Geomagnetic data in China at Zô-Sè and Tsingtao Magnetic Observatories

1947 ◽  
Vol 52 (3) ◽  
pp. 398
Author(s):  
M. Burgaud
2019 ◽  
Vol 43 (6) ◽  
pp. 1053-1063 ◽  
Author(s):  
G.R. Vorobeva

Monitoring of geomagnetic field parameters and its variations is mainly carried out using ground-based magnetic observatories and variational stations. However, the imperfection of equipment used and the communication channels involved causes the presence of gaps in the time series of geomagnetic data, which, along with the spatial anisotropy of data sources, creates significant obstacles to their automated processing. In addition, the well-known methods for imputation of time series gaps provide the root-mean-square recovery error significantly exceeding the level acceptable for geophysical observations. Thus, the paper proposes a method for recovering geomagnetic data based on statistical methods for processing time series and machine learning principles using marked data and characterized by the fact that a pair of the time series fragments preceding and succeeding a missing fragment provide an indicative description of the time series fragment of interest, which together form a training sample to search for the missing fragment by a set of its attributes, followed by linear scaling to restore the original trend of an information signal. Analytical estimates of parameters of geomagnetic data time series are given, under which it is possible to apply the proposed method to recover both daily variations and several-minutes-long fragments.


1995 ◽  
Vol 38 (3-4) ◽  
Author(s):  
L. Cafarella ◽  
A. Meloni

The analysis of geomagnetic data from magnetic observatories demonstrated the existence of very rapid changes, or jerks, in the secular variation, especially the occurrence of the well known geomagnetic jerks of 1969 and 1978. A new geomagnetic jerk seems to have appeared around 1990 and is clearly visible at a selec- tion of European magnetic observatories as a rapid and sudden change in the secular variation pattern. The comparison between all day and quiet day means for two different observatories, respectively at high and middle latitude, suggests that this phenomenon, as stated by many authors for the other jerks, could be generated by an internal source.


2020 ◽  
Vol 44 (5) ◽  
pp. 782-790
Author(s):  
A.V. Vorobev ◽  
V.A. Pilipenko ◽  
T.A. Enikeev ◽  
G.R. Vorobeva

The paper is concerned with an approach to developing a specialized web-GIS based on a microservice architecture that provides analytical control of the disturbed component of geomagnetic field variations, according to observation data from magnetic observatories and variational stations published on the SuperMAG portal (http://supermag.jhuapl.edu/). A method of spatial interpolation of geomagnetic data implemented in the proposed web-GIS, together with the proposed scheme for ranking and interpreting them, as well as a visualization method in the form of isolines, allows a user to track the structure, observe the dynamics, identify probable regions, duration and time intervals of the occurrence of extreme geomagnetic disturbances.


Author(s):  
Daniel R. Franco ◽  
Gelvam A. Hartmann ◽  
Marcelo B. Bianchi ◽  
Ozana Hannesch ◽  
Ana Cristina de Oliveira Garcia ◽  
...  

1976 ◽  
Author(s):  
J.B. Townshend ◽  
J.E. Papp ◽  
M.J. Moorman ◽  
C.E. Deadmon ◽  
S.P. Tilton
Keyword(s):  

1980 ◽  
Author(s):  
John B. Townshend ◽  
J.E. Papp ◽  
E.A. Sauter ◽  
S.P. Tilton
Keyword(s):  

1988 ◽  
Author(s):  
John B. Townshend ◽  
R. V. O'Connell ◽  
L.Y. Torrence
Keyword(s):  

1988 ◽  
Author(s):  
John B. Townshend ◽  
R. V. O'Connell ◽  
L.Y. Torrence
Keyword(s):  

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