“…Both lines have thus been used intensively for studies of the chromosphere, where useful spectral lines are scarce. Ground-based observations are mainly limited to Ca ii H and K (e.g., Jensen & Orrall 1963;Beckers 1968;Liu 1974;Teplitskaia & Firstova 1976;Cram & Dame 1983;Rutten & Uitenbroek 1991;Lites et al 1999;Rezaei et al 2007;Beck et al 2008b;, Hα (e.g., Bray 1973;Schmieder et al 1984;Tsiropoula et al 1993;Balasubramaniam et al 2004;López Ariste et al 2005;Sánchez-Andrade Nuño et al 2008;Cauzzi et al 2009;Bostancı 2011), the Ca ii IR triplet (e.g., López Socas-Navarro 2005;Pietarila et al 2007b;Cauzzi et al 2008a;Vecchio et al 2009), and He i at 1083 nm (Lites 1986;Rüedi et al 1995;Socas-Navarro & Elmore 2005;Sánchez-Andrade Nuño et al 2007;Kuckein et al 2009;Felipe et al 2010) by the absorption in the Earth's atmosphere, whereas from space also Mg ii h and k, Lα, and other lines in the extreme UV are accessible (e.g., Kneer et al 1981;Bonnet 1981;Fontenla et al 1988;Curdt et al 2010) 1 .…”