Season Fishing Forecast for 2011:
Unusual Year So Far, But Likely to Improve
By Mitchell A. Roffer, Ph.D.
Background:
Since 2003 we have been developing an objective method for forecasting the overall fishing
action at all of the Bahamas Billfish Championship (BBC) tournaments. The hypothesis for forecasting
the seasonal marlin fishing action stems from the location and geographic extent of the bluer and
often warmer water that occurs from the Cat Island – San Salvador Island area where it is presumed
that the marlin concentrate before and during spawning. We have been calling this water “blue marlin
water.” We assume that the marlin are associated with this water and the more “blue marlin water”
that exists in the Abaco Islands and Eleuthera Island areas, the greater the marlin relative apparent
abundance will be in these areas.
Based on our observations of the fishing action in the Bahamas over the last 20 years it
appears that excellent fishing action overall occurs within the BBC tournament area when there is a
substantial volume of the “blue marlin water” pushing over the 100 fathom ledges along the eastern
side of Eleuthera and Abaco. Relatively good fishing seasons occur when this water occurs over the
1000 fathom curves, but not the 100 fathom curve of both areas. Mediocre years occur when there is
a lack of this water over these areas. Good fishing action is also linked to favorable currents and
when the water mass boundaries of these currents are stable for three to five consecutive days over
good bottom topography to concentrate the bait. For the BBC tournament areas, the dissolved
oxygen concentration does not appear to be a major factor compared with the temperature and clarity
of the water. In other areas south, the dissolved oxygen is a major controlling factor on fish
distribution.
During the last several years, the conditions were particularly favorable as early as January
and February in terms of the presence of “blue marlin” water off Abaco and Eleuthera. However, due
to the currents generated by relatively large eddy features located 60-90 miles northeast of Eleuthera,
the “blue marlin” water was pulled away from the BBC tournament area. In these years there have
been several days when some of this water moved into the tournament area and catch rates
increased. Unfortunately, these favorable conditions were not persistent throughout the entire
tournament season.
One of the challenges of producing a forecast of the oceanographic conditions for the BBC
Tournament is that these fishing events extend over a relatively long time frame, from the last week in
April through the third week of June, 2011, and that conditions are likely to change dramatically from
one event to the next. In addition, there are no reliable numerical oceanographic models or even
atmospheric models to use to make high resolution forecasts. The models provide some guidance,
but for the needed spatial and temporal resolution, we are forced to rely on our qualitative experience
as we have been monitoring the conditions over the Bahamas for over 20 years. This experience is
based on the satellite observations of the ocean conditions derived by Roffer’s Ocean Fishing
Forecasting Service, Inc. – ROFFS™ (www.roffs.com) on a near hourly basis. The satellite data
(infrared for sea surface temperature and ocean color for indices of phytoplankton, clarity, and
colorized dissolved organic material) are received from a variety of sources including, but not limited
to NASA, NOAA, and the European Space Agency. We also use data derived from drifting buoys and
from satellite altimeters. The altimeters provide a very course resolution and the time delay (10 day
mean) limits the data’s utility. In addition, we also rely on climate data, analyses, and forecasts
provided by Columbia University’s International Research Institute for Climate and Society, known as
IRI (http://portal.iri.columbia.edu/portal/server.pt), and NOAA’s climate prediction website
(www.cpc.noaa.gov/), as well as, the Florida State University Center for Ocean-Atmospheric
Prediction Studies program (www.coaps.fsu.edu).
Each year we are asked about the El Niño – La Niña situation although there are no obvious
direct effects on the ocean conditions during the BBC tournament season. Perhaps by next year we
will learn to use another index like the North Atlantic Oscillation (NAO) index. In the meantime we will
discuss the popular conditions. Presently there is a La Niña condition in the eastern tropical Pacific
Ocean that is weakening. By June the El Nino Southern Oscillation (ENSO) index conditions are
forecasted to be neutral by the NOAA Climate Prediction Center. However, this suggests an
enhanced chance for below-average precipitation and above average air temperatures across a
substantial portion of the U.S. southern states west of Florida. However, Florida and the northern
Bahamas are forecast to have “normal” or mean air temperature conditions. The southern Bahamas
and Caribbean Sea area is forecast for below normal conditions. The forecast for south Florida is for
slightly below normal precipitation, normal for the Bahamas and slightly below normal for the
Dominican Republic. As we enter ENSO neutral conditions, we anticipate that the air temperature and
precipitation will not be controlled by the ENSO circulation, but more zonal with tropical conditions
dominating the control of the weather.
We have learned that it is important to consider the present conditions (end of February –
beginning of March) in the area covering south Florida to the Bahamas as an indicator for determining
if we are experiencing warm, cool, or mean conditions. [We have learned this because big and bad Al
Behrendt (ruler of the BBC Tournament) makes me “an offer I can’t refuse”, without payment into
making a long term fishing forecast.] The nine year (2003-2011) mean sea surface water
temperature (SST) for the core of the Gulf Stream off Miami is 78.2°F during our standard March 05-
06 measurement period. The range has been as low as 74.8°F (2009) to a high of 80.5°F (2007).
This year the SST was 78.1°F. While have not been recording the SST off Cat Island during this
same period, the four year mean (2008 – 2011) SST for the Cat Island area is 75.6°F and this year
the SST was 74.3°F. However, the blue marlin water is not presently surrounding Cat Island, rather it
is around the San Salvador area and farther south which is not a good omen for blue marlin fishing
action during the BBC. |
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Figure #1 and Figure #2 represent the ocean conditions at the end of February, 2011. Figure #1 is a
false color enhanced thermal infrared image for sea surface temperature composed of satellite data
observed on February 20th and 22nd. Figure #2 is a false color enhanced ocean color image for the
same period ( February 20th and 22nd ).
The warmest and bluest water in Figures #1 and #2 is the “blue marlin water” and extends
from the area southeast of Cat Island to the area northeast of Cat Island, east of Eleuthera and east
of Abaco. The motion of the water is complex and since a movie often provides more details than the
space here allows for a text description, we have made a movie loop for your viewing. See the QuickTime movie below that allows you to visualize the motion. This movie is composed of daily
satellite images looped into a movie. Overall the “blue marlin” water is being pulled offshore of Long
Island (south of Cat Island) by a relatively large clockwise eddy that is centered approximately 45
miles east of San Salvador. This eddy is pulling the water northeastward and a significant amount of
this water is being pulled farther offshore from Cat Island and Eleuthera by a counter-clockwise eddy
that is centered approximately 60 miles east of Eleuthera. This is not favorable for good blue marlin
action over the ledges off Cat Island and Eleuthera. See Figure 3 (below) for a better view of these
eddy features during March 10-11, 2011 despite the cloud interference in the northern part of the
satellite image. Due to other eddy features located farther northeast (east of Abaco), the “blue marlin”
water is being pulled mostly away from Abaco. However, due to circulation east of Abaco, within 60
miles, some of this “blue marlin” water has been pulled relatively close to Abaco. Unfortunately,
during the first 10 days of March, much of this water has been pulled away from Abaco resulting in
relatively poor blue marlin conditions. This is seen in the movie loop. These conditions would normally
suggest that the oceanographic conditions over the BBC tournament areas are unfavorable for a
productive blue marlin season.
2011 SEASONAL FORECAST
While the present conditions over the BBC tournament areas are not optimal for productive
blue marlin fishing action, we have evidence that the non-favorable conditions will change and
improve substantially. Figure #3 is a false color enhanced infrared satellite image derived from March
11-12, 2011 that shows the surface ocean circulation based on the signature temperatures of the
currents from the area east of Eleuthera to Mayaguana. Evaluation of the satellite data (see below) from the
Bahamas to Venezuela along with the freely available U.S. Navy NLOM model
(www7320.nrlssc.navy.mil/global_nlom32/ias.html) and HYCOM model
(www7320.nrlssc.navy.mil/GLBhycom1-12/intram.html), as well as, the satellite altimetry data
available NOAA Atlantic Oceanographic and Meteorological Laboratory
(www.aoml.noaa.gov/phod/altimetry), it appears that the two eddy features shown are likely to move
northwestward over the next several weeks. We have included the two model movies on our website
as well. As these circulation features move northwestward, they will pull the “blue marlin” water
toward both Eleuthera and Abaco. When this occurs, the conditions over the BBC Tournament areas
will improve substantially. The final path and timing of the motion of these and other eddy features are
a function of many factors including the size and motion of the eddies that presently occur east of
Abaco, north of the northern Bahamas island chain and along the eastern side of the Gulf Stream
east of Florida. Also it remains to be seen if the currents and water mass boundaries of the “blue
marlin” water become favorable and stable for 3-5 days during the tournaments to concentrate the
bait over specific areas where good bottom structure exists (e.g. the Bridge, Pocket, Jurassic Park) to
produce excellent hookup rates. For this one must evaluate the circulation just prior to and during the
tournaments. However, at this time we are forecasting a good blue marlin season for the BBC
tournaments, even though it does not look good presently. |
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Figure #3 is a false color enhanced infrared satellite image derived from March 11-12, 2011 that shows the surface ocean circulation based on the signature temperatures of the currents from the area east of Eleuthera to Mayaguana.
Safe and Successful Fishing,
Mitchell A. Roffer, Ph.D.
( www.roffs.com) |
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February 18 - March 9, 2011 - ROFFS™ QuickTime Movie of the Ocean Circulation in the Bahamas |
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February 15 - March 16, 2011 - Inter-American Seas SST Nowcast Naval Research Lab HYCOM Model |
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February 09 - March 10, 2011 - Inter-American Seas SST Global NLOM Model |
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