Sentence examples for blue inverse from inspiring English sources

The mean time coefficient of EOF1 averaged for the period between 1951 and 2012 changed sign around the 29th pentad (late May) and the 71st pentad (mid-December), as shown by the red and blue inverse triangles in Fig. 1b.

The red (blue) inverse triangles on the horizontal line indicate the first pentad when the sign of the time coefficients changed after (before) the 18th pentad from negative to positive (from positive to negative) for each cluster.

The red and blue inverse triangles in b denote the first pentad (the 29th and 71st pentads) when the sign of the mean time coefficients for the EOF1 changed.

We invert the transverse component of broadband waveform data for 131 deep and intermediate earthquakes (orange stars in Fig. 1a, parameters in Additional file 1: Table S1) with (5.5 le {M_{rm w}} le 7.3) that occurred in western Pacific subduction zones using receivers in North America from the USArray and other networks (blue inverse triangles in Fig. 1a).

For the multi-polarized capacitors, more than 80% of the capacitors show slanted hysteresis loops [see curves consisting of red circles, blue inverse-triangles, and green triangles of Figure 4(a)].

A continuous red shift phenomenon in emission wavelength with the increase of m value and an inverse blue shift with the increase of n value were both observed and rationally uncovered.

A "best fit" map is produced by goodness testing all four fitted models and mapping the chosen best-fitted model in different colours, white for Gaussian, green for Laplacian, red for K-distribution, and blue for normal inverse Gaussian.

When an expression coefficient of ≥0.5 (highlighted in purple) was set for positive correlation and a coefficient of ≤ −0.5 (highlighted in light blue) was set for inverse correlation, NH2 showed seven positive correlations and three inverse correlations out of the 32 sets of data examined.

Figure 7 Two-part discrete mixture of Gaussians (black) fitted as Laplacian (green), K-distribution (red) and normal inverse Gaussian (blue dashed).

Observe that the Laplacian (in green) fits higher up the peak and lower in the tails, whereas the K-distribution (red) and normal inverse Gaussian (blue dashed) are almost identical and fit most tightly in the tails.

Inverse representations, (blue saltire on a white field), of the Scottish Saltire are also used outside Scotland.