ALL forecasts contained on this site,  are based on my analysis and knowledge of various forecast tools, including information contained in NHC products, and are not copies from any other entity.

 You may click on the graphics for animations and close in views.

YOUR DONATION IS NEEDED… Your donation helps keep this site operational.  Funds assist in web hosting, weather software purchases and upgrades, and monthly professional site subscriptions (advanced computer model products for various forecast tools, Severe weather forecasting tools, etc.)  Your help is appreciated.

Funny dog holds dollars in mouth, isolated white background

Good day everyone!

While there is a lull in the weather, and we are not to the point yet of that possible low, I figured this would be a good time for a discussion on the 2014 Atlantic Hurricane Season, and the negative factors contributing to a below average season.

The 2014 Atlantic Hurricane Season ended at midnight, Dec. 01, 2014 (the season runs from June 01, to November 30 of each year).  The season closed out with the following totals:


Even with the inhibiting factors, the season wasn’t that far below average.  On average, a “normal” or “average” season produces 10 named storms, 6 hurricanes, and 2 major hurricanes…this average is prior to the upswing in 1995.  Averages over the 100+ year time frame were increased to 11 named storms, 6 hurricanes and 2 major hurricanes.

There were some numerous factors involved this season, which led to the reduction in activity in the Atlantic Basin, in which some of them work hand in hand.

A news article citing information from NOAA provided an explanation of why activity was suppressed, and most of what I will cover is contained in the report.  However, the following is sort of contradictory in the explanation of non development of El Nino, and wind shear over the Atlantic basin, in which I will explain my take on this, and may as well use it as a starting point.  From the article:

* A small note on the article by Bell…the use of the term atmospheric instability should state, atmospheric stability.  The sentence speaking of convergence, should read divergence, as divergence in the upper atmosphere causes sinking air.

The 2014 hurricane forecasts were more accurate than last year’s predictions. The 2013 hurricane forecast called for an above-average season, but had one of the slowest starts on record and fewer storms than predicted. This year, storm-crushing conditions in the Atlantic Ocean were already in place by spring, leading forecasters to predict fewer tropical storms. In May, NOAA projected for eight to 13 named storms, three to six hurricanes and two major hurricanes.

“What really suppressed the season was the strong wind shear and atmospheric instability across the Atlantic,” Bell told Live Science.

Most hurricanes begin as tropical disturbances offshore Africa or in the central Atlantic Ocean, a region called the Atlantic’s hurricane nursery. Strong vertical wind shear above the hurricane nursery can prevent these baby storms from growing stronger. That’s because wind shear, or winds blowing in different directions, tear apart a storm by pulling its bottom and top in opposite directions.

Other inhibiting factors over the central tropical Atlantic included dry air and an atmospheric phenomenon called convergence, which leads to sinking air. The sinking motion prevents storms from building tall thunderclouds, and dry air lacks the moisture that fuels storms. A weaker western Africa monsoon season is also one of the reasons for this year’s below-average hurricane season, Bell said. The monsoons kindle the tropical lows that eventually become hurricanes.

Another year

A quiet Atlantic hurricane season often occurs during an El Niño year, because the climate pattern triggers conditions that inhibit hurricanes. However, in the Pacific Ocean, the El Niño’s failure to launch meant the phenomenon had little impact on Atlantic hurricanes, Bell said. “El Niño never did form and it couldn’t affect the season,” he said.

I have read over the ENSO updates from the ENSO WRAP UP site over the past few months, and according to the findings, the teleconnection between the warmer sst’s in the Equatorial Pacific, and the atmosphere never occurred.  This has me a little perplexed, in the fact that an increase in wind shear over the Atlantic, is a result from El Nino conditions, as the subtropical Jet, which is mainly a winter time feature, becomes energized from the extra heat energy added to the atmosphere on the PAC side, strengthening the flow, creating strong westerlies over the Atlantic ocean.  Another phenomenon this season was, hurricane activity affecting Hawaii, which normally only occurs during an El Nino phase.

The Southern Oscillation Index (SOI) has been negative since the beginning of July.  This tends to indicate a shift in the trade winds over the Equatorial Pacific to which they blow from west to east.  To me, this would appear to signal at least some teleconnection between the atmosphere and the Nino regions.  So in closing on this aspect, wind shear did play a factor, however observations I made during the season, indicated shear was not a constant.



The SAL (Saharan Air Layer) or African dust seemed to have some increase in episodes this season, which added to the drier air we noted almost all season.  I don’t really have the time to research why, but a good portion of this dust seemed to originate over the same area as last season, NE of the Sahara, and flowing down just north and into portions of the MDR (Main Development Region).


To make it clear as to where the Main Development Region (MDR) is located, as it will be mentioned here, I have an old sst map which has the outline of the region


You will note, in the following sst (Sea Surface Temperature) anomaly images, anomalies were cooler than average over the MDR for the majority of the season.  You will also note, anomalies were much warmer north of 20N Latitude.  SST Anomalies were at average or below for most of the season, especially during the peak months.  One main factor for average to cooler anomalies, is the fact, that when averaged out, the NAO (North Atlantic Oscillation) pretty much stayed on the positive side.  As noted during my daily analyses during the season, we began with a strong Azores Bermuda high, or sub-tropical ridge, with this reoccurring during various times within the season.  This allows for a few things to happen…stronger trade winds allow for too much of an evaporation rate at the oceans surface, not allowing for heat to build vertically, and cooling the sea surface in the process, thus the heat is spread out over a larger area vice being concentrated for the energy needed to build thunderstorm activity.  Stronger trade winds also negate any surface convergence.

Stronger trade winds also allow for upwelling of colder water off of the African coast.  Along with this, heavier outbreaks of SAL block out the sun, which cuts down on insolation (Incoming Solar Radiation).

ALL of this together creates the following effect:  With warmer sst anomalies to the north, this is where most of the net upward motion, of lift occurred in the Atlantic, as although the Atlantic sst’s were warm, nature “sees’ these anomalies, and responds accordingly.  So by the convective process, if we have rising air north of the MDR, we have air spreading out in the upper atmosphere, cooling, and then sinking to the south.  As the air sinks, it warms due to compression.  As the air warms, it dries out the surrounding atmosphere, hence all of the dry air we noted for a majority of the season.  Another factor was a slightly stronger than average subtropical ridge, which enhanced the sinking motion.  This is why we experienced a lack of atmospheric instability over the Atlantic for the season.


The Atlantic Ocean Tripole was lacking during the season as well.  The Tripole is where we notice warmer sst anomalies above 40N Latitude, as a general rule, colder sst anomalies extending from approximately 40N, south to 30N, then much warmer sst anomalies in the MDR.  The difference in the colder anomalies, and warmer anomalies in the MDR allow for maximum net upward motion (warm rising air) in the MDR, thus creating a reversal in what I just mentioned previously.  This enhances moisture in the tropics, and vertical motion for thunderstorm development.  These warmer anomalies in the Atlantic occur when the subtropical ridge is weaker than normal, or during a sustained negative NAO phase.  The first graphic shows a fairly good Atlantic Ocean Tripole setup, which favors enhanced tropical activity.


The next SST map shows a classic tripole setup on May 17, 2010


The following sst anomaly maps are from this season during mid month from June through September.  Notice the difference in the anomalies from 2010


JULY 14, 2014

AUGUST 14, 2014

SEPTEMBER 11, 2014

The one last item I’ll mention is, I’m sure everyone noticed we did not really have a Cape Verde season to speak of.  This was attributed to a weaker African Monsoon season. Albeit we saw the West African Monsoon trof modulate almost every two weeks in the far Eastern Atlantic, energy and moisture was just not available to energize it.  The main contributing factor in this is the mainly negative phase of the Indian Ocean Dipole.  There is a positive and negative phase of this phenomenon, not too much unlike the Atlantic Ocean Tripole.  When sst anomalies are cooler over the western portion of the Indian Ocean, the Dipole is said to be in a negative phase, and vice versa.


As you can notice, a NEGATIVE IOD phase doesn’t allow for energy or moisture to cross into the African continent, pretty much leaving dry conditions.  Not very favorable for formation of African waves over the continent.



This pretty much summarizes the combination of factors which led to below average Tropical Cyclone Activity for the 2014 Atlantic Hurricane Season.

Have a blessed day!

GMCS, USCG (ret)


About palmharborforecastcenter

I am a Tropical Forecast meteorologist, providing hurricane forecasts during the Atlantic Hurricane Season. I retired from the U.S. Coast Guard in July of 2001. Meteorology became my passion in high school, and I have continued my educational background in meteorology since 1996, when I undertook the study of Tropical Meteorology. While working toward my degree, I had to unexpectedly withdraw from college due to my oldest sons medical reasons. I do however, meet the educational criteria of the AMS to be recognized as a meteorologist. Studies include, but are not limited to the Navy Aerographers Mate course, Naval METOC meteorology course, Meteorology 2010 Sophomore level course while attending St. Petersburg College, Clearwater, FL., Basic Forecasting course for operational meteorologists from Rapid WX, meteorology institute, a four month meteorological internship, and extensive research on numerous meteorological topics such as the MJO, NAO, satellite imagery interpretation, etc. I have been forecasting Tropical Weather (Tropical Storms and Hurricanes) since 1996, with my main client being three different Coast Guard Commands.
This entry was posted in Tropical Synopsis. Bookmark the permalink.


  1. Mac says:

    Thanks for the excellent report. And I vote with Della! My mother, brother and sister all lost their homes to Katrina. 2 were demolished and one gutted and rebuilt.

  2. Monty says:

    Thanks Storm. Great explanation as always. This makes you wonder when another 2005 season will roll around??

    • Right? If the NAO doesn’t get out of the positive, I’m not sure next season will be any more active

    • dellamom says:

      Can I go on record as voting AGAINST another 2005 season? SE Louisiana was decimated by Katrina, and then Rita came and destroyed portions of SW Louisiana and Texas. My sister’s family was still relocated to Beaumont when Rita hit, but visiting her brother-in-law in Baton Rouge for the weekend to get the kids out of the confines of the hotel room for the weekend. So … due to Rita, they lost everything they had brought with them for their Katrina evacuation and the little bit they had accumulated in Beaumont. They came to me in Mandeville with only the clothes they had taken for their Baton Rouge weekend. It was heartbreaking and my sister still has issues related to that time. So, again, I vote against another 2005.

      • I don’t want to see another 05 either. Not only because of what you just posted, but I had so many storms going at once and had to analyze each set of conditions for each one, I spent 7 hours straight at my PC one day.

  3. originallt says:

    Thanks Storm for your research and posting part of they article. Another”contradictory” factor that seems to be off, is the statement by Bell that “instability” played a part in lessening the amount of hurricane/ tropical storms. That doesn’t add up. I would have thought that “Stable” conditions would be an inhibiting factor for development, not instability? A stable atmosphere would inhibit “lift” which you need to have tropical development.

Leave a Reply

Fill in your details below or click an icon to log in: Logo

You are commenting using your account. Log Out / Change )

Twitter picture

You are commenting using your Twitter account. Log Out / Change )

Facebook photo

You are commenting using your Facebook account. Log Out / Change )

Google+ photo

You are commenting using your Google+ account. Log Out / Change )

Connecting to %s