Classic MJO & Kelvin Wave Signal TAO maps show classic MJO SST Behavior
#1
Posted 27 September 2009 - 10:11 PM
The MJO has some legs with all variables that go into the EOFs saying "it's a go" here with -h2 anomalies, +h85 anomalies and -OLR anomalies. Finally, some progression was noted on the 9/26 update and this was explained why in the ENSO thread.
http://i10.photobucket.com/albums/a127/HMisdead/phaseLast40days.gif
http://i10.photobucket.com/albums/a127/HMisdead/hov_u200gif.png
http://i10.photobucket.com/albums/a127/HMisdead/hov_u850gif.png
http://i10.photobucket.com/albums/a127/HMisdead/tlon_vpot_mjo.gif
There is a +6 SD h85 positive anomaly located around 150E with actual MEAN surface winds out of the west here! It is quite an +u anomaly at the surface when the actual mean winds are coming out of the west INVOF a classic atmospheric Kelvin Wave (please don't confuse this with the oceanic type). What also is classic is the coupling going on here with a retrograding Rossby Wave across 5-10°N around 120E. In between the two systems, you'll find the MJO signal in a classic position with a strong water vapor/divergence gradient right near the Kelvin Wave. This system is very organized and straight out of a book! That westerly surface wind is heading right for the Dateline!
http://i10.photobucket.com/albums/a127/HMisdead/sfcwnd_01afnl26.gif
http://i10.photobucket.com/albums/a127/HMisdead/sfcwnd_01afnl27.gif
http://i10.photobucket.com/albums/a127/HMisdead/sfcwnd_01afnl28.gif
http://i10.photobucket.com/albums/a127/HMisdead/sfcwnd_01afnl29.gif
http://i10.photobucket.com/albums/a127/HMisdead/sfcwnd_01afnl30.gif
Another sign that this system is classic is how it is also impacting the subtropics and water. The negative tendency to the AAM that has persisted for so long around 10°N is now over as the -AAM propagates into the Mid Latitudes and westerly momentum is added across the subtropics from the organized convective system. Expect the mean AAM to become more positive over the next couple of weeks as this system propagates east towards the Dateline. Also, anticipate the SST to cool across the Maritimes somewhat where the MJO-related -OLR has focused and cooled the water. There is already some anecdotal indication of that in the dailies focused around 140-150E but I want to wait for some SST change maps to verify this. It will be interesting to see how this Westerly Wind Burst handles the -u vector pool focused over the Tropical Pacific right now. If it can get beyond this increasingly hostile battle in the ENSO regions, it may be able to start warming the western edges.
The -AAM propagation into the Mid Latitudes has already been discussed and is the reason the Pacific has had such a radical shift in the modeling. The anticyclonic wave breaking has been rather persistent lately and the mean geopotential flow is expected to shift poleward some, giving a more La Niņa-like appearance to general circulation and less meridional. However, this should be brief if this system in the tropics holds the course and it continues to add +AAM to the subtropics. This would help to extend the Pacific Jet some, position a classic El Niņo-like Aleutian low and initiate a Rossby Wave Train perhaps in later week 1 or week 2. We'll see what happens here!
But what a classic system down there!
#2
Posted 27 September 2009 - 10:26 PM
http://www.cpc.ncep....m_monthly.shtml
I correctly predicted 1 storm during the peak of hurricane season and a rather boring peak. I said the next wave of potential would come later in the month with the next CHI wave. I may have rushed the second wave in the original call but the general idea is right. There could potentially be more named storms POST peak than during the peak if my ideas (both seasonal and medium range) are correct.
The El Niņo is not the only reason for the lackluster season. I warned of the potential for subtropical lows this year in the upper troposphere given the timing of the +QBO descent. The latest 50mb winds are beginning to weaken and mean temperatures are beginning to cool here. This may combine with the next wave in CHI to perhaps bring some more named storms, despite climatology and El Niņo.
#3
Posted 27 September 2009 - 10:41 PM
Attached File(s)
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MJOsst926.jpg (108.35K)
Number of downloads: 8
#4
Posted 27 September 2009 - 10:45 PM
Quote
There is a +6 SD h85 positive anomaly located around 150E with actual MEAN surface winds out of the west here! It is quite an +u anomaly at the surface when the actual mean winds are coming out of the west INVOF a classic atmospheric Kelvin Wave (please don't confuse this with the oceanic type). What also is classic is the coupling going on here with a retrograding Rossby Wave across 5-10°N around 120E. In between the two systems, you'll find the MJO signal in a classic position with a strong water vapor/divergence gradient right near the Kelvin Wave. This system is very organized and straight out of a book! That westerly surface wind is heading right for the Dateline!
Hey
Hard for me to follow, which system are we talking about?
#5
Posted 27 September 2009 - 10:50 PM
WX1996, on 27 September 2009 - 10:45 PM, said:
Hard for me to follow, which system are we talking about?
Sorry for the confusion! The first use of system refers to the Kelvin Wave and Rossby Wave system. In a classic MJO model, you will have 2 symmetrical (about the equator) RWs moving westward positioned west of the MJO and 1 KW moving eastward positioned east of the MJO. This places the MJO right smack in the middle of these two waves. Therefore, the final use of the word system is referring to the entire process just outlined.
This whole thing right now is about as classic as it gets and comes right at a time when it should, given the QBO behavior and the repositioning warm pool in the Western Tropical Pacific. I am glad I got the this early autumn MJO wave right, even if I was a little quick with its genesis in the seasonal outlook. However, I did say that it would be in phase 4 for most of early September...but I didn't think it would stay that way right through the end of the month.
#6
Posted 28 September 2009 - 04:10 AM
#7
Posted 28 September 2009 - 04:50 AM
HM, on 27 September 2009 - 10:26 PM, said:
Hey, thanks for covering the tropical angle. :thumbsup:
I assume the pattern change will also have a positive impact on E-Pac activity?
#8
Posted 28 September 2009 - 04:54 AM
#9
Posted 28 September 2009 - 05:26 AM
#10
Posted 28 September 2009 - 06:26 AM
#11
Posted 28 September 2009 - 08:06 AM
map_last3days.JPG (589.5K)
Number of downloads: 4
Westerly mean zonal wind anomalies also increasing once again behind the MJO wave in the Indian Ocean which should help bolster the convective centres further east, possibly nudging it towards the dateline:
TAO zonal.JPG (328.68K)
Number of downloads: 4
So every prospect for continued enhanced forcing 170W-180 corresponding with projections into phase space Octants 6 and 7. However, as observed, the extratropical ocean-atmosphere dynamic is not fully embracing the tropical signals and September's phase 4 stall was a good example of shackling that the GWO is currently exerting on the tropics.
Relative angular momentum is still below climo as per last Friday (we seriously need these to update faster):
http://www.cdc.noaa....g1-21.90day.gif
and the GWO is unlikely to orbit quickly into phases coherent with the MJO for the time being until we see mean westerly zonal wind propagation polewards in addition to strong tropical forcing (mid October ??).
Probably the best summation for the pattern would be for a GWO phase 4 type (although long range modelling looks to have conflicting signal with Atlantic trough):
phase 4 nino.JPG (159K)
Number of downloads: 2
with increasing tendency towards phase 5 / 6 type into October:
phase 5 nino.JPG (160.21K)
Number of downloads: 1
#12
Posted 28 September 2009 - 09:00 AM
Good posts. I think HM is right about the mjo helping to tilt the GLAAM to more positive nino like conditions in a couple of weeks time.
#13
Posted 28 September 2009 - 09:16 AM
HM, on 27 September 2009 - 10:11 PM, said:
Agreed totally. I noticed this before reading your post this morning and I posted something about it in the El Nino thread earlier. Your discussion here expounds on what I was thinking very well.
#15
Posted 28 September 2009 - 09:29 AM
#16
Posted 28 September 2009 - 09:43 AM
I'm trying to expand my wx knowledge beyond a 7 day forecast :)
usedtobe, on 28 September 2009 - 09:00 AM, said:
Good posts. I think HM is right about the mjo helping to tilt the GLAAM to more positive nino like conditions in a couple of weeks time.
#17
Posted 28 September 2009 - 02:01 PM
#18
Posted 28 September 2009 - 02:23 PM
rfhpsu, on 28 September 2009 - 09:43 AM, said:
I'm trying to expand my wx knowledge beyond a 7 day forecast :)
Behind the mjo induced convection, the easterlies are suppressed and there often is warming of the pacific and actually there can be westerly flow near the equator. That will tend to change the GLAAM towards positive values. As the convection shift eastward towards the dateline you also often get a pattern change away from an rpna towards a pna. A couple of Weickmann and Berry articles discuss the impact.
These papers explain it better than me. The first explains how the mjo can change the low level winds and how it can help with the nino.
http://www.bom.gov.a...racts/HWZ07.pdf
The next is a paper by weickmann and Berry that explains how the convection moving eastward across the pac to near the dateline can help induce a nino like pattern.
http://www.cdc.noaa....ions/wb2006.pdf
Finally, the latest Weickmann and Berry article. Figure 3 shows how as the convection changes locations in response to the mjo and gwo, the GLAAM tendencies change.
http://www.cdc.noaa....vised_final.pdf
Hope this helps.
The
#19
Posted 28 September 2009 - 09:17 PM
VAwxman, on 28 September 2009 - 04:10 AM, said:
I am fully on board for the ideas expressed on the models in the 6-10 day period of an Aleutian Low developing. This one will be more classic of a west-based El Niņo setup whereas the last North Pacific low (before the anticyclonic wave breaking) was more like that of an East-Based event. I don't know about you, but I like a cold eastern 1/3 for November and December! :scooter: :popcorn:
#20
Posted 28 September 2009 - 09:20 PM
HurricaneJosh, on 28 September 2009 - 04:50 AM, said:
I assume the pattern change will also have a positive impact on E-Pac activity?
No problem Josh! For the most part, I think the experimental calls this year went pretty darn well. So, I am excited to try this again but in a year a little bit more active than this one! :arrowhead:
Anyway, this current MJO system is already responsible for producing a couple of TDs in the Western Pacific and now the divergence anomalies have spread all across the tropical Pacific. It is quite possible the East Pacific produces another named storm very soon and they will likely be the first to feel the effects of this wave, before it heads into the Atlantic. But usually, the lag is very short because the anomalies like to pulsate quickly beyond the Dateline.


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