SST Analysis
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Tropical cyclones thrive in waters warmer
than 26° C and degenerate in waters below that temp. Areas south
and east of the red line have the potential for a tropical storm
strike
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Last year was a tough year for meteorologists in the Atlantic. Based on
data through January of 2006 they forecast an Atlantic Hurricane Season
nearly twice as intense as normal. Instead, a far lighter than normal
season occurred giving forecasters the black eye of a 67% error. Some
of those who believe that global warming is a fairy tale were quick to
seize on this error to discredit science. There were a number of factors
that materialized following the January data that were responsible for
the error in forecasting. The current degree of sophistication in weather
forecasting is a very new science and forecast models are built on historical
data. This historical data reaches back maybe 100 years in the Pacific
Basin. The accuracy of this data has improved exponentially over the last
40 years. Early satellite tracking of storm paths began in the late 1960's,
satellite radar, infrared and Doppler radars have only become an effective
tool in the last 25 years and wind speed satellite imagery has been around
less than a decade. As you can see, the data sample is probably less than
200 hurricanes worth of detailed Pacific (specific) data.
Despite this the Eastern Pacific long range forecast has
held to a much better batting average than it's Atlantic counterpart.
The Pacific forecast holds to about a 89% accuracy rating compared to
the Atlantic's 78%. This is good news for us here in Baa Sur, as they
are predicting a lighter than
average hurricane season for 2007
SST Anomaly
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The colors represent deviation of this years water
temperatures from the norm. Green is normal, blue colder than normal
and yellow warmer than normal waters.
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We have two active tropical cyclones at the time of the
writing of this article, TD Alvin, expected to wither away harmlessly
in the Pacific and TS Barbara which may pose a Hurricane 1 threat to southern
Mexico this weekend. Neither of these storms were spawn by tropical waves.
looking at the wide angle Surface chart below we can see there is our
first
tropical wave of the season in the pipeline.
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With 2 tropical cyclones active in the Pacific (red arrows) there
is one tropical wave (yellow arrow) on its way across the Atlantic.
(click to enlarge)
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Tropical waves are supercharged waves of air coming off
the deserts of Africa. These waves travel along the Inter Tropical Convergence
Zone or
ITCZ across the Atlantic and the Pan-American Isthmus to the Pacific.
Those waves that don't spawn storms in the Atlantic stand a pretty fair
chance of stimulating a cyclone in the Pacific. This is why in July of
2005, when there was a plethora of storms in the Atlantic/Caribbean side
the Pacific was relatively tranquil.
Sea Surface Temperatures are another factor to look at
when we look at the chance of tropical cyclone formation. First let's
look at the SST Analysis above. Tropical Cyclones need water warmer than
26°C to form and strengthen. Storms dissipate fairly rapidly once crossing
the 26°C thermo cline, indicated by the red line. Areas north of that
line have little chance of being struck by a tropical cyclone. In the
animation, you can see how the red line has begun to advance northward
as the ocean warms. Also note the growing area of +30°C water in what
we will call the Eastern Pacific Hurricane Birthing Zone. Almost all of
our Eastern Pacific hurricanes form in this region. It will be early August
before the 26°C thermo cline advances far enough north to include Baja.
The earliest tropical cyclone to make landfall in Baja is August 15th
and the latest is October 17th.
Sea Surface Temperature Anomalies are a second tool to
look at when anticipating hurricane formation. SST measures the amount
of kinetic energy in the surface of the ocean. The more energy, the greater
the likelihood of cyclonic formation. When we look at the anomaly, or
difference over normal years, water above normal presents a greater than
average threat of storm formation. On this animation we can see the La
Nina event occurring at the bottom of the frame, near the equator. The
dark blue represents colder than seasonal water. Light blue water represents
normal temperatures while yellow and eventually red, represents warmer
than normal water. The scale in in °C. Of slight concern to us early in
the season in the above normal temperatures in the hurricane birthing
zone off the southern coast of Mexico. The entire region is up to a little
more than 1°C warmer than normal. This is only significant when you think
about how much energy it takes to make a region that large, warmer than
normal. With Barbara active in that region we can expect that next week
some of that energy will be dissipated.
So now the fun part... what is in store for the week ahead?
I think Alvin is a done deal, headed out harmlessly into the Pacific to
fall apart. On the other hand, the jury is still out on TS Barbara. The
NHC models have consistently overestimated the durability of tropical
cyclones over the last year. I think Barbara may strengthen some, but
never reach the peak intensities the forecasts currently call for. Our
first tropical wave has to travel across the jungles of northern South
America before reaching the Pacific. It will need 4-6 days to reach the
basin and in that time adequate moisture and energy may reform, following
the passage of Barbara. I am going to bet that the tropical wave will
fall on dry air if it even makes it to the Pacific and we'll probably
have to wait a week or two for the next storm formation. Either way, we
will be warm and dry here in Baja Sur.
Until June 12th... Clear skies and fair winds!
Tomas
Our Eastern Pacific Hurricane
Watch is an editorial analysis of data from the National Hurricane Center,
NASA and NOAA and is based on information provided by the same, but is
an amateur endeavor. For actual storm information readers should refer
to
notices and warnings posted by the National Hurricane Center.
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