Due to a variety of reasons, ranging from the lack of knowledge among the general public regarding El Niño events to the fact that a volcanic eruption in Mexico from El Chichón distracted many scientists from noticing the telltale signs, this event escaped the notice of the scientific world until 1983. As pointed out by Walter Sullivan, signs began to appear in early 1982, when a noticeable and measurable drop in atmospheric pressure was noted in the central and southeastern Pacific compared to pressures found off the coast of Darwin, Australia.[2] As the year progressed, more and more signs pointed towards an upcoming powerful El Niño event; from the collapse and subsequent reversal of the trade easterlies that traditionally prevent upwelling from occurring in the Western Pacific[5] to the various atmospheric signatures that can all be associated with the El Niño-Southern Oscillation, these indicators all pointed to the fact that one of the most powerful El Niño events of the 20th century had begun.[2]
Effects on tropical cyclone development
As a result of the event, the 1982 Atlantic hurricane season and 1983 Atlantic hurricane season both saw a reduced number of storms and a decrease in their average strength. Over this two-year period, the most notable storm that formed over this period was Hurricane Alicia, a minimal Category 3 storm that made landfall in Texas, causing US$3 billion dollars worth in damages.[2] The rest of the storms that formed during these two seasons were relatively unremarkable; over the two seasons, there were only 10 named storms, 5 hurricanes, and two major hurricanes. One can expect to equal or even beat these numbers in a single season, as the tropical Atlantic typically churns out 10 named storms, 5 to 6 hurricanes, and 2 to 3 major hurricanes in a single year.[2] Despite Hurricane Debby in 1982 reaching Category 4 strength, it never made landfall.
Despite expectations of diminished tropical cyclone activity, the western Pacific typhoon seasons of 1982 and 1983 were hardly affected by the ongoing El Niño event.
In Ecuador, heavy rainfall and flooding led to high fish and shrimp harvests; however, the large amounts of standing water also allowed mosquito populations to thrive, leading to large outbreaks of malaria.[11] In just this country alone, the economic impact from this event in regards to damages caused by this flooding were estimated at over US$400 million.[12]
Warm water to the south of the Hawaiian Islands around November allowed a late tropical disturbance to develop into Hurricane Iwa,[13] which became the sixth wettest tropical cyclone ever recorded in Hawaii, and the costliest up to that point,[14] causing damage totaling $312 million (1982 USD, $985 million 2025 USD)[15] and leaving 500 Hawaiians homeless.[16] The last female Kauaʻi ʻōʻō bird was lost in the storm; her mate was recorded singing in solitary until he went silent and presumably died in 1987, marking the extinction of their species.[17]
In Indonesia and Australia, one of the worst droughts ever occurred as a result of this event. The cooler waters led to the formation of less convection in the region, and less rainfall as a result. The damages from crop failure and loss of livestock easily surpassed US$100 million.[1]
North America and Eurasia also faced unusually warm temperatures as a result of this event. The eastern United States in particular saw the warmest winter in roughly 25 years. Other side-effects, such as an uptick in mosquitoes, a loss in salmon off the coast of Alaska and Canada, and an increase in shark attacks off the western United States coast can all also be at least partially blamed upon this event.[18] Several temperature records across both landmasses were broken as a result.[1] In addition, tornado activity significantly increased across the Florida peninsula and even reached as far south as Cuba.
^Edgar, G. J.; Banks, S. A.; Brandt, M.; Bustamante, R. H.; Chiriboga, A.; Earle, S. A.; Garske, L. E.; Glynn, P. W.; Grove, J. S.; Henderson, S.; Hickman, C. P.; Miller, K. A.; Rivera, F.; Wellington, G. M. (19 August 2010). "El Niño, grazers and fisheries interact to greatly elevate extinction risk for Galapagos marine species". Global Change Biology. 16 (10): 2876–2890. Bibcode:2010GCBio..16.2876E. doi:10.1111/j.1365-2486.2009.02117.x. ISSN1354-1013. OCLC660819334. S2CID83795836. Desmarestia tropica Tropical acidweed * EF$, herbivore overgrazing associated with interactions between El Niño and overfishing
^Alvarado, J.J. & Solis-Marin, F.A. (2012) Echinoderm research and diversity in Latin America. Springer Science & Business Media, 658 pages.
^Valle, Carlos A; Cruz, Felipe; Cruz, Justine B; Merlen, Godfrey; Coulter, Malcolm C (1987). "The impact of the 1982–1983 El Niño-Southern Oscillation on seabirds in the Galapagos Islands, Ecuador". Journal of Geophysical Research. 92 (C13): 14437. Bibcode:1987JGR....9214437V. doi:10.1029/JC092iC13p14437.
^Carlowicz, Mike; Schollaert-Uz, Stephanie (2017). "El Niño". earthobservatory.nasa.gov. Design by Joshua Stevens. Archived from the original on 2008-12-02.