Sentence examples for bottom latitude from inspiring English sources

Total diurnal (left) and semidiurnal (right) exosphere temperature amplitudes in a longitude vs. month format at -40° (top), 0° (middle), and +40° (bottom) latitude, obtained by vectorally superimposing the structures illustrated in Figures 3, 4, 5, 6 and 7 with the corresponding migrating diurnal and semidiurnal components.

The stations are plotted from low (top) to high (bottom) latitudes.

The stations are shown from low (top) to high (bottom) latitudes.

The H component of the magnetic field fluctuations as observed at 1028 00 1030 00 UT on February 27 , 2009at the five stations from higher (top) to lower (bottom) latitudes.

Dynamic spectra of the H component of the magnetic field fluctuations at 0.1 32 Hz as observed on February 27 , 2009at the five stations from higher (top) to lower (bottom) latitudes.

From top to bottom Dst, latitude (θ B ), and longitude (ϕ B ) of the magnetic field in GSE coordinates.

We checked for collinearity among the three predictors included in the GAM model (bottom oxygen, latitude and depth).

The results for SS (a) and CP (b) are presented in succession varying from the negative bottom magnetic latitudes for the Southern hemisphere (indicated at the right border of each panel) towards the positive magnetic latitudes upward for the Northern hemisphere.

Bottom: low-latitude station of CP.

Kikuchi et al. (2000) separated out the convection and shielding electric fields during the substorm as shown in Fig. 6 where the solid/dashed curves indicate the convection/shielding electric fields at (top) auroral and (bottom) subauroral latitudes.

Fig. 6 Convection (E 1) and shielding (E 2) electric fields shown with the solid and dotted lines, respectively, at the (top) auroral and (bottom) subauroral latitudes as deduced from the electric field measured by EISCAT and IMAGE magnetometer array data.