http://iri.columbia.edu/climate/ENSO/currentinfo/technical.html
http://www.pmel.noaa.gov/tao/jsdisplay/
http://www.cdc.noaa.gov/forecast1/IndoPacific.frcst.html (note the initial projection)
http://www.cpc.ncep.noaa.gov/products/precip/CWlink/MJO/index.primjo.html (link 18).
Full disk satellite imagery shows tropical convective forcing literally breaking up into tropical cyclones from the Bay of Bengal into the
The first point to make is that MJO variability is currently strongly impacting
For the
Official forecasts have not yet picked up on this (at the time of this writing), being fooled by model disagreement, etc.. This again demonstrates the need of an atmospheric dynamics based weather-climate linkage framework to intelligently evaluate numerical model guidance (insert my angry Rottweiler)! One purpose of the WB (2007, 08) GWO is to facilitate the latter. There is no cookbook to making subseasonal forecasts, and that includes blending numerical model predictions!!! Ensemble prediction schemes such as from ESRL/PSD as well as the deterministic ECMWF model have provided the most realistic solutions for the
http://www.cpc.ncep.noaa.gov/schemm/z500ac_wk2_na.html .
The final point is that a potentially explosive pattern for severe local storms on the Plains exists for at least week-2 (exact timing is white noise). Locations to get hit the hardest may be farther north than observed during the last few weeks (climatology understood). The latter may extend from portions of
Locations from portions of the Bay of Bengal into Indonesia/Southeast Asia and the Philippines are still likely to get hammered with intense to severe thunderstorm activity week-1 including tropical cyclones (please see JTWC). This activity is probable to weaken weeks 2-3 as tropical thunderstorm activity increases from Africa into the
The best shot for enhanced Western Hemisphere convection, impacting northern South America into the Atlantic ITCZ appears to be weeks 1-2. I trust the expertise of the appropriate weather centers internationally to alert the public of additional weather hazards worldwide.
Appendix
An experimental quasi-phase space plot of the GSDM utilizing time series of normalized global relative AAM time tendency (Y-axis) and normalized global relative AAM anomaly (X-axis) can be found at
http://www.cdc.noaa.gov/map/clim/gsdm.shtml
This phase plot is being re-done, as is the web site. Stay tuned. We call the behavior of this plot the Global Wind Oscillation (GWO). While the intent of the legacy GSDM is to extend current thinking beyond the MJO, the GWO quantifies variations used to derive the original GSDM in a manner that is “user friendly” analogous to the WH (2004) “convention”. In addition, the GWO plot does not have the ENSO signal removed.
Please see the revised description of the GSDM per above link. Also, I encourage the readers to study the annotated MJO and GWO phase space plots to help relate the global variations explained by those techniques to “weather”.
Links to CPC and PSD ENSO discussions:
http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/enso_advisory/index.shtml
http://www.cdc.noaa.gov/people/klaus.wolter/MEI/
The following is a link to information about the stratosphere and other nice monitoring tools:
http://ds.data.jma.go.jp/tcc/tcc/products/clisys/index.html
These are probabilistic statements, and work is ongoing to quantify in future posts (for example, risk assessment maps, signal to noise ratio plots and shifts of probability). We hope that an opportunity will arise for us (soon) to have a dedicated web page effort to expedite more objectively, with rigor, thoroughness and verification.
The WB (2007) paper on the GSDM has been published in the February issue of MWR. In addition, a two-part paper is in ACTIVE preparation by WB that will formally introduce the GWO along with subseasonal composites for variables such as surface temperatures. We want to emphasize notions such as global-zonal mean-regional scale linkages as well as forcing-response-feedback (with subsequent interactions) relationships.
Given shift work and travel, updates are extremely difficult. I should be able to post another discussion the weekend of 24-25 May.
Ed Berry
7 comments:
Wow...where I do not understand much of what you say, I am glad you bring in the physics behind making these extended forecasts. I cannot see how the models going crazy with the ridge /trough dilemma in the southwest should give anyone a 4 out of 5 confidence level. I also do not know what scientific basis there is for using 10% of the GFS operational, 40% of the Mean, 45% of the operational ECMWF and 5% some other nonsense. I just do not know how one makes these decisions.
I think this is one important topic for future forecasters to understand! Thanks Ed for your atmospheric insights!
Paul Sirvatka
Hey Ed, Matt C here. I, like Paul
do not totally understand your methods, but looking at he latest
operational guidance all of the deterministic models are now coming around to your forecast. I actually used your confidence in the pattern to take a flyer on a flight to the Plains next Friday.
If I am in DDC maybe I can drop by the office.
Matt Crowther
Hi Paul,
Thank you for the comment! Klaus and I are working on a two-part paper (likely for MWR) that we hope will communicate what the GWO is, along with composites. The latter should help forecasters get a better feel for the subseasonal synoptic evolutions. An important point is to have a complete forecast process that includes a diagnostic weather-climate linkage framework and the models are only a component. Hopefully we will have a web page with "everything" on-line, along with more frequent ~week 1-4 predictions. Stay tuned!
Regards,
Ed Berry
Hi Matt,
Good to hear from you! Thank you for the comment. You can see the comment I left for Paul. We are seeing a good example of the models catching up to the atmosphere. The deterministic ECMWF and the PSD ensemble were one of the first models to catch on, even out to ~day 10 for the EC.
We felt confident this upcoming retrogression was likely nearly a couple of weeks ago based on the MJO/GWO. What adds confidence is when the models start to give solutions consistent with our atmospheric dynamics based weather-climate linkage framework.
Look forward to seeing you if you are in DDC!
Ed
Ed, one thing that does worry me about this upcoming pattern- could the amplification in the EPAC be so pronounced that the trough will end up digging too far west for a really good Plains severe outbreak? To me that seems like the main "fly in the ointment" that could ruin my upcoming chase trip. The new Canadian SEF shows this, and I have noticed in the past with this type of retrogressive pattern that we sometimes end up with a closed low near CA and ridging in the Plains.
Hi Matt,
Obviously there are issues with the unpredictable details. However, while the large amplitude notion appears correct, I do not think it is probable for the trough to dig along the west coast. For all the reasons the trough digging into the Rockies is reasonable leading to several days of severe storms on the High Plains. This pattern should shift east loosing amplitude with more western states troughs probable ~weeks 3-4. Of course, there will be a northwest shift with the seasonal cycle.
Ed
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