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KW - U.S. extreme precipitation

JO - Journal of Geophysical Research: Atmospheres

T2 - Journal of Geophysical Research: Atmospheres
14,449-14,461 ()Applicable publications, involving five languages, have been reviewed toobtain information on El Niños that occurred over the past fourand a half centuries.

JF - Journal of Geophysical Research: Atmospheres

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Relative strengths of events are based on such considerations as windand current effects on travel times of ancient sailing ships, degree ofphysical damage and destruction, amounts of rainfall and flooding, massmortality of endemic marine organisms and guano birds, extent ofinvasion by tropical nekton, rises in sea temperatures and sea levels,affects on coastal fisheries and fish meal production, etc.


Emphasis isplaced on strong and very strong events.

It wasdesirable to have cross-correlated reports from independent sources.
Our tropical Pacific thickness analyses and cumulativeplots of Southern Oscillation index anomalies over the southeast Pacifictrade wind zone showed additional evidence as to the unusual strength ofthe 1982-1983 event.

For example, the 1940-1941,1957-1958, and 1972-1973 events fall into the strong category, whereasthe 1891, 1925-1926 and 1982-1983 events are considered very strong.

Weakevents are not included here.

T1 - A comparison of the effects of El Niño and El Niño Modoki on subdaily extreme precipitation occurrences across the contiguous United States

Shadow People and Dark Demonic Entities During Sleep Paralysis

Since this information refers strictly to ElNiño occurrences, a regional manifestation of the large-scale (ElNiño-Southern Oscillation (ENSO)) event, it is based primarily onevidence obtained from the west coast region of northern South Americaand its adjacent Pacific Ocean waters.