International audienceIn a previous paper, Khokhlov et al. introduced a method to test the compatibility of so-called `giant Gaussian process' (GGP) statistical models of the palaeomagnetic field against any palaeosecular variation database. This method did not take measurement errors into account. It therefore lacked practical usefulness. In the present paper, we remedy this and generalize the method to account for measurement errors in a way consistent with both the assumptions underlying the GGP approach and the nature of those errors. The method is implemented to test GGP models against any directional data set affected by Fisherian errors. Simulations show that the method can usefully discriminate which GGP model best explains a given ...
Summary. This paper presents three statistical methods for testing the reproducibility or compatibil...
© 2015, Pleiades Publishing, Ltd. The quadrature formula is obtained for the distribution function (...
Most applications of geomagnetism operate under the assumption that the time-averaged geomagnetic fi...
International audienceIn a previous paper, Khokhlov et al. introduced a method to test the compatibi...
International audienceRecent studies of the palaeomagnetic field behaviour over the past 5 Myr rely ...
International audienceWe introduce and apply the concept of 2-D probability uniformization to palaeo...
International audienceBy relying on two numerical dynamo simulations for which such investigations a...
© 2019, Pleiades Publishing, Ltd. Abstract: The consistency of the empirical data on the paleointens...
Statistical models of geomagnetic secular variations in terms of a Giant Gaussian Process (GGP) are ...
International audienceIn the present paper, we address symmetry issues in the context of the so-call...
A commonly used family of statistical magnetic field models is based on a giant Gaussian process (GG...
A commonly used family of statistical magnetic field models is based on a giant Gaussian process (GG...
The behaviour of the Earth's magnetic field, at the timescale of a polarity interval, can be represe...
In this study, we examine the role of palaeosecular variation (PSV) in the use of statistics for pa...
The Fisher distribution is central to palaeomagnetism but presents several problems when used to cha...
Summary. This paper presents three statistical methods for testing the reproducibility or compatibil...
© 2015, Pleiades Publishing, Ltd. The quadrature formula is obtained for the distribution function (...
Most applications of geomagnetism operate under the assumption that the time-averaged geomagnetic fi...
International audienceIn a previous paper, Khokhlov et al. introduced a method to test the compatibi...
International audienceRecent studies of the palaeomagnetic field behaviour over the past 5 Myr rely ...
International audienceWe introduce and apply the concept of 2-D probability uniformization to palaeo...
International audienceBy relying on two numerical dynamo simulations for which such investigations a...
© 2019, Pleiades Publishing, Ltd. Abstract: The consistency of the empirical data on the paleointens...
Statistical models of geomagnetic secular variations in terms of a Giant Gaussian Process (GGP) are ...
International audienceIn the present paper, we address symmetry issues in the context of the so-call...
A commonly used family of statistical magnetic field models is based on a giant Gaussian process (GG...
A commonly used family of statistical magnetic field models is based on a giant Gaussian process (GG...
The behaviour of the Earth's magnetic field, at the timescale of a polarity interval, can be represe...
In this study, we examine the role of palaeosecular variation (PSV) in the use of statistics for pa...
The Fisher distribution is central to palaeomagnetism but presents several problems when used to cha...
Summary. This paper presents three statistical methods for testing the reproducibility or compatibil...
© 2015, Pleiades Publishing, Ltd. The quadrature formula is obtained for the distribution function (...
Most applications of geomagnetism operate under the assumption that the time-averaged geomagnetic fi...