And so, summer heat begins!

   In case you haven't heard we are on the verge of a prolonged spell of summer heat set to arrive right after the 4th of July. Years ago, it seemed summer would always begin right after the 4th of July in the Spokane however is that really true? According to statistics, perhaps not. Interestingly enough, we can define summer by looking at the warmest 91 (3-month period) of the year which according to our climate statistics occurs around June 16th. Also interesting is the fact, that the beginning of the summer season has been getting later and later each year, however there is a significant amount of disparity when looking at the chart below.  

Also interesting is noting the abundance of red dots since 2000 signifying a warmer than normal summer. Since 2000, 75% of the summers have been warmer than normal with a current streak of 12 warmer than normal summers. Below is a closer examination of that factoid plotted against the 30-year moving average.  The blue line represents the average summer temperature (based on June-August data and not the 91-day period shown above. 

So enough of the summer background, let's take a look at the upcoming forecast and heat-filled details. This burst of heat will arrive care of a very strong ridge of high pressure. If we look at the 500 mb charts (~18,000') in the atmosphere we can see how this scenario is going to play out. On Friday, the ridge will begin to build off the coast and this should begin the heat event.

500 mb heights Friday

By Sunday the ridge will migrate toward the center of Washington ensuring we warm up even further. 

500 mb heights Sunday

By Tuesday the ridge axis shifts into eastern Washington and then the heat will really get going across the Inland Northwest. 

500 mb heights Tuesday

But that's not the end of it, as it looks like the heat will peak on Wednesday or Thursday with the ridge shifting to the Montana/Idaho border. 

500 mb heights Thursday

So how confident are we this scenario is going to pan out? At this point, quite confident. In the past we only had a few weather models at our disposal and run-to-run changes were common, especially at the latter ends of the forecast (for instance days 4-7). However now we utilize ensemble forecasting which takes multiple models (over 100 for the days 1-2 forecast and 100 for days 3-7) and complies them for us. This method can show us the range of possible outcomes and in this upcoming pattern there just aren't a lot of outcomes other than just plain hot. The easiest way to determine how uncertain the forecast is by examining a chart that shows the different model solutions and plotting them on top of one another. 

Let's start by examining the model possibilities for Sunday.  Note the ridge positioned along the West Coast and the pale-yellow shading over the region. The shading represents the differences in the 500 mb heights between the 100 model runs. In this case, the differences are only around 2 decameters, which signifies good model agreement. If you look farther west, over the Gulf of Alaska note the purple shading which signifies large model differences (13 decameters, which is significant). Seeing model agreement only 2-3 days into the forecast isn't unusual, especially for a ridge. 

500 mb ensemble model differences on Sunday 7/7/24

By Tuesday the model differences with the ridge increase, but not by much (only 1 decameter over the Pacific Northwest). This still suggests high forecast certainty. 

500 mb ensemble model differences on Tuesday 7/9/24

By Thursday the model differences increase slightly, but again not to the point where we would think the ridge will be replaced by the offshore trough, delivering cooler weather. All the significant model differences remain on the eastern or western periphery of the ridge. 

500 mb ensemble model differences on Thursday 7/11/24

If we go out even further to next Saturday, there still is a higher-than-normal chance that the ridge is going to stick around, however we'd have to imagine we'd see some cooling by then. 

500 mb ensemble model differences next Saturday 7/13/24

So far, we've only examined the 500 mb heights, which are indicative of sinking air and generally fair weather, but how does that translate to temperatures on the ground?  First, we will examine the mean temperatures forecast by the National Blend of Models. This represents the most likely outcome. 

NBM mean temperature forecast for the Inland Northwest

However, what would we expect if the warmest 25% of the model solutions came to fruition? That would certainly support a historic heat wave. There's no reason to believe this will occur, however it just hints at a possibility. 

NBM 75th percentile temperature forecast for the Inland Northwest

So, what are our chances of exceeding 100°F during the next week or so? It's a done deal for the LC Valley, as well as the Columbia Basin and Okanogan Valley. There's a slightly lesser chance for Spokane, while the "cool" escape will be to Sandpoint. Below is a list of the chances:

Chances of hitting 100°F or hotter

As you can see, the odds are quite good that a large portion of the Inland Northwest will see a multi-day period of triple digit heat. Currently our forecast doesn't suggest we will break any records for consecutive 100°F days however once again we could easily see 4 consecutive days of triple digit heat in Spokane. Something which occurred in both 2021 and 2022 but not many years other than that. The record is 6 set in 1928. 

Other daily records could be broken beginning on Sunday and continuing at least through Thursday. Spokane's records are as follows: 7/7 99°F, 7/8 99°F, 7/9 100°F, 7/10 102°F, 7/11 103°F. All are certainly within reach. We also got the question is Spokane's all-time record in peril? Just 3 years ago Spokane set a new record of 109°F (6/29/2021). While we don't expect to break this record during this spell, it is not a 0% chance. In downtown Spokane, the chance is around 10% on Thursday (in other words 10% of the ensemble model runs are forecasting temps of 109°F or warmer), while at the Airport (the official forecast spot for Spokane) the chance is around 2%. 

Chance of 109°F or warmer on Thursday 7/11/24. 

So far we've discussed the daytime highs which will be trying enough to those who don't tolerate heat well. But we also have to factor in the nighttime lows. Unfortunately, these won't cool off too much either. The table below reveals overnight lows only dipping into the mid 60s to mid 70s for most locations. That means folks without air conditioning will have a tougher than usual time cooling off their houses during the night. And the length of this event will only exacerbate this issue. 

Nighttime low temperature forecasts

If you add these factors together, we are looking at a trying environment for many denizens of the Inland Northwest. We can characterize this using an index we call HeatRisk. By Sunday a large portion of the region will experience Major heat risk which means the heat will impact anyone without effective cooling and/or having access to adequate hydation. 

Sunday HeatRisk

By Tuesday (the last day available for the HeatRisk as of this blog post), we begin to see extreme values popping up around the area. Remember, we expect the heat to peak on Wednesday or Thursday which suggests the magenta will become more widespread. 

Tuesday HeatRisk

Needless to say, we urge all of our friends to take the necessary precautions ahead of time and prepare for this upcoming heatwave. Here are a few hints from the CDC to help you beat the heat. We also want you to treat your loving pets with the utmost care to keep them safe during this heatwave. Please stay tuned to our latest forecast to see how hot it is going to get. 

Safety advice from the CDC and the NWS for you and your pet

A worsening drought over parts of eastern Washington?

   Springtime across portions of the Inland Northwest has been very dry at least compared to climatology. We can measure just how dry using various tools in our meteorological tool box. One of the conventional tools we use is simply looking at precipitation maps across the region. So how have things looked over the past 90 days? 

As you can see things are highly variable across the region. near the Cascades it has actually been quite wet, with precipitation amounts nearly twice the average amount over the past 90 days. Also near the Washington/Idaho border amounts have been close to normal (aside from the southern Palouse, LC Valley, and Blue Mountains). However one area that  stands out is a portion of central Washington in the lee of the Cascades stretching from Omak down to Moses Lake and The Tri-Cities and Yakima areas. Some of these locations have seen only a quarter of the normal precipitation during this period. 

If we add the November precipitation amounts to the mix, the resulting map doesn't look much different for the dry areas. 

So that got us thinking is this a record of some sort? Now granted these statistics are rather arbitrary, After all, who calculates records from 11/23 through 3/21? Not many people, but just for fun we will examine some of these odd records. First we will look at Yakima. 

Yakima, WA precipitation 11/23-3/21

So in fact this is a top 10 driest period for Yakima, but it was actually drier in 2018. Now how about Omak? Not quite top 10 but close. 

And finally lets look at the Ephrata:

Only in 16th place out of the last 70 years and the driest since 2014. So although this is noteworthy, it isn't really a historic dry spell. 

But precipitation alone does not tell the entire story about a dry spell of weather. Other things to take into consideration during this period include; winds, temperatures, relative humidity levels, and solar radiation. All of these parameters will impact the amount of evaporation or evapotranspiration that can take place and how quickly the soils will dry out. That is a lot of information to keep track of, however fortunately we have a relatively new and very useful tool called the  Evaporative Demand Drought Index or EDDI. This takes all the aforementioned parameters into account and states how thirsty the atmosphere is. So what is this index showing for the area? If we go back to November things look particularly bad:

Over the entire Lower 48, no area has seen  more widespread and harsh drying conditions compared to normal. The categories on the map correspond to our typical drought outlooks. In this case the shading over eastern Washington corresponds to an ED4 or an exceptional drought. Does that mean this area is now in an exceptional drought? Not necessarily. A drought is not built on four months of weather alone, but if these trends continue we will certainly be faced with worsening drought conditions over this portion of eastern Washington. Since November here is how the drought monitor has been evolving across Washington.

These images start in the middle of November and advance two weeks at a time. The last image shows the drought conditions as of the middle of March.

Specifically looking at the March 17th the outlook:

This map shows that almost 23% of Washington is in a D1 or moderate drought which just so happens to correspond closely to the first precipitation maps we showed. But what is interesting is the EDDI maps show worse conditions than what's depicted by official drought maps and sometimes this can foretell the trends. EDDI itself is not a drought prediction, but at short timescales (such as what we have shown), it indicates the potential for drought (or trends). So this area certainly bears watching.


So looking past the EDDI values what do the longer range weather forecasts tell us? That is always a tough question to answer, but lets look. The 8-14 day outlook through the beginning of April calls for near normal precipitation and cooler than normal temperatures. Near normal precipitation amounts would certainly help. The cooler than normal readings should also temper the thirstiness of the atmosphere however that could be overcome by having unusually dry air masses in place or prolonged windy conditions.

As for the April outlook, things don't look terrific for a dramatic improvement at this point with below normal precipitation favored at this time with an equal chance of normal temperatures.

And finally, if we want to peer even farther into the future (April-June) the prognostication right now would suggest worsening drought conditions. But we will just have to wait and see.

So what are the ramifications of a drought over the Columbia Basin? While much of the area is irrigated for agriculture, there are areas which also have a considerable amount of sagebrush which could eventually lead to quick burning fires this spring. It could also lead to more blowing dust than normal on a windy day.  Part of this dry area also encompasses some denser fuels both east and west of Omak. Right now the nearest snotels (snow measuring sensors) depict a snowpack around 65%. It's too early to say if this will lead to a busier than normal fire season in these areas as we have found the leading cause of a big fire season is a hot and dry summer.

We will revisit this topic later this Spring to see how things panned out.

Much warmer weather is expected next week after prolonged cold!

If you think this winter has a rather drastic change from the past several winters your senses are not deceiving you. When we began the month of November is seemed we would see yet another mild November, however as the calendars changed to December that notion came to an abrupt halt. The start of 2017 has continued that trend. Look at these statistics for Spokane and this will put things into perspective.

It certainly seems the mild winters of the past several years are a distant memory. This has been the snowiest winter since 2008-09 and the coldest since the early 90s. But the cold wasn't just in Spokane. Check out this list of sites that have seen their record coldest December-early January period on record (keep in mind some of these station records don't go back too far, see last column for details).

So we can see it's been cold and somewhat snowy. To see how snowy its been look at this comparison graphic of satellite pictures from early December vs. early January. 

Satellite comparison of snow cover via visible satellite. The January image suggests just about all of the Inland NW is covered with snow. 

This is quite a change. But its winter and it's not unusual to see widespread snow cover at the beginning of January across the entire Inland Northwest is it? Here is a look at the amount of water in the snow (Snow Water Equivalent- SWE) on each January 10th since 2008. 

Based on this, we actually saw the entire region covered by snow in 2016 as well. But this year and that were the only ones since 2008.  So if there is snow covering the entire region should this lead to concern? Well it depends. If we could melt all the snow at once it could cause a great concern due to runoff and potential flooding. This time of year it is improbable that we can melt all the snow over the mountains (where you can see the dark blue, purple, and red shading) as it doesn't get warm enough but we can melt some. But it is quite a bit easier to melt a significant (if not all the snow) in the valleys where we see the abundance of white and pale blue shading. Any area shaded in white has at least an inch of water tied up in the snow pack while the light blue shading represents values ranging from 2-4" of water. So what does it take to melt this? Obviously we need to see temperatures above freezing for a prolonged period. But that's not all. It also helps immensely to add wind into the equation. Warm winds and prolonged temperatures above freezing are an enemy of the snow and can cause it to quickly disappear. Imagine taking that 1 to 4" of water trapped in the snow and sending it into the rivers and streams. How about taking that same 1 to 4" of water over urban areas and sending it toward snow-clogged storm drains? That can cause quite a mess and obviously would lead to flooding issues. This scenario can be further complicated by rivers and streams choked with thick ice. 

So why are we telling you this? Well it just so happens we are looking at a dramatic change in the weather pattern early next week. Since December, we have been stuck in a persistent weather pattern featuring cold weather systems coming from our northwest. These are notoriously cold systems, and generally pose little threat from a hydrology standpoint. 

Mean 500 mb (18,000' above ground) since December. Note how the colors (or heights) buckle north into Alaska and then drop SE into the remainder of the county. This is indicative of cold NW flow. 

When we compare this weather pattern to what's normal for this time of year we see a clear signal. The blue shaded areas represent below normal heights which generally result in cold weather whereas the orange, yellow, and green shading represent warm conditions. 

500 mb height anomaly values. 

This is quite unusual. Typically we see some warmer systems invading from the southwest tied to a nice tap of relatively warm sub-tropical moisture. When these systems arrive they can bring a rapid warming in temperatures as well as significant precipitation and snow melt. Well after a long respite from such systems, we see hints of one on the horizon. Here is what many of the forecast models are hinting at for next week. 

Weather pattern for next Monday evening (500 mb heights in white, precipitable water is shaded)

What this reveals is our northwest flow of late will be replaced by southwest flow early next week. Of even more concern is the swath of green and blue shading headed into the Pacific Northwest. This indicates we will be subject to a very moist and warm air mass, which could do a very effective job of melting the low-level snow pack. Now if this feature were only going to be over us for a day it may not do much to the snow pack. However look at this map below for Wednesday. Not much difference is there?

Weather pattern for next Wednesday (500 mb heights in white, precipitable water is shaded)

So this at least indicates the potential for warm weather. Here are our forecast highs for next Wednesday. 

Forecast temperatures for next Wednesday

Notice most of the valley temperatures are above freezing. This will be good for potentially melting the snow, especially over the SE portions of Washington and NC Idaho where you see the greens (temperatures above 45°F) during the day. But what we aren't showing here is many locations across the same area will also see nighttime temperatures remaining above freezing. So its conceivable that some locations across SE Washington and NC Idaho could see temperatures above freezing anywhere from 48-72 hours. We will also see robust south to southwest winds during portions of this period. Below is the wind forecast for Tuesday. These are sustained winds. The gusts will likely range from 20-35 mph. 

Tuesday wind forecast

So remember earlier when we said about above freezing temperatures and good winds can result in some rapidly melting snow. It's conceivable that a good portion (if not most) of the snow over the Palouse, southern Columbia Basin, LC Valley, and even parts of the the Spokane/CdA could melt during this episode. So that's a significant chunk of the 1 to 4 inches of water tied up in the snow pack which could runoff into the area rivers. What we haven't talked about yet is how much precipitation can we expect in this upcoming weather pattern. The map below shows the GFS model forecast for precipitation amounts possible in a 48-hr period ending Wednesday afternoon. 

Tuesday-Wednesday precipitation forecast

This is a very impressive amount and is one of the wetter model runs. Locations shaded in yellow are amounts ranging from 1.50" (around Spokane) to nearly 3.00" over parts of the Idaho Panhandle. We suspect the valley precipitation will likely be overdone, but perhaps the mountains aren't showing enough precipitation. The combination of snow melt combined with ample precipitation could lead to some bad things across the region including:

• Flooding of small rivers and streams (especially over SE Washington and the southern ID Panhandle).
• Lowland flooding where the ground is frozen prohibiting infiltration into the soil. 
• Ice jams could give way and enhance the flooding potential.
• Urban flooding is a distinct possibility given snow-clogged storm drains.

But since we like to be purveyors of positivity let's not dwell on the negative and instead focus on some of the potential good:

• We will finally be able to walk on snow-free sidewalks, 
• We can drive on snow-free roads, 
• Just imagine how warm and refreshing 40s will feel compared to more single digit and teens. 
• The ice dams on snow-covered roofs may finally melt thus alleviating our worries of potential roof damage.
• Much smaller worry of frozen pipes.  
• We won't have to bundle up in countless layer of clothes just to shovel the latest dump of snow. 
• Spring is only 68 days away!!

Is the end of fire season expected soon?

So while we can't argue that the worst of fire season is behind us, it should be noted there are still fires burning across portions of the Inland Northwest. Here's is what satellite information was showing on the last day of September:

MODIS Visible Satellite Imagery from 9/30/15

While these fires are far from the raging infernos we saw earlier this summer, it's still rather impressive for the end of September or beginning of October.  However, as we all know this year is different. First off, look at these precipitation totals since the beginning of April

Idaho Precipitation % of normal 4/2/15-10/1/15

Washington Precipitation % of normal 4/2/15-10/1/15

That is a lot of red and dark red shading over the Inland Northwest which correlates with meager precipitation amounts ranging 25-70% of normal. That's pretty dry. In fact, since the beginning of April through the beginning of October it was the driest period on record for both Spokane and Boundary Dam, WA (extreme NE corner of the state).

So combine the record dry conditions with nearly record warmth for both sites and it is no wonder the fire season has been so long. Here is a look at the temperatures for both sites.

So obviously record warm and dry conditions led to our active fire season, but unlike a typical year, things just aren't winding down as quickly as we are accustomed to. Climatologically, the days of active fires will be limited. We say that because the shorter days are leading to cooler temperatures and higher relative humidity levels  (both items are generally detrimental to good fire growth) while the chances for measurable precipitation are rising quickly. Climatologically the chance of measurable rain ranges from 20-25% over locations where the fires are currently burning. However by the end of the month those chances nearly double. So despite these facts, look at the latest fire danger ratings for the Inland Northwest:

Current Fire danger ratings

That map shows the fire danger is still high (yellow) or even very high (orange) across a sizable portion of the Inland Northwest, with moderate conditions (light green) found everywhere east of the Cascades. So what does that mean? According to the Wildland Fire Assessment System (WFAS) a high fire danger means, "All fine dead fuels ignite readily and fires start easily from most causes. Unattended brush and campfires are likely to escape. Fires spread rapidly and short-distance spotting is common. High-intensity burning may develop on slopes or in concentrations of fine fuels. Fires may become serious and their control difficult unless they are attacked successfully while small.

So is this danger level unusual for the beginning of October? Since 2006 (earliest year of  the graphical archive), the current fire danger has only been matched one time. That was in 2012. All other years saw low to moderate fire danger ratings across the area.

So what was the fire weather like in 2012? This satellite picture tells the story

MODIS Satellite imagery from 10/4/12

Just like this year, there were quite a few fires burning during the beginning of October. In fact, based on the satellite image, they were much bigger and included the Wenatchee Complex (southwest of Wenatchee) and the St. Mary's Misson Rd fire south of Omak. So what happened that year? The dry weather and fires continued to burn through the middle of the month, but several days of rain (not necessarily heavy) and cooler temperatures put an end to that fire season.

So what did the weather pattern look like for the end of that fire season? Well leading up to the end of the fire season, the upper-level pattern exhibited a large ridge parked right off the BC/WA coast with dry northwest flow over the region. Also, note the low-pressure area off the California Coast.

Early October 2012 500 mb pattern. 

So how does the pattern look for most of this week? Although it's far from identical, it does have some similarities, including the low near California, and the ridge over the Pacific Northwest.

500 mb pattern for Monday afternoon (10/5/15)

So what did the weather pattern that led to the end of the fire weather year in 2012 look like? The ridge broke down quite quickly and was replaced swift southwest flow into the Pacific Northwest and a deep low over the Gulf of Alaska. Again this brought cooler temperatures, periods of light rain (moderate in places), as well as significant cloud cover.

Mid-October 2012 500 mb pattern (Oct12-14)

How about this year? Is anything similar expected? Again although not a perfect match, there are some good similarities including a deep Gulf of Alaska low and deep southwest flow pointed into the Pacific Northwest from the eastern Pacific.

500 mb forecast for Oct 10, 2015

So how is our confidence in this solution and will this be the end of the fire season?  There are a few additional tools we can look at. One of the more interesting ones is called the NOMADS ensemble probability tool. This tool queries 21 GFS ensemble members or model runs and calculates the chances of any given parameter. Using this tool we can look at things such as what is our chance of seeing over a tenth of an inch of rain in a day?  When asking that particular question, here is the answer for the Grizzly Complex located over northern Shoshone County, ID.

The probability of seeing 0.10" of rain or more in 24 hrs over northern Shoshone County. 

So if you key in on the clustering of the blue bars, you can see that there is some consensus that by next weekend (10/10 and 10/11) that the weather pattern will support an increasing chance of rain (it peaks at 25% for the 24 hrs between 5pm Saturday through 5pm Sunday). Notice also that there is a small chance of light rain during the middle of the week.

Stay tuned and we shall see if this will truly be the end of a historically warm and dry fire season across the Inland Northwest.