Abstract
An interpretation of the ridge phenomenon found in collisions at 7 TeV is given in terms of enhancement of soft partons due to energy loss of semihard jets. A description of ridge formation in nuclear collisions can directly be extended to collisions since hydrodynamics is not used and azimuthal anisotropy is generated by semihard scattering. The observed ridge structure is then understood as a manifestation of soft-soft transverse correlation induced by semihard partons without long-range longitudinal correlation. Both the and multiplicity dependencies are well reproduced. Some predictions are made about other observables.
- Received 8 November 2010
DOI:https://doi.org/10.1103/PhysRevC.83.024911
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