We consider rotating Rayleigh-Bénard convection of a fluid with a Prandtl number of Pr = 0.8 in a cylindrical cell with an aspect ratio Γ = 1/2. Direct numerical simulations were performed for the Rayleigh number range 10 5 Ra 10 9 and the inverse Rossby number range 0 1/Ro 20. We propose a method to capture regime transitions based on the decomposition of the velocity field into toroidal and poloidal parts. We identify four different regimes. First, a buoyancy dominated regime occurring as long as the toroidal energy e tor is not affected by rotation and remains equal to that in the non-rotating case, e 0 tor . Second, a rotation influenced regime, starting at rotation rates where e tor > e 0 tor and ending at a critical inverse Rossby number 1/Ro cr that is determined by the balance of the toroidal and poloidal energy, e tor = e pol . Third, a rotation dominated regime, where the toroidal energy e tor is larger than both, e pol and e 0 tor . Fourth, a geostrophic turbulence regime for high rotation rates where the toroidal energy drops below the value of nonrotating convection.