Report On the Present State of Our Knowledge Respecting the General Circulation
Report On the Present State of Our Knowledge Respecting the General Circulation
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I cannot set out here, for want of space, the various theories which have been recently suggested to explain the general circulation of the Atmosphere theories generally incomplete and uncorroborated by observations. Most of them borrow their essential features from Ferrel. INFLUENCE or THE DISTRIBUTION OF TEMPERATURE ACCORDING TO LONGITUDE. For fifteen years I have endeavoured to separate the influence of the distribution of tempera- ture upon the general circulation, by adopting the following... line of thought. Having observed the well-known apparent relation of certain barometric maxima, of the small low temperature areas, as well as those of certain barometric minima with high temperature areas, I have tried to ascertain whether that is a general phenomenon ; and, when drawing the thermic isanomals (1879), and comparing them with Woeikoff's isobars, I was led to frame the following law : (1) When a region, of a certain extent, shows an excess of temperature, either absolute, or relative to the temperature of other points in the same latitude, there is a tendency to the formation of a minimum in that region, and almost precise coincidence between the barometric minimum and the maximum of temperature, and moreover there is a certain proportionality between them.
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To quickly assess the difficulty of the text, read a short excerpt:
I cannot set out here, for want of space, the various theories which have been recently suggested to explain the general circulation of the Atmosphere theories generally incomplete and uncorroborated by observations. Most of them borrow their essential features from Ferrel. INFLUENCE or THE DISTRIBUTION OF TEMPERATURE ACCORDING TO LONGITUDE. For fifteen years I have endeavoured to separate the influence of the distribution of tempera- ture upon the general circulation, by adopting the following... line of thought. Having observed the well-known apparent relation of certain barometric maxima, of the small low temperature areas, as well as those of certain barometric minima with high temperature areas, I have tried to ascertain whether that is a general phenomenon ; and, when drawing the thermic isanomals (1879), and comparing them with Woeikoff's isobars, I was led to frame the following law : (1) When a region, of a certain extent, shows an excess of temperature, either absolute, or relative to the temperature of other points in the same latitude, there is a tendency to the formation of a minimum in that region, and almost precise coincidence between the barometric minimum and the maximum of temperature, and moreover there is a certain proportionality between them.
What to read after Report On the Present State of Our Knowledge Respecting the General Circulation?
You can find similar books in the "Read Also" column, or choose other free books by Lon Philippe Teissserenc De Bort to read onlineMoreLess
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