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Pacific Storm and Surf Forecast
Updated: Tuesday, November 3, 2015 7:14 PM
Buoys: Northern CA - Southern CA - Hawaii - Gulf of Alaska - Pacific Northwest
Buoy Forecast:
Northern CA - Southern CA - Hawaii - Gulf of Alaska - Pacific Northwest
Pacific Links:  Atmospheric Models - Buoy Data - Current Weather - Wave Models
Forecast Archives: Enter Here
A chronology of recent Mavericks Underground forecasts. Once you enter, just click on the HTML file forecast you want to review (e.g. 073199.html equals July 31, 1999). To view the maps that correspond to that forecast date, select the html file labeled 073199 maps.html
3.5 - California & 2.0 - Hawaii
Using the 'Winter' Scale
(See Swell Category Table link at bottom of page)
Probability for presence of largest swells in near-shore waters of NCal, SCal or Hawaii.    

Issued for Week of Monday 11/1 thru Sun 11/7

Swell Potential Rating Categories
5 = Good probability for 3 or more days of Significant swell
4 = Good probability for 1-2 days of Significant swell
3 = Good probability for 3 or more days of Intermediate/Advanced swell
2 = Good probability for  1-2 days of
Intermediate/Advanced swell
1 = Good probability for 3 or more days of Impulse or Windswell
0 = Low probability for 1-2 days of Impulse or Windswell   

Small Storm Forecast for North Dateline
Inactive Phase of MJO Having an Impact

Swell Classification Guidelines

Significant: Winter - Swell 8 ft @ 14 secs or greater (11+ ft faces) for 8+ hours (greater than double overhead).
- Head high or better.
Advanced: Winter - Swell and period combination capable of generating faces 1.5 times overhead to double overhead (7-10 ft)
Summer - Chest to head high.
Intermediate/Utility Class: Winter - Swell and period combination generating faces at head high to 1.5 times overhead (4-7 ft).
- Waist to chest high.
Impulse/Windswell: Winter - Swell and period combination generating faces up to head high (1-4 ft) or anything with a period less than 11 secs.
- up to waist high swell. Also called 'Background' swell.


On Wednesday, November 4, 2015 :

  • Buoy 106 (Waimea Bay): Seas were 3.6 ft @ 8.3 secs with swell 2.4 ft @ 8.5 secs from 277 degrees.
  • Buoy 46025 (Catalina RDG): Seas were 5.9 ft @ 14.0 secs with swell 2.5 ft @ 12.9 secs. Wind northwest 16-18 kts. Water temperature 69.4 degrees. At Santa Barbara swell was 2.6 ft @ 12.3 secs from 260 degrees. At Santa Monica swell was 1.8 ft @ 13.8 secs from 245 degrees. Southward from Orange County to San Diego swell was 3.0 ft @ 13.8 secs from 255 degrees.
  • Buoy 46012 (Half Moon Bay): Seas were 16.9 ft @ 11.4 secs with swell 12.1 ft @ 10.6 secs from 305 degrees. Wind northwest 21-25 kts. Water temp 59.9 degs.


    Buoy 46059 has been reactivated.
    Pt Reyes buoy 029 scheduled for reactivation.  

    Hi-res Buoys New!

Current Conditions
On Tuesday (11/3) in North and Central CA raw local short period swell was producing waves in the 10 ft range on the face at exposed breaks and chopped with brisk northwest winds in effect. Down in Santa Cruz the same swell was producing waves in the head high to 1 ft overhead range and clean but lumpy. In Southern California up north locally generated swell was producing waves in the shoulder high range but pretty ragged with a northwest flow in effect. Down south the same swell was in the chest high range and chopped and junky. Hawaii's North Shore was small with a few chest high sets at top breaks but mostly waist high with clean conditions. The South Shore was getting some wrap around swell at exposed breaks with waves waist high or so and textured. The East Shore was also getting wrap around northwest swell with waves waist to chest high but heavily textured from light trades.  

See QuikCASTs for the 5 day surf overview or read below for the detailed view.

Meteorological Overview
For the North Pacific swell from a local gale that was off British Columbia producing 24 ft seas late in the weekend into Mon (11/2) was fading in California.

Looking at the forecast charts a small storm is forecast for the north dateline region on Wed-Thurs (11/5) with up to 42 ft seas aimed and tracking east eventually pushing into the Gulf Friday (11/6). Some swell to result for all if this does as forecast. Some residual fetch is to redevelop off British Columbia on Sat-Sun (11/8) producing up to 20 ft seas aimed southeast. But overall the pattern is not extraordinary, mainly attributable by weak destructive interference of the El Nino base state by the Inactive Phase of the MJO.  

Current marine weather and wave analysis.cgius forecast conditions for the next 72 hours

North Pacific

On Tues AM (11/3) the jet was .cgiit over Asia briefly consolidating off the Kuril Islands with winds to 150 kts riding northeast, then .cgiitting over the dateline with the northern branch tracking east over the Eastern Aleutians. The jet somewhat consolidated in the Northern Gulf then was pushing south down the US West Coast with a backdoor trough centered over Pt Conception before pushing inland. In all there was no real support for gale development from the jet. Over the next 72 hours a small trough is forecast developing off Kamchatka and ahead of the .cgiit easing off the Kuril Islands moving over the North Dateline region on Wed (11/4) with 110 kts winds flowing into it offering support for gale development. That trough is to track east over the Aleutians reaching the North Gulf of Alaska on Fri (11/6) with 110 kt winds continuing to feed it modestly all the way offering some support for gale development in lower levels of the atmosphere, and pushing up to British Columbia on Saturday. Beyond 72 hours that trough is to start to fall southeast down the Washington Coast into early Mon (11/9) then moving onshore over North Oregon but with winds down to only 100 kts offering less support for gale development. Back to the west the entire jet is to be reasonably consolidated but running well to the north up at 50N basically tracking over the Aleutians with one pocket of winds to 140 kts over the dateline region and holding into Wed (11/11). The issue remains that the supposed Inactive Phase of the MJO is in effect, restricting energy to the jet, resulting in a weaker, .cgiit and northward di.cgiaced flow.

Surface Analysis
On Tues AM (11/3) strong high pressure at 1032 mbs was 700 nmiles off North CA ridging into the US West Coast while low pressure was tracking east over Nevada, forming a pressure gradient with the high and generating 20-25 kt north winds pushing down the coast producing windswell but also blowing out whatever swell was in the water from previous low pressure system off British Columbia.

Over the next 72 hours a small but reasonably strong storm is to start building west of the dateline and a bit south of the Western Aleutians Tues PM (11/3) with winds building from 45 kts over a small area lifting northeast. By Wed AM (11/4) this system is to be developing more over the North Dateline region with winds to 55+ kts from the northwest just south of the Aleutians and seas building to 36 ft at 49N 179E. In the evening 50 kt west winds to hold just south of the Central Aleutians aimed east with 42 ft seas at 50N 173W. On Thurs AM (11/5) fetch is to be pushing into the Western Gulf at 50 kts over a small area and partially obscured over the Eastern Aleutians with seas 39 ft at 52N 166W targeting mainly the US West Coast with sideband energy down into Hawaii. In the evening 45 kt northwest fetch is to move into the Gulf of Alaska generating 36 ft seas at 52N 159W targeting mainly the Pacific Northwest and points north of there. Fetch is to fade from 40 kt Fri AM (11/6) in the North Gulf with seas fading from 32 ft at 54N 151W targeting only North Canada. This system is to fade from there. Something to monitor but this one is to be small and well to the north meaning swell is to pretty north angled relative to the US West Coast and producing only sideband energy relative to Hawaii.

  North Pacific Animations: Jetstream - Surface Pressure/Wind - Sea Height - Surf Height


Tropical Update
No tropical systems of interest were being monitored.

California Nearshore Forecast
On Tues AM (11/3) strong high pressure at 1034 mbs was off the California coast with low pressure inland creating a gradient resulting in 20-25 kts north winds along the coast and 15 kts northwest winds down into Southern CA. A foot of snow has fallen at higher elevations of the Sierra and 4 inches at lake level due to Mondays front and cooler temps. Northwest winds to start fading Wed dropping to 15-20 kts late as low pressure moves out of the area then finally relaxing Thurs (11/5) to 10 kts from the north and holding Friday and Saturday though maybe 15 kts isolated to Pt Conception. Low pressure is to be building in the Gulf with a light flow on Sunday into Monday AM but high pressure is again pulsing into the coast late with north winds back to 20 kts from the Channel Islands northward. north winds holding Tues (11/10).


South Pacific

Surface Analysis  
On Tues AM (11/3) small southern hemi swell from a gale off New Zealand on Sat (10/31) was hitting Tahiti and bound for Hawaii and California (see New Zealand Gale below). Also another gale followed behind on Mon (11/2) (see 2nd New Zealand Gale below).  

Over the next 72 hours no swell producing fetch of interest is forecast.

New Zealand Gale
On Sat AM (10/31) a nice little gale developed generating 40 kt southwest winds lifting northeast just east of New Zealand generating a solid area of 27 ft seas at 48S 174W. In the evening 40 kt southwest winds were fading tracking northeast with seas at 30 ft at 46S 168W targeting Tahiti well. This gale faded after that.

Tahiti: Swell hit on Tues (11/3). Expect residuals on Wed AM (11/4) fading from 6.6 ft @ 14 secs(9.5 ft). Swell Direction: 208 degrees

Hawaii: Expect swell arrival on Sat AM (11/7) at 2 ft @ 16-17 secs (3 ft) holding through the day. Residuals fading on Sun AM (11/8) from 2.2 ft @ 14 secs (3 ft). Swell Direction: 192 degrees

SCal: Expect swell arrival on Tues (11/10) at 1.6 ft @ 15 secs (2.5 ft faces) fading Wed (11/11) from 1.5 ft @ 14 secs (2 ft). Swell Direction: 214 degrees


Second New Zealand Gale
A gale formed south of New Zealand on Sun PM (11/1) generating 45 kt west winds over a small area with seas building to 35 ft at 59S 167E. On Mon AM (11/2) 40 kt west winds held while easing east with seas fading from 32 ft at 58S 175E. Fetch was fading in coverage from 40 kts in the evening with seas 32 ft at 57S 177W. Winds were down to 35 kts over a broad area Tues AM (11/3) with seas fading from 31 ft at 56S 173W aimed mainly east. No additional fetch of interest is forecast.

Limited sideband swell is possible for Hawaii with more direct but still not great size for Southern CA.


South Pacific Animations: Jetstream - Surface Pressure/Wind - Sea Height - Surf Height




Marine weather and forecast conditions 3-10 days into the future

North Pacific

Beyond 72 hours remnants of the North Dateline gale are to try and redevelop off British Columbia starting late Sat (11/7) generating 35 kts northwest winds falling southeast on Sun AM (11/8) and fading to 30 kts with seas building to 21 ft at 50N 140W (319 degs NCal). This fetch is to be fading in the evening while tracking southeast with 19 ft seas fading at 47N 137W (316 degs NCal) and then gone from there. Something to monitor.    

Nothing else is on the charts with high pressure at 1036 mbs filling the Southern Gulf and weak low pressure in the Northern Gulf on Wed (11/11) generating only 30 kts west winds good for windswell production, but nothing more.

South Pacific

Beyond 72 hours noswell producing fetch of interest is forecast.  

More details to follow...


Kelvin Wave #3 Second Pulse Eruption Slowly Fading
Subsurface Kelvin Wave #4 Intensifying

The Madden Julian Oscillation is a periodic weather cycle that tracks east along the equator circumnavigating the globe. It is characterized in it's Inactive Phase by enhanced trade winds and dry weather over the part of the equatorial Pacific it is in control of, and in it's Active Phase by slack if not an outright reversal of trade winds and enhanced precipitation. The oscillation occurs in roughly 20-30 day cycles (Inactive for 20-30 days, then Active for 20-30 days) over any single location on the.cgianet, though most noticeable in the Pacific. During the Active Phase in the Pacific the MJO tends to support the formation of stronger and longer lasting gales resulting in enhanced potential for the formation of swell producing storms. Prolonged and consecutive Active MJO Phases help support the formation of El Nino. During the Inactive Phase the jet stream tends to .cgiit resulting in high pressure and less potential for swell producing storm development. The paragraphs below analyze the state of the MJO in the Pacific and provide forecasts for MJO activity (which directly relate to the potential for swell production).E.cgianation of data layout below: Major sections are organized in cause-and-effect sequence starting with wind conditions/forecasts for the Kelvin Wave Generation Area (KWGA - equatorial West Pacific) followed by subsurface ocean temperature conditions (i.e. monitoring for Kelvin Waves), then ocean surface temperature conditions (i.e Nino 1.2 and 3.4) followed by atmospheric co.cgiing analysis. The 1st paragraph in each section is new/recent data and is typically updated with each new forecast. The 2nd paragraph, where present, provides analysis and context and is updated as required.

Overview: A strong El Nino is developing. It began its lifecycle in late 2013 as a primer WWB and Kelvin Wave developed. Then in early 2014 a historically strong push by the Active Phase of the MJO resulted in a large Kelvin Wave, and anomalies continued in the Spring into early Summer transporting more warm water eastward. But the cycle faltered in July due to a protracted bout of the Inactive Phase of the MJO which enabled the upwelling phase of the Kelvin Wave cycle to manifest driving cooler water east, muting warm water buildup along the Ecuador coast. Still the warm water pipe remained open, but surface temperatures near the Galapagos never recovered and any atmospheric momentum was lost. Then in early 2015, another historically strong push from the MJO occurred, effectively a repeat of the early 2014 event, invigorating the warm water transport process and, adding more heat to an already anomalously warm surface pool off Ecuador. That pool has been building steadily in spurts ever since. The paragraphs below describe the current status of various El Nino indicators, followed by a few paragraphs that tie all the pieces together and provide our analysis of what is to come.      

KWGA/Equatorial Surface Wind Analysis & Short-term Forecast:
Analysis from TAO Buoys: As of Tues (11/3) down at the surface, the TOA array (hard sensors reporting with a 24 hr lag) indicated light west winds on the equator on the dateline only. Inspecting the 00hr frame from the GFS model, light winds were over the bulk of the KWGA with no west winds indicated, and light east winds at 12 kts over the northern portion of the KWGA (see New! East Kelvin Wave Generation Area Wind Model here). Anomalies were modest from the west from the dateline to 160W and weak eastward to 140W. Nice anomalies in a normal year, but not over the top as has been the norm for months. Previously a very strong WWB burst (third of the year) associated with a robust Active Phase of the MJO (historically strong) occurred 6/24-7/17 and was followed by solid west anomalies for a 29 day window (7/19-8/19), or nearly 2 months of west anomalies or stronger. Then starting 9/2, strong west anomalies redeveloped with patches of westerly winds embedded holding to 9/17, then intensified again on 10/1 (to WWB status) holding to 10/18 and was comparable to the previous one in late June-early July, but lasting 6 weeks instead of 8.  
1 Week Forecast: The CFS model indicates very light west anomalies between the dateline and the Galapagos for the next week through Tues (11/10). Actual winds per the GFS model are to be pretty much a d.cgiicate of today through Fri (11/6) then going calm over the entire KWGA beyond. No east anomalies have occurred this year in the KWGA, not one day, and none are forecast. The thought is the anomalies are continuing to push warm water from the West Pacific to depth and the last 6 weeks worth of west winds/anomalies has set up a new distinct Kelvin Wave (#4), moving into the semi permanent reservoir already present west of the Galapagos. But with the Inactive Phase of the MJO appearing, warm water transport will be significantly reduced, at least for a while.    

A huge WWB occurred in March followed by a second smaller one (9 day duration) in early May with weaker but still solid west anomalies continuing after that through 6/10. Anomalies faded to neutral for 8 days through 6/18 as the Inactive Phase of the MJO interfered with the pattern (the first such event of the year), then weak westerlies started again on 6/18. A significant WWB (#3), the strongest of the year, started on 6/26 peaking near 7/4 then held nicely through 7/17 (22 days), the result of a historically strong Active Phase of the MJO which produced a strong and large Kelvin Wave #3, the third this year and the strongest by far. Moderate westerly anomalies redeveloped 7/29 when a Rossby Wave started interacting with the building El Nino base state, enhancing the westerly flow, developing a mini-WWB at 175E through 8/5. And westerly anomalies continued through 8/19. That is nearly 2 months of non-stop anomalies if not out and out west winds (6/26-8/19). From 8/19-8/25 lesser westerly anomalies occurred and those were mainly east of the KWGA, with dead neutral anomalies in the West KWGA. West anomalies started rebuilding on 8/26 and turned to legit west winds up at 9N on 9/3 and held in some fashion up there into 9/29 while calm winds held in the KWGA proper.  And then strong west winds redeveloped in the Northeast KWGA on 10/1 and held through 10/18, resulting in a yet another defined WWB event (#4) rivaling WWB #3 in June-July. And another small WWB started further east on 10/22 through 10/30. West wind anomalies at the surface are the hallmark of the Active Phase of the MJO and El Nino and drive Kelvin Wave production. We certainly have had a lot of that so far this year.  

Kelvin Wave Generation Area wind monitoring model: West and East New!

Comparison of 2 Strong Westerly Wind Bursts (WWB)

On left the massive WWB in late June/July that created large Kelvin Wave #3. On right the current WWB that is generating Kelvin Wave #4.
Scales are a little different but notice anomalies in the July event at 12-14 m/s est (24-28 kts) and now in Oct at 13-14 m/s (26-28 kts)
(Click to Enlarge Images)

June/July WWB October WWB


Longer Range MJO/WWB Projections: As of 10/24: 
OLR Models: Indicate an Inactive MJO signal over the equatorial dateline region, atypical of a strong El Nino. Both the Statistic and Dynamic models depict this pattern holding for the next 15 days, moving directing into the KWGA. In essence a mini-Inactive pattern is in.cgiay over the far West Pacific. Also a solid Active MJO Pattern is over the Central Indian Ocean and is to hold it's position if not easing east over the next 2 weeks. The Statistic model has it moving into the West Pacific 15 days out. That is not believable, at least not in a pure sense. But seeing how some form of weak Inactive Phase is being manifest in the jetstream today, perhaps it is not unrealistic to have some mild enhancement from an Active Phase a month out.  
Phase Diagrams 2 week forecast (ECMF and GEFS): Both models indicate some form of building 'MJO-like' active signal building over the West Indian Ocean and easing east over the next 2 weeks, consistent with the OLR models above. The ECMF has it reaching the Maritime Continent, while the GEFS does not.  
40 Day Upper Level Model: This model has all the sudden changed it's configuration. It depicts a very weak Inactive Phase in the far West Pacific tracking east with a very weak Active pattern moving into the West Pacific late Nov. This model has been well off the mark for months and we've written it off. But maybe it's getting a better handle on things now.
CFS Model beyond 1 week (850 mb wind): An Inactive MJO is in control over the dateline region and is to track east through 11/23, consistent with the models above. West anomalies are now at peak weakness and are to hold into 11/18. A Rossby Wave is to pass through this region somewhere in the middle of that time span, but not offering any help. But by 11/25 the Active Phase of the MJO is to move into the picture from the west with westerly anomalies strengthening at that time enhanced also by the same Rossby Wave, with westerly anomalies back in.cgiay at decent force and continuing through December with a nice pulse in mid-January with the MJO holding Active. That seems a bit far fetched, but given what's occurring in the KWGA area now (Inactive Phase influence) and what is forecast the next few weeks, it seems.cgiausible that a mild MJO-like influence (both Inactive and then later Active) is possible and reasonable. Still, the El Nino base state is the primary driver of Westerly Anomalies from here forward. No easterly anomalies are forecast. We are now in the core of the El Nino cycle (Oct-Dec). WWB #4 has produced Kelvin Wave #4 (10/1-10/19) with anomalies behind that continuing to fuel the subsurface warm reservoir into Dec. As of this run of the model, core westerly anomalies are to remain strong, but start easing east in the early Jan timeframe, pushing to 165W. This would shut down the warm water conveyor once anomalies start becoming centered at 170W, with the warm pool in the east starting to decay.

CFSv2 3 month forecast for 850 mb winds, MJO, Rossby etc

Subsurface Waters Temps
TAO Array: (11/3) Actual temperatures remain impressive. A tongue of 29 deg temps are pushing east from 140E to 132W and continuing to make limited daily east headway. The 28 deg Isotherm is steady at 125W. Anomaly wise +2.0 degs anomalies are bulging from 177W eastward and drifting east. +4 deg anomalies cover from 158W eastward (building west), the result of WWB #4. A large warm reservoir of 5+ degs anomalies is building in coverage from 150W. That reservoir has peak anomalies at +6-7 degs C building west to 140W and with +5 deg anomalies extending east to the Galapagos. This pocket is a combination of water from strong Kelvin Wave #3 and the slow addition of Kelvin Wave #4. The pipe is wide open and warm water continues falling to depth near the dateline and into this reservoir. This is a great scenario. Warm water appears to continue erupting west of the Galapagos per the hi-res subsurface animation (10/25) primarily at +3 degs from 140W to 100W (steady). But no +4 degs tentacles of warm water extend to the surface.
Sea Surface Height Anomalies (SSHA):  (10/30) Heights have upgraded again. 0-+5 cm anomalies are over the entire equatorial Pacific starting at 179W (fading some). Peak anomalies have reappeared at +20 cm between 120W and 140W (expanding). +15 cm anomalies extending from 105W to 157W and reaching from 5N to 5S (steady). +5 cm anomalies are pushing to Ecuador and reach the coast. +10 cm anomalies were isolated from the Galapagos westward (evidence of the westward di.cgiacement of this El Nino event). All this is indicative of a wide open pipe with a large Kelvin Wave in flight. This is a classic major El Nino setup.
Upper Ocean Heat Content: (10/30) has upgraded again indicating +0.5-1.0 deg anomalies are steady between 175W and the Galapagos. +1.0-1.5 degs anomalies are holding easing east from 169W eastward attributable to WWB #4 and the formation of Kelvin Wave #4. +1.5 deg anomalies are expanding west to 160W. A large pocket of +2.0 degs anomalies are expanding at 155W-->106W. And +2.5 deg anomalies remain present and are significantly expanding between 145W->111W. 1.5-2.0 anomalies are no longer pushing into Ecuador (only 1.0-1.5 degs anomalies). The Downwelling Phase of Kelvin Wave #4 is underway in the west while di.cgiacement to the west is preventing extreme heating between the Galapagos and Ecuador. The focus remains slightly westward di.cgiaced (but nowhere near as much as '82).   

A strong Kelvin Wave impacted the Ecuador Coast in May-June with a second somewhat weaker one impacting it in June. The third and strongest so far is erupting, but somewhat westward di.cgiaced just west of the Galapagos and not as overtly strong as one would expect, being rather a steady bleed rather than a gully washer. In fact, a careful analysis indicates it has peaked. A previous pause in warming near Ecuador occurred starting mid August, attributable to the Upwelling Phase of the Kelvin Wave Cycle, but ended on 9/20. The subsurface configuration suggested there were 2.5+ months of warm water in the reservoir (till Dec 15) and some of that water is extremely warm (7 degs above normal). And now Kelvin Wave #4 is developing, expected to extend the life of the reservoir. The peak of Kelvin Wave #3 was forecast to occur roughly on 10/4.  We revised it a few times since then, but looked back we've determined it was correct if not a little late (more below). But another equally strong WWB occurred peaking in 10/10 resulting in Kelvin Wave #4, which should peak 2.5 months later, or near 12/25 (nice Christmas present) and advecting west a month after that into Nino3.4 on 1/25. Typical of the character of this El Nino event, it is maddeningly slow and under whelming if viewed on a daily basis. But the overall impact, is marked and historically strong. And with the current WWB/Kelvin Wave in development, a more aggressive face of this El Nino is now appearing.  

Surface Water Temps: The more warm water in the equatorial East Pacific means more storm production in the North Pacific during winter months (roughly speaking). Cold water in that area has a dampening effect. Regardless of what the atmospheric models and surface winds suggest, actual water temperatures are a ground-truth indicator of what is occurring in the ocean. All data is from blended infrared and microwave sensors.
Satellite Imagery
(11/2) Overall the picture remains solid and now is getting more defined. Warmer waters are building up into Central America but retracting from the coast down into Peru while advecting west.  The big change over the past 2-3 weeks remains a solid increase in volume/concentration of warm water flowing into the Nino3.4 area. The warm water signal covers the entire equatorial Pacific from the dateline eastward with embedded pulses of warmer water from the Galapagos west. The overall signature is the strongest of any point so far this year and of any time since mid-July 1997. Compared to '97, 2015 anomalies are warmer in the Nino3.4 region, but have less concentration and coverage in Nino1.2.  Coverage south of the equator is not growing any down the Peruvian coast, and cannot complete with '97 in that regard, but is still very solid. Along the West African Coast, cool water is all but fading out there, being r.cgiaced by neutral temp water. This is not a worry as the same thing happened during the '97 event. Very warm water continues off the US West Coast 'the blob' and is holding and extending west the whole way to Japan but unrelated to this years El Nino, attributable to the building warm phase of the PDO. Cool water is building its strength and coverage over North Australia extending north of New Guinea and up into the Philippines and east almost to the dateline (Maritime Continent), typical of a strong El Nino. Warming water continues near Madagascar suggestive of a building Indian Ocean Dipole.  
Hi-res Nino1.2: Per the latest image (11/2) things are steady but not impressive from a Super El Nino perspective. Over the past 5 days temps have are holding nearshore to Peru and off Ecuador. A pocket of +4 deg anomalies is depicted approaching and impacting the Galapagos. This suggests the Kelvin Wave eruption area is westward di.cgiaced, with occasional pockets of warmer water sneaking in, but not steadily. Warming in this area peaked on 7/14 then crashed and has been trying to rebuild ever since. Given its been 3.0 months, and warming has not redeveloped to previous levels, di.cgiacement still remains the operative e.cgianation.
Galapagos Virtual Station: (11/2) Anomalies were steady between 10/2-10/26, running between +3.4-3.8 degree above normal, but then moved into the +4.0-4.3 range.  Today's reading was +4.2 degs, driven by the aforementioned hot pocket impacting the area. But for the most part this data is irrelevant since the main Kelvin Wave Eruption Area is focused west of the Galapagos.
Hi-res 7 day Trend (11/2): Modest warming is occurring well off the Peruvian Coast and just south of the Galapagos, but with a broad area of warming occurring between 120W to the dateline.
Hi-res NINO 3.4: 
(11/2) The latest image has upgraded again, and remains very impressive if not getting more that way from a Super El Nino perspective. It appears Kelvin Wave #3 is reenergizing it's eruption. Girth of the area continues increasing over the past 7 days with 3 pockets of +4 degs water embedded. This is great news, and we are exceeding peak coverage at any time previous, including 9/19. Temps between 160W-180W continue surging in girth and to the west and are on par with peak levels from 9/19 if not beating it. This warm pool is advection west of warm water resulting from eruption of Kelvin Waves #1, #2 and #3, though mostly attributable to #3. 
Hi-res Overview: (11/2) Like the low-res image, the El Nino signal is unmistakable and the strongest since 1997, and stronger than anything in the satellite age prior to that. And it beats anything so far in this event too, especially considering the new eruptions ports that have developed in the past 7 days. The intensity of warm anomalies in the eruption site west of the Galapagos is not as intense as the peak at 9/19, but is covering far more area. 5 large +4 deg vent ports are strung between the Galapagos and 140W, erupting in Nino3.4 Very impressive. And this warm water is advected west. A careful analysis of archived images indicates Kelvin Wave #3 peaked on 9/19 with mult.cgie pockets of +5 degs anomalies occurring at that time. The number and intensity of those vent ports faded, but are on the upswing now. There were none on 10/19 but as of 10/30, the picture has significantly upgraded. We can't stress enough the importance of this upgrade and the effect this will have a few weeks out as it advects west into Nino 3.4 proper. Still, we are saying Kelvin Wave #3 peaked on 9/19 (we estimated 10/4). As those waters advect west, peak warming should therefore occur in Nino3.4 one month later, or 10/19 (right now). Still, a steady flow of +3 deg anomalies is venting and advecting (with mult.cgie +4 deg pockets in.cgiay). Looking at all the satellite imagery, that seems about right.


Historical Comparison of Strong El Nino's
(Based on Nino3.4 Sea Surface Temp Anomalies)

Updated! Images built using 2 data sets - Monthly OISSTv.2 (left) & ERSSTv4 (right) This years data valid through October.
Left image suggests 2015 is already the third strongest El Nino in recorded history (beat only by '82 and '97). The right image suggests it's the 4th strongest.
In both images this years event is either the 2nd or 3rd strongest for this time of year, a bit of downgrade from last month when it was in the top 2.
Requisite Disclaimer - Current performance is no indication of future performance.
(Click to enlarge)

OISSTv2 data ERSSTv4 image


Kelvin Wave #3 Eruption Evolution
(click to enlarge)


Other Sources
TAO Data: +1.0 anomalies are in control over the entire equatorial East Pacific, the warmest in years, advecting west from the Galapagos covering the entire area west to the dateline and beyond (expanding west to 165E). We're monitoring the +0.0 anomaly line on the equator to see if it's moving east. Today its off the charts but was formally at 140E (steady and well west). +1.5 deg anomalies are steady in the west reaching unbroken to 180W. There is also a fragmented area of +2.0-2.5 deg anomalies extending from the Galapagos to 175W but most concentrated from 145W to 100W (shrinking dramatically - but we suspect there are some data errors here with mult.cgie buoys in the array down). A previous pocket of +3.0 deg anomalies has reappeared at 117W (Kelvin Wave #3 vent port). Overall the warm water signature is steady and moving west and impressive.
Nino1.2 Daily CDAS Index Temps: (11/3) Temps are on the rise after falling hard, down to +0.866 on 10/28 but up to +1.51 today. Previously temps peaked for 5 days at +2.581 near 10/8 and previously spiked at +3.0 degs on 7/3, faded, then spiked again on 7/13 at +3.0 degs and yet again at +3.0 degs on 7/22.
Nino 3.4 Daily CDAS Index Temps: Temps are steady at +2.24 today, and have been hovering in that range for a week. The all time peak for this event was at +2.512 (10/24 06z) besting the previous record of +2.468 (10/20), up from +1.824 on 10/8, and beating the previous peak of +2.44 on 10/3. The 30 day running average is at 2.0 degs with the Oct average at 2.1 degs. If those Oct readings were to hold they would be on par with '97 and '82. The new peak today is likely just coincidence, but roughly.cgiays well into the theory that Kelvin Wave #3 peaked on about 9/19.  The thought is Nino 3.4 temps are about peaked out now (until Kelvin Wave #4 starts to erupt and advect west). Previously temps were up from +2.037 on 10/1 and +2.077 on 9/17. The previous all time peak for this event was +2.24 degs on 8/23 (one day). That was crushed on 10/3 at +2.44, and now bested on 10/20 at +2.4678. By any standard we are at a Strong El Nino levels. We expect these temps to continue upward for the foreseeable future. (Note: These temps are ERSSTv.4 - biased low compared to OISSTv.2).

SST Anomalies on 9/14/2015 and what is driving them from below
(Click to enlarge)

SST Image

This years event is westward di.cgiaced somewhat like the '82/83 super El Nino event, but not as strongly so. The main evidence for this is the continued eruption of Kelvin Wave #3 west of the Galapagos with weakened warming east of there.  This suggests the Walker circulation is not di.cgiaced as far east as in '97 but more like '82/83. Best analysis from upper level charts suggests it's core is at 120W. At this time we're unsure what the effects on rainfall would be. Total rainfall in San Francisco in '82/83 was 38.17" (+16.38") versus 47.22" in '97/98 (+25.43"). The long term average is 21.79". In LA in '82/83 it was 31.28" (+16.47) versus 31.01" in '97 (+16.2"). Long term average 14.81". Regardless, both events were well above average. This also suggests the core of storm production will be north of the most warming. So rather than the Eastern to Central Gulf of Alaska being the focus, it might be more in the Western Gulf. This is actually a good thing relative to California by perhaps giving resulting swells more room to groom themselves before hitting the coast. This might bode not so well for Hawaii, with large stormy conditions the result. Of course, this is just speculation at this time.  

Pacific Counter Current:  As of 10/27 the current was moderate from the west but not overtly impressive. The current is pushing modestly west to east mostly north of the equator from 125E to 120W, with a large pocket of solid westerly velocity from 165E to 140W. There were 2 pockets of east current at  90W and 120W but tiny in coverage. Anomaly wise - modest west anomalies were spread mostly north of the equator over the West Pacific, with a strong pocket north of the equator from 165E to 120W but a little fragmented, then fading. One pocket of east anomalies was indicated south of the equator at 125W and another at 140E.  This is reasonably impressive as long as one does not compare it to '97, because if you do, there is no comparison. In '97 the current was raging east from 150E to 130W on and north of the equator.   

SST Anomaly projections
CFSv2 model - PDF Corrected:
 We are disregarding this charts from here forward. The last run we reviewed run on 10/24 for the Nino 3.4 region, peak temperatures for this event have supposedly already occurred on 10/1 at +2.2 degrees. +1.95 degs anomalies are to hold till Dec 1, then a big crash is to occur. Considering temps in Nino3.4 now and the size of the Kelvin Wave #3 below and developing Kelvin Wave #4, we suspect this projection is well on the low side. 
Uncorrected Data we continue monitoring.  It looks more realistic suggesting a peak to +2.55 degs on Nov 8, then starting a fast fall. We'll venture a guess of somewhere around +2.3 degs for a one month average peaking in Dec, later than what the model suggests.
IRI Consensus Plume: The mid-Oct Plume has upgraded again, suggesting peak temps between +2.3 degs (Statistical models), +2.5 degs (Dynamic) with the CPC consensus at +2.45 occurring during Dec. The mid-July consensus was spread between +1.5-2.0 degs, the mid-Aug between +2.0-2.5 degs and the mid-Sept between +2.1-2.5 degs. See chart here - link. 

If one is to make a direct comparison of the 2015 event to '97 at this time of year based on the areal coverage of water temps, there is no comparison. '97 imagery leaves this years event in the dust. The '97 event built non-stop from this point forward (in terms of areal coverage). Instead, the 2015 event, though warming nicely with comparable to stronger anomalies in Nino3.4 and Nino4, is weak in Nino1.2 and the coverage of warm waters is a worm in this area compared to '97s mammoth coverage. A clear and significant downgrade occurred in the Galapagos area 8/12-8/20 the result of a pause in upwelling of warm water in that region, a break between the first and second Kelvin wave eruptions and the third poised just off Ecuador. But Kelvin Wave #3 is having a good impact west of this area (9/19-11/3) but it has hurt the overall coverage compared to '97. But compared to the other super El Nino in '82, this years event crushes it. We continue solidly.cgiaced between '97 and '82. There could be no better.cgiace to be.

Atmospheric Co.cgiing Index's (lagging indicators rather than driving oceanic change):   
Daily Southern Oscillation Index (11/3): Was steady at -9.10. Of note: The 97 El Nino had daily values at -40 to -50 in early Nov with one spurt to -76 Jan 30-31st. A peak reading so far in this 2015 event was -49.70/-46.60 on Oct 3 & 4 and then -42.20 on 10/14. 
30 Day Average: Was rising from 17.21. The peak low was recorded on 10/9 at -22.72, beating the previous peak low of -20.95 on 8/21, with the previous lowest at -20.49 on 7/18/15. This is exactly where we want to be (at -20 or lower).  
90 Day Average: Was rising from -17.85. A record low of -19.28 occurred on 10/16 and was matched on 10/20. The previous record low was -18.56 on 9/16. This is the critical threshold we've been anticipating (values -18 or lower), providing yet more evidence of strong atmospheric co.cgiing. We want to see it hold there, and that goal is looking more possible. It has been at or below -10.0 since early July and -15.0 since 9/4 and on a steady fall ever since. The 90 day SOI bottomed out at a low reading on 8/5 at -14.17, then beat it on 9/2 at -15.23, beating that on 9/16 at -18.56 and now -19.28 on 10/16. 
Trend (looking for negative SOI numbers, indicative of the Active Phase of the MJO or El Nino): The near term trend based on the daily average was indicative of a fading El Nino base state. The longer term pattern was indicative of a steadily building El Nino base state.
SOI Trend - Darwin (looking for high pressure here): Weak low pressure was over Southeast Aust on Tues (11/3) and forecast to fade but not be r.cgiaced by high pressure. More low pressure is forecast by Mon (11/9). It looks like the Inactive Phase of the MJO really is having a negative impact on El Nino.       
SOI trend - Tahiti (looking for low pressure here): On 11/3 weak low pressure was south and moving east and away from of Tahiti (11/3) but with a new weak low pressure system forecast developing south of Tahiti into Fri (11/6). Weak high pressure to follow with another low behind that on 11/11. This will keep the SOI a bit higher than what it has been of late. If a Super El Nino is in development one would want to see continuous local lows near or over Tahiti. We're not seeing that.  
SOI 1 week Forecast: The net result is to be a trend of SOI values moving to neutral. The Inactive Phase of the MJO is having some impact.           
SOI Analysis: During El Nino, the SOI functions as a measure of how well the ocean and atmosphere are co.cgied. Current numbers suggest good co.cgiing though not great, but getting better footing slowly but steadily (notice the 90 day average trend). This pattern is to only change for the better as the El Nino base state builds as we move into Fall. A consistent 90 day average of -18 is our target, indicative of a strong El Nino.
Southern Hemi Booster Index (SHBI) Analysis (which is theorized to supercharge a developing El Nino): Per the past 5 day 850 mbs anomaly charts there was no evidence of a south flow in.cgiay. Per the GFS model no real south flow is projected. It is high pressure over Southeast Australia that sets up the required southerly surface flow in the Tasman Sea. South and southeast wind anomalies have been in this region off and on for weeks now (previous run 7/29-8/10, this run 8/13-8/18), then returning consistently 9/18 through 10/25, then fading. The SHBI appears to only be slightly influencing El Nino development, but we have no hard numbers to confirm. 
ESPI (like SOI but based on satellite confirmed cloud cover): (11/3) today's value is falling at +1.71, and has been trending down since a reading of +2.40 on Sat (10/17), but still well within the average of late (which is well above normal). It has been holding in the +1.95-2.20 range for weeks (thru 10/13) with only minor fluctuation. The ESPI was steady in the +2.5 range through 8/10, then began falling, to +2.42 on 8/18 and bottoming out at +1.78 on 8/26. It started rebuilding on 8/29 at +1.89 holding at +1.87 on 9/18 and up to +2.2 on 9/24 reaching +2.3 on 9/26, then down to 2.02 on 9/29. Historically the peak of the '82 El Nino was +2.2 and the '97 event +2.85. This suggests the '15 El Nino is reasonably well co.cgied with the atmosphere, more so than some of the other indices indicate. Monthly ESPI values are as follows: July 3.76, Aug 2.34, Sept 2.1. We need to see values +3.0 or higher for the next 2 months to complete with '97.
Multivariate ENSO Index (MEI) (Sept) The current ranking is up again, rising from +2.37 (Aug) to +2.53 (Sept) or up 0.16 standard deviations (65). The July MEI was 1.97 SD (65). At this same time in '97 the ranking was 3.00 SD (66) and in '82 it was 1.85 SD (62). So we continue between the '82 and '97 events but closer to '97, in strong El Nino territory presumably moving towards the Super El Nino range. The top 5 events since 1950 in order are: '97, '82, '91, '86, and '72 with '97 and '82 classified as 'Super El Nino's' because they reached 3 standard deviations (SD) above normal. '91 and '86 were at about 2.2 and 2.1 respectively with '72 peaking at 1.8 SD's above the norm. We've already beat all those. Suffice it to say we are somewhere between '82 and '97 in term of of atmospheric co.cgiing per this index. Most impressive.  
North Pacific Jetstream (11/3) Detailed analysis is in the NPac Short Term Forecast above. In short, the jet has started the Fall transition influenced by El Nino, looking decent but not exceptional yet. But it appears the Inactive Phase of the MJO, no matter how slight, is having a dampening effect and will continue for the next 2 weeks.  

Comparing the 2015 El Nino to '82 and '97
Full Sized Chart
(Click to enlarge)

Conclusion (Updated 10/20): WWB #3 peaked on July 4, with the resulting Kelvin Wave peaking on Sept 19 west of the Galapagos, or a roughly 2.5 month travel time.  Likewise those warm waters advected into Nino3.4, peaking about one month later, or 10/20 (all evidenced by hi-res SST anomaly data and Nino3.4 indices). Theoretically this would be the peak of our El Nino event from an ocean perspective (and as projected by PDF corrected CFS model), with peak atmospheric influence occurring approximately 2 months later or 12/20. But yet another WWB has occurred (WWB #4) of near equal strength peaking on 10/17, which has resulted in formation of Kelvin Wave #4. 

Using the same te.cgiate, peak eruption of Kelvin Wave #4 is expected on 1/2/2016 (westward di.cgiaced) with eruption port temps at +4-5 degs, and advecting into Nino3.4 and peaking roughly 2/2/2016 with peak atmospheric influence on approx 4/2/2016. This suggests peak atmospheric perturbation will occur in the window from 12/2/2015-4/2/2016, or well di.cgiaced later in the Winter as compared to the '97/98 event, and somewhat like the '82/83 event. 

In terms of comparative strength based on Nino3.4 temps, '97 peaked at +2.32 degs with 4 months of +2.0 degs anomalies and '82 at +2.21 degs with 2 months temps greater than +2.0 degs. 2015 is looking to produce a +2.1 degree one month average based on very rough data today, with a huge reservoir of +3-4 deg anomalies still venting to the surface and likely continuing for the next month of more, with yet another burst of warm water (Kelvin Wave #4) moving into position. 

The real question is: How much (if any) cooling will occur in Nino3.4 between the downslide up of Kevin Wave #3 and the ramp-up and peak of Kelvin Wave #4? Assuming steady state anomalies in Nino3.4 not falling below +2.0 degs in in that window, there could be 4 months of +2.0 anomalies in Nino3.4 (with higher peaks), providing a strong and long su.cgiy of energy to fuel jetstream enhancement and similar to '97 and besting '82. It's not just magnitude of the peak temps that make a difference atmospherically, but also the duration of those anomalies. The longer and stronger the anomalies, the greater the atmospheric response. At this time the expected atmospheric affects should be significant, though di.cgiaced somewhat later in the season. The above analysis is not a definitive statement, just informed speculation based on previous similar events.         

See imagery in the ENSO Powertool


External Reference Material: El Nino Southern Oscillation (ENSO), Madden Julian Oscillation (MJO), Pacific Decadal Oscillation (PDO), Southern Oscillation Index (SOI), Kelvin Wave

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