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5) for the same model. Note that the corresponding distribution of current along the lightning channel is shown in Fig. 6 ms, λ p = 5000 m, n = 2). In Fig. 10a–d, fields contributed by each term of Eq. 5) are shown as well as the total field. It follows from Fig. 10 that at r = 50 m the contribution of the so-called electrostatic field component to the total field is dominant, at r = 5 km each of the three field components contributes significantly to the total field, and at r = 100 km the contribution of the radiation field component is dominant, as predicted by Eq.

Reproduction of lightning electromagnetic field waveforms by engineering model of return stroke. IEEE Trans. Electromagn. , 46:130–133. 20 Y. A. Rakov Baba, Y. and Rakov, V. A. (2007). Electromagnetic models of the lightning return stroke. J. Geophys. 1029/2006JD007222. , Anderson, R. , and Kroninger, H. (1975). Parameters of lightning flashes. Electra, 80:223–237. Cooray, V. (2003). On the concepts used in return stroke models applied in engineering practice. IEEE Trans. Electromagn. , 45:101–108.

102:6987–7006. Thottappillil, R. and Rakov, V. A. (2001). On different approaches to calculating lightning electric fields. J. Geophys. , 106:14191–14205, 2001. Uman, M. A. and McLain, D. K. (1969). Magnetic field of the lightning return stroke. J. Geophys. , 74:6899–6910. Uman, M. , Swanberg, C. , Tiller, J. , Lin, Y. , and Krider, E. P. (1976). Effects of 200 km propagation in Florida lightning return stroke electric fields. Radio Sci. 11: 985–990. Visacro, S. and Silveira, F. H. (2004). Evaluation of current distribution along the lightning discharge channel by a hybrid electromagnetic model, J.

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