Hurricanes, Typhoons, & Tropical Cyclones
Learning Goal 9e: Describe hurricane structure, and how and where they form and move.
Climatology of these Storms
Source: NASA.
A hurricanes, also known as a tropical
cyclones or typhoons
in other parts of the world, are rotating storms about 150 to 300 km in horizontal
diameter, and about 15 km thick in the vertical. They have extremely strong winds and high waves, so
==> all ships should avoid them <==.
Hurricanes form over tropical oceans having sea-surface
temperatures greater than about 26°C, because these high temperatures
cause very strong evaporation rates from the ocean into the air.
Thus, most hurricanes form between the
Tropic of Cancer (23.5o N)
and the Tropic of Capricorn (23.5o S), where the warmest ocean-surface waters are located (see first figure below).
However, hurricanes cannot
form at the equator, because Coriolis force is zero there. The Coriolis effect is what gives hurricanes their rotation, which is needed for storm longevity. As a
result, the latitude bands that favour hurricane formation are
indicated by the green bars in the second figure below.
Source for figure above: NOAA ESRL PSD. https://www.esrl.noaa.gov/psd/map/clim/sst.anim.year.html
Because hurricanes form in the tropics in regions of the trade
winds,
most hurricanes are initially blown by the trade winds from east to
west across
the tropical oceans. As the hurricanes reach the westward side of
ocean
basins, the turning winds around the climatological high-pressure areas
(the Bermuda High over the North Atlantic oceanm or the Hawaiian High
over the North Pacific Ocean, see Learning Goal 9d) cause the hurricane
tracks to turn poleward. As these storms continue away from the
tropics, they move over colder water or land, and thus die because they
lose their fuel supply of warm humid air. Typical tracks are
shown in the figure below. From this figure, you can see that the
largest number of most intense storms occur in the western North
Pacific as typhoons.
Tracks of hurricanes, typhoons & other
tropical cyclones during 1945 - 2006. No hurricanes at the equator. Attribution: Citynoise at English
Wikipedia.
https://commons.wikimedia.org/wiki/File:Tropical_cyclones_1945_2006_wikicolor.png
. CC BY-SA 3.0. Captured 15 Feb 2019, and annotated by R. Stull.
These storms typically form in the late summer and fall seasons,
when the ocean surface is hottest. Thus, in the Northern
Hemisphere, these storms are most frequent during 1 June to 30
November, with peak occurrence in August or September. In the
Southern Hemisphere, these storms a most frequent during 1 November to
30 April. But in the Pacific, typhoons and tropical cyclones have
been observed in every month.
If you are sailing in tropical waters at locations where these
storms are found, during months when these storms frequently occur,
then you should carefully monitor all cyclone predictions and warnings
via radio and satellite-internet and sail away from the path of these
storms. Hurricane/typhoon/tropical-cyclone prediction has a lot
of uncertainty, so it is best to stay well clear of the predicted paths
of these storms and frequently monitor the weather bulletins for updates.
Hurricane triggering, structure and evolution
Hurricanes start as clusters of thunderstorms over tropical
oceans. These thunderstorm clusters can be triggered several
different ways. One triggering mechanism is the Intertropical Convergence Zone (ITCZ),
where the horizontal trade winds from the northern and southern
hemispheres converge (come together) force the air to rise to make a
band of thunderstorm clusters (see first figure below). Another
triggering mechanism are meanders (easterly waves)
in a low altitude (3 km above mean sea level) stream of fast moving air
called the African Easterly Jet (see second figure below).
Convergence of air triggers clusters of thunderstorms on the east side
of each crest (poleward meander) of the waves.
As water vapour condenses in these thunderstorm clusters, the
condensation releases latent heat, causing the stormy air to get
warmer. As more heat is released, the atmospheric pressure near
the tops of these storms start to increase, creating a pressure
gradient that drives air horizontally out of the top of the
thunderstorm cluster. This upper-level outflow is the "exhaust
system" for the storm, which removes some air molecules from the stormy
region. The net result is that the air pressure near sea level
begins to decrease, because of the less weight of air above.
A feedback occurs where this low-surface pressure under the
thunderstorms will suck in more low-altitude, warm, humid air from
outside the storm. This is the "intake system" or fuel supply for
the storm, allowing the thunderstorms to intensify by causing more
condensational warming of the core
(center) of the storm, thereby creating faster outflow at the top of
the storm (exhaust system). The first level of progression is a tropical
depression, which has winds of 37-63 km/hr. As the storm intensifies, the tropical
depression then becomes a tropical storm
as winds continue to build to 64-118 km/hr, and once winds build beyond
119km/hr, the tropical storm
becomes a hurricane (or typhoon or tropical cyclone).
Hurricane intensity is classified according to the Saffir-Simpson
Hurricane Wind scale (see table below). Similar scales are used
to classify typhoons and tropical cyclones. (Compare this
classification with the Beaufort Wind scale from Learning Goal 8e.)
Source: R. Stull: Practical Meteorology. Used with permission.
The hurricane usually has a well-defined "eye" with nearly calm winds, somewhat clear skies, and no precipitation. Surrounding the eye is an "eye wall"
of intense thunderstorms, which has the strongest winds and heaviest
rain. As near-surface air is drawn in toward the low pressure at the
eye of the storm, Coriolis force
causes the winds to turn to their right in the N. Hemisphere, or to the
left in the S. Hemisphere. As a result, the near-surface winds in
hurricanes spiral counterclockwise in the northern hemisphere and
clockwise in the southern hemisphere.
Hurricanes are some of the most severe weather events experienced on
the planet. Some of the worst hurricanes in history have claimed
hundreds of thousands
of lives.
When planning a sailing trip across the open ocean, it is important
to consider your course and how it relates to areas of hurricane
formation during hurricane season. It is also important to be able to
recognize conditions that could progress into a hurricane and avoid
sailing anywhere near these areas.
Swell
Hurricanes will also produce large ocean swell (recall Learning Goal 8d), which could reach you
days after the hurricane
has died down, or the swell could propagate ahead of the storm and
reach your sailboat before the hurricane arrives. Swell from
distant hurricanes can create large, dangerous waves close to shore.
Storm Surge
As hurricanes
approach land, the winds push large amounts of water up against the shore,
creating what is known as a storm surge
(a local rise in sea level). This mass of water can inundate (flood)
a coastline and destroy its
infrastructure (marinas, docks, port facilities). High tides, high
breaking waves, and onshore winds can increase the severity
of the storm surge. At coasts hit by hurricanes, boats at dock
are often destroyed and/or driven up onto the beach by the wind and
waves.
Additional Resources: (non-required material)
Earth Observatory, NASA – Hurricanes: http://earthobservatory.nasa.gov/Features/Hurricanes/
Videos: (non-required material)
Hurricanes 101: https://www.youtube.com/watch?v=zP4rgvu4xDE
For a more thorough description of hurricanes, see Stull, 2017: Practical Meteorology. https://www.eoas.ubc.ca/books/Practical_Meteorology/prmet102/Ch16-TropCycl-v102.pdf