WELCOME BACK! Be sure to check out our inaugural Anti-Seasonal Outlook, Seasonal Outlook: A Four Part Series. We will have a new post each day, Monday through Thursday (10/20-10/23). Also, we will have new and improved content through the season, so be sure to come back often!

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Thursday, November 20, 2014

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Lil' Somethin' Better Than Nothin'

In the nouveau climate of enhanced aridity in the Sierra Nevada, we have become accustomed to long stretches of little to no precipitation during the cool season. Hopes are high that this season will buck that trend but the possibilities are wide ranging. That said, the recent storms, albeit weak, have provided much needed moisture for parched soils, dry vegetation, and empty reservoirs. Trail conditions could not be better at lower-mid elevations and many resorts are producing snow. The storm making its way into the Sierra this afternoon and another tomorrow (Friday) evening will continue to moisten soils and provide much-needed natural snow to augment snow-making efforts for Thanksgiving groomer runs.

Precipitation from today's event will begin during the early afternoon in the Sierra and continue into the evening. Snow levels will start around pass level and fall rapidly to 5500ft, possibly lower. Favorable orientation of lower and upper level winds will provide orographic and dynamic lifting. Total snowfall on the crest will be in the neighborhood of 8-10". Totals at 6k will be in the 4-8" range. These values are higher than the 3am NWS discussion, but I am using the most recent WRF and GFS simulations; perhaps they are more favorable.


The Friday evening-Saturday morning event will sing a different tune. Copious moisture provided by an errant tropical Pacific moisture plume will result in an enhanced positive moisture flux into northern California. However, the Sierra will be located under the warm sector of the jet stream and snow levels will be around 8k. Low-mid level wind are also oriented much less favorably for enhancing precipitation over the mountains. Therefore, at least 6" of sticky (GOOD!) snow can be expected with this event along the crest. If the jet migrates southward a few 100km, these totals could easily double. The WRF simulation is a bit bullish with over an inch of liquid precipitation for the northern Sierra, given the northwesterly 700mb flow, although the happy face side of the jet exit region does nose into Nevada County and will briefly provide a lifting mechanism. BUT! If it verifies, and we see a foot of rock hiding stump gobbling glop, nobody will be sad.


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Tuesday, November 18, 2014

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3 Storms with the Price of 1...

Good news: We have three separate storms coming our way in the next 5 days.
Bad news: They won't bring that much snow.

The first storm will impact the Sierra tomorrow afternoon and bring about 1-3", the next storm will come through about 24 hours later and bring another 1-4" of snow. The final storm looks the most promising, but the models have been pretty inconsistent over the past week handling the 'breakdown' of the upper level ridge (aka Ridgesaurus). The third and final storm's current forecast is for 3-6", but could be susceptible to rain on snow initially overnight Friday into Saturday. 



11/19
11/20
11/22
1st Storm
1-3” Snow level: ~8000’


2nd Storm

1-4” Snow level: ~7000’

3rd Storm


3-6” Snow level: ~6500’

The first storm is a classic 2011-current storm. Trough hits a ridge, shifts to the NE, Pacific NW gets most of it and we get the southern end. That is why the snow level is higher and the snowfall totals are low (Figure 1).
Figure 1: 3-hour forecast precipitation (in.) and snow level (ft) valid 11/19 at 1pm. Courtesty of DRI/CANSAC.

The second storm is a little colder and is taking an interesting trajectory. A broader trough of low pressure splits into two centers (we have seen this once already this year). The southern one hits the Sierra on a quasi NW-SE path (Figure 2). Additionally, the trough digs and deepens to the south and east especially on the lee side of the Sierra (hello PV conservation). This isn't a common trajectory for the Sierra and place north to north west of Tahoe and especially east, won't see much snow. More of it will be confined further south in the central and southern Sierra. 

Figure 2: 500mb (mid-level) temperature, heights, and winds valid Thursday night. Notice the NW-SE tilt of the trough/shortwave over the Sierra. Courtesy of San Jose State University 


Figure 3: 500mb (mid-level) temperature, heights, and winds valid Saturday afternoon. Notice the NW-SE tilt of the trough/shortwave over the Sierra. Courtesy of San Jose State University 

Finally, the third storm is a disturbance embedded in mostly zonal (west to east) flow (Figure 3). Due to the zonal nature of this storm, it is susceptible to higher snow levels (i.e. rain on snow) early on with falling snow levels coming later in the morning and afternoon on Saturday. This is something that could bring snowfall totals down and make this storm similar to the previous two. However, the two previous storms somewhat break down the ridge or at least undercut it, moving colder air into the area. A better moisture connection stretches across most of the North Pacific as well (Figure 4). This will bring higher snowfall totals and lower snow levels barring the higher snow levels possible overnight Friday into Saturday. A strong zonal cross North Pacific upper level jet is accompanying the storm, which is a good ingredient for Sierra snowfall (Figure 5).

Figure 4: Precipitable water (mm) valid Saturday morning. Plume of moisture stretching from SE of Japan to northern California. Courtesy of University of Hawaii. 

Figure 5: 250mb (upper-level) heights (contoured) and winds (shaded) valid Thursday morning. Upper level jet stretching from Japan to West Coast with an Aleutian low forming (ed). Courtesy of University of Hawaii. 

The pattern is pretty interesting, which is a foreshadow of a future post. However, the here and the now is we have 3 storms coming that will bring at most around a foot to the higher elevations of the Sierra. While it isn't much, it is better than being under the (very stubborn) ridge and watching the little snow we have melt away. 


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Sunday, November 16, 2014

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How a Storm Named Nuri Froze the U.S.


This past week has been highlighted by extremely cold temperatures for the majority of the eastern two-thirds of the country and the Pacific NW. Cold air outbreaks east of the Rockies are typical in November, but this year’s is particularly unique.  Record low highs and lows have been shattered from Montana to Texas and the cold continues to hang around with more records likely to be broken in the Eastern Gulf States midweek.  

So what makes this year’s cold air outbreak so unique and long lived?  Well in this case it all stemmed from super typhoon Nuri.  Super typhoon Nuri developed east of the Philippines and quickly exploded to a category 5 storm with a max wind speed of 180 mph.  At one point Nuri was forecasted to exceed the strength of Haiyan, the storm that devastated the Philippines last year. Instead, Nuri quickly weakened as it tracked northward and lost its tropical cyclone designation east of Tokyo on November 7th.  

The cyclone continued northward and began to phase with the jet stream... Sound familiar?  Superstorm Sandy should come to mind.  With the support of the jet stream, the cyclone underwent “explosive cyclogenesis,” or deepened rapidly, becoming one of the strongest storms ever recorded in the Bering Sea.  The storm track and evolution of Nuri can be seen in Figure 1.

Figure 1: Nuri’s storm track, storm type and recorded wind speeds.

Although Nuri and the ensuing extratropical cyclone was primarily a storm for the fishes, the amount of warm moist air that the storm transported into the Bering Sea was exceptional.  Figure 2 shows the 500 mb (the height in the atmosphere that controls the majority of the weather over the mid-latitudes) state of the atmosphere over the Northern Hemisphere.  The blue box shows the same area for each 24 hour time step. 

Figure 2: 500 mb state of the northern hemisphere


 In panel a. the extratropical cyclone can be seen entering the Bering Sea at the western edge of the box as the circles.  The purple shading below the cyclone represents the wind which is acting to transport warm air (green shading) from the Central Pacific into and over Alaska. At time step b., the cyclone is beginning to weaken (fewer circles) and so is the northward transport of warm air (less purple shading).  Even with the weakening storm and decreasing transport, a huge increase in green shading can be observed over Northwest Canada.  

The warm air continues eastward and expands all the way to the western shores of the Hudson Bay, as can be seen in panel d. This huge influx of warm air displaces the notoriously cold air of the Arctic Circle and drives it southward on a crash course with the Central U.S.   The cold air can be seen overtaking the Northern Great Plains in panel d. as the dark blue shading.  Figure 3 shows the departure from normal temperatures observed over the U.S at the same time as panel d.

Figure 3. Note: the labeled contours represent the true departure of high temperature from normal as the color fill and corresponding color bar does not get negative enough. Source: CPC 

Some areas experienced high temperatures as much as 38 degrees below normal as can be seen in Figure 3. That is extremely rare but not unheard of. Since records began in the mid to late 1800s there have only been two other cold air outbreaks of this magnitude in November, which occurred in 1880 and 1976. If extreme cold air outbreaks in November are any indication of Sierra snowfall, we are in for a dismal snow year.  The winters of 1881 and 1977 were the two lowest on record…






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Wednesday, November 12, 2014

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Small storm with high elevation snow on the way

The weather in the Sierra has been quiet, with above average temperatures and no precipitation since the Halloween storm that brought several inches of snow to Tahoe ski resorts.  During the fall and winter, when the weather is quiet in the west, you could usually bet the pattern is more active in the mid-section of the country or the northeast. 

 This is exactly the case, as shown in Figure 1.  The ridge of high pressure that is over currently over CA is impressive to say the least, and extends all the way into AK and northern Canada (Figure 1).  In fact, at the 500 mb level (~18,000 ft.) the temperatures Tuesday morning were colder over MT and WY than the temps over parts of the Arctic Circle!  The blocking ridge of high pressure has allowed a deep trough to dig into the north-central US, which has already brought frigid temperatures and the first significant snowfall for many places.



Figure 1. 500 mb heights (black contours), valid 12Z Tuesday, show the massive ridge being pumped up into AK and Canada. The 500 mb temperatures (dotted colored lines) show a deep trough and arctic air over the central US. Source: RAP/UCAR.

This mega-ridge (aka Ridgeasaurus) isn't going to break down, but rather it will become nearly closed off over AK, which will allow for the southern branch of the split jet stream to make its way into CA, and bring a rather weak system to the Sierra by late Wednesday night.  Figure 2 shows the jet stream level winds, and you could see the nearly closed high in AK, with easterly winds off the coast of British Columbia, and a jet streak with westerly flow moving into central and southern CA.

Figure 2.  Upper level winds (250 mb; shading indicates wind speed), valid 12Z Thursday, showing a jet streak moving into CA.  Source: RAP/UCAR.


The dynamics are not very impressive with this system, and the cold front that will come through is extremely weak.  Looking at the 700 mb (~10,000 ft.) temperatures for early Thursday morning, you could see that the temperature contours (colored lines) over CA have a lot of space in between them (Figure 3).  A much more dynamic front can be seen moving through the mid-west into the northeast, where the temperature contours are very close together, indicating a strong temperature gradient.  

Figure 3. 700 mb temperatures indicate the freezing level at ~10,000 ft. to be just south of Tahoe during the heaviest precipitation. Source: RAP/UCAR.


The 700 mb temperatures in Figure 3 can also give us a good indication of what the snow level will be.  At the onset of the storm, snow levels will likely be high (above 9000 ft.), and without a deep, digging trough, and cold air advection behind the front, the snow levels may only fall briefly to the 7000-7500 ft. level. The blue contour in Figure 3 shows the freezing level at 700 mb to be just south of Tahoe during the heaviest precipitation.

Ok, so on to the precipitation and snow fall amounts.  The high resolution (2-km) WRF simulation shows about 0.5-0.75 inches of liquid over most of the Sierra crest ski resorts, with slightly higher amounts for the southern areas down to Kirkwood (Figure 4).  


Figure 4. Storm total liquid precipitation.  Notice the slightly higher values just to the south of Tahoe. Source: CEFA/DRI.


With the high snow levels, this should translate into 4-6 inches of snow possible above 8000 ft., with slightly higher totals near the crest and around Kirkwood.  I would expect little to no snow accumulation below 7000 ft.  Sorry, but this will not be the storm to get the ski resorts open (but every bit helps).

The area should stay dry through the weekend, but forecast models are indicating that a stronger (and slightly colder) storm could bring more high elevation snow to the region next week. A lot could change by then, and we will have an update with more details over the weekend.
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Thursday, October 30, 2014

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UPDATE: Halloween Storm Forecast

The storm continues progressing towards the Sierra and will arrive tomorrow evening. The storm arrives a little later than initially thought, but the heaviest snow and precipitation will still fall Friday evening through Saturday morning. It will continue into Saturday afternoon before tapering off Saturday night. Snow levels will begin around 8000 ft. and will drop down to below 5000 ft. Saturday morning. The heaviest precipitation will fall with the snow levels between 5500 ft. and 7500 ft.

  • Around Tahoe: 4-8" of snow with highest elevations totaling 1'+ of fresh snow
  • Further south: 8-12" of snow with highest elevations totaling 18"+ of fresh snow
  • Heaviest snowfall timing: Friday evening through Saturday morning
  • More spillover precipitation than previously thought

Snow accumulation for the next 72-hours. 95% probability of receiving up to but not exceeding the contoured values. So Truckee has a 95% chance of receiving up to 4-6" of snow. Image via WPC.

The strong upper level low pressure system (trough) shifts its overall tilt as it impacts the Sierra tomorrow. The trough becomes more negatively tilted (think of this symbol: \ ), the flow wraps back around on the lee side (east side in this case) inducing more upslope flow for the east side of the Sierra increasing snow and rainfall totals. 

Storm total precipitation forecast. Via NWS WFO Reno. 

Additionally, the cold air in the trough will help produce convection, which will pump moisture up and over the Sierra. A broad area of upper level divergence (supports upward motion) will aid this process and stay intact as it moves over the Sierrra, which does not always happen. And finally, the lack of downslope winds due to the trough's trajectory and vertical temperature and wind profile will not disrupt upward motion on the east side of the Sierra. 

Snow accumulation will be the toughest to gauge with the warmer ground. We could see snowfall totals diminished due to the first brave snowflakes melting. However, as they melt and evaporate, the ground cools and with the near to below freezing temperatures forecast, will set the stage for snowfall accumulation eventually. 


Storm total snowfall forecast. If snow levels drop quickly, snow totals could increase by 10-25%. Via NWS WFO Reno. 

In summary, this system isn't the coldest, it isn't the wettest, but it has plenty of both to give us a nice early season snowfall. It's trajectory and intrinsic vertical temperature and wind profiles will also help give the east side more snow and rain than it would normally receive. 

Enjoy a rainy/snowy Halloween and be safe on the roads this weekend! 

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