Abstract

Abstract We report on a Suzaku measurement of the shock feature associated with the western radio relic in the merging cluster A 3376. The temperature profile is characterized by an almost flat radial shape with $ kT$$ \sim$ 4 keV within 0.5$ \ r_{200}$ and a rise by about 1 keV inside the radio relic. Across the relic region (0.6–0.8$ \ r_{200}$ ), the temperature shows a remarkable drop from about 4.7 keV to 1.3 keV. This is clear evidence that the radio relic really corresponds to a shock front, possibly caused by a past major merger. The observed sharp changes of the temperature and electron density indicate the Mach number $ {\cal M}$$ \sim$ 3. The radial entropy profile is flatter than the prediction ($ r^{1.1}$ ) of numerical simulations within 0.5$ \ r_{200}$ , and becomes steeper around the relic region. These observed features and time-scale estimation consistently imply that the ICM around the radio relic has experienced a merger shock, and is in the middle of the process of dynamical and thermal relaxations.

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