Sentence examples for steeper inclination from inspiring English sources

As shown in our results, we found that capillary ridge height increased with higher surface tension, steeper inclination angle, bigger initial thickness, and more Newtonian fluids.

A higher slope value indicates a steeper inclination.

Memory consumption also exhibits a linear behaviour as profiles in this test require roughly the same amount of memory (Fig. 6b) with the exception of the beginning of the test where a lot of profile pre-fetching and queuing takes place, constituting steeper inclination.

These are characterized by a steeper inclination more suitable for erected organisms, such as massive sponges and corals, depending on the water movement for their feeding activity.

(ii) Horizontal branches accumulate more canopy soil than branches with a steeper inclination (Nadkarni and Matelson 1991).

The inclination records of the two regions show parallel variations, although the two regions are about 5000 km apart; the periods of shallower inclinations in the Okhotsk Sea at about 25 45, 75 90, 110 135, and 185 200 ka coincide with those of negative steeper inclinations in the West Caroline Basin.

In this region, periods of steeper inclinations than the site averages, in which rapid excursional directional swings are intercalated, were observed near the Laschamp excursion (Lund et al. 2001, 2005) and "excursions 13a, 15a, and 17a" (~573, ~573, and ~666 ka, respectively; Lund et al. 2001).

The steep inclination of the CO2 concentrations is in agreement with the gas concentrations observed during HDO of CVO (Figs. 2, 3).

In this way, six new facet classes of the SiGe islands were identified, namely, {5 3 15}, {558}, {313}, {715}, {322} and {12 3 5} facets in the order of increasing inclination angle, where the {12 3 5} facets represent those with the steepest inclination angle of 68°.

They mentioned that besides the influence of the earthquake, the high relief and steep inclination in the source slope and plentiful saturated loose deposits formed by a river or gully in the travel path had a great contribution to the rapid and long runout landslides.

As the decrease in CO concentration in experiment 5 from 0.5 to 0.4 vol % took place very slowly (approximately within 5 h), it may be expected that the process was close to steady state at point C. It can be seen in Figs. 2 and 3 that the main DO of the liquid phase takes place rapidly at the beginning of the experiment due to steep inclination of the gas concentrations.