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In [Braz. J. Phys. 30, 27 (2000)] Dickman et al. suggested thatself-organized criticality can be produced by coupling the activity of anabsorbing state model to a dissipation mechanism and adding an external drive.We analyzed the proposed mechanism in [Phys. Rev. E 73, 025106R (2006)] andfound that if this mechanism is at work, the finite-size scaling found inself-organized criticality will depend on the details of the implementation ofdissipation and driving. In the preceding comment [Phys. Rev. E XX, XXXX(2008)] Alava et al. show that one avalanche exponent in the AS approachbecomes independent of dissipation and driving. In our reply we clarify theirfindings and put them in the context of the original article.

Reply to "Comment on `Self-organized Criticality and Absorbing States: Lessons from the Ising Model'"