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4. Discussion

Bearing in mind the observational proof for the oblate envelope of tex2html_wrap_inline1340 Cas we also examined elliptical gaussian models for interpreting our observed visibilities in natural light. The position angle of the major axis of this elliptical envelope was taken as tex2html_wrap_inline1342 to the East from the North according to Mark III observations (Quirrenbach et al. 1993). Our best fit leads to a major axis of tex2html_wrap_inline1344 mas and a flattening of tex2html_wrap_inline1346. Note that the gaussian model extent taken at 1 tex2html_wrap_inline1348 corresponds analytically to a smaller value than the uniform disk model diameter. The present major axes and flattening estimates are comparable to the results of the Mark III in Htex2html_wrap_inline1350, namely 3.2 mas and .72 for the major axis and the flatenning of tex2html_wrap_inline1352 Cas envelope. On the other hand, from a previous interferometric run on the GI2T Stee et al. reported that the continuum emission of the envelope must essentially originate within 3-4 stellar radii (Stee et al. 1995), a result also inferred from IR studies (Waters & Marlborough 1992). We find the continuum envelope twice as large as those estimates. The discrepancy might be explained by the fact that Stee et al. did not include the scattering of the photospheric light by the envelope for computing their continuum intensity map. This would mean that the free-free and free-bound emissions originate close to the central star whilst the scattering is chiefly produced in the outer regions of the envelope. In principle interfero-polarimetric observations should have confirmed this conclusion if higher accuracies than our upper limit of 1.3 to tex2html_wrap_inline1354/tex2html_wrap_inline1356 were obtained. One can reasonably speculate that improved interfero-polarimetry in the future should ultimately constrain the density and temperature distributions throughout the envelope among line-driven or rotationnally enhanced winds (Cassinelli & Hoffman 1975; Poeckert & Marlborough 1978).


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