Sentence examples for anomaly obtained from inspiring English sources

In this study, we tried to validate groundwater storage (GWS) anomaly obtained from a combination of GRACE and land-surface model based estimates, for the first time, with GWS anomaly obtained from a dense network of in-situ groundwater observation wells within 12 major river basins in India.

In this study, we used the existing gravity anomaly database (Komazawa 2004) which compiled 1 km × 1 km mesh data of the Bouguer gravity anomaly obtained by Bouguer density of 2670 kg/m3.

Nevertheless, the recovered density anomaly obtained using this constraint is about 1/4 its input, so we need to focus on the amount of electron density anomalies of recovered Es patches.

The indirect effect on the geoid due to gravity reduction was evaluated using the planar formula given as (Wichiencharoen, 1982b), (7) The residual gravity anomaly (Δgr) is then given as, (8) where ΔgGGM is the gravity anomaly obtained from the full expansion of EGM2008 2,1900 × 2,159).

Furthermore, Bouguer anomaly obtained from forward modelling (Baillieux et al. [2012]) using a homogenous basement density reveals gradually decreasing gravity from about −44 mgal at the western boundary fault to about −55 mgal in the southeast of the study area (not shown).This is not compatible with the important negative anomalies observed in the centre of the investigation area.

A zonal vertical cross section at 18°N is taken across the center of the storm in the IAA case and shows the IAA temperature anomaly, obtained by subtracting the mean temperature at the same latitude of a section spanning from 80°W to 20°W in longitude.

The conductivity anomalies obtained from this study confirmed the regional-scale geology of the area.

The assessment is based on geometric geoid undulations, obtained from 816 GPS/levelling points and free-air gravity anomalies, obtained from 6951 first-order gravity points over Japan.

This assessment was based on geoid undulations, obtained from 816 GPS/leveling points, and free-air gravity anomalies, obtained from 6,951 first-order gravity points.

Symbols are as in Fig. 4. Figure 11b, c, e, f compares the velocity anomalies obtained in the present study with those obtained by Suetsugu et al. (2009).

From 10,000 iterative tests with random data, it was revealed that almost all the anomalies obtained here did not result from a stochastic process (Fig. 4b).