Wednesday, May 1, 2024

Hurricane outlook part three

 

Here is part three of 2024 Atlantic hurricane season outlook.

The Atlantic hurricane season officially starts in 31 days. And many want to know what looks to happen. This multipart series as tried to bring you just that. But now is the time to prepare for what could be a busy season. This will be the final part of this multipart hurricane season outlook.   

You can find the first two parts here

Part one

Part two

In those two parts I emphasized the two main factors that will greatly influence how much tropical activity we see in the Atlantic basin this season.  The first is the El Nino Southern Oscillation (ENSO). The second are the well above average sea surface temperatures (SST) in the tropical Atlantic.

I was going to just show basic numbers for the final part of the hurricane outlook. But I’ve decided to do the opposite, and dive into details I didn’t cover in parts one and two. So, if you want to avoid the data and how I’m arriving at my conclusion, you can skip to the end.

This outlook is probabilistic in nature, meaning the stated outcomes fall within a certain likelihood of occurring. It is based on meteorological scientific principles and my understanding of the current global weather pattern and how I think it will evolve. As always, I’ve tried to make everything as easy to understand as I can.    

At the end of this outlook, I will include a look at what our summer pattern might look like.

SST:

 


The Pacific Ocean …

When we look at SSTs, we can see the equatorial eastern Pacific is much cooler than it was a few months ago. So, the El Nino is rapidly weakening. We can also see those above average SST in the Northwest Pacific around the Aleutians with the colder SST in the Gulf of Alaska.   All of this is going to have huge implications on this year’s Atlantic hurricane season.


El Nino Southern Oscillation (ENSO)…

The ENSO sets up a weather pattern that can help predict a strong or weak Atlantic hurricane season. These two phases are called El Nino and La Nina.  EL Nino tends to increased vertical wind shear (the change in wind speed and direction with height) over the Atlantic, this makes it hard for tropical cyclones to develop and strengthen.  La Nina tends to favor lower vertical wind shear; it is generally correlated with a busy Atlantic hurricane season.

Below is an image that shows where the ENSO 1+2, 3, 3.4, and 4 regions are located.

 


Region 1+2 is the smallest and farthest east. Regions 3 and 4 cover the east and west and together cover a large part of the tropical Pacific. Most analyses and forecasts are focused on a combination of regions 3 and 4, seen on the image as the main Nino 3.4 region.

El Nino: characterized by a positive ONI greater than or equal to +0.5ºC.

La Nina: characterized by a negative ONI less than or equal to -0.5ºC.

By historical standards, to be classified as a full-fledged El Nino or La Nina episode,

these thresholds must be exceeded for a period of at least 5 consecutive overlapping 3-month seasons.

The CPC considers El Nino or La Nina conditions to occur when the monthly Nino3.4 OISST departures meet or exceed +/- 0.5ºC along with consistent atmospheric features. These anomalies must also be forecasted to persist for 3 consecutive months.

La Nina is really ramping up.  The La Nina is developing even faster than was expected. As El Nino continues to collapse, we’re close to neutral conditions (we could be neutral already).  But at this time, La Nina conditions are expected to take over by the summer and last well into the winter of 2024-2025. Right now, it looks like we will likely have at least a weak La Nina for the peak of the Atlantic hurricane season (August-October).

Pacific Decadal Oscillation (PDO)…

We’re in a negative (cold) PDO; we know this by the warm SST in the Aleutians and the cold SST in the Gulf of Alaska. This is very important, as negative PDOs tend to enhance the La Nina pattern.

 


A negative PDO generally supports a ridge in the Gulf of Alaska and a trough in the western CONUS into the Plains. It also has a tendency to enhance the southeast ridge in the eastern CONUS.  

Typically, during a negative PDO…

The polar jet stays active which will Increase the risk for severe weather in the Plains, Mississippi River Valley Upper Midwest Tennessee River Valley and Ohio Valley. We've already seen this over the 7 to 10 days.

We also Characteristically see strong high pressure near the Bahamas and Gulf Coast.

This typically has the storm track shift into the Great Lakes and ends up drying out the Middle Atlantic into the Northeast. So, all the rain we’ve been getting is a good thing as it will help stave off drought.

With the shift in the storm track, there is a tendency for tropical air masses coming out of the Gulf, to work their way up the East Coast. This kind of pattern, also means we will have the northwest Atlantic influencing weather in the Northeast and northern Middle Atlantic Region. This would have impacts not only on the tropical season, but also the summer pattern in general.

 

The Indian Ocean

The Indian Ocean is very warm. Positive (warm)/negative (cold) IOD impacts how the La Nina will interact with the atmospheric pattern, it also has some impact on the SOI.  One important aspect of the warm Indian Ocean, is it promotes strong tropical waves moving over Africa. Strong tropical cyclones over the Indian Ocean would bring the increased risk of potent tropical waves moving across Africa, that would emerge into the Atlantic, that could rapidly develop due to the warm Atlantic.  

 

The Atlantic Basin…

The Atlantic is very warm in the Tropics, with SSTs to the north much cooler. This is a result of all the upper-level lows that have been plaguing the Canadian Maritimes.

Ocean heat content in the Atlantic Main Development Region (MDR) is well above the 2013-2023 average. SST in the MDR and Caribbean are 2°C to 5°C above average. That is extraordinary for this point of the year.

 


Currently the Gulf is running average based on the 2013-2023 average. But the Gulf will continue to warm as we get closer to the heart of the hurricane season.

 


The high oceanic heat content in the MDR, means there will be plenty of fuel for tropical waves to tap into. Cape Verdie Season could be very active.

The developing La Nina, is already building a ridge in Mexico, this ridge will push into Texas and the southern Plains during May and June. So, we can expect the southern Plains to be downright hot this Summer.

The developing ridge allows the storm track to shift north, this will tend to lessen the subtropical jets influence, which has been very active. As the troughs move out of the West Coast, they will be forced to move over the ridge. As a result, there will be an increased risk for severe weather outbreaks over the Central Plains into the Ohio Valley. As the ridge continues to lift northward, the Upper Plains, Great Lakes and Northeast could see an uptick in severe weather.  I do expect to see a big uptick in severe activity in the Plains starting during the 2nd half of May into June; as southern moisture streams north rising dew points.  We saw something similar in 2011 where the country experienced big severe events.

As El Nino wanes the eastern half of the CONUS is going to be wet. We’ve already been seeing that during March and April. We should continue to see an overall wet pattern for May into June. But then La Nina should be kicking in, and force the pattern to become drier. So, all this rain we’ve been getting would help reduce the risk for excessive drought this Summer.

The ridge axis is going to be very important. If the axis sets up over the East Coast. This would increase the drought potential.  With the tropical Atlantic looking to be very active. That kind of pattern would have these tropical systems moving into the Gulf. Then as the ridge axis shifts, the tropical systems and remnants tend to drag a lot of moisture up into the Middle Atlantic and Northeast. We saw similar tracks in 2011 with storms like Irene and Lee. 

 

La Nina….

La Nina patterns typically favor more tropical activity in the Atlantic due to the lack of wind shear. Strong wind shear, or the change in wind speed/direction with height into the atmosphere, will usually tear some storms apart and prevent many from forming in the first place. However, this year, that lack of strong wind shear and unusually warm sea surface temperatures could combine to produce a near-record hurricane season.

I’ve been getting a few questions about how sure I am about La Nina developing by this fall? Some people with the Australian Bureau of Meteorology (BOM) have been saying we might not have a La Nina this year at all.  Even though anything is possible. I’m very convinced we will see a La Nina develop. This belief is based not only what’s going on the Pacific, but also in the Atlantic.  The tropical Atlantic being so warm is part of the reason, that the equatorial Pacific is cooling so quickly. Research has shown those warm SST create pressure differences between the Atlantic and the Pacific. This leads to zones of high pressure in the upper atmosphere over the Pacific and low-pressure zones near the surface. These differences produce a setup that increases trade winds over the eastern into central equatorial Pacific. The faster winds lead to cooling of the SST in the eastern Pacific. This is accomplished by something called the Matsuno-Gill response. This is also the likely reason La Nina events have become more common and El Nino less so over the last 10-15 years. So, this is making the change to La Nina even more likely.

La Nina could end up moderate or stronger by the heart of the season. So, things could be very active during the 2nd half of the season.

Rapid intensification (RI)…

The SST in the tropical Atlantic are very warm, with La Nina looking to form in time for hurricane season; the setup in the Atlantic supports the chance for storms to rapidly intensify. 

RI occurs when a tropical cyclones winds increase by at least 35 mph in a 24-hour period.

Wild Cards:

2024 is unique in many ways.  These things are making things harder to interpret.  We just had a three year La Nina, then we had the strong El Nino that has basically ended. If we do see La Nina return this year; that would be the first recorded time this pattern has been seen. I will touch more on this later in the write up. But I’m sure we’re going to see some surprises because of these things.

La Nina can bring lots of Saharan Air Layer (SAL) in the Atlantic, we dealt with this in 2022…this is a big unknown. SAL is dry dusty air that blows off of North Africa on the trade winds. The layer overlies the more humid air. This creates an atmosphere this is more hostile and causes developing storms to struggle.  Currently there is a lot of SAL over the eastern Atlantic.




There has been an extreme heatwave in the Sahel region and West Africa in March and April. Looking at the date, it looks like will be much less rainfall for western Sahel during the Monsoon season, with perhaps more rain over central and eastern Sahel during the wet season. With severe drought over northwest Africa, there is a high likelihood for an increased chance for dust transport from those areas. So Saharan dust over the Atlantic could be above average at times.  

The strength and placement of the Azores/Bermuda High will be very important on the overall tracks of tropical cyclones.

The Atlantic is boiling (figuratively speaking), we’ve never really seen the Atlantic this warm especially the eastern Atlantic. These warm waters will have an impact on the overall wind pattern. These warm SST make it difficult to look to the past to get an overall picture for this season.  So how the cause and effect of all of this will affect the steering pattern and how tropical cyclones behave this season is unclear.  

 

Analogues:

Looking back at the historical record, there are certain years that have oceanic and atmospheric setups that are similar to this year. Yes, the SST in the Atlantic are warmer than we’ve ever seen. But in spite of that, looking at this can give us insight as to what the coming hurricane season may look like.

These seasons followed El Nino and saw La Lina in place by the heart of the hurricane season. These seasons also had similar SST patterns across the globe.

These nine years seemed to be the closes matches to this year’s overall SST footprint.   1878, 1926, 1970, 1975, 1998, 1999, 2010, 2011, 2020

I narrowed those years down to 1970, 1975, 1999, 2010, 2011, 2020

The historical Atlantic La Nina track density shows the western Atlantic Basin is busy during La Nina seasons. 


  

An outline of what all of this means:

Another important fact, is that during El Nino the overall pattern tends to make it much more likely for tropical cyclones to stay out over the open Atlantic. This overall idea, reverses during La Nina. So, the odds of tropical cyclones to make it into the western Atlantic Basin, vastly increasing the risk for landfalling systems on the U.S. main land increases.

The SSTs in the tropical and eastern subtropical Atlantic are at record highs. Give that the trade winds over the Atlantic have been below average, this has greatly added the water to become very warm due to less evaporation and upwelling of the cooler subsurface water. With La Nina taking over, trade winds should continue to be weak, which will allow SST to warm even more.

As I said above, those record warm SST in the Main Development Region will be a catalyst for more and stronger hurricanes. But there is a chance those SSTs could be a dual edged sword. The stronger hurricanes become the more likely they are to pull north. If this happens it could keep some of the stronger hurricanes away from the Caribbean and U.S. Mainland.  This will greatly be affected by what happens with the Azores/Bermuda High.

We’re going to see at least occasional SAL intrusions into the Atlantic Basin this season. How extensive these dust/dry air outbreaks are going to be remains to be seen.

All signs are pointing at a robust Azores/Bermuda High in the Atlantic this year. If this happens there would be increased odds of tropical cyclones making their way into the Western Atlantic Basin.

Above I noted that the SST in the tropical Atlantic are very warm, while the SST to the north is cooler. There is a chance this temperature difference, allows for higher wind shear than is being anticipated. This is something we will have to watch.

When we look at the Euro precipitation anomaly for the heart of the hurricane season; we see a lot of precipitation in the Caribbean into the Gulf and along the East Coast.



The NMME model is showing the same support for a lot of tropical activity in the Caribbean into the Gulf as well as up the East Coast.  





The States of Texas, Louisiana, and Florida look to have the highest probability of a major hurricane making landfall this season.



The NMME SST anomaly is showing support for a moderate to perhaps strong La Nina for the Summer into Fall hurricane season.

 


My Call:

Many outlets are calling for a record-breaking number of Tropical cyclones for this upcoming hurricane season. You can find what some of the other outlets are saying in part two of the outlook. NOAA won’t release their outlook until later in May.

 While I believe this season will feature well above average activity.  The wild card factors I went over will have an impact. This will be especially true when it comes to SAL over the Atlantic.  I think we’re going to be ending up dealing with SAL at times; this is going to help curtail development and strength of tropical cyclones that form out of the African waves; this should keep the 2024 season out of the record books when it comes to overall numbers of named storms. For that reason, my numbers will be a bit lower than some of these other outlets.

Named Storms… 17-25

Hurricanes… 8-12

Major Hurricanes… 4-8

Accumulated Cyclone Energy 200 to 240…

Summer 2024:

A general overview of how this summer looks to unfold. 

Summer in the Northeast and Middle Atlantic is greatly affected by the tropical activity in the Atlantic Basin. So, the same analogues I’m using for the hurricane season, can also be used for the summer outlook.

During the Summer we’re going to be dealing with the Southeast Ridge along with the northwest Atlantic.  Moisture will be streaming up the East Coast. But we also have those colder pockets of cold water off the New England Coast into the northwest Atlantic along with warmer water off the Middle Atlantic Coast. This is going to setup a temperature gradient between the Gulf Stream and those colder SST off of New England. This is likely to lead to areas of upper level low pressure setting up over Atlantic Canada as well as stronger areas of low pressure setting up time to time off the Middle Atlantic and track toward the Canadian Maritimes.

 

Temperatures…

Here is a look at what to models are indicating for the overall temperature pattern for the Northeast and Middle Atlantic.

 


So, while La Nina’s have a tendency to produce warmer summers, what’s going on over the Canadian Maritimes could send back door cold fronts into the Northeast, which might help counter the warm air surging northward. This could also enhance the severe risk this Summer.

 

Precipitation…

When we look at the six analogue summers, they show the propensity for above average rainfall over the Middle Atlantic Region into the Northeast.


 

This is because to the increased potential for moisture to stream north over the eastern U.S.  Just how much rainfall the Northeast and Middle Atlantic gets will, depend on how the tropical systems track. With the Atlantic looking to see an above average season there is an increased danger from tropical cyclones making direct or indirect impacts.  

Well, that’s it. I hope you found this informative and interesting.

I will be happy to answer any questions you may have. If you have questions, you can ask them in the comments here or on my Facebook weather pages.




Tuesday, April 2, 2024

The 2024 Atlantic Hurricane Outlook part two

 

Here is part two of the 2024 Atlantic hurricane outlook. This is an extension of my analysis from my 2024 Hurricane Outlook Part One. I will take you through the reasons I think this is going to be a very busy season.

Link to part one.

The 2024 hurricane season is getting closer. The Hurricane Season starts on June 1’s and will end on November 30th.  The 2024 Hurricane season should be quite different as we transition from El Nino into A la-Nina.

 Sea Surface Temperature Anomalies (SST)…

 




In the Pacific

We still have slightly above average SST in the equatorial Pacific. But these are much cooler than they were a few months ago. We also have very warm SST in the Northwestern Pacific.

Both of these will play a big role in this year’s hurricane season.

In the Atlantic SST anomalies across the Main Development Region (MDR) (the area between the Lesser Antilles and the West Coast of Africa) are well above average. The SST in the Caribbean and Gulf of Mexico (GOM) aren’t quite as warm, but they are still above average. As we approach the heart of the hurricane season, these Atlantic Basin SST will become even warmer.

Average water temperatures since January in the Atlantic’s Main Development Region are 2 °F above last year, crushing previous highs by almost 0.6 °F.

Another thing we see in the Atlantic is cooler SST in the North Atlantic north of the MDR. This is another indicator of an active season. As this temperature contrast helps supply lift that the tropical waves can use to make it easier for convection to develop in the MDR that could lead to Tropical Cyclone development.

 The El Nino-Southern Oscillation (ENSO)…

The ENSO is a climate pattern that involves changing water temperatures in the Central and Eastern equatorial Pacific. There are three statuses of the ENSO: La Nina, neutral and El Nino.

Last year we were in a strong El Nino with SST anomalies peaked in November-December last year.

The primary metric used by NOAA to gage the strength of an ENSO event is the three-month-average temperature of the central tropical Pacific Ocean, specifically in the Nino-3.4 region.

The temperature anomaly—the difference from the long-term average, where long-term is currently 1991–2020—in this region is called the Oceanic Nino Index (ONI). We use a three-month average because ENSO is a seasonal phenomenon, meaning it persists for at least several months.

The threshold is further broken down into Weak (with a 0.5 to 0.9 SST anomaly), Moderate (1.0 to 1.4), Strong (1.5 to 1.9) and Very Strong (≥ 2.0) events.

While we don’t have official strength definitions, but, unofficially, an ONI anomaly of 1.5 °C or warmer is considered a strong El Nino. Last year the ONI peaked at 2.0 °C which would indicate a very strong El Nino.


Since November-December last year, SST have dropped. Some areas in the equatorial Pacific are already showing up cooler, as upwelling is bringing cooler water to the surface. We’re quickly heading toward neutral. We’re most likely going to become neutral sometime next month or in May. After that we should quickly move into La Nina. The chances are growing for a La Nina to develop by summer and hurricane season 2024.



The colder subsurface water temperatures are just beneath the surface. Looking back at the equatorial Pacific Nino regions, we can see region 1+2 off the South American Coast is already showing much cooler SST.

Typically, during La Nina hurricane seasons, the Atlantic Basin sees a more active season due to less wind shear and trade winds and more instability.

During a La Nina year that follows a strong El Nino like the one that is happening in 2024, the tracks of tropical cyclones tend to be more active in the Caribbean and GOM.



The El Nino events in the record (starting in 1950) with the largest Oceanic Nino Index values are 1972–73 (2.1 °C), 1982–83 (2.2 °C), 1997–98 (2.4 °C), and 2015–16 (2.6 °C). 1987-1988 El Nino reached (1.7 °C). 2009-2010 (1.5 °C) These seasons were all followed by a La Nina.

Possible Analogues… 

La Nina seasons following a strong El Nino

1973, 1983,1988,1995,1998, 2010 and 2016

 Other factors that will have an impact on activity…

Saharan air layer (SAL) could be an inhibiting factor, especially during the first part of the season. As I’ve said in the past, the SAL is a layer of hot dry that can contain Saharan dust, blown off of Africa and out over the Atlantic.

SAL creates atmospheric parameters that suppress tropical cyclone formation and intensification. Last season featured less than average SAL over the Atlantic. If that is again the case this year; it would increase the odds for an active season.   

The Bermuda/Azores High (BAH) is a large area of high pressure that develops over the subtropical Atlantic Ocean. It exerts a lot of influence on the track of tropical systems.

The location and strength of the BAH will also be important.  As this will determine how far west the TC can track. If the BAH is weak and farther east TCs will have a greater chance to curve north up into the Atlantic. On the other hand, if the BAH is strong farther west, there will be a greater opportunity of the TCs to make in into the western Atlantic along with the Caribbean and GOM.   

 Other Outlets…

AccuWeather is calling for 20-25 named storms, with 8 to 12 becoming hurricanes, 4 to 7 of those becoming major hurricanes (Category 3 or above with at least winds of at least 111 mph). They are predicting 4 to 6 U.S. landfalling TCs. They say the seasonal Accumulated Cyclone Energy (ACE) will be 175-225.

Colorado State University (CSI) is calling for 23 named storms, 11 becoming hurricanes, 5 of those becoming major hurricanes.

WeatherBELL Analytics says the season will have 25-30 named storms, with 14 to 16 becoming hurricanes. Of these they are calling for 6 to 8 major hurricanes, with a seasonal ACE of 200 to 240.  

Tropical Storm Risk (TSR) calls for 20 named storms, 9 of these becoming hurricanes and 4 of these to become major hurricanes, with a seasonal ACE of 160.

All of these have one thing in common; they are all calling for a very active and possibly explosive hurricane season.

 What does all of this mean?...

 Based on the early signs, everything is pointing toward an above average season in the Atlantic Basin.  Last season had very mixed signals. We had a strong El Nino, which typically leads to less Atlantic hurricane activity, VS, super warm SST in the Atlantic. We saw how that worked out. The 2023 season featured well above average activity in the Atlantic Basin. This season is looking to feature a La Nina, which typically increases the likelihood for tropical cyclone development in the Atlantic, along with SST in the tropical Atlantic even warmer than they were last season. So, I have high confidence that this season will be above average, with a decent chance for the season to become hyperactive.

Based on the SST temperature profiles, I think 2024 should be similar to seasons like 2020, 2017, 2011, 2010, 2008, 2005 and 1995.

While there is no guarantee that an active season results in several U.S. landfalling TCs. It does increase the odds.

 


The data shows that the risk for hurricanes making landfall, are almost double when the Atlantic is warm vs when it is cool. The data also shows the risk for landfalling hurricanes is almost two and a half times greater during La Nina seasons vs El Nino seasons.   

We also have those well above average SST in the Northeast Pacific. This favors a pattern that could be very similar to what we had in 2005, 2007 and 2020. Those years saw several U.S. Tropical Cyclone landfalls.

With the super warm water in the Atlantic there is a greater risk for TCs to rapidly strengthen. When you add in the increased risk for landfalling systems, the idea of rapid intensification is something to worry about.

In part one, I said the eastern Gulf Coast, Florida and the Carolinas are at an above average risk for direct impacts. With a slightly less risk for the Texas Coast, Middle Atlantic and New England seeing possible landfall TC risk.  That still seems to be true. The Caribbean is also going to be at a heightened risk.

 In Summary…

 The early indications are that the 2024 hurricane season is going to be well above average.

The U.S. will likely see multiple landfalling tropical cyclones.

 

I will be releasing part three in May.







You can find part 3 here


Saturday, March 16, 2024

Why are winters so warm in the Northeast?

Some of y’all have been asking why this past winter was so warm with a lack of blocking and snowfall. I’m sure many of Y’all have the same question. So here is a post that will try to explain what is going on. I’m a Meteorologist not a Climatologist. But I do have an understanding of Climatology, so we will see how well I do!   

I’ve been posting a few writeups dealing with the changing climate, in things like the spring and hurricane outlooks. This post will take a look at possible reasons for last winter being so warm and snowless.   

 El Nino Southern Osculation (ENSO)…

 


 



 




When we look back at Sea Surface Temperatures on the 13th of February and compare that to now, we can see there have been a lot of changes in the ENSO region of the equatorial Pacific.  Nino region 1+2 and in Nino region 3 is starting to cool.  Looking at the subsurface water temperatures anomalies, we can see there is a lot of cooler water just below the surface. 

 




During the last 4 weeks, above-average SSTs have weakened across most of the equatorial Pacific Ocean

So, this El Nino is going to flip to La Nina conditions very quickly. 

 During this winter, I received questions or saw statements, about how the ENSO doesn’t seem to matter, in spite of it being a El Nino or a La Nina, all we’re seeing is warm snowless winters here in the Northeast. And those observations have been correct.  Over at least the last 6 years winters have been quite warm. So, the question, why is that is valid?

I’ve mentioned The Tonga’s Hunga volcanic eruption that happened in 2022 many times. It released an enormous amount of water vapor into the atmosphere. The shear amount of water vapor is in part to blame for the recent warming in the Northern Hemisphere. The water vapor is going to continue to cause havoc for several more years.  But the volcanic eruption can’t account for the last several years of warm winters. So, what else is going on?

To answer that we have to look at the state of the Pacific and Atlantic.

We’ve had a positive Pacific Decadal Oscillation (PDO) for the last few years.  We also have warm SSTs north of the ENSO regions. All of this constitutes mixed signals.  Helping to counter what’s going on inside the ENSO regions.

The Atlantic is also very warm. The tropical Atlantic is experiencing well above average SST.

During El Nino/La Nina there are characteristics that are expected, take for example my winter outlook, I based things on the strong El Nino, the overall pattern did resemble what you would expect for an El Nino. But activity in the subtropical jet has been slightly out of what you would expect. Why is that?

 



The El Nino hasn’t exerted much influence on the atmosphere. Based on Oceanic Nino Index (ONI) [The ONI is based on SST departures from average in the Niño 3.4 region, and is a principal measure for monitoring, assessing, and predicting ENSO] tropical SSTs, Nino 3.4 showed a strong El Nino over the Winter. But the Southern Osculation Index (SOI) hasn’t responded like it should have.  The SOI has been indicating a weak to moderate El Nino. This disconnect is very important, as what was going on with the Pacific SST, where the El Nino wasn’t really coupling with the atmosphere, which threw off the tropical forcing.

Based on the data in a paper by Michelle L. L’Heureux with the Climate Prediction Center (CPC), we could see La Nina begin around mid-May. I won’t get into the research in the paper, but if you want to read it, here is a link to the paper.

A Relative Sea Surface Temperature Index for Classifying ENSO Events in a Changing Climate.

The CPC images, do agree with that.



Here is my theory…

The Atlantic is the other side of the issue. It is quite possibly the bigger part of the equation.  The super warm SST in the Atlantic is playing havoc with teleconnections like the Artic Oscillation (AO) and North Atlantic Oscillation (NAO). The warm waters are affecting the polar jet stream and promoting troughing in the west and ridging in the east, this is one reason why the western CONUS has been experiencing colder winters over the last several years. The much warmer than usual water in the Atlantic, is most likely having an impact on the Atlantic Meridional Overturning Circulation (AMOC). The AMOC is like a conveyor belt, where the warm salty water in the tropical Atlantic flows north, meets the colder water in the northern Atlantic, which allows the warm water to cool and become denser and sinks, then this colder air moves south as deeper currents along the North American Coast. All of this explains the very warm water in the Gulf of Maine, and along the Middle Atlantic Coast. This circulating water has a cascading impact around the globe and is a big player in world climate.

 


The AMOC has an effect on the Atlantic Multidecadal Oscillation as well. The last few winters haven’t had a lot of high latitude blocking near Greenland. The poleward moisture and heat transport from the tropics is affecting the NAO and AO.  Since blocking most of the time coincides with negative phases of the NAO and AO. The blocking helps the Northeast experience cold during the winter, and helps improve snowfall across the region. The warming is interfering with the sub polar low and the subtropical high making both stronger than average. This is allowing the NAO to stay in a persistent positive phase. When the NAO is positive, the Northeast is much more likely to see a warmer winter. Subsequently the high latitude blocking is influenced by many oscillations. All of this is influencing storm tracks and is altering wind patterns. This in turn is affecting seasonal temperatures in the Northeast. So the pattern becomes slightly out of tune, making things warmer; along with a storm track that makes it much harder for things to phase, which makes having big snowstorms more difficult.

There is no doubt that the global climate is warming. Since the 1980’s a large part of the CONUS has been trending warmer. The Northeast is one of the fastest warming regions, but it’s the Arctic that’s seeing the most warming. This warming is melting sea ice.  The melted ice flows into the Atlantic, this fresh water dilutes the saltiness, which impacts the AMOC. Research has shown that the AMOC is losing stability and is slowing Down. The warming Atlantic Ocean water has a big hand in making northeast winters milder, much like drought begets drought, our warming winters feed on themselves. The lack of ice and snow, ends up reflecting sunlight back to space, so the ground absorbs more heat, driving temperatures higher. As a result, there are higher odds of a storm bringing rain instead of snow.

There are examples in the past, that show this same general pattern. One of these is the Medieval Warm Period that occurred around 900 A.D. to the mid 1300’s.   A.D.  Increased solar activity and a decrease in volcanic activity, brought about changes in the NAO, which brought about warmer winters and wetter conditions to Europe and eastern North America. Core samples show that Nordic Seas became well above average. The very warm water caused a lot of ice loss in the arctic. As we’re seeing now, this melted ice worked its way into the Atlantic, the fresh water from the melted ice, eventually cooled the ocean which resulted in the AMOC Slowing down and then collapsing. So, the very warm conditions in the late 1300s quickly turn to unprecedented cold conditions in the early 1400s, only two decades later. We know this through core samples and tree rings. This was the beginning of the Little Ice Age, which lasted roughly from the 1400’s to the end of the 1800’s or beginning of the 1900’s.

I’m not saying what’s happening now is going to lead to an event like the Little Ice Age. I’m just drawing a parallel between what looks to be going on and a similar event in the past.  This means winter here in the Northeast is going to continue to be a casualty of what’s going on for the foreseeable future we're still going to get these snowy storms, but very snowy winters are going to become harder and harder to occur.

There is a lot of debate about natural factors causing all of this VS humankind causing all the warming. But regardless of which side you take, we’re stuck with the fact that the climate is warming. And this warming is not only impacting the climate but also the weather.   

IMO a lot of what is going on with the warming has to do with natural cycles and water vapor. I’ve never said that humankind isn’t lending a helping hand. There is no doubt that part of the warming climate is due to human activities. But I think a large part of what is going on is the ocean/atmosphere system and cycles, many of which we know nothing about. I’ve posted many blog post on this subject. You can find them in the blog.

All of this makes longer range forecasting challenging. we're going to have to adapt to the changes that are going on. This is a steep learning curve. We can still use past events to forecast. But we're going to have to alter the rules and tweak things a bit.  


 

Thursday, March 7, 2024

NHC changes for the 2024 hurricane season

The National Hurricane Center (NHC), is making some changes to the way it handles tropical systems.  These changes to their products and services, will be implemented on an experimental basis for the 2024 hurricane season. This stems from the need to better inform the public on the potential multiple impacts that a tropical cyclone may deliver. The changes are…

(1  Spanish Text Products

(2 Watches and Warnings on Intermediate Advisories

(3  Extension of Tropical Storm Wind Radius Forecast

(4 Website Links in Advisories

(5 Forecast Cone with Inland Watches and Warnings

(6  Rainfall Graphics

(7  New marine forecast for offshore waters

(8  Change to the Time zone Reference in the Eastern Pacific


Spanish Text Products…

The National Hurricane Center will expand information provided in Spanish to include:

All public advisories.

The tropical cyclone discussion.

The tropical cyclone update.

Key messages.

The NHC will be using AI to generate the Spanish-language documents.

 

Watches and Warnings on Intermediate Advisories…

The NHC said watches and warnings could now be adjusted more frequently and not during the set times of 5 A.M., 11 A.M., 5 P.M., and 11 P.M. when the full advisory packages are typically issued.

This change will allow for flexibility when issuing tropical storm, hurricane and storm surge watches and warnings and more current and valid watches and warnings to be posted more frequently.

Extension of Tropical Storm Wind Radius Forecast…

The National Hurricane Center currently issues tropical storm wind radius forecasts out three days.

Starting in 2024, those forecasts will extend out five days.

 

Website Links in Advisories…

The public advisory for the 2024 hurricane season will include links that provide "graphical hazard information."

The links are "intended to help reduce the length of the Tropical Cyclone Public Advisory ... and to direct the focus to the most significant and impactful storm surge and rainfall hazards and areas," the NHC said.

 

Forecast Cone with Inland Watches and Warnings…

The NHC will be making changes to its cone of uncertainty, adding watches and warnings for interior areas starting around Aug. 15, 2024. Previously, watches and warnings were issued only for coastal areas.

With this experimental product, both coastal and inland watches and warnings will be shown with the forecast cone to illustrate that storm hazards can extend beyond the inside of a forecast cone.

Here is an example of the experimental version of the cone graphic.

 


The National Hurricane Center warns that since this is an experimental product, it may not be available at the same time that the current cone of uncertainty graphic is released but it should appear within 30 minutes of the advisory release.

 

Rainfall Graphics…

An experimental rainfall graphic for the Caribbean and Central America will be available in the 2024 Atlantic hurricane season.



The graphic will provide forecast rainfall totals for tropical cyclones or disturbances for a particular time period.

 

New marine forecast for offshore waters…

This change starts ahead of hurricane season

The current offshore waters forecast for the southwest and tropical north Atlantic will be divided into two forecasts starting March 26, 2024.

The new offshore waters forecast will consist of:

Offshore waters forecast for Southwest North Atlantic Ocean: Consists of all the Atlantic zones currently north of 19N.

Offshore waters forecast for the Caribbean Sea and Tropical North Atlantic: Consists of the remaining zones in the Caribbean Sea and Atlantic waters south of 19N.

 


 

Change to the Time zone Reference in the Eastern Pacific…

This won’t affect us here in the Northeast.

Most of Mexico no longer observes Daylight Saving

Time, therefore Central Standard and Mountain Standard time will be used in lieu of Daylight

Saving Time within those two time zones. Since Daylight Time is used within portions of Baja

California and the southwestern United States, Pacific Daylight Time will continue to be used

within that time zone when Daylight Saving Time is observed. The time zone of reference in

NHC tropical cyclone products is based on the initial position of the tropical cyclone at the

advisory issuance time, except for the caveat noted below. The time zone that appears in

eastern Pacific tropical cyclone products will be determined by the initial longitude of the tropical

cyclone as follows:

Central Standard Time: longitude at advisory time is east of 106.0W.

Mountain Standard Time: longitude at advisory time is between 106.0W to 114.9W.

During Daylight Saving Time, Pacific Daylight Time: when the longitude at advisory time is

west of 115.0W. Otherwise, Pacific Standard Time will be used. Please note that this

guidance applies to tropical cyclones that may affect Southern California.

CAVEAT: If the final forecast point for a tropical cyclone in the Tropical Cyclone

Forecast/Advisory (TCM) is west of 140W, the advisory will use Hawaii Standard Time.