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Extreme flash evaporation occurs when superheated liquid is sprayed into a low pressure zone.
For the low pressure zone, experiments with nitrogen, air and tetrafluoroethylene were carried out.
The pressure range in the low pressure zone was comprised between 0.05 and 1 bar.
The result shows that a low pressure zone is formed in the inner part of cyclone and causes an upward flow.
The climatic condition of the site is characterized by alternating wet and dry seasons and is bimodal, largely reflecting the annual movements across the country of an equatorial low pressure zone, caused by the convergence of dry northeasterly winds with moist winds of southwesterly origin (Erikson and Stern 1987, Zebene 1990).
The simulations show that a low pressure zone between the two polarizable conducting particles will be induced if the external electric field is applied parallel along the imaginary line connecting the two particles, resulting in an attracting effect between the two particles.
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This spatial structure, linked to the trajectories of the low pressure zones, seems to be the "normal" atmospheric situation of cold spring/summers during the 20th century.
Fluid motion forms vortices that alternate according to low pressure zones located around the object.
The monsoon air masses flow into that monsoonal low-pressure zone from a cell of high pressure just off the eastern coast of southern Africa.
The doldrums, therefore, do not exist in the western Pacific during northern summer because of the immense flow of maritime air into the Asian low-pressure zone.
During the northern winter, South and Southeast Asia are affected by northeasterly winds that blow from high-pressure areas of the North Pacific Ocean to the equatorial low-pressure zone.
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