Well it's getting close to
that time of year, when thoughts start to shift toward winter, and what might
it be like.
One question I've seen a
lot is, because our Summer was cool and wet does that mean this winter will be
cold and wet? My answer is sure, there
is a chance. But then there is a chance it won't. For several years, I've looked at the analog
data hard; I've never found any direct correlation between a cool summer and a
cool winter.
This year I want to start
out listing my analog winter seasons. I used these to try an come up with a
reasonable idea on how this winter should behave.
Analog years:
I looked at the years that
had a weak La Nina along with a negative QBO.... 1950, 1954, 1956, 1962,
1964,1967, 1970, 1974, 1983, 1988, 1995, 2000, 2005, 2007, and 2011
Analog years ended up
being 1952/1953, 1953/1954, 1958/1959,1960/1961, 1962/1963 1964/1965, 1967,1968, 1969/1970, 1970/1971, 1975/1975,
1977/1978, 1979/1980, 1981/1982,1995/1996, 2000/2001 2004/2005, 2006/2007, 2007/2008, 2014/2015. I gave the seasons in red the most weight,
with 1974/1975, 1981/1982 and 20006/2007 being
double weighted.
The thing that directly
impacts our weather is the jet stream. To refresh Y'all, the jet stream is a
narrow river of fast moving air that resides above us in the upper atmosphere.
There are many jet streams, but the two that effect the Northeast the most are
the sub tropical jet and the polar jet. The polar jet sits around the 500mb level
(25,000-30,000 feet), while the subtropical jet is a little higher, around the
300mb to 115mb level (30,000 to 50,000 feet ) During the Summer the polar jet
is typically found well to the north in northern Alaska and northern Canada.
While the subtropical jet pushes south to near the Gulf Coast.
The wavering of these two
jet streams is what causes the day to day variations in our weather. When the
polar jet drifts south, we see cooler weather. When the subtropical jet moves
north we see warmer weather.
But our weather is also
effected by other teleconnection flows. the El Nino and the Southern
Oscillation, the North Atlantic Oscillation. the Quassi-Biennial Oscillation, The
Pacific Decadal Oscillation, and others. We also are effected by things like
sea surface temperatures, snow and ice extent, and even sun spots. All of these
things play a role in how cold and snowy our winter will be.
Sea Surface Temperatures
and the El Nino and the Southern Oscillation (ENSO):
There are four regions in
the tropical pacific that we track, El Nino region 1+2, 3, 3.4, and 4.
I think Winter 2017-2018
will be more of a negative ENSO or a weak La Nina. The La Nina could get close
to moderate, but I rather doubt it. The SST in Nino regions 1,2 3, 3.4 were
dropping off fairly quickly. Then there was a warming trend. The last couple of
weeks have seen the Nino region start to cool off again. They are currently
below normal and are approaching La Nina levels. Because of the up and down
cooling most atmospheric indicators have remained ENSO neutral. Winter
2016-2017 was a mix of El Nino and La Nina.
The type, timing and
strength of the La Nina will be critical. an east or central based is more
favorable for a cold east of the Rockies, compared to a west based event.
Currently, sea surface
temperatures (SST) in the eastern tropical Pacific are slightly below average.
The mid eastern Pacific has seen the biggest departure from average, right now
that's about one degree Celsius. The
coolness does extend down a few hundred meters below the surface. We should see
the east - central Nino regions will continue to cool . Last winter, regions 1
and 2 got warm, I don't see them getting that warm this winter. So It seems likely that my idea of a
cool ENSO neutral to weak La Nina seem
likely. If we do see a weak La Nina I expect it would reverse back to ENSO
neutral for late winter. So a cool neutral or weak La Nina for November into
the end of December or so, then we should see the La Nina reverse as we get
closer to late winter.
There has been a big
change in the ENSO from this Spring compared to now.
Here is a look at the mid-April International Research Institute for Climate and Society (IRI) chart.
If we do end up with a
weak La Nina; I do think the La Nina will be leaning toward the east based
idea.
I have to remind you that
many other factors are involved besides just the ENSO and La Nina.
The Indian Ocean Dipole is
neutral
The Quassi-Biennial
Oscillation (QBO):
The QBO started trending
easterly back in April. So it looks like a moderate to strong east based QBO is
likely. During last year's winter of 2016-2017 we had a La Nina with an west
based QBO. So an negative east based QBO would have a completely different
impact on our winter. When we have an eastern based QBO we tend to see a warmer
stratosphere over the northern polar region, as opposed to a cooler
stratosphere when the QBO is west based. Looking at past east based QBO years,
the East does tend to see more troughiness.
The Pacific Decadial
Oscillation (PDO):
As it has been for the
last few winters, The PDO remains positive. But because of the double La Nina,
it is weaker than it was last year. The positive phase of the PDO involves
warmer than average water temperatures off the West Coast of North America. The
cool negative phase is the opposite.
The PDO has a big impact
on where ridging and troughing sets up.
The more positive the PDO the more persistent and deeper the western
ridge. I think the PDO will stay a weak positive into the Spring of 2018, where
as it would go neutral. Being weaker than last year and the year before that.
Will mean the western trough and eastern trough won't be as strong and dominate
has they have been. This would have a impact on the storm track and how far
south the cold extends.
There are many other
teleconnections that I looked at. But I don't want to overwhelm Y'all with all
of that data. More or less they support my idea on how winter will turnout.
It is important to
remember, how a season turns out is based on a mixture of different
teleconnections and other patterns, not the individual teleconnections
themselves.
Solar Activity:
This Winter will feature
low solar activity. There is a correlation between winter temperatures and sun
spot activity. Years with low solar activity tend to run colder with
more of a negative AO and negative NAO, than winters with high solar activity.
Winter's that experience low solar activity also tend to see higher increases
of higher latitude blocking around Greenland and Iceland. Which is good if you
like colder weather.
Here are a couple of
charts that show how all of this characteristically works out .
Here are a few images that
show Ap solar activity and NAO index
values.
Here is one from,
International Climate and Environmental Change and Assessment Project (ICECAP).
You can see there is a
coloration between solar activity and the NAO and AO
When we have negative NAO
and AO index values we tend to see more outbreaks of cold air moving out of
Canada do to blocking over Greenland.
The Hurricane Season:
This year we have seen a
lot of low pressure over North America. This happened when prevailing high
pressure set up in the Atlantic. We have seen a lot of high pressure over
eastern Canada into the Northeast. So with lower pressure over the Southeast
into Caribbean and Gulf land falling tropical cyclones were going to be a
given.
I have found that there is
a weak association between Atlantic and Pacific tropical activity and winter
snowfall. It all comes down to
Accumulated Cyclone Energy (ACE). ACE measures the strength and duration of
individual tropical cyclones.
As of Hurricane Olivia this
seasons ACE sits at 212. An average year has an ACE of 111. OK but how does
this impact our winter? The atmosphere is always seeking a balance. When I
looked back at years that had above average ACE. The years that came up were
1950, 1969, 1980, 1989, 1995, 1996, 1998, 1999, ,2000, 2001, 2003, 2004, 2005,
2008, 2010, 2011, 2012. Over 60% of the
time, When ACE was above average, the Northeast saw above average snowfall overall,
while the Southeast saw below average snowfall overall.
Going into Winter:
October, November, and
into the first part of December will see temperature swings back and forth.
That doesn't mean we won't see cold, it just means it won't be really long
lasting or widespread. We could see a decent cold outbreak in a couple of weeks. But I do expect to see some early season snows end of October or November, especially in the Snow Belts and higher elevations of New York State
and Northern New England. Based on the analogs, there is a good chance for an end of October into November big storm.
The real winter cold will
most likely hold off until around Christmas into January. Making January, February, into March
feeling the most winter-like. Mid to late winter should see more longer lasting
cold in the Great Lakes and Northeast.
So, October is going to be
very transitory in nature. The overall temperatures in October will be above
average. The Northeast has been very dry the last three to four weeks. But Nate
is going to bring some much needed rain. So precipitation wise October will end
up close to average.
November will see the pattern flip to more in the way of troughing, so we should end up with overall temperatures being below average, how much is uncertain. But we will have quite a bit of cold locked in Canada. Unless we see another tropical system, It will also be rather dry, (unless we see something tropical).
November will see the pattern flip to more in the way of troughing, so we should end up with overall temperatures being below average, how much is uncertain. But we will have quite a bit of cold locked in Canada. Unless we see another tropical system, It will also be rather dry, (unless we see something tropical).
December should see
temperatures also below average with the end of December ending up most likely well below average.
Northern Hemisphere
snowpack:
Snow has been falling in
Siberia and we've had a few early season snowfalls in the Rockies into Montana.
The models are bullish on the idea of snow in Siberia into China over the next
two months.
Here is a look at the snow
and ice extent.
With snows flying in
Siberia, the more snowpack there is in Siberia and northern Canada, the better
the chance for high latitude blocking. So
there is a good chance for negative NAO and a negative AO.
Wild Cards:
Pacific Jet. for winter
2016-2017 we had a zonal (west to east) flow due to a strong Pacific jet. This
is the main reason for the warmth and
wild swings we saw. There is a chance we could see a strong pacific jet again
this winter.
There would be cold air in
Canada and into the middle of the CONUS (Continental U.S.). depending on how
the polar jet acts it could overwhelm the pattern during the last half of
winter.
Blocking, How much we see
and where it sets up is as of yet, a little unclear. But I don't think the
warmth of this fall will last all the way through winter 2017-2018.
Summary:
Where the prevalent ridge
sets up will be key, as to where the core of the cold sets up. I do expect to
see some level of a southeastern ridge. But I don't think it will be as
prevalent as last winter. why? Because I think we will see more Greenland
Blocking than we saw last Winter.
While the core of the
winter cold looks to setup in the Great lakes into the Plains. The Northeast
and Mid Atlantic can expect a chilly winter especially from mid winter to end
of winter.
The Southeast is going to
see a very warm Winter, that combined with cold air invading the Rockies into
the Great Lakes, will allow for plenty of opportunities for wintertime
precipitation. Blocking is going to be a
wildcard for winter 2017-2018. But it looks to setup so that the Midwest and
Great Lakes will be quite cold, with the Northeast not getting quite that cold.
The analogs I looked at, show the storm track should be fairly active. So I
don't think snowfall will be all that bad here in the Northeast into the
northern Mid Atlantic. An active clipper and Colorado Low storm track will bring many chances
for lake effect snows downwind of Lakes
Erie and Ontario. But, the water temperatures in the Great Lakes are warmer
than last winter, so unless we can get some really cold air toward the end of
November, lake effect snow could be less
than last year.
Temperatures:
Temperature profiles in
the Northeast are going to be very tricky this winter. This year we will have
an east based La Nina. Typically La Nina winters tend to be colder in the
Northwest, Central US, and the Great Lakes. The Southeast tends to be quite
warm. The Northeast and the Mid Atlantic tend to be in-between somewhere. The
strongest widespread cold will be mid it late winter. November will feature
some cold . But, I don't expect to see longer lasting cold
for the first third of winter. But end of December thru March have the potential to be
cold.
Here are my temperature
ideas.
Precipitation:
During an La Nina, the
typical precipitation pattern sets up as above average over the Northeast. So,
snowfall and mixed events for much of New York State and northern New England should be above
average. With the Pennsylvania, southern New England, and Mid Atlantic seeing average to slightly above average, there is a bigger risk for mixed events in the Mid Atlantic region. The
relatively warm waters off the East Coast could allow for a few bigger
snowstorm events.
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