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We present direct ground based observations of the plasma flow sunward and tailward of the nucleus of comet P/Swift-Tuttle. The observations are long-slit high resolution spectra of the H2O+ emission centered at 6199Å with a velocity resolution of about 7 km s−1 (FWHM) and a spatial resolution of about 104 km at the comet. Emission is visible from just inside the predicted position of the cometopause on the sunward side of the nucleus out to 5×105 km on the tailward side. The deceleration of the solar plasma on the sunward side is clearly observed as is the acceleration of cometary ions into the tail. These observations show the effectiveness of ground based methods for the systematic study of cometary plasmas and point to the need for a better theoretical understanding of their acceleration mechanisms.