Observations reveal cloud lines linked to meteorological interactions in the atmosphere, suggesting new atmospheric phenomena.
Shortly before sunset on 10 November 1983, two spectacular low cloud lines were observed and photographed from a CSIRO research vessel about 50 km offshore, northwest of Port Hedlund in Western Australia. These clouds were similar in ap-pearance to the well-known 'morning glory' cloud lines of the Gulf of Carpentaria region. They were orientated approximately east-west and moved from the south at an estimated speed of close to 10 m s-1. An analysis of available meteorological data suggests that the clouds were associated with a bore-like disturbance which was gener-ated by the interaction of a thunderstorm gust front with the sea breeze front and which propagated on a waveguide provided by the low-level stable layer capped by a deeper adiabatic layer.
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Roger K. Smith (1986) studied this question.
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