Question: What was the least active Atlantic hurricane season on record only one known tropical storm, and following up behind it in second place is the second least active Atlantic hurricane season on record with only three systems reaching tropical storm intensity ?

Context articles: 1914 Atlantic hurricane season
2007 Atlantic hurricane season
1979 Atlantic hurricane season
1965 Atlantic hurricane season
Timeline of the 1983 Atlantic hurricane season
1983 Atlantic hurricane season
1887 Atlantic hurricane season
Hurricane Olga
1930 Atlantic hurricane season
1935 Cuba hurricane

The 1914 Atlantic hurricane season was the least active Atlantic hurricane season on record, with only one known tropical storm.
 Although hurricane season typically encompasses a much larger time-span, actual activity was confined to the middle of September.
 The only tropical cyclone of the year developed in the region of The Bahamas on September 15 and drifted northwestward, moving inland over Florida and Georgia.
 Thorough warnings before the storm prevented any major damage.
 The 1914 season is one of only two that did not produce any hurricanes (the other being the 1907 season).
 Due to the lack of modern technology, including satellite imagery, information is often sparse, and an additional tropical depression may have existed in late October.
 Additionally, this was the first hurricane season to take place during World War I.
The 2007 Atlantic hurricane season was an active Atlantic hurricane season, although most of the storms were weak and short-lived.
 However, the 2007 season was the first season to feature more than one Category 5 landfalling hurricane, a feat that would not be matched until 2017.
 It produced 17 tropical cyclones, 15 tropical storms, six hurricanes, and two major hurricanes.
 It officially started on June 1 and ended on November 30, dates which conventionally delimit the period during which most tropical cyclones form in the Atlantic Ocean.
 The first tropical cyclone, Subtropical Storm Andrea, developed on May 9, while the last storm, Tropical Storm Olga, dissipated on December 13.
 The most intense hurricane, Dean, is tied for the eighth most intense Atlantic hurricane ever recorded as well as the third most intense Atlantic hurricane at landfall.
 The season was one of only six on record for the Atlantic with more than one Category 5 hurricane.
 It was the second on record in which an Atlantic hurricane, Felix, and an eastern Pacific hurricane, Henriette, made landfall on the same day.
 September had a record-tying eight storms, although the strengths and durations of most of the storms were low.
 Aside from hurricanes Dean and Felix, none of the storms in the season exceeded Category 1 intensity.
The 1979 Atlantic hurricane season was the first season to include both male and female names, as well as the common six-year rotating lists of tropical cyclone names.
 The season officially began on June 1, and lasted until November 30.
 These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.
 It was slightly below average, with nine systems reaching tropical storm intensity.
 The first system, an unnumbered tropical depression, developed north of Puerto Rico on June 9.
 Two days later, Tropical Depression One formed and produced severe flooding in Jamaica, with 40 deaths and about $27 million (1979 USD) in damage.
 Tropical Storm Ana caused minimal impact in the Lesser Antilles.
 Hurricane Bob spawned tornadoes and produced minor wind damage along the Gulf Coast of the United States, primarily in Louisiana, while the remnants caused flooding, especially in Indiana.
 Tropical Storm Claudette caused extensive flooding, due to torrential rainfall.
 There were two deaths and damaged totaled $750 million.
The 1965 Atlantic hurricane season was the first to use the modern-day bounds for an Atlantic hurricane season, which are June 1 to November 30.
 These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.
 It was one of the least active seasons on record, with only 6 tropical cyclones developing and reaching tropical storm intensity.
 Four of the storms strengthened into hurricanes.
 One system reached major hurricane intensity – Category 3 or higher on the Saffir–Simpson hurricane scale.
 The first system, an unnamed tropical storm, developed during the month of June in the Pacific Ocean, while located south of Guatemala.
 The storm moved northward across Central America, but caused no known impact in the region.
 It struck the Florida Panhandle and caused minor impact across much of the Southern United States.
 Tropical cyclogenesis halted for over two months, until Anna formed on August 21.
 The storm remained well away from land in the far North Atlantic Ocean and caused no impact.
The 1983 Atlantic hurricane season was the least active Atlantic hurricane season in 53 years, during which four tropical cyclones formed.
 The season officially began on June 1, 1983, and ended on November 30, dates which conventionally limit the period of each year when tropical cyclones tend to form in the Atlantic.
 The first named storm, Hurricane Alicia, formed on August 15.
 The last storm of the season, Tropical Storm Dean, dissipated on September 30.
 This timeline documents tropical cyclone formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipations during the season.
 The timeline also includes information which was not operationally released, meaning that information from post-storm reviews by the National Hurricane Center, such as information on a storm that was not operationally warned upon.
The 1983 Atlantic hurricane season was the least active Atlantic hurricane season in 53 years, during which only four tropical storms formed.
 The season officially began on June 1, 1983, and lasted until November 30, 1983.
 These dates conventionally delimit the period of each year when most storms form in the Atlantic basin.
 The season had very little activity, with only seven tropical depressions, four of which reached tropical storm strength or higher.
 This led to the lowest Accumulated Cyclone Energy count since 1950, but not since 1900.
The 1887 Atlantic hurricane season was the most active Atlantic hurricane season on record at the time.
 However, it has been surpassed by the 1933 and 2005, now tying with the 1995, 2010, 2011, and the 2012 seasons for having the third most number of storms.
 The season ran through the summer and almost all of the fall in 1887, and was surpassed in total number of tropical cyclones only by the seasons of 1933 and the record-breaking 2005.
 The 1887 season saw tropical activity as early as May, and as late as December.
 Tropical cyclones that did not approach populated areas or shipping lanes, especially if they were relatively weak and of short duration, may have remained undetected.
 Because technologies such as satellite monitoring were not available until the 1960s, historical data on tropical cyclones from this period may not be comprehensive.
 An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 and zero to four per year between 1886 and 1910 has been estimated.
 Of the known 1887 cyclones, Tropical Storm One and Tropical Storm Three were first documented in 1996 by Jose Fernandez-Partagas and Henry Diaz.
 They also proposed large alterations to the known tracks of several of the other 1887 storms.
 Later re-analysis led to the known duration of Hurricane Six, and also that of Hurricane Fifteen, being increased.
Hurricane Olga was a late season Category 1 North Atlantic hurricane that formed during the 2001 Atlantic hurricane season.
 The fifteenth named storm, ninth and final hurricane of the 2001 season, Olga formed as a subtropical cyclone on November 24.
 After acquiring tropical characteristics later that day, Olga meandered westward, and eventually reached hurricane status on November 26.
 Olga’s winds peaked at 90 mph (150 km/h) before the storm turned southwestward and weakening back into a tropical storm.
 On November 30 it deteriorated further to a tropical depression, although it re-intensified two days later to tropical storm intensity.
 Olga then dissipated as a tropical cyclone on December 4 east of the Bahamas.
 Its damaging effects were limited to ships at sea.
 The cyclone's remnants produced heavy rainfall across the Bahamas and Florida.
 It was a relatively rare storm to exist in December, which is outside of the normal Atlantic hurricane season.
The 1930 Atlantic hurricane season was the second least active Atlantic hurricane season on record – behind only 1914 – with only three systems reaching tropical storm intensity.
 Of those three, two reached hurricane status, both of which also became major hurricanes, Category 3 or higher storms on the Saffir–Simpson hurricane wind scale.
 The first system developed in the central Atlantic Ocean on August 21.
 Later that month, a second storm, the Dominican Republic hurricane, formed on August 29.
 It peaked as a Category 4 hurricane with winds of 155 mph (250 km/h).
 The third and final storm dissipated on October 21.
The 1935 Cuba hurricane was an intense and deadly tropical cyclone which caused devastation across many areas of the western Atlantic, particularly Cuba and The Bahamas, in September and October 1935.
 The fifth tropical storm and third hurricane of the 1935 Atlantic hurricane season, the storm formed from a tropical depression in the central Caribbean Sea on September 23.
 The disturbance gradually organized as it moved to the west, and strengthened to tropical storm intensity less than a day after formation and further to a hurricane by September 25.
 Subsequently, the hurricane curved northward from its initial westward motion.
 On September 27, the storm reached major hurricane intensity before making landfall near Cienfuegos, Cuba as a modern-day Category 3 hurricane the next day.
 After passing the island, the hurricane reintensified, and reached a peak intensity with a minimum barometric pressure of at least 945 mbar (hPa; 27.91 inHg) and maximum sustained winds of 140 mph (220 km/h), making it a modern-day Category 4 hurricane.
 At the same time, the tropical cyclone passed over the Bahamian island of Bimini before moving out to sea.
 As it progressed northeastward, the hurricane gradually weakened before transitioning into an extratropical storm by October 2.
 The extratropical remnants made landfall on Newfoundland shortly after before dissipating late that day.