2021 Spring outlook update

 

Here is a update to my earlier Spring Outlook for 2021

The Spring Outlook can be found here.

 

Teleconnections:

Images from WeatherBell

Looking at Sea Surface Temperatures (SST) in the Pacific, it’s clear we’re still in a weak La Nina. But as I’ve been saying, we should see the La Nina conditions strengthen again as we head toward Summer. We also have those cool SSTs off the Southwest Coast. These extend north along the West Coast into the Gulf of Alaska.  These two teleconnections will play a big role in the trough and ridge pattern across North America this Spring. Add to that the severe drought conditions across the Southwest CONUS, means we have an interesting and possibly quite dangerous Spring ahead of us.

 

 

The North Atlantic Oscillation (NAO) has been strongly positive, but now it looks to go negative.

 

 

The Eastern Pacific Oscillation (EPO) is also turning negative

 

Currently the Madden Julian Oscillation (MJO) is currently active over the western Indian Ocean. The MJO will continue to move across the Indian Ocean, currently Phases 2 and 3 (cold phases for this time of year), then Into Phases 3 and 4 where it intensifies.  This means that our warm weather of late, is coming to an end.  MJO phase 2 and 3 are showery and cold here in The Northeast.   As we move toward April the MJO is in phase 4 and 5, which are still cold phases but they are also dryer here in the Northeast and Middle Atlantic Region. As we get into April the MJO looks to move into Phase 6 and then Phase 7.  Phase 6 is Warm and Dry in April, but phase 7 is a cool and wet phase. If it gets into Phase 8 that is slightly a warmer phase but it does tend to be a little dry.  

 

 Spring Temperatures:

 

The MJO is indicating that the warmth of the last couple of weeks could be a false spring. Meaning that we’re still not out of the woods as far as cold intrusions and possible snow events.  I do think the Pacific will tend to stay in the driver’s seat. So, as we get closer to late-April, the threat of real cold and snow should be over. The setup in the Pacific is a strong indicator that the predominate pattern during the second half of Spring heading into Summer, will feature a lot of ridging over the East. So, my earlier thoughts for overall temperatures to be above average for the Northeast into Middle Atlantic Region is spring are still looking right. But April could see real cold invade around mid month.

Generally, the March, April, and May time period look to see overall temperature anomalies to be +1.0°F to +3.0°F above average.

Spring Precipitation:

 

 

Here is a look at the current drought conditions from the Climate Prediction Center. The Map shows, some areas in across the Northeast into the Middle Atlantic are currently experiencing dry conditions and, in some cases, a moderate drought.

Below is a look at the latest Soil Moisture Anomaly for the CONUS.

 

We’ve had yet another week of below-normal precipitation across our region. As a result, Moderate drought has expanded in western Vermont and northern New York, while abnormal dryness expanded in western Maine, northeastern Massachusetts, and western and northern New York. Conditions remained unchanged elsewhere in the region. The U.S. Drought Monitor released on March 25 showed 8% of the Northeast DEWS region in a moderate drought and 39% as abnormally dry compared to 7% and 33%, respectively, last week.

The Standardized Precipitation Index (SPI) is a simple measure of drought (absolute, departure from normal, maximum, and minimum) and is based solely on the accumulated precipitation for a given time period. For this map is show precipitation departure over the last 60 days, compared with the long-term average.

The pattern that is looking to setup, would indicate that Spring 2021 will end up with overall above average precipitation. the pattern does support the idea that conditions across the Mid Atlantic, Pennsylvania, New York State into western New England, could end up with above average precipitation over the Spring. Maine looks to see average to below average precipitation. 

Snowfall: For the Middle Atlantic into Pennsylvania your chances for accumulating snow is very low, so you’ve most likely seen the last of the white stuff. But some accumulating snow is still a real possibility across the northern tier of Pennsylvania, New York State, and New England.  The odds of significant snowstorms are over in my opinion.

 

 Springtime Severe Weather:

In the 2021 Spring Outlook part 2, I talked about how the widespread severe to exceptional drought across the Southwest CONUS into the Central Rockies, and how it would play a big role in the Spring severe pattern.  Between that and the cooler than normal Pacific explains why the severe season is starting out a little earlier than average.   Typically, during years like this the tornado season starts around 4 weeks earlier and tends to be more active than average.

In the first part of the Spring Outlook; I also talked about how the tropical Pacific are similar to the infamous year 2011. Remember, back in April 2011 there was a very extreme with deadly historic tornado outbreak.

From January into March, we saw a slow start of the storm season. By March 1^st there were only 24 reported tornadoes across CONUS.  But the severe weather activity has started to trend upward.  La Nina years do see to start earlier than usual. Also, when the Pacific is cool Dixie Alley, often experiences significant tornado outbreaks.  And with pattern the weather models seem to be indicating, this year’s tornado season could again be an above-average this spring.

 

 

2011, also had a slow start, that too was due to the cooler Pacific waters. But those cool Pacific SST led to a vigorous and stronger Jet Stream.  So, with a similar SST and atmospheric pattern this year could also be very active. In last than a week, the month of March has seen to severe tornado outbreaks, both of which had the Storm Prediction Center raised rare High Risk severe chances. Currently the tornado count stands a 163, which means we’re almost to the yearly mean for this time of year.

 With these same conditions looking likely for April, and the idea that recent Aprils have been active. Surely means the chances for more significant severe outbreaks are possible for April and beyond. the typical northward shift of the jet stream will occur. But the winds will likely remain stronger than normal, so the tornado season will probably continue as above-average during the peak season. With the gradual northward retreat of the upper-level jet stream the severe season will move north with it.  So, May and June, will probably continue as above-average during the peak season.

 The same setup that looks to bring the Northeast into Midwest seeing maybe a soggy spring. The Ohio Valley, Maryland, Delaware, Much of Pennsylvania, and Western New York State will most likely experience enhanced severe activity this Spring. For the rest of New York State, far eastern Pennsylvania, New Jersey and New England, severe chances look to be around average for spring 2021. 

Well that is it, Just a reminder, my 2nd part of the Atlantic Hurricane Outlook, will be released in a couple of weeks.

The 2021 Atlantic Basin Hurricane Season part one.

 

We’re moving closer to the start of the official 2021 Atlantic Hurricane Season. I’ve been fielding questions as to what I think will occur.

This is long but it does dive into my current thoughts on how things are looking at this time.

As is always the case with my long-range outlooks; if you don’t want to read the analysis (but you will miss a learning opportunity) you can skip to the verdict at the end.

 

I will start with a few basic definitions:

  

For starters, a tropical cyclone is the generic name given to low-pressure systems that form over warm tropical or subtropical seas. When the NHC and I or other forecasters discuss categories of tropical cyclones we use the Saffir-Simpson Hurricane Wind Scale. On this scale (which IMO is outdated, but that’s a discussion for another time) tropical cyclones are rated as follows.

Tropical Depression: a tropical cyclone with maximum sustained wind speeds less than 39 miles per hour.   Also, in order to be classified as a tropical depression, a tropical disturbance must develop a closed surface circulation with organized thunderstorms.

Tropical Storm: a tropical cyclone with maximum sustained wind speeds of at least 39 mph to 73 mph. When a tropical storm is identified, it formally receives a name. Tropical cyclones retain their tropical storm status as long as their maximum sustained winds remain between 39 mph to 73 mph.

Hurricane: a tropical cyclone with maximum sustained winds of at least 74 miles per hour. Category 1 hurricanes have sustained winds of 74 to 95 mph; a category 2 has sustained winds of 96 to 110 mph Once a hurricane’s sustained wind speed reaches 111 mph it becomes classified as a major hurricane. Category 3 is 111 to 129 mph, Category is 4 130 to 156 mph, and a Category 5 has sustained winds of 157 mph or greater.

 The Atlantic Basin consists of the entire North Atlantic Ocean, the Caribbean Sea, and the Gulf of Mexico. An average Atlantic Basin season has 12 named storms, six hurricanes, and three major hurricanes.

 

Tropical Weather Outlooks:

The official Atlantic hurricane season has been from June 1^st to November 30^th.

The National Oceanic and Atmospheric Administration (NOAA) has been discussing the idea of changing the official start date of the Atlantic hurricane season from June 1 to May 15^th.  For the 2021 season the National Hurricane Center (NHC) has said, they have decided to keep the start date at June 1^st. So far, there has been no final decision on if the 2022 season will be pushed forward 2 weeks to May 15^th.  But there is still a change occurring this season. The NHC has said they will start issuing their normal Tropical Weather Outlooks on May 15th at 8 am. These outlooks usually don’t happen until June 1st.

Analog years:

These are the analog years that I’ve chosen; as they seem to match the closest to the current weather pattern.

1899, 1950, 1956, 1996, 1999, 2003,2004, 2005, 2008, 2012, 2017, 2020

The ones that I’m placing special emphasis on are 1996, 2003, 2004,2005, 2008, 2012, 2017, and 2020. 

Sea Surface Temperatures (SST):

Hurricanes thrive on warm sea surface temperatures.

Image from WeatherBell

Image from weatherBell

When we compare the SST from this time last year, to the what they look like right now. We can see they look similar. But the eastern Atlantic Main Development Region (MDR) is a bit cooler, and the north Atlantic in general is a bit warmer.

One of the major determining factors this season, will be how much the Atlantic south of 25 North warms during April, May and June. For the last four seasons the MDR was below average in SSTs at this time; but it reversed during the Hurricane Season, resulting in active tropical seasons. I do expect 2021 will see the same general idea with the MDR warming to above average SST levels during July, August, and September. 

As was the case last season; the 2021 hurricane season looks to see an active West African Monsoon, so as was the case last year, we should see some strong tropical waves move off of Africa.

 A little more on the West African monsoon season and its impact on the Atlantic hurricane season.

Saharan Dust can come off the African coast and move west across the tropical Atlantic. Saharan dust is the result of lower humidity profiles which adversely impacts atmospheric moisture and the ability for tropical disturbances to develop and maintain convective (thunderstorm) activity for further development. So, years that see a weak West African monsoon season, tend to see weaker than average tropical waves and disturbances. Over the last 5-6 years, spring rainfall totals across west Africa has been well above normal. These wet spring conditions can decrease dust transport off the African Coast during summer. This in turn elevates the potential for tropical formation in the Atlantic tropics. 

 Teleconnections:

The El Nino Southern Oscillation (ENSO)

The Pacific Ocean has a significant influence on the Atlantic hurricane season. 

Oceanic Nino Index (ONI) is the most common indices used to determine the sate of the ENSO, defined as the three-month average of SSTA in the Nino 3.4 region.

Sea Surface Temperature Anomaly (SSTA) are generally -0.5°C in Nino 4, -0.3°C in Nino 3.4, 0.1 °C in Nino 3, and 0.9 in Nino 1 + 2 across the Eastern into Central equatorial Pacific. This would indicate we’re still in a technically in a La Nina. But there is warming occurring in region Nino 1 + 2. This would seem to indicate that the La Nina from the Winter, is weakening.

The Climate Protection Center (CPC) defines ENSO phase anomalies as

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 new official CPC/IRI outlook issued earlier this month is similar to these model forecasts, calling for a 60% chance of La Niña to transition to ENSO neutral in the Apr-may-Jun timespan. The CPC has a La Nina advisory in effect.

 

Since late January, a large area of positive anomalies in the western Pacific has shifted eastward to around 145˚W at depth. Also, positive subsurface temperature anomalies from around 25m to the surface have persisted in the far eastern Pacific Ocean.

Many of the models are agreeing saying the current La Nina is going to fade and the summer will feature ENSO neutral conditions. I’m not so sure of that.  I’ve been talking about the possibility for the current La Nina to try and reestablish itself as we get closer to the fall. In 2020 we saw what a la Nina hurricane season is capable of.  But many of the analog years I’m using showed a tendency for a La Nina with some staying power, with some extending into a 2^nd year La Nina.    

 

Atlantic Multi-Decadal Oscillation (AMO)

The AMO is an ongoing series of long-duration changes in the sea surface temperature of the North Atlantic Ocean, with cool and warm phases that may last for 20-50 years.   

IMO the AMO is also a very important teleconnection in long range tropical forecasting.  There is some correlation between phases of the AMO and the frequency of severe hurricane events. This is because it causes variations in large-scale features over the tropical Atlantic, such as sea surface temperatures, vertical wind shear, and low-level convergence. the AMO cycle involves changes in the south-to-north circulation and overturning of water and heat in the Atlantic Ocean.

In the negative (cold) phase of the AMO, sea surface temperatures are typically below normal in the Atlantic MDR, the eastern subtropical Atlantic, and the far North Atlantic. They are typically near or above normal in the western subtropical Atlantic.

In the positive (warm) phase of the AMO, sea surface temperatures are typically above normal in the Atlantic Main Development Region (MDR), the eastern subtropical Atlantic, and the far North Atlantic. Sea surface temperatures are typically below normal or near normal in the western subtropical Atlantic near the United States East Coast.

The AMO cycle involves changes in the circulation patterns and overturning of water and heat in the Atlantic Ocean. This is the same circulation that we think weakens during ice ages, but in the case of the AMO the changes in circulation are much more subtle than those of the ice ages. The warm Gulf Stream current off the east coast of the United States is part of the Atlantic overturning circulation. The Atlantic Ocean Thermohaline Circulation (THC) is also something that is impacted by the phase of the AMO.  When the overturning circulation decreases, the North Atlantic temperatures become cooler.

The current state of the AMO isn’t clear cut, many experts disagree on whether we are in a positive or negative AMO phase. IMO we’re still in a positive (warm) AMO phase.  During a positive warm phase there isn’t a real correlation between the AMO and the frequency of tropical storms and category 1 and category 2 hurricanes – But during warm phases of the AMO, the numbers of tropical storms that mature into severe hurricanes is much greater than during cool phases, at least twice as many.

Since 1950 the seasons with the most ACE are 2005,1995, 2004, 1950, and 1961 have all occurred during a positive AMO phase. Also, the five Atlantic hurricane seasons since 1950 with the least ACE were 1983, 1977, 1972, 1982, and 1994 have all occurred during a negative AMO phase.   

 

Pacific Decadal Oscillation (PDO)

The Pacific Decadal Oscillation (PDO) is a long-lived ENSO-like pattern of Pacific climate variability. While the two climate oscillations have similar spatial climate fingerprints, The PDO and ENSO influence sea surface temperatures, sea level pressure, and surface winds in very similar ways.

While ENSO is primarily an interannual phenomenon, the PDO is decadal in scale. The PDO phases can be associated with El Nino or La Nina. The positive phase of the PDO which has the water surface with warm temperatures in the equatorial Pacific, can enhance an El Nino episode, amplifying the effects of the latter. This same phase of the PDO would weaken the La Nina events that would occur during this period. Similarly, during a negative phase of the PDO, events La Nina would be rather enhanced, and El Nino events would be weakened.

Currently we’re in a Negative PDO.  

The negative PDO and La Nina favor increased Atlantic hurricane activity.

 

The Quasi-Biennial Oscillation (QBO)

During QBO negative (easterly) years, tropical cyclones tend to form north of the main development zone.  Tropical Cyclones also seem to form closer into the CONUS, increasing the likelihood of a landfall. So, this could counter that idea of the La Nina allowing storms to form father east.

 

The Madden-Julian Oscillation (MJO)

The Madden-Julian Oscillation is a major fluctuation in tropical circulation and rainfall that moves eastward along the equator, and circles the entire globe.  It takes on average 30 to 60 days to complete that trip around the globe. The pattern typically starts in the Indian Ocean, it then moves east into the Pacific, and then into the Atlantic.

The MJO has two phases, one is the enhanced precipitation phase; the other is the suppressed precipitation phase.  that bisect the planet. Usually, half of the planet will be experiencing   increasing trend in rainfall amounts, while the other half of the planet will experience drier conditions.

Normally, when the enhanced phase of the MJO pushes into the Gulf of Mexico or the Atlantic Ocean, tropical activity is more favored due to an increase in rising air (Convergence) and decreased windshear, which leads to thunderstorm (Convection) development. So, during this phase, tropical cyclone development or strengthening is possible. On average Major are up to five times more likely to develop during the enhanced phase of the MJO, while hurricane formation can be up to four times as likely.

When the Atlantic Basin is under the suppressed phase of the MJO. The phase will hinder tropical development; because of sinking air (divergence) along with increased windshear. That doesn’t mean there can’t be tropical development, but it makes it much less likely to see thunderstorm development across the tropical basin. This will often lead to a multi-week lull in tropical development in the basin.

Phases 1 and 2 are the phases most favorable for Atlantic tropical activity.

 

The MJO will end up being a wildcard, as it is unclear as to how it will influence the Atlantic Hurricane Season.

 

A little this and that

 

There is a coronation that 2nd year La Nina ends up with tropical cyclones developing farther east.  A negative PDO tends to lead to stronger tropical cyclones.  A positive Atlantic Multidecadal Oscillation (AMO) tends to lead to increase tropical activity.  

 

Accumulated Cyclone Energy (ACE):

Ace is used to measure the intensity of a hurricane season as well as individual   tropical cyclones. The higher the number the more active the season and the danger level during the season and the greater the damage potential of individual storms.

Based on what I see right now, I’m thinking this year’s Atlantic ACE will be between 150- 200.

Here is a chart that shows how ACE values generally corresponds with  tropical cyclone activity.     

1933 is the record holder with an ACE of 258.57 that season saw 20 named storms, 2005 comes in 2^nd with an ACE of 250.13 that season saw 28 named storms (which was the record, until 2021. In spite of the record setting 2021 season, which saw 30 named storms; 2021 comes in at 10^th place in terms of ACE. 2021 ended up with ACE of 182.22.  Why was it so low but had a record-breaking number of named storms?  Many of the storms last season were weak short lived tropical cyclones; Also, the tendency of the NHC naming storms that wouldn’t have been named in previous years. The increased number of named storms is due in part to increased technological methods.

 

List of names for the 2021 Atlantic Hurricane Season:

It’s too soon to know, if this season will be as active as the record-breaking season of 2020. In 2020 ran out of names on the traditional list of names, and had to go into the Greek alphabet. Last season they used Alpha, Bata, Gamma, Delta, Epsilon, Zeta, Eta, and Theta.

Another major change for 2021 is that the World Meteorological Organization has voted to eliminate the use of the Greek alphabet in future seasons because it created potential confusion. Starting in the 2021 season, there will be a supplemental list of names that will be used in the event we run out of hurricane names in a given year.

 

 For 2021 the official list of names will be…

Ana

Bill

Claudette

Danny

Elsa

Fred

Grace

Henri

Ida

Julian

Kate

Larry

Mindy

Nicholas

Odette

Peter

Rose

Sam

Teresa

Victor

Wanda

The supplemental list of names

Adria

Braylen

Caridad

Deshawn

Emery

Foster

Gemma

Heath

Isla

Jacobus

Kenzie

Lucio

Makayla

Nolan

Orlanda

Pax

Ronin

Sophie

Tayshaun

Viviana

Will

 

The Verdict:

I am forecasting an above average tropical season in the Atlantic Basin. 

Total named storms 18-24

Hurricanes 8-15

Major Hurricanes 4-8

 

The Landfall Threat

Any long track tropical cyclones that form in the eastern Atlantic moving west, the turn to the north could come farther east than we saw last year. The analog data does support the idea that a ridge is likely over the Northeast and southeast Canada.

This would mean North Carolina and South Carolina, along with the Eastern and Central Gulf Coast (from the Big Bend of Florida over to Louisiana) would be the area of greatest concern. The Leeward Islands, the Northeast Caribbean, entire Florida Peninsula, and the Bahamas will also be at a heightened risk.  The pattern that looks to develop, would mean the Northeast and Atlantic Canada will have to be very watchful this season.   Last year we saw the western Caribbean quite active. For this season I think the active focus will shift north and east of there. The central and eastern Gulf is likely to be much more active than the western Gulf.

Right now, I’m thinking for the CONUS there is a chance of 5-6 landfalling hurricanes. 1-2 of these could be major hurricanes of Category 3,4, or even 5.

 

Well, that is it for part 1. I will most likely issue part 2 around mid-April.  Then if a part 3 is needed that will be issued around the middle of May.

 I hope you found this interesting and informative. Remember this is only part one, so this could all change as the season gets closer. But as of mid-March, this is what looks to occur. 

Part 2 can be found here