ALFVEN WAVE REFLECTION AND TURBULENT HEATING IN THE SOLAR WIND FROM 1 SOLAR RADIUS TO 1 AU: AN ANALYTICAL TREATMENT

被引:119
作者
Chandran, Benjamin D. G. [1 ]
Hollweg, Joseph V.
机构
[1] Univ New Hampshire, Ctr Space Sci, Durham, NH 03824 USA
基金
美国国家科学基金会;
关键词
MHD; solar wind; Sun: corona; turbulence; waves; INTERPLANETARY MEDIUM; MAGNETOHYDRODYNAMIC TURBULENCE; CORONAL HOLES; LOW-FREQUENCY; TRANSITION REGION; POWER SPECTRUM; CROSS HELICITY; FLUCTUATIONS; GENERATION; EVOLUTION;
D O I
10.1088/0004-637X/707/2/1659
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We study the propagation, reflection, and turbulent dissipation of Alfven waves in coronal holes and the solar wind. We start with the Heinemann-Olbert equations, which describe non-compressive magnetohydrodynamic fluctuations in an inhomogeneous medium with a background flow parallel to the background magnetic field. Following the approach of Dmitruk et al., we model the nonlinear terms in these equations using a simple phenomenology for the cascade and dissipation of wave energy and assume that there is much more energy in waves propagating away from the Sun than waves propagating toward the Sun. We then solve the equations analytically for waves with periods of hours and longer to obtain expressions for the wave amplitudes and turbulent heating rate as a function of heliocentric distance. We also develop a second approximate model that includes waves with periods of roughly one minute to one hour, which undergo less reflection than the longer-period waves, and compare our models to observations. Our models generalize the phenomenological model of Dmitruk et al. by accounting for the solar wind velocity, so that the turbulent heating rate can be evaluated from the coronal base out past the Alfven critical point-that is, throughout the region in which most of the heating and acceleration occurs. The simple analytical expressions that we obtain can be used to incorporate Alfven-wave reflection and turbulent heating into fluid models of the solar wind.
引用
收藏
页码:1659 / 1667
页数:9
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