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At 45 km, Dw1 is still characterized by broad mid- and high-latitude maxima in each hemisphere and a secondary maximum at the equator.
In the empty-state mode, short blocks look like two lines separated by ~8 Å (the distance is measured between brightness maxima in each line).
Below 60 km, the structure is still characterized by the mid- and high-latitude maxima in each hemisphere, but hemispheric asymmetry is obvious in both eCMAM30 and SABER.
In this last procedure as we are only interested in rare extremes, low to medium values of rainfall depth were neglected leaving a small number of L days of ranked daily maxima in each set per year, whose sum typically comprises about 50% of each annual rainfall total.
Most likely the different times represent accumulation maxima in each organ.
The data were normalized so that the maximum intensity value for each FA equaled 100 (arbitrary units), and the number of local maxima in each intensity profile was quantified.
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(The maximum in each match is 25 victory points).
Scientists explain that, to the extent comparison between poles makes sense, the correct way to do it is to look at summer minimums and winter maximums in each hemisphere.
The parameter k determines how many handovers can be performed at maximum in each time slot.
The equatorial maximum below 90 km is tilted toward the SH in both eCMAM30 and SABER, and the mid-latitude maximum in each hemisphere contains multiple peaks at different altitudes.
However, our method is more efficient, because our method computes the curvature of the residual graph at only one point where the residual takes a maximum in each segmented arc.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com