Tropical cyclones in 1997

The 1997 El Niño observed by TOPEX/Poseidon. The white areas off the tropical coasts of South and North America indicate the pool of warm water

In January 1997, satellites gathering information on water temperatures and sea level heights discovered an area of unusually warm water situated across the western half of the Pacific Ocean. About 150 m (490 ft) below the surface, water temperatures were about 3 °C (5.4 °F) above normal, signifying that an El Niño–Southern Oscillation (ENSO) event was beginning. By this time, the Scripps Institution of Oceanography had forecast that an ENSO was likely to take place during the latter half of 1997.[1] Throughout February, water temperatures began increasing over much of the Pacific as well as in shallower waters off the coast of Peru. The above-average water temperatures covered an area roughly 11,000 km (6,800 mi) across, almost stretching from New Guinea to South America.[2] By April, the ENSO became fully established; a column of warm water extended to the surface in the middle of the Pacific Ocean and water anomalies exceeded 5 °C (9 °F) about 150 m (490 ft) below the ocean surface. At the surface off the coast of Peru, water temperatures averaged 3 °C (5.4 °F) above normal.[3]

Exceedingly warm waters became apparent by May, especially off the coast of South America where anomalies were reaching 7 °C (12.6 °F) above normal. Further north, sea surface temperatures along the Pacific coast of North America were increasing, with a large pool of water being 3 °C (5.4 °F) above normal.[4] By September 1997, the ENSO became very powerful, with surface temperatures between South America and the International Date Line averaging 2–4 °C (3.6–7.2 °F) above normal, roughly a quarter of the planet's diameter. Additionally, waters along the Pacific coast of North America continued to expand, now stretching from Alaska to southern Mexico. A contrasting area of abnormally cool waters took shape near the coast of Australia by September as well, with waters 150 m (490 ft) below the surface averaging 4 °C (7.2 °F) below normal.[5] Along the Pacific coast of the Americas, the volume of 21 to 30 °C (70 to 86 °F) water was roughly 30 times greater than that of all the water in the Great Lakes combined. The extra heat energy created by this anomaly was also about 93 times more than the energy produced by fossil fuels in the United States during 1995.[6]

There are a total of 9 tropical cyclone basins, 7 are seasonal and two are non-seasonal, thus all 8 basins except the Mediterranean are active. In this table, data from all these basins are added.

• Tropical cyclones by year
• List of earthquakes in 1997
• Tornadoes of 1997

Regional Specialized Meteorological Centers

• US National Hurricane Center – North Atlantic, Eastern Pacific
• Central Pacific Hurricane Center – Central Pacific
• Japan Meteorological Agency – NW Pacific
• India Meteorological Department – Bay of Bengal and the Arabian Sea
• Météo-France – La Reunion – South Indian Ocean from 30°E to 90°E
• Fiji Meteorological Service – South Pacific west of 160°E, north of 25° S

Tropical Cyclone Warning Centers

• Meteorology, Climatology, and Geophysical Agency of Indonesia – South Indian Ocean from 90°E to 141°E, generally north of 10°S
• Australian Bureau of Meteorology (TCWC's Perth, Darwin & Brisbane) – South Indian Ocean & South Pacific Ocean from 90°E to 160°E, generally south of 10°S
• Papua New Guinea National Weather Service – South Pacific Ocean from 141°E to 160°E, generally north of 10°S
• Meteorological Service of New Zealand Limited – South Pacific west of 160°E, south of 25°S

 This article incorporates public domain material from websites or documents of the National Weather Service.