35 results were found for 화전역건전마사지♤텔레 GTTG5♤繯화전역남성전용鹊화전역딥티슈ן화전역딥티슈출장鄹화전역로미로미🚇correlation/.

Results:

• 21. 2010_003rs

  location method and to map the faults that they occur on. Due to the high clock-accuracy of the Icelandic SIL seismic network, the method can, through cross- correlation, reduce the uncertainties in relative arrival times and thus increase relative location accuracy to as far as tens of meters. This enables fault mapping by grouping together relocated events that form apparent lineaments /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 22. VI_2017_009

  (Dowdeswell et al., 1997; Björnsson and Pálsson, 2008; Cubasch et al. 2013; Agústsson et al., 2015). General Circulation Models (GCMs) simulate climate changes on a large spatial scales. They can be downscaled in several ways to study climate in more details. When this is done statistically, a correlation is found between observations and results from GCMs modelling of the past /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 23. Refsgaard_etal-2007-Uncertainty-EMS

  (e.g. Gaussian; second-order stationarity; degree of temporal and spatial autocorrelation). Furthermore, correlation in time and space is characterised by correlogram/variogram functions. Categorical data (3) dif- fer from numerical data (1, 2), because the categories are not measured on a numerical scale. A software tool, the data uncertainty engine (DUE), for supporting the assessment of data /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 24. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  but for precipitation changes. Changes in local temperature are strongly controlled by the large-scale temperature change. This is reflected both by the small amplitude of the regression residuals (typically 0.1-0.3°C) and the large explained variance (mostly above 80%, with some exceptions like the Baltic Sea). For changes in precipitation, the correlation between the local and the large-scale changes /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 25. Refsgaard_2-uncertainty

  model Somewhat plausible Competing schools 1 Weak correlation but commonalties in measure Educated guesses indirect approx. rule of thumb estimate Preliminary theory Grey box model Not very plausible Embryonic field 0 Not correlated and not clearly related Crude speculation Crude speculation Black box model Not at all plausible No opinion Example from Refsgaard et al /media/loftslag/Refsgaard_2-uncertainty.pdf

• 26. ces-oslo2010_proceedings

  ), with the intention of illustrating the relationship between temperature and nature of trends in snow parameters. To further investigate snow parameters‟ sensitivity to variations in winter climate, we performed an analysis of correlation with time series of mean winter temperature and accumulated winter precipitation. Results show a transition from more and more negative trends in number /media/ces/ces-oslo2010_proceedings.pdf

• 27. 2010_012rs

  to a subset of near-by events from the event library via cross-correlation of P and S waveforms. The relative times are inverted for best location, resulting in a high-precision automatic location for the new event available within minutes. As more waveforms arrive, the process is repeated to improve the location. The location accuracy that can be achieved is from tens of meters to a few hundred meters /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 28. VI_2009_013

  Recorded seismicity by the SIL-system in Eyjafjallajökull and nearest vicinity between 1991 and August 2006. 3.2 Method We used a multi-event, double-difference relocation method to relocate the earthquakes (Slunga et al., 1995). The method uses cross-correlation of similar wave forms to determine relative travel times of waves from events to stations with increased accuracy. This can /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 29. 2013_001_Nawri_et_al

  difference in averages alone. This amounts to minimising local normalised mean squared deviations, without changing the correlation between modelled and measured time-series. However, the linear transformation is only applicable to mean fields, with a sufficiently long averaging period, to allow for representative averages and standard deviations to be calculated. An application of the linear /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 30. Reykholt-abstracts

  fields); automated feature tracking (using the VISICORR software (Dowdeswell and Benham, 2003)); and a semi-automated Fourier-transform based cross- correlation technique. In this paper, we extend this analysis to investigate the impact of various pre-processing steps (such as slope shading of the surface derived from the point cloud); the impact of the window size used to calculate the Fourier /media/vatnafar/joklar/Reykholt-abstracts.pdf