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State of the NAO

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Title: State of the NAO


1
State of the NAO
Positive phase of the NAO is not conducive for
HSEs in the Delaware Valley. Snowstorms can
happen during a positive phase, but it is rare
for PHL to receive a HSE during a NAO (January
2000 was an exception to the rule). A positive
NAO usually exhibits a fast west to east zonal
flow and/or ridging east of the Mississippi
River.
NAO Site
2
State of the NAO
A negative NAO in conducive for East coast
snowstorms because it usually allows for cold air
to spill into the eastern United States. It also
allows for a blocking to take place in Eastern
Canada, a subsequent trough to develop over the
eastern United States, and coastal cyclogenesis
to sometimes occur. A negative NAO is by far the
most important factor in East coast snowstorm
development. Negative NAOs and their associated
blocks usually last 10 to 14 days. Models
sometimes break them down too early.
3
Importance of High Latitude Blocking (-NAO)
  • Of course we are going to have to watch this
    very carefully as there is a window of
    opportunity for some sort of wave to develop warm
    front over the southeast JAN 16-18. But notice
    what most of the models ate doing here. Without
    any High latitude blocking the trough becomes
    very deep and the strong High pressure area drops
    or falls into the trough... tracking from western
    Canada along the east side of the Rockies all the
    way into Texas and Oklahoma. This is a very bad
    sign for significant snowstorm activity for the
    East Coast and especially the Northeast.This is
    WHY the blocking pattern over Eastern Canada is
    SO important because it forces the arctic High
    pressure systems to stay to the North and track
    along the US Canada border.... instead of falling
    into the central and Lower Plains. The High to
    the north keeps temperatures cold over the East
    coast but also provides access to ocean moisture
    as well as being BIG player in the set up all of
    ageostrophic flow when East coast Low pressure
    development is underwaycontinued

4
Importance of High Latitude Blocking (-NAO)
  • On the other hand when you do NOT have any high
    latitude blocking then you have got real problems
    in terms of getting a good winter pattern
    cooking. There is a tendency among weather
    hobbyists to really downplay the significance of
    high latitude blocking ....such as a sustained
    negative phase of the NAO. I know that there are
    some out there who say while you can still get
    big snow oin the Northeast without a Greenland
    block as long as you have lots of cold air. Often
    times the February 1995 noreaster is cited as a
    classic case of a good snow for the I-95 cities
    that and as rain and there was no high latitude
    blocking.Well that may be true but also proves
    the rule. You see the issue is not whether you
    can get a good snow in the Northeast without any
    high latitude blocking or negative phase of the
    NA O. You most certainly can BUT it won't stay
    all snow and that in my opinion is always the big
    issue. The February 95 system was such a rapid
    moving system that by the time the warm air got
    into the big cities of the Northeast most of
    precipitation had already fallen so we ended up
    with 85- 90 of the precip fell as snow and then
    the rest as drizzle or freezing drizzle. If the
    2/1995 had noreaster move at a more typical speed
    OR if the Noreaster had closed off in the upper
    levels the High latitiude blocking would of been
    far more important. Tthe warm air would have had
    more time to drive inland into the I-95
    cities.... meaning less snow and more rain. DT
    on January 11, 2007 -

5
Major Snowstorms and the NAO Index
Most big snowstorms for Philadelphia occur during
periods of negative NAO when it is trending
sharply towards neutral or positive. Sometimes
they occur when the NAO is positive or neutral
trending sharply negative. Click here to see
current NAO values http//www.cpc.ncep.noaa.gov
/products/precip/CWlink/pna/new.nao_index_ensm.htm
l
6
December 9, 2005-2.2 Inches at PHL. Regional 10
Inch Coverage of 2-
7
Major Snowstorms and the NAO Index
The NAO index at times can be deceiving. For
example, the NAO can be negative (good for
snowstorms) yet there could be no classic
Greenland block (High Pressure over Greenland).
The block is instead situated elsewhere or not in
the most favorable position for northern
Mid-Atlantic snowstorms.
8
Major Snowstorms and the NAO Index (DT)
  • There are several of the various manifestations
    of the phenomena   known as  the Negative NAO
  • A) IRELAND / - NAO  The height anomaly  seen on
    the Upper level maps may be placed as far east as
    IRELAND and still qualify as a -NAO.

Ireland
9
Major Snowstorms and the NAO Index (DT)
  • B) GREENLAND BLOCK / - NAO    The height anomaly
    is over central Greenland--- which would qualify
    the -NAO.
  • C) DAVIS STRAITS - LABRADOR  / -NAO   The height
    anomaly appears as far west as the Davis Straits
    into Labrador and northeast Quebec.

10
Major Snowstorms and the NAO Index
Also, the NAO index can be extreme negative which
can prompt a suppression of storms. In this
case, the lower Mid-Atlantic and/or southeastern
states could receive the heaviest
snow. Therefore, when it comes to the NAO, the
following must be taken into consideration. 1.
Negative or positive? 2. Trend? 3. How
negative or positive? 4. What type of NAO?
Where is the block?
11
-NAO Causing COLD or COLD Causing NAO (February
5, 2007)
Attack of cold not because of the -NAO. The
continental cold is what created the NAO. This
occurred as a result of the insurgence of cold
air which caused a storm to bomb out off the east
coast and set up the features necessary for a
NAO. -JB-
12
NAO Index (Blizzard of 2006)
  • NAO was weak negative prior to the storm, but
    trending sharply positive (this is called
    relaxing).
  • This NAO trend of negative to neutral of positive
    is often key in the development and propagation
    of East coast snowstorms.

13
NAO (Monthly Indices)
14
NAO, Blocking, and U-Shaped Cold
  • MY THINKING ON THE PATTERN AHEAD.. If you
    think if the current pattern we are in you see
    the cold air comes down like a U shape. We are
    on the left or center side of the U shape so the
    storm miss off the coast and go out. Once the
    blocking starts and shifts this entire U shaped
    cold you will see the storms roll up the coast.
    You can see the blocking going on at the top of
    the looped maps below. Follow along with your
    mouse and watch the U shaped cold shift west.
    Once you see how that works than you see not one
    but 2 storms roll up the coast. I can see can
    you?
  • -Rob Guarino Fox 29- (Jan 2007)

15
NAO, Blocking, and U-Shaped Cold
  • LONG WAVE TROUGH SWINGS WESTWARD.BLOCKING
    STARTS JAN 28TH AND BEYOND Oh you can see the
    long wave trough swing westward. The digging of
    the cold will shift to the west a bit and that is
    the SIGNAL OF THE NAO KICKING IN. This
    correlates with the NAO going negative and the
    pattern changing from southern sliders to
    noreasters. It is interesting to watch on the
    loop below
  • -Rob Guarino Fox 29- (Jan 2007)

16
NAO (U-Shaped Cold Swing to the West)
  • THURSDAY SYSTEM AND THE NAO...IS IT TOO SOON !
    The NAO is on the negative side today but is
    the "U" shaped cold not fully in swing yet ? My
    previous blog I mentioned that "U" shaped cold
    has to swing back to the west to get a phasing
    going on or get a system up the coast. CLICK
    HERE THE NAO INDEX Maybe it is too soon and the
    GFS jumped the gun ? I also showed the comparison
    to the Jan 2000 NAO and the result on the UPSWING
    of the NAO as it came from negative to neutral
    after the dip. CLICK HERE NAO PATTERN WE ARE
    GOING INTO
  • -Rob Guarino Fox 29 (January 2007)-

17
NAO (U-Shaped Cold Swing to the West)
  • In January of 2000 the NAO dipped on the 13th
    and we had snow by the 22nd, which is 9 days
    after the dip. We are now negative today and 9
    days from now it the 30th. See my point here is
    the 30th may be the real deal for snow and this
    is the transition snow. JANUARY 2000 DATALOOK
    HOW WARM 1ST HALF, COLD SECOND HALF Notice how
    we got .1 of snow the other and probably .5 to
    .8 in Philly for this one. Each system gets a
    little closer as the WHOLE PATTERN starts to
    swing NAO. This is not a GUARANTEE be any means
    that it will follow this pattern but I do see so
    many similarities in the 2 months. Notice the
    last GFS run and all the snow is after the 30th.
    Yeah, this is beyond or near 240 marker on the
    GFS but it is the pattern you must watch. This
    has been very frustrating for the snow lovers on
    here, including me. This as I noted is the tiny
    steps or STEP DOWN to winter that we have to deal
    with this season.
  • -Rob Guarino Fox 29 (January 2007)-

18
February 6, 2007 (Cold Has Nothing To Do With NAO)
  • NAO neutral AND IS NOT, AND HAS NOT HAD
    ANYTHING TO DO WITH THIS COLD. It is one week of
    negative did not change the pattern as the seeds
    of this pattern change have been outlined and
    tracked since December, and formed the basis for
    the winter forecast of a harsher mid and late
    winter. However, if it pops negative again, and I
    think it will there are some very interesting
    repercussions, and later today I will explain
    that. I just don't buy the pat answers as to what
    is causing this or that change from "El Nino" to
    "negative NAO" since it is a combination of
    things that not only I, but others have talked
    about

19
February 6, 2007 (Cold Has Nothing To Do With NAO)
  • As far as this goes, if the snow can come in
    the areas still lacking, then this will go down
    with the great El Nino flip winters that we had
    looked at. Keep in mind that we were colder than
    normal when it was rising into the lower end of
    the scale and now that we are falling back we are
    there too. The big message here is that I don't
    believe simple answers from models, or labeling
    one feature as the reason is anything I would
    consider correct. I have taken great pains, right
    or wrong to make sure our subscribers knew how
    this can evolve, and again to be fair, I do think
    there are others that have seen it too. The
    weather occurs in the real world, not the virtual
    world and the only way to judge right and wrong
    is to look at the facts. One week of a negative
    NAO should not and cannot be the reason for this.
    In any case, later today I will explain how if it
    forced negative again it can keep this going into
    mid-March, which would be the normal course of
    the great arctic outbreaks we have seen before as
    they reluctantly pulse back out -JB-

20
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