The Magnetic Storm of Sept 25 1909
The Magnetic Storm of Sept 25 1909
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6 TABLE XVIII.
Sept. 28— 29th Midnight.
^X dY dZ Tokio —56. 0 + 4. 5 —25.
Berlin —41. +10. 0 +35.
Baldwin —50. 5 —10. 7 + 17.
TABLE XIX Sept. 30th 2^ a. M.
dX dY dZ Tokio —29. 0 — 9. 5 —28.
Berlin —28. +6. 0 +38.
Baldwin —31. 4 —8. 4 +26.
From the values in these tables, the most probable num- bers for dX\ dY and dZ' have been calculated for each of the four points of time and are compared in the follow- ing table.
TABLE XX.
dX' dY' dZ' Sept. 26th Noon —109. — 1. 9 —10. 5 » 27th Noon — 72. 8 — ...5. 0 — 3. 5 > 28-29th Midn. ... — 44. 0 + 8. 7 —15. 6 » 30th 2^ a. M. .... — 10. 9 — 6. 6 + 8. 0 57 For a more detailed analysis of the course of the storm, it would have been advantageous if Glauss' method, enlarged by Ad. Schmidt^), could have been used. The superposed, accidental field during the storm would then have been able to be divided up into 3 parts, as Schmidt does with the normal terrestrial magnetism, viz.
1) the part of the field, caused by electrical currents or magnets outside the earth.
What to read after The Magnetic Storm of Sept 25 1909?
You can find similar books in the "Read Also" column, or choose other free books by David Stenquist to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
6 TABLE XVIII.
Sept. 28— 29th Midnight.
^X dY dZ Tokio —56. 0 + 4. 5 —25.
Berlin —41. +10. 0 +35.
Baldwin —50. 5 —10. 7 + 17.
TABLE XIX Sept. 30th 2^ a. M.
dX dY dZ Tokio —29. 0 — 9. 5 —28.
Berlin —28. +6. 0 +38.
Baldwin —31. 4 —8. 4 +26.
From the values in these tables, the most probable num- bers for dX\ dY and dZ' have been calculated for each of the four points of time and are compared in the follow- ing table.
TABLE XX.
dX' dY' dZ' Sept. 26th Noon —109. — 1. 9 —10. 5 » 27th Noon — 72. 8 — ...5. 0 — 3. 5 > 28-29th Midn. ... — 44. 0 + 8. 7 —15. 6 » 30th 2^ a. M. .... — 10. 9 — 6. 6 + 8. 0 57 For a more detailed analysis of the course of the storm, it would have been advantageous if Glauss' method, enlarged by Ad. Schmidt^), could have been used. The superposed, accidental field during the storm would then have been able to be divided up into 3 parts, as Schmidt does with the normal terrestrial magnetism, viz.
1) the part of the field, caused by electrical currents or magnets outside the earth.
What to read after The Magnetic Storm of Sept 25 1909?
You can find similar books in the "Read Also" column, or choose other free books by David Stenquist to read onlineMoreLess
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