Meteorology And Aeronautics
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Such an air mass may, of course, be resting on the earth's surface. This air mass in motion over the earth's surface, or over an "aerial bottom," will tend to conform with the "bottom" over which it flows.
If the bottom or supporting surface be of irregular contour, like the earth's surface, this tendency to conform with it will result in aperiodically alternating expansion and contraction of the air in Suestion, with attendant changes in temperature, pressure, and motion, onvective units of th...is type are called gusts and the wind in which they occur carries them for some distance beyond the irregularity in the bottom which caused them. If this bottom be the solid earth, there is no response by the rigid earth to the traveling gust, which ceases to exist as originally formed. Either equilibrium will be restored in uninterrupted flow over level surface or other irregu- larities in the bottom will superpose new gusts.
If the bottom or supporting surface be aerial and the irregularities in its contour be in the nature of pressure variations originating in the lower stratum, there will be reaction in the lower stratum to the gust initially caused by it in the upper stratum.
What to read after Meteorology And Aeronautics?
You can find similar books in the "Read Also" column, or choose other free books by United States. National Advisory Committee for Aeronautics to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Such an air mass may, of course, be resting on the earth's surface. This air mass in motion over the earth's surface, or over an "aerial bottom," will tend to conform with the "bottom" over which it flows.
If the bottom or supporting surface be of irregular contour, like the earth's surface, this tendency to conform with it will result in aperiodically alternating expansion and contraction of the air in Suestion, with attendant changes in temperature, pressure, and motion, onvective units of th...is type are called gusts and the wind in which they occur carries them for some distance beyond the irregularity in the bottom which caused them. If this bottom be the solid earth, there is no response by the rigid earth to the traveling gust, which ceases to exist as originally formed. Either equilibrium will be restored in uninterrupted flow over level surface or other irregu- larities in the bottom will superpose new gusts.
If the bottom or supporting surface be aerial and the irregularities in its contour be in the nature of pressure variations originating in the lower stratum, there will be reaction in the lower stratum to the gust initially caused by it in the upper stratum.
What to read after Meteorology And Aeronautics?
You can find similar books in the "Read Also" column, or choose other free books by United States. National Advisory Committee for Aeronautics to read onlineMoreLess
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