2016
DOI: 10.1016/j.spasta.2015.12.003
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Universal Kriging of functional data: Trace-variography vs cross-variography? Application to gas forecasting in unconventional shales

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Cited by 25 publications
(12 citation statements)
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“…This was expected since the boundaries between areas cannot be entirely steady. Considering the presence of 3 different areas in the SWTA demonstrating a lack of thermohaline stationarity in the SWTA domain, an alternative approach for future studies accounting for the no stationarity would be the use of Universal Kriging (Menafoglio et al, 2016(Menafoglio et al, , 2013, which supposes that the random field has an expectation that depends of the area.…”
Section: Discussionmentioning
confidence: 99%
“…This was expected since the boundaries between areas cannot be entirely steady. Considering the presence of 3 different areas in the SWTA demonstrating a lack of thermohaline stationarity in the SWTA domain, an alternative approach for future studies accounting for the no stationarity would be the use of Universal Kriging (Menafoglio et al, 2016(Menafoglio et al, , 2013, which supposes that the random field has an expectation that depends of the area.…”
Section: Discussionmentioning
confidence: 99%
“…We assume square integrability, that is for all . We can thus define the expectation of the process as , and the trace-covariogram ( Menafoglio et al, 2013 , Menafoglio and Petris, 2015 , Menafoglio et al, 2016a ) of the process as where, for all , that is the infinite-dimensional analogue of the covariogram of a real-valued process ( Cressie, 1993 ). If we assume second-order stationarity and isotropy, the trace-covariogram reduces to a function of a real non-negative variable, i.e.…”
Section: Modeling Death Data As Functional Compositionsmentioning
confidence: 99%
“…To set the background, we recall that over the last decades considerable work has been done on extending classical statistical methods to the case of data embedded in functional Hilbert spaces (see, e.g., Ramsay and Silverman, 2005 , Ferraty and Vieu, 2006 , Horváth and Kokoszka, 2012 , Wang et al, 2016 and references therein). Moreover, an important body of literature has focused on developing a consistent theoretical framework for geostatistical modeling and spatial prediction for functional data, developing the infinite-dimensional counterparts of techniques such as spatial variography and Kriging ( Giraldo et al, 2010 , Nerini et al, 2010 , Giraldo et al, 2011 , Ruiz-Medina, 2012 , Menafoglio et al, 2013 , Caballero et al, 2013 , Ignaccolo et al, 2014 , Menafoglio and Petris, 2015 , Menafoglio et al, 2016b , Menafoglio et al, 2016a ). Recent works have specifically targeted the case of constrained functions and other object data, in a stream of literature that we refer to as Object Oriented Spatial Statistics (O2S2) ( Menafoglio and Secchi, 2017 and references therein).…”
Section: Introductionmentioning
confidence: 99%
“…Particular attention has been paid to the problem of spatial prediction, especially to the development of novel notions of functional Kriging, both in the stationary (see, e.g., Delicado et al, 2010, for a recent review) and in the non-stationary setting (e.g., Caballero et al, 2013;Ignaccolo et al, 2014). This theory was widely applied, e.g., in climatology (prediction of daily temperature profiles, see Delicado et al, 2010, and references therein), oceanography (temperature profiles along depth of the ocean, see Nerini et al, 2010), air quality monitoring (Ignaccolo et al, 2014), wireless sensors networks (Lee et al, 2015), petroleum system modeling and production forecast (Menafoglio et al, 2016a).…”
Section: Recent Approaches To the Analysis Of Object Datamentioning
confidence: 99%