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Sea-Surface Temperature Anomalies: El Niño

OceansPhysical Environment

A composite of sea-surface temperature anomalies during El Niño from November to March during the following years: 1958, 1966, 1973, 1983, 1987, 1992, 1996, and 1998. When sea-surface temperatures in the tropical eastern Pacific rise well above normal, it is known as an El Niño event.

NOAA

Sea-surface temperature anomalies during El Niño. The most intense warming (2 to 2.25 degrees Celsius, dark brown) occurs off the coast of South America. Cooler areas (negative 2.25 to negative 2 degrees Celsius, dark blue) are in the Arctic Ocean.

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Sea-Surface Temperature Anomalies: El Niño

Distribution of Neritic (Nearshore) and Pelagic (Open Ocean) Sediments

-0.25 to 0.25

0.75 to 1.0

1.0 to 1.25

1.25 to 1.5

1.5 to 1.75

Abyssal clay

Calcareous ooze

Continental (lithogenous)

Diatom

Radiolarian

Rhode Island
4.64%
Alaska
0.318%4.76%0.351%
Northwest Territories
3.51%
Florida
0.596%0.488%2.42%
Washington
0.513%1.71%
Nunavut
0.352%7.75%
Maine
0.133%1.41%
Nova Scotia
0.847%12.7%
Virginia
0.126%1.95%
Delaware
0.762%0.888%
Prince Edward Island
1.25%0.264%100%
Texas
0.183%0.242%
Louisiana
0.184%0.456%1.85%
Hawaii
1.74%1.20%0.113%0.444%2.10%29.4%7.02%22.4%
North Carolina
0.319%0.789%
New Brunswick
0.522%1.14%
British Columbia
0.126%2.00%
Newfoundland and Labrador
0.392%4.95%
New Jersey
0.329%0.212%
South Carolina
0.109%
Massachusetts
1.78%0.884%11.7%
New York
0.105%2.58%
Maryland
0.874%1.35%
Québec
1.05%
Ontario
0.313%
California
0.110%0.884%
0.16.0