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- W2130621728 abstract "Two rubidium narrow line magnetometers were operated in a differential mode along a 12-km base line near Boulder, Colorado, and the total field gradient measured to high accuracy. A number of runs of difference field were made from March through September of 1974. The results showed that daily averages were generally constant to within ±0.1 γ during quiet or disturbed periods with the exception of a few days in late August and early September. The agreement is excellent between the observed difference field and a difference field calculated from the measured east-west field Y and a transfer function appropriate to a local conductivity anomaly. Accounting for the effect of the anomaly typically permits a reduction of a factor of 3 in the standard deviation of the daily average; on very disturbed days a reduction of a factor of 5 in gradiometer noise was achieved. For periods of more than several days the corrections for anomaly edge effects are comparatively small." @default.
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- W2130621728 date "1976-12-10" @default.
- W2130621728 modified "2023-10-08" @default.
- W2130621728 title "Geomagnetic field gradient measurements and noise reduction techniques in Colorado" @default.
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- W2130621728 doi "https://doi.org/10.1029/jb081i035p06276" @default.
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