IOP 5: The big one?

With the new year comes a new cold air pool, and this one could be the big one we've been hoping for. More on that in a moment, but first I'd like to reflect a bit on what we've learned thus far through one month of operations that involved 4 IOPs and numerous sub-IOPs.

Potential temperature deficit for the month of December as a function of height and time.

Values are calculated relative to a dry adiabat from the mountain top crest level.

I think the most significant realization that we've come to is that cold air pools are essentially the climatological base state during the heart of the winter when the sun angle is low. And to that end, it is more the lack of solar heating than the prominance of nocturnal cooling that seems to allow these events to persist for days at a time. I say this because December has been one of the cloudiest winter months in memory in Salt Lake... and the presence of clouds has severely limitted the number of nights with strong radiational cooling. Instead the synoptic-scale flow has frequently produced warming (advective and subsidence) in the lower mid levels (600-700 hPa) that has effectively capped the valley's of the great basin. The lack of surface heating then limits our ability to 'burn through the cap.' So it has been warming above, not cooling below that has generated most of our stability (although we have had a few nights were cooling played a big role).

Furthermore, we went into the project expecting most of our events to occur during strong ridging... well we haven't seen many strong ridging situations, with the month as a whole having anomalously strong SW and moist flow, and yet we've had some impressive cold air pools. So while the synoptic flow has exerted a strong control on the strength of the cold air pools, it has done so in ways that we may not have expected. Its not all about ridging!

We've also had a chance to observe two break up periods during strong southerly winds. Data seems to reveal a competition between advective terms (forcing the cold air pool north) and density current or thermally driven terms (trying to drive the cold air pool to the south). As the balance between these terms shifts in time so does the position of the interface between the cold air pool and the dry, warm and well mixed air. The lake has also been seen to be a 'resevoir' of cold and moist air, which can contribute to the density current nature of the cold air pools.

Okay so now to IOP 5.

Ridging?... not exactly. Clear skies?... maybe. Warming aloft?... definitely. Snow on the Ground?... yes sir. Cold air intrusion?... You betchya!

A pretty good recipe for a persistent cold air pool.

The precondition for IOP 5 may be the single most important factor for what looks to be a very long lived event. An extremely cold air mass (-22 C at 700 hPa) has moved across Utah for the last day of 2010 and a combination of lake effect and frontal snow has left the salt lake valley coated in high albedo white. As the upper level cold air shifts east this weekend warm air will begin to move in aloft trapping residual frigid air in the valleys below... in other words, a Cold Air Pool (CAP).

With some clear skies likely tonight and through the weekend, we could see additional cooling at the surface. The snow on the ground may allow the surface energy balance to remain near zero during the daylight hours... which are still very short.

The best news from our perspective though is that currently there are no strong systems forecast to impact the area in the next 5 or so days (and if you believe the long range models, and I don't, none for 7 or more days). As such we are anticipating a very significant persistent cold air pool for the first week of 2011 and will be iniating IOP 5 tonight. Air quality will likely become an issue and fog and clouds may be possible as the event matures. We'll probably start some additional observations in the coming week to focus on some of these sub-processes.

What a great start to the new year... for us at least.

Lake breeze captured during glider flight

Yesterday December 13, 2010 part of the PCAPS team and volunteers headed out again to the Great Salt Lake for more glider "sounding" data. With a strong possibility for lake breeze development, we hoped to capture at least some of the event mid-day. Meeting around solar noon allowed for time to setup and train our volunteers in initializing GRAW sondes and configuring radios for communications.

Some of the Team: Erik Crossman, Chris Santacroce, Chris Ander, David Reim, Neil Lareau

Our pilot, Chris Santacroce, met us shortly after noon. Surface winds were strangely calm at the lake's edge, and after waiting for several minutes, Chris decided to make a no-wind launch with his powered paraglider.

Chris setting up the powered paraglider

The flight plan was to fly long north-south cross sections, stepping up 100m each leg. Half way through the 50 minute flight we noticed a strong increase in surface winds pushing off the lake. Temps dropped rapidly and rh values spiked. We managed to capture the lake breeze as Chris was sampling data at the inversion top, so changed plan and sampled an east-west cross section at the mixing level as the lake breeze persisted inland. No one anticipated the lake breeze to penetrate deep into the Salt Lake Valley, but within the hour it had channeled across the length of the valley into Sandy. This helped strengthen the inversion and justified one more sounding transect the next day at 12 and 18 UTC across the valley before ending sub IOP 3 operations.

Chris flying north over the GSL at 6000 ft MSL.

More analysis is needed on the data collected, and we hope to review this last glider data-set during the upcoming downtime as the next series of troughs move through northern Utah.

IOP 3: How much cold air can we produce in one night?

IOP 3 is now underway, but it won't be for long as we are expecting a short lived event. But that is part of the point. We want to see how quickly the Salt Lake Valley can form a cold air pool under clear and calm conditions.

A strong ridge built across the region on Sunday, a scenario that we typically associate with cold pools during the winter months. However, with no cold air in place and thick clouds the preceding night, only modest stability was generated in the lower atmosphere leading into today. The clear skies today lead to significant surface heating, and the the atmosphere became nearly dry adiabatic through the mountain top level during the day. As a result temperatures in town spiked into the low 50s, which was a welcome change.

Tonight however, we expect to develop a substantial nocturnal inversion under clear and calm conditions. In fact we can already see this cooling in progress. The net radiation measurements from the evening are strongly negative, especially as compared to last night. The balloon launched at 06 UTC from the ISS facility now shows a strong inversion near the surface, which is very different than the sounding from the airport shortly after sunset.






One interesting observation is the weakening of the subsidence inversion near 700 hpa during the past 6 hrs. Loosing a strong cap aloft could have a big impact on the evolution of this event.

We're also launching additional balloons tonight and tomorrow morning from Antelope Island in order to observed the cooling that occurs in the boundary layer over the lake.

Tomorrow with clear skies again expected for at least part of the day we'll have a look at how much of the surface inversion is removed by surface heating, how the lowering subsidence inversion (if it still exists) may couple with the nocturnal inversion, and how the diurnal wind reversal advects air from over lake into the valley. We'll have the motorized gliders out for those operations!

On Tuesday if conditions warrant we'll then be looking at the potentially rapid break up of the cold air pool by strong winds associated with an approaching vigorous trough.

IOP2 Ends

Despite my forecasting thinking to the contrary, heavy rain, strong winds, and a potent frontal passage have removed the cold pool from the Salt Lake Valley bringing and end to IOP2. The lake tried to hold onto a shallow lens of cold air for a bit longer, but it too succumbed to the exchange of momentum from aloft. The differences in mix out time can be seen in the following figure:



The sharp temperature rise at the airport occurred about 6 hrs prior to the mix out at Hat Island in the middle of the (not so) Great Salt Lake. The temperature then crashed shortly later as a well defined surface front pushed south across the lake and into the Salt Lake Valley bringing heavy rain and then ice pellets and snow. Strong NW winds with gusts to 43 mph helped to ensure that any residual pockets of cold air at the surface were completely eradicated.



The view across the valley is now as clean as it ever is in the winter and we're all breathing a bit deeper this afternoon. Out next cold pool event looks to be a shorter lived episode (maybe around 72 hrs) starting on Saturday night or Sunday morning and persisting until sometime Wednesday.

IOP 1: Fog front

Before PCAPS began, the team of U of U scientists met with some of the experts from the National Weather Service (NWS) here in SLC. We were curious as to what they considered to be the most pressing forecast challenge associated with Persistent Cold Air Pools (PCAPS). The onset of dense fog, particularly at the airport, was the unanimous reply.

Fog in some ways seems like an easy forecast issue. For fog to form the ambient air temperature must cool to its dew point, at which point water vapor is forced into condensate in the form of fog (or cloud) droplets. Alternatively, sufficient moisture can be added to air through evaporation from the ground (water vapor flux) or through evaporation from rain to bring the air to saturation. Easy right? In principal yes, in reality no.

Throughout much of IOP 1 the atmospheric boundary layer seemed continually on the verge of forming fog, and in fact on a few occasions the airport reported mist (which is basically thin fog), but no truly dense fog. In some ways the forecast question became "why isn't dense fog forming?", after all the air was nearly saturated, the ground was wet and cold with snow and melted snow, and overnight temperatures were within measurable accuracy of the dew point.

Things changed on Sunday Dec 5th.

Light rain fell on Saturday evening across the Salt Lake Valley and much of the northern Great Basin. As skies cleared behind the departing weak system and temperatures dropped, dense fogged formed over much of NW Utah and NE Nevada.


However, dense fog did not form within the Salt Lake Valley. There were some areas of mist overnight and in the morning, but nothing like what was seen over the west desert. Why? I have no clue. Something to do with the urban environment? maybe there were more clouds overnight due to the proximal Wasatch Range? Very tough to say.

Despite the lack of in situ fog production, SLC would not remain fog free for long! With strong differential daytime heating between fog covered areas and the sunnier Salt Lake Valley organized northerly flow developed which would soon advect a 'fog front' from our west and north into the valley. The airport was the first to see its arrival, which was marked by visibilty plummeting from 2 miles (haze and mist) to less than 1/8 of a mile which caused numerous delayed flights. By early afternoon downtown Salt Lake disappeared into the murky ground based cloud. A ragged boundary of fog continued to progress south through the valley throughout the afternoon, with all of the valley eventually 'going under' by dark. Visibility was minimal, and may even have played a major role in the crash of a small aircraft attempting to land near Ogden.

What tipped the scales to allow for dense fog versus thin mist? Was the precipitation contribution of moisture to the cold pool the straw that broke the camels back? What role did the melting snow play in both forming and maintaining the fog? And why did the Salt Lake valley behave so differently?

It is tough to draw any conclusion as of yet, but fortunately PCAPS has two phases: 1.) observing and 2.) analysis. The analysis of the data we collect now will be ongoing for years to come, and perhaps we'll be able to answer some of these questions.

IOP 1: Time of Death? IOP 2: Time of Birth?

Nature seems to shun the clean distinctions that we'd like to apply to it. Categorization is useful, but nearly always an over simplification. We've run into this issue as we try to decide when to end Intensive Operation Periods (IOPs) and when to initiate new ones. What constitutes the end of a Persistent Cold Air Pool? In general we assume that if the atmosphere experiences a period of free overturning (with respect to either a saturated parcel or a dry one), then the event is over. But then the question turns to issues of location... if it mixes out in town but not over the lake, is the cold air pool destroyed? What about if it retreats from the airport, showing a well mixed profile for an hour, but then returns the next hour?

This much we do know, we declared IOP1 to have ended sometime between 00 UTC on Dec 7th and 00 UTC on Dec 8th. The below figure summarizes the observed soundings from 12 UTC on the 6th through 00 UTC on the 8th.

The figures in black and green are sounding conducted at the PCAPS NCAR ISS facility, while those in white are from the NWS.


Probably the most signifacant changes occured during Monday morning, where the 12 UTC (5 AM local) sounding showed a strong surface based inversion with dry and warm air above. By 18 UTC (11 AM local) rain was falling across the valley and the temperature profile was very close to the wet bulb temperature shown in the earlier 12 UTC sounding (light blue line), indicating that evaporative cooling and moistening had been substantial. Despite the rain and nearly moist nuetral lapse rate, there remained a very shallow surface layer of cold air... the cold pool was not yet dead.

We have two soundings for 00 UTC on the 7th (5 PM local), both of which show very similar profiles. A fairly shallow and nearly isothermal layer extends from the surface, capped by a well mixed (dry adiabatic profile). In fact these soundings even support the possibilty of some weak convection (assuming it a parcel can either be lifted out of the shallow stable layer or from an elevated source... like the mountains). This potential was realized shortly after these soundings as a semi-organized band of precipitation pushed across the Wasatch Front providing locally heavily rain (in the mountains there was a lot of graupel). A big question for us was what happended during this period (around 02 UTC Dec 7th?). Fortunately we have some continuously monitoring intstruments to help figure that out, namely the Radio Acoustic Sounding System (RASS). Data indicated that around the time of this precipitaiton, a monotonically decreasing temperature profile existed with a fairly consistent lapse rate. See for yourself here. This would suggest that during the rain fall and convective burst that the atmosphere was able to freely mix for some short period of time. So was the cold pool dead as of then?




The plot thickens as we look at the 06 UTC sounding. Despite the rain and convection, we once again observe a shallow isothermal layer. If the cold pool was destroyed previously where did this layer come from and why is it so similar in structure to that observed before the rain?

By Wednesday morning (12 UTC Dec 7 th), conditions at the surface had cooled a bit, converting the previously isothermal layer to a true inversion. The air above this layer was once again nearly dry adiabatic. The more significant change observed at this time was appearance of a subsidence inversion aloft, indicative of large scale processes that would soon favor the trapping of air within the valley. But there was another variable, SUN!

Daytime heating, something that had been in short supply, helped to remove the surface based inverison by late moring (18 UTC) favoring a lapse rate that was close to moist nuetral up through 700 hPa. A tell tale sign of surface heating was observed at this time... fair weather cumulus over the valley (not just the mountains). The 00 UTC sounding further coroborates this notion showing a nearly dry adiabatic lapse rate from the surface up to the lowering subsidence inversion, which was now just below the crest level of the Wasatch Mountains.

So IOP 1 ended either during the mix out phase near 02 UTC on Dec 7th or during the day on Tuesday (between 12 UTC and 00 UTC) right? And IOP 2 began as the new subsidence inversion descended into the valley...

Well it did in our books, but there is a bit of a hitch and its name is the Great Salt Lake. While the atmosphere was well mixed over the land, surface observations (shown below) indicated that the lake remained cold and foggy (not shown, but RH values > 95 %) during this time.



We would in fact see the influence of the lake on Wednesday, as a lake front was observed which advected colder and damper air into the Salt Lake Valley during the afternoon. That air was the remains of the Cold Pool from IOP 1... so did it ever end? In the end it is just a semantic issue, but it certainly highlights the potential for the lake to act as a source of cold and poluted air.

The wind transition associated with that lake front was well captured by the U of U mini Sodar deployed at the Playa site near the lake. Note the strong and organized NW flow near 21 UTC:



We have scaled back observations for IOP 2 to conserve resources, but we are still very much in the midst of a persistent cold air pool. A weak system on Friday will try to mix it out, but it doesn't look promising. Over the weekend a strong ridge will build across the Mountain west and Cold Air Pool conditions are expected!

Morning inversion

This morning there was a pronounced nocturnal inversion visible across the Salt Lake Valley. The below photo was taken from above the Salt Lake City Cemetary at 11th Avenue around 9:30AM. What's interersting about this photo is the very distinct two layers against the East bench. Here we are looking south across the valley at Big and Little Cottonwood canyon in the distance.


Reviewing the 12z SLC sounding, there was a pronounced ground inversion capped at 860mb with a small flattening near 750mb and then a relatively deep layer extending up to 650mb. By mid day the entire valley was likely well mixed to 650mb with surface-driven cumulus across the region. And with a northwest flow aloft, perhaps we will see some of the trapped valley aerosols disperse a bit more before the next Cold Air Pool event settles in for a stay.


The ingredients are right for another Cold Air Pool event, which will give us IOP2 over the next period, but the duration and strength is in question. I'll let Neil or Erik post the details on IOP1 ending and IOP2 starting up.

IOP1: Cold Fronts and Warm Fronts

We've been quite busy with PCAPS operations for the past few days so sorry for a lack of updates.

Weather conditions within cold air pools are frequently described as quiescent. This cold pool apparently hasn't read the published literature! Dense fog fronts, strong winds, rapid temperature variations, freezing rain and drizzle, horrendous air quality have all been observed since my last posting... not really quiescent if you ask me. And that is why we've been so busy... and why I'll post a few installments to get you up to speed.

Lets start with some of the interesting events on Thursday night and early Friday morning (Dec 2nd-3rd). A weak short wave trough moved just north of the region, clouds overspread northern Utah, and some light rain fell across the Salt Lake Valley, especially up on the east bench. Accompanying the shortwave trough aloft was a regional pressure gradient that accelerated low altitude winds from the South (low pressure to the north, high pressure to the southeast). Terrain channeling may have helped to orient these winds along valley. The net result was that strong south winds penetrated to the surface at the south end of the valley, effectively 'mixing out' the inversion and advancing a 'warm front' like structure north through the valley. At 06 UTC on Dec 3rd (11 PM local) the advance of the cold pool edge accomplished its northern most extent. Some of the PCAPS team members who live in the south end of the valley observed this transition in person at their homes and described a sudden whoosh and temperature warm up.

However this localized 'mix out' was relatively short lived. In the predawn hours of Friday morning a weak pressure trough swung south across the valley, and effectively reversed the local pressure gradient. The cold pool responded by running back to the south, now resembling a cold front, rapidly engulfing all of the valley.

This evolution is summarized in the following figures:

06 UTC 12 UTC

13 UTC 14 UTC

The temperature/humidity and vector wind traces from around 9000 S and I-15 show both the retreat and return of the cold pool at that location.




Later during Friday afternoon another interesting transition took place. The incredibly hazy air trapped within the cold pool ascended in altitude engulfing locations that had been clear earlier in the day. It is unclear without more detailed analysis what caused this vertical expansion but one hypothesis is that a very shallow cold front moved across the region, gliding over the top of the colder air within the cold pool. This may have knocked some of the strength off of the capping portion of the cold pool and allowed for the upward expansion. Some evidence for this can be seen by comparing the morning sounding with the evening one:


It is readily apparent that nearly all of the cooling in the lower atmosphere took place near the inversion top and that overall the stability in the lowest levels has decreased. While there was no clear indication at the surface of a true cold frontal passage, analysists at the Hydrometeorological Prediction Center (HPC) seem to believe that a cold front passed during this time.




Overall it was an exciting 24 hour period and one that will be examined with more detail in the future.

Tomorrow I'll bring you all (if anyone actually reads this blog) up to date on some of the more recent changes in the cold pool including dense fog and possible break up.

Glider Test Flight Over Saltair a Success

In anticipation of today's potential mix out, local paraglider pilot Chris Santacroce and a small team from the U of U finally had a good window to test deploying an instrumented Powered Paraglider (PPG) at the edge of the Great Salt Lake over Saltair yesterday (December 2, 2010). The goal was to sample the land / lake interaction in a strong Cold Air Pool and capture the vertical structure in detail. By attaching a GRAW Sonde to the pilot controlling the glider we hoped to create a "new" type of instrumentation that could sample cross sections and vertical profiles of the air.

Paragliders can fly at very low speeds without stalling (around 15 to 20 mph) which allows unique sampling of the air by a human pilot. Imagine being able to ask a balloon to stop at a certain height, sample a cross section, spiral back to the ground, then ascend just above the cold pool and take pictures before returning to the launch location.

A powered paraglider is also unique because of the small space required to take off. This allows us to deploy the glider quickly and with few resources from any number of locations within the Salt Lake Valley. Of course, most first prototypes suffer in the glamor department but this is what we ended up with (sonde mounted on helmet):


The first flight attempt yielded no problems and good quality data. Chris flew for around 40 minutes completing cross sections out to the lake's edge, then back over I-80. Each transect was 100 meters higher than the last until finally the glider was above the Cold Air Pool, where he was met with a 20 knot south wind. We communicated by texting via iPhone and two-way radio. Chris was able to snap a few photos along the way to document the flight in a little more detail.

Photo by Chris Santacroce, Dec 2, 2010.

Looking south over Saltair from 350 meters AGL.

Photo by Chris Santacroce, Dec 2, 2010.
Looking NNW over Saltair from 325 meters AGL.

Yes. Those are feet at the bottom of the photos. Note in the second photo: the lake fog to the west of Lake Point was still quite thick mid day.

Initial analysis of the observations showed that within 150m starting at 250m AGL, temperatures increased just over 9C, which validated well with nearby balloon launches. And where a regular sonde only samples a single vertical profile with few observations in a shallow Cold Air Pool, we were able to maintain flight within the inversion and gather considerably more data.

Our thanks to Chris Santacroce for helping design a working prototype. Chris is a talented pilot and co-creator of the Red Bull Airforce team. We are extremely lucky to have his skills and time donated for PCAPS and we hope to deploy many more glider flights throughout the project.

Persistent indeed!

The purpose of this field campaign is to study Persistent Cold Air Pools (PCAPs), and that is exactly what we've got. The Salt Lake Valley has now been in continuous Cold Air Pool conditions since Monday night, and it is not exactly clear just when its going to end. Persistent indeed. We've decided to really ramp up observations this evening and into tomorrow morning in the hopes of capturing some modifications to the cold pool structure accompanying the advent of strong winds above the inversion followed by arrival of some moderately colder air aloft tomorrow. Will we mix out? Will parts of the valley mix out? ... tough to say, which is a big part of why we're studying this. If we don't mix out the already dismal air quality is wont to get worse (courtesy of Utah DAQ).



To give you a sense of what dismal air quality looks like, here is a picture I took this morning from high on the slopes above downtown Salt Lake and the University of Utah.




Today also marked a first for the PCAPS team: With the help of expert pilot and weather enthusiast Chris S. we conducted soundings of the boundary layer with instrumentation mounted on a motorized paraglider. We hope to continue to use this sampling method to augment our measurements of the lower portions of the Cold Air Pools especially near the Great Salt Lake, the influences of which can play an important role. Hopefully we'll be able to share some of the pilots perspective in a future post here.

The cold pool itself has reduced in vertical extend over the past 36 hours, but has only gained in potency. Here are some of the soundings from today:


A few of the issues at play today were strong warm air advection above the inversion top, possible low level jet type dynamics caused by topographic channeling and regional pressure gradients, and the inability of strong winds to penetrate to the surface due to such immense stability.

All eyes are now on tomorrow, which will be a make or break day for this event.

IOP1: Now that is an inversion !

We couldn't have asked for better weather for the official start to PCAPS... which is to say cold, damp, and hazy in the midst of a robust cold air pool. Lets hope our good luck continues throughout the experiment.

Yesterday I left off pondering the overnight evolution of the present cold pool. Today we have the answers, which is one of the great things about studying atmospheric science... you get to test your hypotheses everyday.

The 12 UTC sounding from the Salt Lake Airport indicated a nearly isothermal lapse rate between the surface and 700 hPa (with some shallow inverted layers). The modifications of the thermal structure overnight where relatively modest, with slight warming near 700 hpa and virtually no change in the surface temperature.



In fact the surface temperature at the Salt Lake Airport was 27 F at both 5 Pm on Tuesday and 6 AM on Wednesday. Why so consistent? Well, the surface temperature and the cloud base temperature were nearly identical, meaning that the longwave radiation emitted from the surface was nearly identical to that received from the clouds... and now that we have all this fancy instrumentation in place we can even demonstrate that this was the case. Below is a plot of the net radiation at the ISFS sites which are scattered throughout the valley.



Note that most sites were almost exactly zero through the overnight hours, where as on a clear night (when the earth tries to equilibrate with the background temperature of the vacuum of space) the net radiation would be negative as it is at the right hand side of the plot (clearing this evening). Despite the lack of production of cold air at the surface, the presence of warm air aloft (which is potentially warmer than the air at the surface) maintained strong stability, a scenario which qualifies as a cold air pool.

Stability would only increase through the day as warm air advection (or possibly still subsidence) pushed temperatures in the layers between 750 and 800 hPa up above the freezing point while surface temperatures remained cool due to the limited insolation and snow on the ground. Much of the temperature contrast was realized in a shallow but extreme inversion layer near 800 hpa. These changes are shown below in the 18, 00, and 06 soundings. The 18 and 06 soundings (green) are the first rawinsondes launched as part of the PCAPS campaign and are already proving to be an amazing asset in understanding the evolution of these events.




It is also apparent from ceilometer measurements, visual clues, and increasing relative humidity that this event is trying hard to transition to a cloudy/foggy cold pool.

Check out the ceilometer plot, which shows the possible onset of boundary layer clouds around 10 PM on Wednesday night here

Now the big challenge for the PCAPS team is trying to assess when and how this event will conclude. A relatively weak system is expected to impact the region midday Friday, but it is unclear whether the cold pool will persist or not. With air quality rapidly deteriorating in the valley with each passing day the outcome of Friday may have significant impacts on the inhabitants of the Salt Lake Valley.

If you want to keep tabs on the data stream yourself please link here and browse the various data sources which are now online.

IOP1: Complexity at the onset

It is satisfying when forecaster intuition adds value to the model out put. Such was the case last night. Despite the dainty surface cold pool projected by the models, a more robust nocturnal inversion formed during the clear overnight hours. Strong drainage flow was observed from the major canyons and some truly frigid temperatures could be found throughout the Salt Lake and adjacent valleys.

The 12 UTC sounding shows both the existence of the surface based inversion and indicates that the strong subsidence layer has descended to crest level as expected. The elevated subsidence inversion was also evident in mountain top observations where warming and drying were observed. Between these two layers a region of much weaker static stability is found.


While it is tempting to assume that the whole valley is represented by this sounding, significant variations in temperature and cold pool structure are suggested by some of the observations in the south end of the valley near the Jordan Narrows and the Traverse Ridge.



Examining the temperature time series at 4 stations (Point of the Mountain, Flight Park, Bluffdale, and a site near Bangeter Highway) drastic differences in the temperature evolution are apparent.
The flight park and I-15 Point of the Mountain both show nearly steady cooling through the night. The 'Murray' site shows rapid cooling with a potent cold pool forming and temperatures near 0 F, then a rapid temperature increase. The Bluffdale site has more modest cooling, interrupted towards morning by successive temperature jumps and drops.

Taking a cursory look at the data from the ISFS sites around the valley we can see that this temperature jump behavior is unique to this portion of the valley. The Riverton site behaves similarly to the 'Murray' site, with a rapid warm up before 12 UTC. The other sites show a more consistent behavior and can roughly be subdivided into two groups (indicated by the departures from the group mean plot below), those that develop robust cold pools (the cold group) and those that experience less cooling.



What drives these variations? It is difficult to say.... internal turbulence and strong associated heat flux? Hydraulic jumps in the stable flow near terrain? Sloshing of the cold pool? These are all questions that we hope to be able to further explore during PCAPS.

Further complexities within the cold pool developed during the day as some locations where able to mix out the nocturnal surface based cold pool, a substantial accomplishment in light of the snow pack on the ground. Nonetheless the strong subsidence inversion descended further below crest level, keeping the valley air trapped in place. Above this inversion, thick altostratus moved in during the afternoon and some very weak radar returns are now apparent. Just what changes are in store for the cold pool structure overnight?

Here is the starting point this evening... what will we see in the morning?


OPERATIONS NOTE: ISS soundings at 18 UTC and 06 UTC will commence tomorrow (Dec 1st) and continue until the demise of the current cold pool which is currently anticipated to occur on Dec 3rd.

And so it begins. IOP 1 sort of...

Following the passage of a cold trough that brought significant snowfall to all of the Salt Lake Valley conditions are seemingly ripe for a cold pool to form as a ridge builds into the region from the west. Strong subsidence warming is expected near crest level, but at issue is the degree to which a nocturnal surface based inversion forms under the partly cloudy skies on Monday night. Models have suggested that the boundary layer will remain fairly well mixed through the night... however forecaster intuition would suggest that the widespread snow pack and only partly cloudy skies will favor rapid cooling at the surface. While the 00UTC sounding from the Salt Lake airport does indicate a relatively well mixed lower troposphere,


surface observations show rapid cold pool formation in the neighboring valleys and more modest cooling within the Salt Lake Valley proper. This pattern is quite familiar as the less urban and more natively vegitated Rush and Tooele valleys tend to develop stronger nocturnal cold pools. Within the Salt Lake Valley many stations have shown their typical diurnal windshift to the SE which is a well known indicator thermally driven drainage flows, and presumably a precursor to the formation of a nocturnal surface based inversion.



Infrared satellite images after sunset also indicate that skies are mostly clear and the surface is in fact largely snow covered and quite cold especially compared to the nearby Great Salt Lake. Good conditions for a cold pool if you ask me.




Beyond tomorrow the future of this event becomes less certain with thick altostratus possible, a very weak shortwave trough, and then continued 'dirty' ridging expected. It will be of great interest to our group to see how the cold pool responds to these variations.

With the official start of PCAPS just two days away, if this event comes together as we currently anticipate we will start operations in the midst of a Cold Air Pool. The PCAPS team hopes to use this event as our first IOP, though we will be scaling back from full operations and using this event as a shakedown for our operations, forecasting, data analysis, communications and decision making processes. The current plan, pending revision, is to use twice daily (18 and 06 UTC) NCAR ISS balloon launches to supplement the NWS operational soundings and to monitor the continuously operating observation platforms.

Now I guess we'll just have to wait and see how much cooling occurs tonight.