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Exact(7)
In North America, the main variability (mode 1, Fig. 11a) is a strong annual variation with a maximum in March June.
In Oceania, the main variability (mode 1, Fig. 14a) is an annual variation, with the highest values occurring during the December solstice.
In the Oceania region (Fig. 6), the main variability (mode 1, Fig. 6a) is an annual variation, with the highest values occurring during the December solstice.
In the Asia region, the main variability (mode 1, Fig. 13a) is a strong annual variation, with the highest values occurring during the June solstice, with a strongly latitudinal variation (Fig. 13b), increasing toward lower latitudes.
In the South American region (Fig. 4) the main variability (mode 1, Fig. 4a) is a strong annual variation, with the highest values occurring in the December solstice and the lowest values occurring in the June solstice.
In the South America region, the main variability (mode 1, Fig. 12a) is a strong annual variation, with maximum values occurring during the December solstice located in a region centered approximately at − 60° in latitude and − 70° in longitude and decreasing radially (Fig. 12a, b).
Similar(53)
In the North American region (Fig. 3), the main vTEC variability (mode 1, Fig. 3a) is a strong annual variation, with the highest values occurring in the later March equinox and the lowest values occurring in the December solstice, with a semiannual component overlapped (and at maximum near the equinoxes).
Using this methodology, Nieto et al. [19] [21] identified the major sources of Sahel moisture, as well as of Iceland and Orinoco Basin, while Drumond et al. [22] investigated the main sources of moisture over Central Brazil and La Plata Basin, regions that coincide with two centers of action of a dipolar precipitation variability mode related to the South American Monsoon System (SAMS) [23].
These are called "modes," and there are 4 main ones - Mode 1, Mode 2 etc.
It is found that the bathymetric changes of NC include two main modes, with the first mode representing 64% of the NC variability, which indicates observable deposition in the mouth bar and its outer side area (lower reach); the second mode representing 11% of the NC variability, which further demonstrates channel deepening along the inner side of the mouth bar (upper reach) during 1970 2013.
In case of the main mode, the proposed main mode is performed with the procedure as described in Figure 7.
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