Mathematical tools are needed to screen out sites where Joule Thomson cooling is a prohibitive factor for CO 2 geosequestration and to design approaches to mitigate the effect. In this paper, a simple analytical solution is developed by invoking steady-state flow and constant thermophysical properties. The analytical solution allows fast evaluation of spatiotemporal temperature fields, resulting from constant-rate CO 2 injection. The applicability of the analytical solution is demonstrated by comparison with non-isothermal simulation results from the reservoir simulator TOUGH2. Analysis confirms that for an injection rate of 3 kgs−1 (0.1MTyr−1) into moderately warm(>40°C) and permeable formations(>10 −14 m 2 (10 mD)), JTC is unlikely to be a problem for initial reservoir pressures as low as2 MPa (290 psi).