WASHINGTON – It was a hurricane season almost without hurricanes. There were just two, Humberto and Ingrid, and both were relatively wimpy, Category 1 storms. That made the 2013 Atlantic hurricane season, which ended Saturday, the least active in more than 30 years — for reasons that remain puzzling.
The season, from June through November, has an average of 12 tropical storms, of which six to seven grow to hurricane strength with sustained winds of 74 mph (119 kph) or greater. Typically, two storms become major hurricanes, Category 3 or stronger, with winds of at least 111 mph (179 kph).
In 2013, there were 13 tropical storms, a typical number, but for the first time since 1994 there were no major tempests in the Atlantic. The last time there were only two hurricanes was 1982.
The quiet year is an outlier, however, in the recent history of Atlantic cyclones. The National Oceanic and Atmospheric Administration notes that 2013 was only the third calmer-than-average year since 1995.
The most intense storms this year had maximum sustained winds of only about 86 mph (138 kph). Phil Klotzbach, a researcher at Colorado State University, said that is the weakest maximum intensity for a hurricane during a season since 1968.
In terms of accumulated cyclone energy (ACE), the seasonal total stands at 31.1, the lowest since 1983 and just 30 percent of average. Looking back to 1950, only four other years had lower ACE totals: 1972, 1977, 1982 and 1983. ACE is the sum of the squares of all of the storms’ peak wind speeds at six-hour intervals, and is a good measure of a storm season’s overall power.
To put that in perspective, Hurricane Igor (2010) alone racked up about 140 percent of this season’s total.
Heading into the season, all signs pointed toward a very active one. Forecasters predicted seven to nine hurricanes, with higher-than-average ACE.
Why was this season so inactive? What did the forecasts miss? Although there are some hypotheses, it is not entirely clear. We may have to wait another couple of months, but in the meantime, there are some possible explanations.
Major signals such as the El Nino Southern Oscillation, surface pressure and sea-surface temperature all pointed to an average to above-average season. But there were some possible suppressing factors.
Dry air: Even over the long three-month window of August to October, the vast majority of the tropical Atlantic was dominated by drier-than-normal air, especially in the deep tropics off the coast of Africa. Dry air can quickly weaken a tropical cyclone, or inhibit its formation.
Stable air: The average temperature profile in the region was less conducive to thunderstorm growth and development during the core months, which means that the amount of rising air in the region may have been reduced as well.
Weak African jet: Tropical waves, the embryos of many tropical cyclones, have their origins over Africa. A persistent feature called the African easterly jet stream — a fast-moving river of air in the low and middle levels of the atmosphere — extends from Ethiopia into the tropical Atlantic Ocean. It breaks down into waves, and every few days another wave leaves the coast. Some are barely noticeable, while others become tropical storms. This year they were weaker. One would expect that to have a big impact on the amplitude of easterly waves, and the hurricane season.
One question that inevitably is asked is how the season’s inactivity relates to climate change. It is not accurate to associate any particular season (and definitely not a specific storm) with climate change. One season’s activity does not allow any conclusions about the role of climate change. The reason is that intra- and inter-seasonal variability is so large that any subtle signals of influence from climate change are overwhelmed.