On October 30, a low-latitude
tropical wave exited the coast of
West Africa over the Atlantic Ocean. Disorganized
convection east of the wave axis accompanied the wave as it moved west over open waters. During November 7–8, the wave turned northwest and traversed northern
South America, crossing
Guyana,
Venezuela, and the
Windward Islands before emerging over the
Caribbean Sea. Largely favorable environmental conditions ahead of the disturbance led to the
National Hurricane Center (NHC) issuing outlooks for potential
cyclogenesis at this time. Turning back to the west and slowing, interaction with an
upper-level trough fostered the development and expansion of convection. Strong
wind shear inhibited organization as the system approached
Hispaniola on November 10–11; however, the system made an unusual turn southwest in response to a mid-level
ridge over the southwestern Atlantic and a surface low developed by 12:00
UTC on November 12. Lessening wind shear in this region enabled convection to concentrate around the center of the low and the system became a tropical depression on November 13, the record-tying thirty-first of the season, approximately northwest of
Aruba. The depression strengthened into Tropical Storm Iota six hours later, bolstering the already record-breaking number of named storms during the 2020 season to 30. Large-scale environmental conditions consisting of
sea surface temperatures of and ample low- to mid-level moisture favored significant intensification of the cyclone. As Iota moved farther from land on November 14,
banding features became more pronounced and deep convection blossomed over a tightening circulation. With Iota becoming more compact and organized within the aforementioned favorable conditions and shear relaxing, the system underwent an exceptional period of
explosive intensification from 18:00 UTC on November 14 to 12:00 UTC on November 16. The environment surrounding Iota was ideal for this to occur: wind shear fell below , lower- to mid-level
relative humidity values exceeded 70 percent, and
sea surface temperatures averaged . A symmetrical
central dense overcast with temperatures averaging and broad
outflow developed on November 15. Data from the
53rd Weather Reconnaissance Squadron revealed Iota to have become a hurricane by 06:00 UTC that day, Iota's core wobbled northwest at the onset of this intensification as the overall trajectory shifted west in response to a strengthening ridge spanning from the western Atlantic to the
Gulf of Mexico. The most rapid phase of intensification occurred early on November 16, during which recorded a six-hour pressure drop of , including a drop of in a single hour, was observed by aircraft reconnaissance. The eye featured six
mesovortices, and reached Category 4 intensity by 06:00 UTC. Around 10:45 UTC, the center of Iota passed less than north of
Providencia and Santa Catalina and its eyewall struck the islands directly. It was estimated that the islands experienced sustained winds of at least . as well the second-most intense hurricane at Category 4 strength in terms of pressure, behind
Hurricane Opal's 916 mbar. Iota's intensification was one of the fastest on record in the Atlantic basin. During a 42-hour period from 18:00 UTC on November 14 to 12:00 UTC on November 16, its central pressure fell by and its maximum sustained winds rose by . The pressure drop in this time span was the fourth-greatest on record, only behind
Rita (),
Wilma () in 2005, and
Milton in 2024 (). After reaching its peak strength on November 16, Iota slowly weakened on approach to Nicaragua. Lower sea surface temperatures and
ocean heat content, likely the result of
upwelling from
Hurricane Eta, caused convection to diminish and its eye structure to deteriorate. In the hours leading up to the hurricane's
landfall on November 17, there were no reconnaissance missions and Iota's intensity was uncertain. Furthermore, land-based measurements were nearly non-existent given the devastation wrought by Eta. An unofficial gust of was reported in southern Bilwi two hours prior to landfall while the highest reliable observations at
Puerto Cabezas Airport had sustained winds of and peak gusts of . Based on calculations using the SHIPS inland decay model, Iota was estimated to have weakened into a tropical storm by 18:00 UTC near the Nicaragua–Honduras border. By the start of November 18, the remaining deep convection was confined to a rainband well to the northwest of the storm's core.
Scatterometer data indicate the system continued producing tropical storm-force winds off the northern coast of Honduras throughout the morning. After weakening to a tropical depression by 12:00 UTC, the surface circulation of Iota dissipated over east-central El Salvador several hours later; The system was last noted the following day well to the southwest of
Guatemala.
Peak intensity analysis Operationally, Iota was classified as a Category 5 hurricane with maximum sustained winds of based on
stepped-frequency microwave radiometer (SFMR) measurements of and aircraft flight-level winds of . This would have made it the latest such storm during a calendar year on record in the basin and the only Category 5 hurricane of the season. However, after post-season analysis, the NHC determined the SFMR values to have a high bias as the highest observations were coupled with lower flight-level winds, a problem that had recently been discovered with other intense hurricanes. The peak SFMR value was co-located with flight-level winds of , which would typically reduce to at the surface using flight-level to surface reductions. NHC meteorologists determined that
breaking waves along the west side of Providencia and Santa Catalina interfered with the instrument's measurement quality. Accordingly, the peak intensity was revised downward to , downgrading Iota to a Category 4 hurricane; however, this was within the normal range of uncertainty. Meteorologists noted that research into these errors was ongoing and the peak intensity of Iota could be revised in future analyses. == Preparations ==