Sentence examples for basin velocity from inspiring English sources

Hereafter, we call this model the 'smoothed basin velocity structure model (SBVSmodel

On the other hand, increasing wind velocity, basin insulation thickness, evaporation and condensation surface areas, condenser emissivity, and saline water mass has little effect on productivity.

Using the estimated source model together with a one-dimensional (1-D) velocity basin structure model, long-period (> 4 s) ground motions were simulated at a site located in the Kathmandu basin, where strong ground motions with predominant components in a 4 5s period were observed during the 2015 Gorkha earthquake.

In the southern part of the Tekirdag Basin, low-velocity values are detected at a depth of 15 km.

The KPR Vp models in Region 4 (Fig. 4) differ from line to line, but there are some common features: thicker crust and especially middle crust than in the adjacent basins, Pn velocities less than 8.0 km/s, thin crust and high Pn velocities over 8.0 km/s at the eastern boundary with the PVB.

The impulse travels the length of the basin at a velocity dependent on the water depth and is reflected back from the basin's end, generating interference.

Analytical expressions for water temperature, glass cover temperature and yield as a function of climatic parameters — namely solar intensity, ambient air temperature and design parameters (water depth, absorptivity of basin liner, wind velocity, bottom insulation and cover inclinations) — were also derived.

Both models share the following common features throughout most of the study area: high Pn velocities under the Indian Plate and in the Tarim basin, low Pn velocities under the Hindu Kush and in Myanmar and the adjacent region.

As an initial step in the 3-D simulation of Kathmandu Valley basin, a 1-D velocity structure estimation was conducted using forward modeling of an observed long-period S-wave from the mb4.9 earthquake.

To investigate the characteristics of the predominant period of long-period ground motions in deep sedimentary basins, we analyzed the velocity seismograms from seven moderate to large shallow earthquakes (magnitude 5.8 to 7.5) that occurred around the Kanto Basin (Figure 1a).

The first onset of S waves propagated from north to south with almost the same velocity outside the basin area as in the trench-like basin area.