Studies On the Meteorological Effects in the United States of the Solar And Terr
Studies On the Meteorological Effects in the United States of the Solar And Terr
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3; and on fig. 21, 20. 2 forms the cusps to 20. 1.
By referring to Maxwell's Electricity and Magnetism, Volume I, Plate III, an analogue to this typical construction in electro- statics is to be found; his Plate I is an analogue to a cyclone in relation to the general circulation around the pole, and Plate II is an analogue to an anticyclone. These figures are con- structed by the precepts on page 169, so that the resulting isobar is by analogy B= B^ + E v where B t refers to the gen- eral isob...ars and B 2 to the local isobars. In the electrostatic analogue the potential is found by the law V=, where the successive values 1, 2, 3 are assigned to V, and r is computed from a given value of e. In the case of the isobars, the dif- ferences are nearly equal to each other in the general system, and in the local system the gradients may be taken, for example, about twice as great. Specifically, on the normal charts the pressure difference is O = 0. 1 inch for about one and three-fifths degrees in latitude, or 180, 000 meters, or 112 miles.
What to read after Studies On the Meteorological Effects in the United States of the Solar And Terr?
You can find similar books in the "Read Also" column, or choose other free books by Frank H Frank Hagar Bigelow to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
3; and on fig. 21, 20. 2 forms the cusps to 20. 1.
By referring to Maxwell's Electricity and Magnetism, Volume I, Plate III, an analogue to this typical construction in electro- statics is to be found; his Plate I is an analogue to a cyclone in relation to the general circulation around the pole, and Plate II is an analogue to an anticyclone. These figures are con- structed by the precepts on page 169, so that the resulting isobar is by analogy B= B^ + E v where B t refers to the gen- eral isob...ars and B 2 to the local isobars. In the electrostatic analogue the potential is found by the law V=, where the successive values 1, 2, 3 are assigned to V, and r is computed from a given value of e. In the case of the isobars, the dif- ferences are nearly equal to each other in the general system, and in the local system the gradients may be taken, for example, about twice as great. Specifically, on the normal charts the pressure difference is O = 0. 1 inch for about one and three-fifths degrees in latitude, or 180, 000 meters, or 112 miles.
What to read after Studies On the Meteorological Effects in the United States of the Solar And Terr?
You can find similar books in the "Read Also" column, or choose other free books by Frank H Frank Hagar Bigelow to read onlineMoreLess
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