Exact(3)
The distance between two longitude lines varies by latitude, so there is no simple, universal solution to this.
Therefore, this paper proposed a GeoHash algorithm to implement this step: through a certain rule [12, 13], a string to represent the latitude and two longitude coordinates.
In an attempt to explain the dipole field decay since 1840, Finlay et al. (2016a) invoke fluctuations of meridional flux advection present in two longitude bands, namely an equatorward flow around longitude 100°E and a poleward one around 90°W, as parts of a planetary gyre.
Similar(56)
In each case, we give map views at two different altitudes, namely 90 120 km (a1 a3) and 240 270 km (b1 b3), and latitude height profile in (e1 e3), and two longitude-height profiles in (c1 c3, d1 d3).
Figure 7 The observed variability in EEJ strength between the two longitudes during D-season.
This further substantiates the high degree of day-to-day variability between the two longitudes.
The differences become increasingly marked from around 10 00 to 17:00 LT between the two data sets at the two longitudes.
The observed monthly averaged EEJ amplitudes correlated well with the global model EEJM-2.0 at the two longitudes (Figure 5).
Figure 7 emphasizes the relative degrees of variability of the two longitudes vis-à-vis the number of days.
Rastogi et al. (2007) showed a strong correlation of equatorial electrojet between two longitudes separated by 2,000 km (approximately 18° longitude).
The observed variability in EEJ strength between the two longitudes during D-season is shown in Figure 7 on the basis of Kp values.
Write better and faster with AI suggestions while staying true to your unique style.
Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com