Sentence examples for time scale 1 from inspiring English sources

Since carbonate δ18O values reflect both temperature and seawater δ18O, the JS planktonic foraminifera δ18O values reflect two kinds of minima on a glacial interglacial time scale: (1) during interglacial maxima (warm conditions) and (2) during glacial maxima (low seawater δ18O; i.e., low salinity).

We especially provide new insights into the dynamics of elongation of lithostathine protofibrils and fibrils on a relatively short time scale (1 image/s).

Interestingly, previous work has shown that PKA influences thermotolerance of neural function in an opposite fashion to PKG and in a much slower time scale (1 hr vs. several min) [19].

The dependency matrix of the interaction graph (computed for time scale 1, Figure 2) displays all functional dependencies between each pair of species.

Although we are unable to determine the dynamic error for a complex fluid such as mucus, we minimize contributions of dynamic error by comparing data at a long time scale (1 s) relative to the time interval between frames.

For example, p53-induced protein with a death domain (PIDD) binds to NEMO (interaction 44, time scale 1), and later, PIDD binds to RIP1-associated ICH-1/CED-3 homologous protein with a death domain (RAIDD) (interaction 43, time scale 2) [ 28].

On the time scale (1/varepsilon), we have that (x t -y(t)=O(varepsilon)), as (varepsilonrightarrow0).

Then the following statements hold: (a) On the time scale (1/varepsilon), we have that (x t -y(t)=O(varepsilon)), as (varepsilonrightarrow0).

When considering the medium- to long time scale (1 47 years) using archival terrestrial (and aerial) photographs, headcut retreat rates proved to be significantly higher than those in the short term.

Injection of >500 keV electrons into the slot region (L≈3) near equatorial plane is occurred on time scale ≈1 hour, when, during the magnetic storm maximum, the extreme low-latitude position of auroral electrojets is reached and ring current becomes more symmetrical.

As in Matsuno (1966) and Gill (1982), we use a time scale (1/sqrt {c^beta ^) and a length scale (sqrt {c^/beta ^) to nondimensionalize the equation system (1a)–(1c) to give begin{array}rcl@ &&u_{t} - y v + p_{x} = 0, end{array} (7a).