The energy dependences of amplitude (top) and phase (bottom) of the first harmonics of the CRs anisotropy obtained in this work, and reported from previous measurements. They are underground muon observations: Norikura (1973; Sakakibara et al. 1973), Ottawa (1983; Bercovitch & Agrawal 1981), London (1983; Thambyahpillai 1983), Bolivia (1985; Swinson & Nagashima 1985), Budapest (1985; Swinson & Nagashima 1985), Hobart (1985; Swinson & Nagashima 1985), London (1985; Swinson & Nagashima 1985), Misato (1985; Swinson & Nagashima 1985), Socorro (1985; Swinson & Nagashima 1985), Yakutsk (1985; Swinson & Nagashima 1985), Banksan (1987; Andreyev et al. 1987), Hong Kong (1987; Lee & Ng 1987), Sakashita (1990; Ueno et al. 1990), Utah (1991; Cutler & Groom 1991), Liapootah (1995; Munakata et al. 1995), Matsushiro (1995; Mori et al. 1995), Poatina (1995; Fenton et al. 1995), Kamiokande (1997; Munakata et al. 1997), Marco (2003; Ambrosio et al. 2003), SuperKamiokande (2007; Guillian et al. 2007); and air shower array experiments: PeakMusala (1975; Gombosi et al. 1975), Baksan (1981; Alexeyenko et al. 1981), Norikura (1989; Nagashima et al. 1989), EAS-TOP (1995, 1996, 2009; Aglietta et al. 1995, 1996, 2009), Baksan (2009; Alekseenko et al. 2009), Milagro (2009; Abdo et al. 2009), IceCube (2010, 2012; Abbasi et al. 2010, 2012), Ice-Top (2013; Aartsen et al. 2013), ARGO-YBJ (2015; Bartoli et al. 2015), Tibet (2005, 2013; Amenomori et al. 2005b, 2013).