Abstract. Pulsed laser methods for OH generation and detection were used to study atmospheric degradation reactions for three important biogenic gases: OH + isoprene (Reaction R1), OH +α-pinene (Reaction R2) and OH + -3-carene (Reaction R3). Gas-phase rate coefficients were characterized by non-Arrhenius kinetics for all three reactions. For (R1), k 1 (241-356 K) = (1.93 ± 0.08) × 10 −11 exp{(466 ± 12)/T } cm 3 molecule −1 s −1 was determined, with a room temperature value of k 1 (297 K) = (9.3± 0.4) × 10 −11 cm 3 molecule −1 s −1 , independent of bath-gas pressure (5-200 Torr) and composition (M = N 2 or air). Accuracy and precision were enhanced by online optical monitoring of isoprene, with absolute concentrations obtained via an absorption cross section, σ isoprene = (1.28 ± 0.06) × 10 −17 cm 2 molecule −1 at λ = 184.95 nm, determined in this work. These results indicate that significant discrepancies between previous absolute and relative-rate determinations of k 1 result in part from σ values used to derive the isoprene concentration in high-precision absolute determinations.Similar methods were used to determine rate coefficients (in 10 −11 cm 3 molecule −1 s −1 ) for (R2)-(R3): k 2 (238-357 K) = (1.83 ± 0.04) × exp{(330 ± 6)/T } and k 3 (235-357 K) = (2.48±0.14)×exp{(357±17)/T }. This is the first temperature-dependent dataset for (R3) and enables the calculation of reliable atmospheric lifetimes with respect to OH removal for e.g. boreal forest springtime conditions. Room temperature values of k 2 (296 K) = (5.4 ± 0.2) × 10 −11 cm 3 molecule −1 s −1 and k 3 (297 K) = (8.1 ± 0.3) × 10 −11 cm 3 molecule −1 s −1 were independent of bathgas pressure (7-200 Torr, N 2 or air) and in good agreement with previously reported values. In the course of this work, 184.95 nm absorption cross sections were determined: σ = (1.54 ± 0.08) × 10 −17 cm 2 molecule −1 for α-pinene and (2.40 ± 0.12) × 10 −17 cm 2 molecule −1 for -3-carene.