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Atmospheric Electric Potential Gradient at Bangalore, {Plate XXkX) 1, Introduction, The determination of the Electric data of the atmosphere has passed into the ordin~ry mutine of the most important observatories in Europe and other parts of the civilised world. In India, a consistent and continuous aeries of obsemationa has not been made. G. C. Simpson published the results of observations at Sinla covering a period December 1908- May 1910.' Only relative values are given, as it was not found feasible to obtain the factor of reduction to IeveE. No other atation appears to have taken up this work ayetematic- ally since? One of the difficulties whioh sema to have discouraged nome obmrvera is the difficulty of preserving insulation, especially during the extremely humid months of the South-West Monsoon, It was therefore thought desir- abIe to obtain reaults continuously over a fairly long perid &t Bangalore. I Memoire of the Indiuu Meteorological Department, Vol, XPf, Pt. VI. R~oently obaerrrtion# hsve bean atartad at tho Colebp Obssnatq, Eombrp.

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Page 1: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording

Atmospheric Electric Potential Gradient at Bangalore,

{Plate XXkX)

1, Introduction,

The determination of the Electric data of the atmosphere has passed into the ordin~ry mutine of the most important observatories in Europe and other parts of the civilised world. In India, a consistent and continuous aeries of obsemationa has not been made. G. C. Simpson published the results of observations at Sinla covering a period December 1908- May 1910.' Only relative values are given, as it was not found feasible to obtain the factor of reduction t o IeveE. No other atation appears to have taken up this work ayetematic- ally since? One of the difficulties whioh s e m a to have discouraged nome obmrvera is the difficulty of preserving insulation, especially during the extremely humid months of the South-West Monsoon, It was therefore thought desir- abIe to obtain reaults continuously over a fairly long perid &t Bangalore.

I Memoire of the Indiuu Meteorological Department, Vol, XPf, Pt. VI. R~oently obaerrrtion# hsve bean atartad at tho Colebp Obssnatq , Eombrp.

Page 2: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording
Page 3: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording
Page 4: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording
Page 5: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording
Page 6: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording
Page 7: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording
Page 8: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording
Page 9: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording
Page 10: Atmospheric Electric Potential Gradient Bangalore,core.ac.uk/download/pdf/49287221.pdf · the potential gradient on the level, simultaneous observations were made with the recording
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