Hot White Dwarfs

Abstract

Research on hot white dwarfs during the past 30 years has greatly expanded, as many new discoveries and the new questions they raise have emerged from increasingly larger, deeper surveys conducted with multimeter class ground-based telescopes, the International Ultraviolet Explorer (IUE), the Hubble Space Telescope (HST), the Extreme Ultraviolet Explorer (EUVE), and the Far Ultraviolet Spectroscopic Explorer (FUSE). This review will focus on white dwarfs ranging in temperature from 20 000 up to 200 000 K and higher, which are the hottest white dwarf stars known. Since the mid-twentieth century, the earliest spectroscopic surveys of white dwarf candidates from the proper motion selected samples of Willem Luyten and Henry Giclas were carried out by Jesse Greenstein, Olin Eggen, James Liebert, Richard Green, and others. The selection criteria employed in many of these surveys did not reveal a large number of hot white dwarfs because the surveys lacked ultraviolet sensitivity and also missed objects with low flux levels in the optical. Nevertheless, the earliest surveys quickly revealed that white dwarfs divide into two basic composition groups with hydrogen-rich (the DA stars) and heliumrich atmospheric compositions (the DB and other non-DA stars). The origin of this dichotomy still represents a major unsolved problem in stellar evolution, although theoretical advances in late stellar evolution made starting in the 1980s, as well as advances in modeling envelope physical processes and mass loss, have shed important new light on this puzzle (Chayer et al., 1995; Fontaine and Michaud, 1979; Iben, 1984; Iben et al., 1983; Schoenberner, 1983; Unglaub and Bues, 1998, 2000; Vauclair et al., 1979). The spectroscopic properties of white dwarfs are determined by a host of physical processes which control and/or modify the flow of elements and, hence, surface abundances in high gravity atmospheres: convective dredge-up, mixing and dilution, accretion of gas and dust from the interstellar medium and debris disks, gravitational and thermal diffusion, radiative forces, mass loss due to wind outflow and episodic mass ejection, late nuclear shell burning and late thermal pulses, ro-