Examining Each individual sounding, major amounts of pink area are present, indicating which the environment around the night of May possibly 11, 1970, has loads of instability to operate with. This instability, coupled with the escalating dampness for the decrease stages, confluence and lifting of air alongside the dryline, as well as weak disturbance at five hundred mb, conspired jointly to generate a number of incredibly powerful thunderstorms throughout West Texas.
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The maps higher than are samples of maps meteorologists place collectively using the weather balloon info from May eleven, 1970. These maps are referred to as constant force maps for the reason that in place of measuring altitude in height, they evaluate it in pressure (recall that air results in being a lot less dense with altitude.
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The series of illustrations or photos display no radar echoes at six pm. The initial storm starts off off as a small radar echo south and southwest of Lubbock. After some time, this echo grows as it slowly but surely moves off for the north and east.
Whilst thunderstorms generally form alongside advancing drylines through the afternoon and can produce big hail and even tornadoes, thunderstorms that kind alongside retreating drylines are a lot less Regular, and only not often deliver tornadoes. That is thanks in part on the air turning out to be more secure (air temperature decreases much less speedily with top) as the air cools in the vicinity of the ground following the Sunshine sets.
This was evident with the Lubbock tornado, in which swaths of maximum problems ended up located straight away adjacent to areas of quite gentle harm, all throughout the tornado route itself (see the above mentioned aerial photograph).
Particularly, the two nearby radars detected a hook formed radar echo (generally known as a hook echo), which can be a characteristic that is usually produced by a rotating storm, and could be a signature related to the development or presence of the tornado.
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The more robust space of winds shaded in blue centered near Midland may also be a sign of the wave. Winds from the ambiance are produced by stress variances, which consequently are a result of temperature dissimilarities. Areas of larger winds at this altitude are sometimes due to sharp temperature contrasts. This Increased temperature contrasts ensures that there might be a pocket of cold air aloft (cold air aloft offers the Vitality for instability and raise).
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