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For 10 years, from 1877 through 1886, the farmers on the Plains had the benefit of an abnormally generous rainfall, leading many to assume that climatic conditions had changed and that the rain belt had moved westward to provide adequate rainfall for the Plains.
As the Pacific Subtropical High moves northward in the summer, a rain belt center is formed north of the Yellow River basin, which controls the ending time of the spring drought (Zhai and Feng 2008).
The results indicated that annual maximum precipitation, 3-day (5-day and 7-day) maximum precipitation and extreme precipitation of the peak over threshold 90%, 95 % and 99 shows an increase from Northwest to Southeast and from west to east in SWC, which is consistent with the path of the rain belt moving.
Because of this, the Tropical rain belt may not have risen to its northern latitudes, thus causing an absence of seasonal rains.
Annually, the rain belt within the tropics marches northward by August, then moves back southward into the Southern Hemisphere by February and March.
Precipitation could potentially increase in mountainous regions in the northern EMME, and possibly also in the southern EMME owing to the northward expansion of the tropical rain belt (Önol and Semazzi 2009; Evans 2010).
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At Soundwave in 2007, the rain belted down and we moshed to Carrion so hard that steam poured off the pit.
It was mid-afternoon in August but the floodlights at Goodison were already burning full on as the rain belted down from a sky as bruised as some of the players would be an hour and a half later.
During the mid-Cretaceous, the subtropical high-pressure arid climate belt of the planetary wind system controlled the palaeolatitude distribution of humid belts in Asia as well as the spatial distribution of rain belts over the massive continental blocks at mid-low latitudes in the southern and northern hemispheres.
It lies within 5.03°N and 5.09°N of latitude and 7.41°E and 8.10°E of longitude in the tropical rain forest belt of Nigeria and form part of the low lying coastal/deltaic plains of the southern Nigeria.
Uyo, the capital city, is located in the rain forest belt of Nigeria with an annual rainfall of 2430.0 mm.
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