Exact(1)
These components have latitude structures corresponding to the respective Hough functions calculated using the algorithm by Swarztrauber and Kasahara (1985).
Similar(59)
The observed latitude structure of O/N2 therefore imposes constraints on external sources of energy to the thermosphere ionosphere system, and is valuable information for use in physical models.
(1) The solar wind latitude structure is affected by the low inclination of the heliospheric current sheet (HCS) which prevents fast high latitude wind from reaching down into the ecliptic and leads to three distinct zones, the middle or transition zone consisting of large periodic Corotating Interaction Regions (CIRs).
The present paper is focused on the global spatial (altitude and latitude) structure, seasonal and interannual variability of the most stable in amplitude and phase eastward propagating diurnal and semidiurnal tides with zonal wavenumbers 2 and 3 derived from the SABER/TIMED temperatures for full 6 years (January 2002 December 2007).
The peak at 0 degrees quasi-dipole latitude is primarily due to the equatorial electric field strength, while the higher latitude structure is primarily due to the neutral wind field (Fambitakoye et al., 1976, p. 114).
The latitude structure at 90 km is shown in the upper panel and the height structure of the same wave over the equator is shown in the lower panel.
This type of latitude structure is consistent with the first symmetric Hough function for DW1 plotted in Figure 2. The approximately 12-h shift in phase between the equator and ±20° −40° latitude in 'Additional file 1: Phases for Figure 6' support this interpretation.
Figure 2 upper panel shows the latitude structure of the spectral amplitude of the 5.5-day Kelvin (E1) wave in temperature (in K°) at 90 km as obtained from the TIMED/SABER data for the period from 1 August to 31 October 2005.
On the other hand, D0 has minimum amplitudes near the equator, and its latitude structure is similar to that of the first antisymmetric mode of D0 plotted in Figure 2. As shown in 'Additional file 2: Phases for Figure 7', D0 is nearly in anti-phase between the N. and S. hemispheres and, moreover, does not change much throughout the year.
There was no latitudinal trend in the ordination plot among the main localities, indicating that other factors than those associated with latitude structure the root associated fungal community of D. octopetala at a larger geographic scale.
In this section, we present the climatological altitude-latitude structures of the migrating component Dw1 and three nonmigrating components De3, Dw2, and Ds0 from both eCMAM30 and SABER.
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