous referee for the constructive comments that improved this manuscript. We thank Ester Antonucci, Alexi Baker, Angie Cookson, Martina Exnerova, Bernhard Fleck, Detlef Groote, Laurent Koechlin, Libor Lenza, Mustapha Meftah, Werner Potzi, Roger Ulrich, John Varsik, and Hubertus Wohl for providing information about various Ca II K data. This work was supported by FP7 SOLID, and by the BK21 plus program through the National Research Foundation (NRF) funded by the Ministry of Education of Korea. This research has received funding from the European Union's Horizon 2020 research and innovation program under grant agreement No 824135 (SOLARNET). The Coimbra researchers thank the project ReNATURE (CENTRO-01-0145-FEDER-000007-BPD16). We acknowledge the "Observateurs associes" for their commitment to image acquisition and processing; IRAP for the instrumental and database management; Universite de Toulouse, CNRS, and Fiducial for the funding. We acknowledge Paris Observatory for the use of spectroheliograms and the Royal Observatory of Belgium, Brussels for USET data. The Kanzelhohe Ca II K data were provided by the Kanzelhohe Observatory, University of Graz, Austria. ChroTel is operated by the Kiepenheuer-Institute for Solar Physics in Freiburg, Germany, at the Spanish Observatorio del Teide, Tenerife, Canary Islands. The ChroTel filtergraph has been developed by the Kiepenheuer-Institute in cooperation with the High Altitude Observatory in Boulder, CO, USA. We acknowledge www.observethesun.com and www.solarstation.ru for storing the Kislovodsk data. This work used data provided by the MEDOC data and operations centre (CNES/CNRS/Univ. Paris-Sud). The Kenwood observations used here are from lantern slides in the Division of History of Science and Technology at Yale University's Peabody Museum of Natural History (objects YPM HST.340744, HST.340745, HST.340747, and HST.340752). The Yerkes observations are courtesy of the University of Chicago Photographic Archive, Special Collections Research Center, University of Chicago Library. This research has made use of NASA's Astrophysics Data System.