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Global climate phenomenon
El Niño–Southern Oscillation (ENSO) is a global climate phenomenon that emerges from variation in winds and sea surface temperatures over the tropical Pacific Ocean. Those variations have an irregular pattern but do have some appearance of cycles. The occurrence of ENSO is not easily predictable. It affects the climate of much of the tropics and subtropics, and has links (teleconnections) to higher-latitude regions of the world. The warming phase of the sea surface temperature is known as "El Niño" and the cooling phase as "La Niña".
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Early-Season Nor’easter Brings Historic Flooding to New Jersey’s Coast The New Jersey State Climate Office at Rutgers University is available today and this week for comment and press inquiries. Contact John Krasting, New Jersey State Climatologist at Rutgers University, directly at krasting@rutgers.edu or (848)…
A slow nor’easter cut power to about 136,000 customers as full moon tides fueled repeated coastal flooding. Why the tides mattered and what comes next.