I expected that moving to the East coast of India for college would be all about the beaches and the Rassagulas. However, 2 years into my stay in Odisha I experienced FANI. Being in the eye of the storm (literally) of something that used to be an ignoreable news story was genuinely scary and I have been obsessed ever since. And as Hurricane Beryl follows the Indian cricket team in taking the Caribbean by a storm, I wanted to take a look at tropical storm climatology. Stronger storms are occurring earlier in the season and getting intense faster, exposing generally vulnerable coastal communities to even greater risk of destruction. But first we actually have to gather this data.
Storm classifications and reporting depend upon the meteorological agency that is monitoring the region. If the storm begins life in the North Indian Ocean basin it will be monitored by the Indian Meteorological Department. IMD will apply it's own storm categorisations to it and will name the storm accordingly. There are 7 such major basins, some of the basins are monitored by more than one agencies. Not only are the category labels different between the different scales, the method of measurement also differs. The World Meteorological Organisation recommends using 10 minute sustained winds, 10 m above the surface for categorisation of storms. However, the IMD scale uses 3 minute averages, the US scale uses a 1 minute average. The Australian scale is a further departure using a combination of 10 minute sustained winds and wind gusts for their categorisations.
This makes comparisons between basins somewhat difficult, although alternative scales with more useful parameters have been developed to make this task easier. It is also why this handy graphic I have made is only useful for educational purposes. In practice, due to the differences in measurement methods only the Tokyo and Meteo France scales are comparable.
Researching storm classifications made me pretty pessimistic about finding homogenous data that would be easy to plot. But then WMO to the rescue, working with the various meteorological departments that monitor the different basins, WMO compiles International Best Track Archive for Climate Stewardship (IBTrACS), talk about a laboured acronym. This is a near real time dataset that compiles information about tropical and extra tropical storms all in a single file, information from each meterological agency is given alongside the WMO reported values for every storm in the list that goes back to 1842. The entire dataset is available on the NOAA NCEI website. So, let's ask some questions of it, first up, are we getting more cyclones?
There certainly appears to be a large increase in number of reported storms between 1960 to 1980, plateauing out in the more recent decades. Is this climate change?
flashback to April 1960... . The space race is rapidly approaching, new avenues of Earth observation are about to open. The value of satellite weather observations continues to be unproven because of the repeated failures of the Vanguard 2 satellite. It's successor, The Television Infrared Observation Satellite Program (TIROS) was the first weather satellite to successfully reach orbit and begin observations. An explicit goal of the TIROS satellite was to improve decisions that are otherwise hard to make from Earth-bound observations like "should we evacuate the coast because of a hurricane?". and with TIROS beginning continuous coverage of the Earth's weather in 1962 we began to identify more storms that might have otherwise gone unnoticed or would have lacked enough observations to be included in the archive. Since, 1960 we have continued to add more weather satellites into orbit around the planet and today we have a near continuous and universal coverage of the entire surface of the planet in multiple spectral bands. And that is the steep increase in storm counts from 1960 to 1980.
Zooming in on the storms from the last 44 years, we see that there is no appreciable increase in number of storms of any category.
Tropical storms acquire their energy from the rising latent heat from the ocean surface. So it stands to reason that tropical storms are able to gain energy more easily when sea surface tempertures are higher.
The large scale shifts in ocean and wind circulation that are caused by the EL Nino cycle effect nearly all weather patterns around the world, Hurricane formation is no different. The coming of a strong El Nino period results is significantly higher East pacific temperatures and a break down of the Easterly trade winds. This forms the perfect conditions for storm formation in the Pacific and much more stable conditions in the Atlantic. The resulting effect is that American shores find reprieve from being bashed around by hurricanes. We can see that whenever there is a positive El Nino period, for instance the one that begins around 2016, it coincides or is just preceded by a sharp decline in tropical storms.
The dominant effect of internal climate variability on storm formation also makes it harder to observe any changes that may be caused due to climate change. While it is a welcome realisation that the number of tropical storms is not increasingly drastically with climate change it does not mean that the process is immune to the effects of a warming planets. One effect is that the storms that do take shape have more food to available and so they grow stronger and more violent.
By food I mean latent energy and by stronger I mean they-have-faster-wind-speeds. Rapid intensification is when a storm undergoes an increase in sustained winds that is greater than 30 knots (55 Kmph) within 24 hours.
With greater average Sea Surface Temperatures the storms more and more storms are undergoing more and more violent intensification events.
The most dramatic of weather events that cause the most visceral damage to humans does not appear to be undergoing a dramatic worsening because of climate change. But the damage they cause is worsening, storm surges get higher every year as sea level rises, exposing new regions to storm flooding. The increasing amounts of latent energy that is being taken up by storms leads to changes in their dynamics, causing greater amounts of rainfall. All these effects have been shown to be caused by anthropogenic climate change and will continue to become more extreme as temperatures rise.