Mo delling Variability in Hot- Winds

1

Stanley P.Owocki

Bartol Research Institute University of Delaware, Newark, DE 19716 USA

Abstract. I review 2-D hydro dynamical simulations of rotating hot-star winds with

azimuthal structure induced by mo dulation of the radiative driving force near the wind

base. As a rst step toward examining more realistic p erturbation mechanisms (e.g.,

nonradial pulsations, or magnetic elds), the driving mo dulation here is taken to arise

from bright and dark sp ots in the stellar photophere. These sp ots induce decreases or

increases in wind ow sp eed, and as the star rotates, spiral \Co-Rotating Interaction

Regions" (CIRs) form, much as in the solar wind, from from interaction b etween fast

and slow ow streams. A new feature unique to line-driven owisavelo city-gradient

kink that propagates inward from interaction fronts at a fast radiative-acoustic mo de

sp eed. The slowly evolving velo city plateaus that form b ehind suchkinksgiveriseto

absorption features with a slow apparent acceleration, muchlike the Discrete Absorp-

tion Comp onents (DACs) often observed in UV wind lines from hot-. In simulation

mo dels with base driving sinusoidal ly mo dulated b etween increases and decreases, there

arise alternating spiral streams of enhanced or decreased density, asso ciated resp ec-

tively with decreased or increase ow sp eeds. These sp eed variations have substantial

impact on the line pro le, and so these dynamical simulations are not as successful as

analogous kinematic mo dels of corotating density streams in repro ducing the \phase-

bowing" of p erio dic absorption mo dulations observed in the recent IUE `Mega' pro ject.

1 Intro duction

Several pap ers at this meeting (e.g. by Prinja, Kap er, Kaufer, Massa, and Wolf )

have summarized the extensive observational evidence for explicit variability,

cyclical or otherwise, in the winds from hot, luminous, early typ e (OB) stars. A

general challenge for theory is to understand the nature of the physical changes

and/or structures asso ciated with this variability.To b e visible as direct varia-

tions in line-pro les formed from globally integrated radiative ux, the asso ciated

ow structure must b e on a relatively large scale, on order the stellar radius. This

makes it unlikely that suchvariations could stem from pro cesses entirely intrin-

sic to the wind out ow, such as the inherent instability in the line-driving of the

wind to small-scale p erturbations (Rybicki 1987; Owocki, Castor, and Rybicki

1988; Owocki1994b). The dynamical evolution of such large-scale structure can

be simulated using the lo cal, computationally ecient, CAK/Sob olev expres-

sions for the line force (Castor, Abb ott, and Klein 1975; Sob olev 1960), making

it feasible to carry out multidimensional simulations of the wind structure re-

sulting from large-scale p erturbations from the underlying, rotating star.

In this review, I will fo cus on recent e orts to develop initial dynamical

mo dels for two distinct classes of suchvariability, namely the `classical' Discrete

2 Stanley P.Owocki

Absorption Components (DACs) and the more recently identi ed Periodic Ab-

sorption Modulations (PAMs) discovered in the IUE `Mega' pro ject (Massa et al.

1995). Unlike the quasi-episo dic, slowly evolving, net absorption enhancements

that characterize most DACs, the PAMs recur regularly at p erio ds a loworder

fraction of the rotation p erio d, include b oth reductions and enhancements of

absorption, and evolve relatively quickly over the line pro le. Indeed, in contrast

to the slow blueward evolution of DACs, the PAMs in one case (BO I star HD

64760) show a \phase-b owing" that re ects apparentredward as well as blue-

ward propagation (Owocki, Cranmer, & Fullerton 1995; ; Fullerton et al. 1997).

These distinct observational characteristics likely re ect di erences in the under-

lying p erturbation mechanisms, p erhaps, for example, with the more sto chastic

DACs b eing induced by magnetic activity, and the regular PAMs b eing initiated

by Non-Radial Pulsations (NRPs). But given the present uncertainty, the initial

simulations here simply induce wind variations rather arti cially, through direct

mo di cation of the radiative driving in the inner wind, much as might o ccur

from \sp ots" on the underlying star (Cranmer and Owocki 1996, hereafter CO).

I rst (x 2) describ e the e ect of isolated sp ots, b oth brighter and darker than

the ambiant photophere. As the star rotates, Co-rotating Interaction Regions

(CIRs) form along spiral patterns by collision b etween faster and slower wind

streams originating from di erent longitudes relative to the sp ot. These simula-

tions thus represent the rst dynamical test of the original prop osal by Mullan

(1984a,b; 1986) that the wind density enhancements in such CIRs could cause

the DACs. A central goal here is to determine whether key characteristics of ob-

served DACs, particularly their apparent slow acceleration, can b e repro duced

in synthetic line-pro les generated from dynamical mo dels with CIRs.

I also examine (x 3) the e ect of a sinusoidal modulation of the radiativedriv-

ing near the wind base, assuming a xed number (m = 4) no des around the star.

This is intended as a dynamical version of the simple kinematic picture prop osed

to explain the \phase b owing" of the PAMs in HD 64760 (Owocki, Cranmer, &

Fullerton 1995.) In this picture the PAMs arise from corotating streams of al-

ternating increased or decreased density, within the key simpli cation that the

velo city is xed to a sp eci c law, una ected by the density p erturbations. The

dynamical simulations here self-consistently include suchvelo cityvariations, and

so allow us to examine their e ect in the line-formation.

2 CIRs Induced by Isolated Sp ots

Let us rst review the CO simulations of wind structure induced by isolated

sp ots on a rotating hot-star. The aim is to mimicphysical pro cesses { e.g. mag-

netic eld, NRPs { that might increase or decrease the mass ux emerging from

some lo calized region of the star, and then study howsuchvariations are prop-

agated through the radiatively driven . To reduce the complexity

and computational costs, the simulations are con ned to 2-D variations in ra-

dius and azimuth (r , ) within the equatorial plane. The line-driving force is computed using the standard CAK/Sob olev formalism (Castor, Abb ott, Klein

Mo dellin g Variability in Hot-Star Winds 3

Fig. 1. Grayscale p olar plots showing the spatial dep endence of the deviations from

a steady mo del for a. density, b. radial velo city,c.azimuthal velo city, and d. Sob olev

optical depth.

1975; Sob olev 1960), mo di ed by the nite-disk correction factor for a spherical

out ow(Friend and Abb ott 1986; Pauldrach, Puls, and Kudritzki 1986). This

ignores the azimuthal force that should arise from sideview p ersp ectives of the

sp ot, and simply mo di es the radial force by a xed enhancement/reduction

factor determined by the relativeproximity to the sp ot.

The sp ot parameterization allows sp eci cation of b oth a longitudinal width

 and an amplitude A, with 1 0 for bright

sp ots. Of the mo dels listed in Table 1 of CO, I con ne attention here to the rst

o

two, for which  =20 and A = 0:5, representing a standard bright and dark

sp ot. The stellar parameters represent those for the canonical O-typ e sup ergiant

 , with a rotation sp eed V = 230 km/s, corresp onding to a rotation

rot

p erio d of P  4:2days. For convenience, let us assume two identical sp ots

p ositioned on opp osite hemispheres, allowing restriction of the computation to

o

an azimuth range of just 180 with p erio dic b oundary conditions.

For the bright sp ot case, gure 1 shows grayscale plots of the resulting density,

radial velo city, azimuthal velo city, and radial Sob olev optical depth, all relative

to values in the corresp onding steady, spherically symmetric, CAK wind mo del

without anyspot.Thespothereiscentered on the x-axis, at the origin the

spiral pattern of enhanced densitythatcharacterizes the resulting CIR. Note

that regions of enhanced density generally corresp ond to regions of lower radial

velo city. Because of the enhanced brightness over the sp ot, the wind driven from

there initially has a higher mass ux, and thus higher density. As the enhanced

brightness fades with increasing heightabove the sp ot, the higher densityofthis

4 Stanley P.Owocki

Fig. 2. left panels: Radial variation of velo city (upp er panel) and density (lower panel)

along selected, xed azimuthal angles in the bright sp ot mo del.

Fig. 3. right panels: Same as g. 2, but for the dark sp ot mo del.

material makes it harder to accelerate, re ecting the characteristic scaling of the

line-acceleration with the inverse of the density ,

 

1 @v

r

g  (1)

lines

 @r

where is the usual CAK exp onent. The lower velo city gradient @v =@ r asso-

r

ciated with the lower acceleration also contributes, through eq. (1), to a further

reduction in the acceleration. As the brings this higher-density,

lower-sp eed material into interaction with faster ambient wind originating away

from the sp ot, there results a sho ck compression of the gas into the dense spiral

stream that characterizes the CIR.

Though the general CIR formation here is analogous to that o ccuring in the

solar wind (Hundhausen 1972; Zirker 1977), there are imp ortant di erences. The

much higher density of hot-star winds makes radiative co oling very ecient, and

so the sho cks are e ectively isothermal. Unlike the nearly adiabatic sho cks in

the solar wind, whichhave a maximum compression ratio of four in the strong

sho ck limit, the density compression in such isothermal sho cks scales with the

square of the Machnumb er, and so can b e arbitarily large. Moreover, whereas

the nearly adiabatic sho cks of the solar wind propagate backward into the faster

wind at roughly a quarter of the sho ck sp eed, these isothermal sho cks remain in

close proximity to the compressed layer.

Mo dellin g Variability in Hot-Star Winds 5

Another signi cant di erence arises when we consider the nature of the pre-

shock ow. In ordinary gas-dynamics (or even MHD) sho cks, the presho ck ow

is assumed to b e completely una ected by the imp ending sho ck, simply b ecause

the sp eed of this material exceeds the sound sp eed (or in MHD, the fast-mo de

sp eed), preventing anyupwind information propagation that a disturbance lies

ahead. However, as rst shown by Abb ott (1980), the characteristic sp eeds c in



a line-driven ow are substantially mo di ed by the op eration of the line force,

given by

p

2 2

c = U=2  (U=2) + a ; (2)



where a is the ordinary (isothermal) sound sp eed, and U  @g =@ (@v =@ r )

lines r

is a new characteristic sp eed, nowadays often called the \Abb ott sp eed". From

eqn. (1) we ndU  g =(@v =@ r ), but from the radial equation of motion,

lines r

we exp ect v @v =@ r  g , which suggests U  v , i.e. this Abb ott wave sp eed is

r r r r

typically of order the radial ow sp eed. Since most the wind is sup ersonic, we

nd v  U  a, implying that inward wave propagation can now o ccur at a

r

sp eed c U v that is much faster than the propagation of an ordinary

r

sound wave (Owocki and Rybicki 1985, 1986; Rybicki, Owocki, & Castor 1990).

Figure 2 shows line plots of the radial variation of (a) velo city and (b) den-

sity along selected, xed azimuthal angles. The lo cation of the compressed CIR

is apparent from the velo cityminima and density maxima. But note that the

velo city has a decreasing outward gradientover a broad region ahead of this

CIR, extending backtoavelo city gradient discontinuity, or \kink", that marks

the connection to the unp erturb ed, outward-accelerating wind. This weak, kink

discontinuity propagates inward (relative to the wind out ow) at roughly the

characteristic sp eed c U , and since this is nearly as fast as the lo cal out-

ow sp eed, it has only a slow net outward propagation in the xed stellar frame.

Such fast inward-propagation of a velo city-gradientkinkisanovel and quite

unique feature of a line-driven ow, and it has p otentially imp ortant conse-

quences for interpreting observed line-pro le features, particularly DACs. To

identify which wind structures should yield the most prominent pro le varia-

tions, let us examine the radial Sob olev optical depth,

v (r;)

th

: (3)  (r;)=

r

j@v =@ r j

r

The line absorption co ecient  and the ion thermal sp eed v are assumed to

th

have the same, constantvalue in the p erturb ed and unp erturb ed wind. Thus

the variations in optical depth ratio plotted in gure 1d re ect changes in the

ratio of densityover velo city-gradient. Surprisingly,we see from comparison

with gure 1a that the regions of strongest optical depth enhancements do not

o ccur within the dense CIR compression, but rather within the shallowvelo city-

gradient region immediately after the kink.

The emergent ux line-pro les from this wind structure can b e readily syn-

thesized using the standard SEI (Sob olev source function with Exact Integration)

metho d of Lamers et al. (1987), generalized for 3-D integration as describ ed in

CO. For this purp ose, the 3-D latitudinal structure is derived byinterp olation

6 Stanley P.Owocki

Fig. 4. Line pro le variation for marginally thick line as a function velo city and time.

In the middle b ox, the solid line shows the unp erturb ed wind pro le, and the dashed

lines show the extrema for eachvelo city. The b ottom b oxshows the pro le standard

deviation.

from the equator to a p olar mo del characterized by a 1-D, unp erturb ed wind so-

lution. For a mo derate strength line that is marginally optically thickinthewind,

gure 4 shows a grayscale plot of the pro le variation as a function of frequency

(in velo city units) and time. The latter is derived from simple mapping of the

azimuthal co ordinate  using the star's rotation frequency ,i.e.t =(  )= ,

o

where  is de ned such that the observer is directly over the sp ot at the initial

o

time t =0.Following observational convention, the gray scale here is scaled to

the range from mininum to maximum ux at each frequency, with the maxi-

Mo dellin g Variability in Hot-Star Winds 7

Fig. 5. Apparent acceleraton vs. velo city for bright-sp ot mo del DAC, compared to

velo citylaws with various exp onents .

mum ux (i.e., minimum absorption) corresp onding to the lightest shade. This

convention is suitable for describing the observed DACs that represent mainly

enhanced absorption relative to the background wind. But the synthetic pro le

variations here also showintervals of reduced absorption, re ecting the relative

reduction of the density in the region just b eyond the CIR.

As noted ab ove, the absorption enhancements here arise primarily from re-

gions of shallowvelo city-gradient near the reverse mo de kinks. Because of the

slow net outward propagation of these kinks, the asso ciated synthetic DACs mi-

grate quite slow ly blueward across the pro le over roughly  3:9day, in general

agreement with the slow apparent acceleration of observed DACs. Often this

slow accleration is characterized in terms of large values of the exp onent in

the canonical velo citylawgiven by v (r )=v (1 R =r ) . Figure 5 plots the ap-

1 

parent acceleration vs. velo city for the synthetic DAC compared with results for

velo citylaws with various . Whereas an unp erturb ed wind is exp ected to have

avelo citylaw with  1, g. 4 shows that the DAC in this mo del corresp onds

more closely to higher exp onents  2 4, much as inferred for observed DACs.

Let us next brie y consider results for the case of a \dark" sp ot, wherein

the radiative driving is reduced at base of the wind out ow. In this case, the

mass ux emerging from the sp ot region is now reduced, and as the radiative

driving recovers at greater heights ab ove the sp ot, the reduced density causes an

enhanced acceleration, which then results in a very fast stream. Figure 3 shows

the radial variation of velo city and density at selected xed angles. Note the

velo cities ranging up to 5000 km/s, more than double the maximum sp eed in

8 Stanley P.Owocki

Optical Density Velocity Depth

-0.5 0.0 0.5 -40 -20 0 20 40 -1.0 -0.5 0.0 0.5 1.0

ρ ρ V-Vo (km/s) τ/τ -1

log [ / o] o

Fig. 6. Spatial variation of density,velo city and Sob olev optical depth, normalized

relative to the unp erturb ed mo del, for the case with m =4 sinusoidal mo dulation in

azimuth.

the unp erturb ed wind, and muchhigherthanisever observed in line-pro les of

such an O-sup ergiant. This implies that such reduced mass ux regions cannot b e

very prominent in hot-star winds. In particular, it argues against the imp ortance

of hot-star analogs of solar coronal holes (Zirker 1977), with very high-sp eed

wind streams arising from regions of rapidly diverging op en magnetic eld (cf.

MacGregor 1988).

3 Co-rotating Streams from Sinusoidal Mo dulations

An imp ortant result of the IUE 'Mega' campaign was the identi cation of the

clearly cyclical PAMs in wind line pro les of several stars. In the case of the

B0 I star HD 64760, these PAMs show a \phase-b owing" that suggests appar-

ent redward as well as blueward propagation. Owocki, Cranmer, and Fullerton

(1996) have shown that suchbowing can b e repro duced from a simple kinematic

mo del with co-rotating spiral streams of alternating regions of increased and re-

duced density. This kinematic mo del ignores any dynamical e ect these density

variations mighthave in inducing corresp onding velo citychanges. As an ini-

tial attempt to extend this kinematic picture into a dynamically self-consistent

mo del, let us next brie y consider the resp onse of a line-driven wind to a p er-

turbation that varies sinusoidal ly in azimuth b etween enhanced and reduced

radiative driving.

Figure 6 shows grescale plots of the changes in density,velo city, and Sob olev

o

optical depth for such a dynamical mo del with an azimuthal p erio d of 90 and

Mo dellin g Variability in Hot-Star Winds 9

Fig. 7. As in g. 4, but for the sinusoidal ly mo dulated mo del.

p erturbations amplitdue of A =0:5. Note that there are substantial e ects on the

velo cityaswell as density, and that the optical depth variations no longer just

follow the density,aswas assumed in the heuristic corotating stream mo del for

the observed phase-b owing. Figure 7 shows the quite complex pro le variability

for the line pro le of a mo deratel strong in this sinusoidal mo dulation mo del. The

complexity re ects the intricate interdep endence of owvariations in density,

velo city, and velo city gradient. The comparitively simple phase-b owing pattern

of the kinematic mo del is not apparent here. Indeed, it is not clear what sort of

dynamically consistent structure could give the observed phase-b owing.

10 Stanley P.Owocki

4 Concluding Remarks

The simulations here demonstrate that the physical dep endencies of line-driving

play an imp ortant role in the dynamical evolution of wind structure, and lead

to phenomena, e.g., the reverse-mo de kink, that have no analog in ordinary gas

dynamics. The inward propagation of this kink yield the slow net outward prop-

agation of a velo city plateau ow pattern that causes the enhanced absorption,

providing one p ossible explanation for the relatively slow apparent acceleration in

observed DACs. However, suchmodelstypically also predict line-pro le features

that not commonly seen, most notably reduced absorption comp onents. Thus,

an alternativemechanism for pro ducing slowDACs is a substantial increase,

i.e. factor of two or more, in the mass b eing ejected into the wind, without a

comp ensating increase in the driving. The acceleration of such material can b e

esp ecially slow, and so the extra absorption from its higher density could also

form slowly evolving DACs (Owocki, Fullerton, and Puls 1994).

As for the PAMs observed in the IUE mega pro ject, we nd that dynamical

mo dels with p erio dic mo dulation typically show substantial velo cityvariations

that complicate the line-pro le signature. In particular, the simple, phenomena-

logical, kinematic picture develop ed to explain phase b owing cannot b e easily

adapted to a fully self-consistent dynamical mo del.

The work describ ed here represents only the rst steps in trying to develop

dynamically self-consistent mo dels of the ow structure assoicated with the ob-

served variability of hot-star winds. In the future, mo dels should address more

directly the twomostobvious p ossible p erturbation mechanisms, namely non-

radial pulsations and surface magnetic elds, with particular emphasis on iden-

tifying observatonal characteristic that could help in distinguishing whichmech-

anism is most resp onsible for eachofvarious kinds of observed wind variability.

Within such studies, it will remain helpful to contrast the inferred owstruc-

tures with those derived for the sun and other co ol stars, and in particular to

identify whichcharacteristics are p eculiar to the dynamics of radiative driving

by line-scattering. The cyclical variability of hot-stars thus provides an unique

p otential for studying this imp ortant asp ect of radiation hydro dynamics.

Acknowledgements: This work was supp orted in part by NASA grant

NAGW-2624. Supp orting computations were carried out using an allo cation of

sup ercomputer time from the San Diego Sup ercomputer Center. Muchofthe

research reviewed here was carried out in collab oration with S. Cranmer, as part

of his Ph. D. thesis. I also acknowledge numerous helpful discussions with A.

Fullerton, K. Gayley, H. Henrichs, L. Kap er, and J. Puls.

Mo dellin g Variability in Hot-Star Winds 11

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Henrichs: We, as observers, would like to thank you very muchforthesomany

of fundamental calculations you did, that help ed enormously to interpret

the data on stellar wind variability.You showed even an example that is far

ahead of any observations I have seen so far. For obvious reasons you put your

p erturbing sp ot on the stellar equator, but in practice such a sp ot is most likely

at higher latitude. Would that not change the predicted b ehavior drastically?

Could you comment?

Owocki: Perturbations away from the equator obviously require a 3-D simula-

tion, which with mo dern computers is readily doable, though not yet attempted.

In the context of CIRs in the solar wind, V. Pizzo in the 1970's already devel-

op ed 3-D mo dels, showing some interesting new e ects not p ossible in 2-D, e.g.

ow around the CIR at other latitudes. In rapidly rotating hot stars, an addi-

tional e ect may b e de ection toward or away from the equator. This remains

a problem to b e investigated.