Researches On the Height Variation of the Atmospheric Electric Potential Gradien
Researches On the Height Variation of the Atmospheric Electric Potential Gradien
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In the highest wind velocity groups there occur certain irregularities in the mean values of the potential gradients and their differences, which to a certain extent finds an explanation in the effect of whirling of sohd particles.
In order to investigate more closely the connection between wind velocity and potential gi-adient a calculation was made, firstly of wind velocity groups and average potential gradients for the different seasons, table 17, and secondly of the corresponding values for... city grinds and country winds, tab. 18. I have namely presumed that the city, with its fireplaces will cause a large excess of heavy ions, which might considerably influence the result of the observations. As city winds were counted NNE, NE, ENE, E, ESE, SE and as country winds SSW, SW, WSW, W, WNW, NW.
According to table 17 the highest values of the potential gradients of winter are to be found in the lowest wind velocity classes, as well as the abnormally high values of d'^v^. The explanation of this fact is, as already has been men- tioned, partially an increase of the ion absorption, occuring in calm weather.
What to read after Researches On the Height Variation of the Atmospheric Electric Potential Gradien?
You can find similar books in the "Read Also" column, or choose other free books by Harald Norinder to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
In the highest wind velocity groups there occur certain irregularities in the mean values of the potential gradients and their differences, which to a certain extent finds an explanation in the effect of whirling of sohd particles.
In order to investigate more closely the connection between wind velocity and potential gi-adient a calculation was made, firstly of wind velocity groups and average potential gradients for the different seasons, table 17, and secondly of the corresponding values for... city grinds and country winds, tab. 18. I have namely presumed that the city, with its fireplaces will cause a large excess of heavy ions, which might considerably influence the result of the observations. As city winds were counted NNE, NE, ENE, E, ESE, SE and as country winds SSW, SW, WSW, W, WNW, NW.
According to table 17 the highest values of the potential gradients of winter are to be found in the lowest wind velocity classes, as well as the abnormally high values of d'^v^. The explanation of this fact is, as already has been men- tioned, partially an increase of the ion absorption, occuring in calm weather.
What to read after Researches On the Height Variation of the Atmospheric Electric Potential Gradien?
You can find similar books in the "Read Also" column, or choose other free books by Harald Norinder to read onlineMoreLess
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