Abstract
In return strokes, the parameters that can be measured are the channel base current and the return stroke speed. For this reason, many return stroke models have been developed with these two parameters, among others, as inputs. Here, we concentrate on the current propagation type engineering return stroke models where the return stroke is represented by a current pulse propagating upwards along the leader channel. In the current propagation type return stroke models, in addition to the channel base current and the return stroke speed, the way in which the return stroke current attenuates along the return stroke channel is specified as an input parameter. The goal of this paper is to show that, within the confines of current propagation type models, once the channel base current and the return stroke speed are known, the measured radiation field can be used to evaluate how the return stroke current attenuates along the channel. After giving the mathematics necessary for this inverse transformation, the procedure is illustrated by extracting the current attenuation curve from the typical wave shape of the return stroke current and from the distant radiation field of subsequent return strokes. The derived attenuation curve is used to evaluate both the subsequent and first return stroke electromagnetic fields at different distances. It is shown that all the experimentally observed features can be reproduced by the derived attenuation curve, except for the subsidiary peak and long zero-crossing times. In order to obtain electromagnetic fields of subsequent return strokes that are in agreement with measurements, one has to incorporate the current dispersion into the model. In the case of first return strokes, both current dispersion and reduction in return stroke speed with height are needed to obtain the desired features.
Highlights
Features of electromagnetic fields from lightning return strokes are needed at different distances in studies related to the interaction of these electromagnetic fields with both the Earth’s upper atmosphere and man-made electrical structures [1,2,3]
Our analysis shows that such an increase could generate an initial peak immediately after the return stroke, it cannot generate a broader subsidiary peak around 10–20 μs as in the measured radiation fields unless the return stroke speed starts to increase after the return stroke front has traveled a distance of around 1 km or so
Even though we have presented a typical set of parameters for the MTLD model that could be used in engineering applications, it is important to point out that MTLD model is a dynamic model with model parameters changing with the features of the radiation field and the channel base current
Summary
Features of electromagnetic fields from lightning return strokes are needed at different distances in studies related to the interaction of these electromagnetic fields with both the Earth’s upper atmosphere and man-made electrical structures [1,2,3]. These fields at different distances are important in understanding the way in which they are attenuated and dispersed as they propagate along rough and finitely conducting grounds [4,5,6]. Engineering models are the simplest, yet they are highly successful in predicting electromagnetic fields of return strokes at different distances from the lightning channel
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