December 18, 2020

New Podcast: The Holiday Week Weather Forecast and the Inside Story on the Northeast Snowstorms



My new podcast is out and I provide a detailed forecast for this weekend and next week, including Christmas Day.  And then I turn to the great Northeast snowstorm of yesterday, telling you about the amazing totals and the nature of the Nor'Easter s cyclones that produce heavy snow over the region.

Here is my podcast:
Click the play button to listen or use your favorite streaming service

Or stream my podcast from your favorite services:

Support the podcast on Patreon and get exclusive content., including my online event tomorrow morning at 10 AM.

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December 17, 2020

Knowing About Rainshadows to Find Sunshine on These Dark Days

 The Seattle Times had a front page article today saying half of Seattle's residents are depressed and by a small margin we are the most depressed major city in the U.S.!

Well, there are many reasons suggested for this depression, including the dismal state of our municipal leadership, but the article mentions an old favorite:  the lack of sun this time of the year.

Fortunately, this is one problem that meteorological knowledge can help with.  

A secret that most meteorologists know:  that on most days even in our sodden area, there are regions of sun in the sea of clouds.  The areas of rainshadows.   And, if you are able to drive a bit, you can often put yourself under the depression-killing rays of the winter sun.

I have talked about rainshadows several times in the blog, but let me provide a brief review.   When air approaches a terrain barrier (such as the Olympic Mountains or Cascade range), it is forced to rise on one side (the windward side) and to sink on the downstream (leeward) side.  When air rises, it cools and can form clouds, but sinking air  on the lee side warms and drys, often providing sunny skies in  the rainshadow.


One sees this effect nearly every day in our region, with clearing skies downstream of the Olympics and Cascades.  But the wind direction and speed varies day by day, as does moisture and other variables, and thus the location and extent of rain shadows can change.

Take today.  Where were the sunny spots around noon (in this case, 12:20 PM PST)?  

The visible satellite image for that time (see below) tells you exactly where to go:  to the southeast of Vancouver island and the Olympic Mountains, as well as downstream of central and southern Cascades.  This makes a lot of sense because the general winds were from the northwest today, so those areas are the ones with sinking air.   The windward sides of the mountains were in clouds and depressing.
 

Can we know where the rain shadow will be ahead of time?  You bet.  Our high resolution forecast models provide cloud forecasts.  For example, here is the forecast for noon from a model run that started at 4 PM the previous day (see below).  Not perfect, but the rainshadows noted above were relatively well predicted.


To show you that this situation is no fluke,   Here is the visible satellite image for Monday afternoon.....some nice rainshadows downstream of terrain.  Cloudy over north Seattle (there was a convergence zone going on), but sun to the north and south.


So, if you want to go sun/rainshadow chasing,what do you do?

First, go to my department website and look at the visible satellite animation (click here).
And if you are adventuresome, you can even look at our model forecasts of the clouds (click here).

Perhaps with more local residents using meteorology to find the light, we can give up first place in big-city depression.   And replacing several on the Seattle City Council might help as well.
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I will do a podcast tomorrow on the forecast for this weekend and the holiday season.  Plus, a special surprise topic for a more in-depth examination.  On Saturday at 10 AM, I will be doing a special zoom session with my Patrion supporters.  Will talk about the BLOB and the effects on local weather, plus answer questions.


December 15, 2020

Dry Conditions over California: What Will be the Impacts?

Although we expect that the Pacific Northwest will experience a wet, cool, snowy La Nina winter, the opposite is projected for California because of La Nina.  Furthermore, California is going into its "wet season" after a dry fall, and its reservoir system is well below capacity.

I will bring you up-to-date on the California water situation in this blog.

Let's start with the precipitation anomaly for the last two months:  how precipitation over California differs from normal for the past 60 days.  For nearly the entire state, precipitation has been below normal, but the normally arid southern portions and far western sections only down by 0 to 3 inches.  In contrast, the Sierra Nevada is down 3- 9 inches and some portions of the mountainous northern portion of the State are as much as 9-15 inches less than normal.


It is interesting to look at the percentage of normal precipitation for the same period.  YIKES. Much of California has received less than 25% of normal for the last two months, particularly southern CA.  This shows you the dangers and potential deceptive impressions of percent of normal plots....in places of little precipitation, just a modest shortfall can create scary low percentages of normal.  But the implications of such small deficits may not be significant.


And then there is  the impressive California reservoir system, which has the capability of holding MULTIYEAR water supplies.  Very different than our region, where our reservoir capacity if far less (generally a few months to a half year).  Below is the latest CA reservoir situation.  The largest reservoirs in the North (e.g., Shasta and Orovile) are significantly below normal, while the reservoirs to the south are near normal.


But to get more insight into the filling of the critical northern reservoirs, here is a plot of the current cumulative precipitation compared to normal (blue shading) for this (blue line) and other years.  You see the problem-- only about 30% of normal this year and just above the historically dry 1976-1977 uber drought year. And last year was dry year as well...but considerable more than this fall.


What about California snowpack today?  Ranges from approximately 29% in the southern Sierra Nevada to around 50% in the north.  But these are early days.

OK....California is starting the season with below normal reservoir capacity and a dry late fall.  The last year has been drier than normal as well.

As noted in my earlier blogs on western U.S. precipitation this fall, California has been dry because of ridging (high pressure) in the eastern Pacific and the jet stream heading north toward our region, western Canada, and southeast Alaska.

A pattern of precipitation consistent with the moderate La Nina that will dominate this winter. 

 But let's look into this more.  Here is the precipitation forecast for the next 46 days from the European Center....more exactly the forecast anomaly from normal precipitation.  Drier than normal over the southwest (brown colors) and wetter than normal to the north (green and particularly blue).  CLASSIC La Nina.  But look closely and you see the deficits in the Sierra Nevada are modest--about an inch.  The greatest dry concern is around Santa Barbara.


The NOAA Climate Prediction Center has a warm/dry overall pattern for the next three months over southern CA...but near normal for the far northern part of the state with the big reservoirs...that is important.



So, at this point there are concerns, but they may be enough storms going south to prevents a severe drought situation this winter in the Golden State.  Will have to watch the situation carefully.   A dry winter brings water resource challenges and fosters higher elevation fires.

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Note:  I will be having a specific online zoom session for my Patreon supporters on Saturday morning at 10 AM.  I will talk about the effects of the eastern Pacific BLOB on Northwest weather and will answer your questions. Patreon information:






December 13, 2020

Snowpack has slid a bit, but substantial Northwest snowfall is ahead

 Our snowpack percentage of normal has declined quite a bit the last week or so, but don't be too concerned.   Bountiful snow is coming.

Here is the latest percentage of normal snowpack from the wonderful SNOTEL website. Slightly below normal in Washington and generally near normal overall in Oregon.  Below normal in Idaho.


Remember a few weeks ago when we are 400% of normal?...it couldn't last.  Climatological snowpack is increasing and we had a dry period for a while.

If you compare our snowpack to a year ago, we are actually doing much better than 2019 (2019 is left, 2020 is on the right).  Hugely more this  year (you are looking at SWE, Snow Water Equivalent, the depth of liquid water that resulst from melting the snowpack at a location).



As I mentioned in an earlier blog, the long-range models are going for cool/wet conditions for the remainder of the winter, something consistent with the energetic La Nina we have in place.

Here is the UW WRF model accumulated snowpack for the next week....several feet of snowfall expected through 4 PM next Sunday.   This will guarantee good skiing over the holiday season in the fresh air of the outdoors.  Just keep away from apres-skiing libations and gatherings,  and avoid crowding in lift lines (although the threat of transmission in outside air is quite low).


The biggest worry is California.  Their snowpack is less than last year and models are not offering significant snow for central and southern CA during the next few weeks.  La Nina years are generally poor snow years for the Golden State.




December 11, 2020

New Podcast: A Deep Dive into La Nina's Effects on Our Winter Weather PLUS the Weekend Forecast



My new podcast is out and I provide a detailed discussion of La Nina--cooler than normal water in the tropical Pacific-- and its influence on our winter weather.   And I will give you the weekend forecast---telling you about the last dry period for perhaps weeks and where you might see some lowland snowflakes this weekend!

Here is my podcast:
Click the play button to listen or use your favorite streaming service

Or stream my podcast from your favorite services:

Support the podcast on Patreon and get exclusive content. 
Your support helps keep the podcast free of ads

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December 10, 2020

A Strengthening La Nina: What Does That This Imply for Our Upcoming Winter?

 La Nina is strengthening and this has a lot of implications for our upcoming winter.

As noted in earlier blogs, La Nina is associated with colder than normal water temperatures in the central and eastern tropical Pacific.  This cold water has global effects, changing the atmospheric circulation around the globe.

Let's start by looking at the current sea surface temperatures anomaly (difference from normal) around the world (below).  Blue indicates cooler than normal temperatures and there is plenty of that color along the equator along the central and eastern Pacific--that is the sign of La Nina.

Meteorologists have a favorite Pacific area we look at to determine if there is a La Nina:  the Nino 3.4 region (see image)


Plotting the sea surface temperature anomaly from normal for this key region shows the water is colder than normal (blue) and by a good amount.  This is La Nina is now a moderate one, on the verge of strong at times.


The National Weather Service Climate Prediction Center is going for a 100% chance of La Nina this winter.

And the model forecasts suggest the cold water anomaly (again difference from normal) will remain large for a while.
Folks, we will have a substantial La Nina this winter and this has substantial implications for the next few months.  Think cool and wet.  Think snow.

A NOAA/NWS graphic shows the typical configuration of the atmosphere for moderate and strong La Nina years (see below).  The jet stream, the conduit of weather systems, tends to head directly into the Northwest or up in Alaska before it swing back down.  High pressure is often observed over the eastern Pacific during La Nina period...something we have seen a lot of during the past month.  California tends to be dry with La Nina, and that is certainly true this year.



The result of this pattern is that the Northwest tends to be wet and cool during La Nina years, and this is exactly what the National Weather Service is predicting for the next three months (see below).  This combination generally means ample snow in the mountains and often a bout or two of lowland snow.


Finally, let's look at the latest extended prediction from the European Center.....covering the next 46 days.

First, the prediction of the precipitation anomaly (difference from normal) through 25 January.  Much wetter than normal in the Northwest, but dry over central and southern CA.   Classic La Nina

Temperature is projected to be cooler than normal for the same period over southwest Canada, the Olympics and north Cascades and most of Oregon.

And the predicted snowfall for the period is bountiful.


There are no guarantees, of course.  But the meteorological dice are weighted towards a cool, wet, and occasionally snowy winter, which is good for water supply and skiing.

December 08, 2020

What are the Secrets to Identifying Clouds? Part I

I often get emails and questions about clouds.  People are particularly interested in learning how to identify clouds and to understand what they imply about upcoming weather.  What is meant by the arcane compound names, such as altostratus, cirrostratus, or the intriguing altocumulus lenticularis?

Your final exam

To address these questions, I am going to write series of blogs, with this being the first, the reveals the intricacies and power of cloud identification.   Knowing about cloud identification will change your life...in a positive way.

Modern cloud identification goes back approximately 220 years to the work of Jean Baptiste de Monet Lamarck in France and Luke Howard in England in 1802-1803.

Their essential approach was to divide clouds into four types depending on how they look and three classifications based on their heights.  First, the four types based on appearance:
  • Stratus or strato-form  layered or sheet-like clouds
  • Cirrus or cirro-form:  thin, wispy clouds
  • Cumulus or cumulo-form:  puffy cotton-ball like clouds that can sometimes have great vertical development
  • Nimbus:  precipitating clouds
Let me show you some examples of each!

Here is an example of a stratus type cloud;  you see how layered it is?


A cirrus type cloud is shown below.... delicate and wispy.


A cumulus cloud has a characteristic cotton ball appearance, although some folks think they look like cauliflowers.

And then there are nimbus-type clouds, from which precipitation is falling:


Once we determine which of the four main cloud types is applicable, we then estimate the height of the clouds, dividing them into three main layers:  low, medium and high.
  • Low:  less than 2 kilometers above the surface, sometimes given the prefix strato
  • Middle: 2-7 km above the surface, often using the prefix "alto"
  • High:  more than 7 km above the surface, often using the prefix "cirro"
Low clouds are usually made of water droplets, high clouds mainly ice crystals, and the middle clouds can be both.

OK, now you are ready to put it all together.  Most cloud names combine a prefix and a suffix, the prefix denoting the height of the cloud and the suffix providing the cloud form.

For example, cirrostratus is a high ice cloud in a layer 


Altocumulus is middle-level cloud that is divided into cumulus-type elements:


And cumulonimbus is a cumulus-type cloud that is precipitating:


Well, there is a lot more to learn about cloud identification, which will have to wait until my next blog on the topic.  But you now have the essentials

But in the meantime,  you might refer to a good cloud chart, such as the online one provided by the National Weather Service (found here).






December 06, 2020

The Sunniest Post Thanksgiving Period in Many Years. Records Broken.

If there EVER was a year we needed a break from the cool, cloudy murk of the Northwest mid-winter period, this is it.


Sun that lessens the seasonal blues that many have this time of the year.

Sun and warmth that allow folks to get outside in healthful air to enjoy recreation and exercise

Sun and warmth that would facilitate outdoor eating during this COVID period when inside dining it closed.

Sun during the period of earliest sunsets (around 4:18 PM today in Seattle)

The weather gods have heard your cries and has provided deliverance, and as their close follower and scribe, let me tell you what they have done for you.

To begin, the solar radiation during the past week (November 29-December 5) has been the greatest on record for several stations (although admittedly the records are only a decade or two long for this parameter).

For example, at Seattle, the WSU AgWeather site (in the field below the UW) enjoyed more sun in this period than any other (see below), with a hefty daily average of 5.03 Megajoules per square meter (Mega=million, Joule is a unit of energy.  Some years have had HALF as much!


The plot of solar radiation on top of the UW Atmospheric Building  for the last three days is enough to make one smile, with the last two days being almost perfect cosines (meaning full radiation), reaching about 6.3 megajoules the last two days.  No wonder some students were sunbathing on the UW quad!

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The sun was also associated with unusual warmth leading to a number of daily high temperature records being broken, such as:

  • Sea-Tac Airport: 58° (prev record 55° in 2014, 1989 & 1954) 
  • Quillayute: 61° (prev record 57° in 2014) 
  • Hoquiam: 59° (prev record 55° in 2007)

Here is a plot of the some of the high temperatures yesterday around the region (click on figure to enlarge).  60F or more at several sites and even lower 60s south of the Olympics.  61F on the coast.

Looking at the temperatures in Seattle for the past two weeks compared to normal (below), shows we have exceeding the normal highs (purple lines) day after day, in some cases by 5-10F.

And the first 5 days of December was one of the driest on record!

The satellite imagery at 1 PM for the past two days shows the generally clear skies west of the Cascade crest and over high terrain.   The only persistent cloudiness is found in the lower elevations of the Columbia Basin.  Such low clouds are the price they pay for the heat and sun of the warm half of the year.   Weather gods obviously think this is reasonable and so should you.



So why have we enjoyed this sunny, warm bounty?   

Because their has been a very persistent and strong upper-level ridge of high pressure over our region.    Such ridges produce sinking motion that evaporate clouds and warms the atmosphere above us.

To illustrate,  here is a map of the ANOMALY (difference from normal) of the heights of the 500 hPa pressure surface (about 18,000 ft above sea level) for the past week.  Yellow and red mean higher than normal (anomalous ridging).  We have a nice ridge feature center centered over Washington!

 

But wait! It is even better than that!  The upper level high is associated with high sea level pressure over eastern Washington (see sea level pressure map for yesterday afternoon below).  Large difference in pressure across the Cascades that produced powerful EASTERLY (from the east) winds above the surface.  As air descended the Cascades and Olympics, it warmed more by compression and prevented the development of fog and low clouds (which can happen with high pressure overhead)


Surely, the weather gods have thought of everything

Now the weather gods are worried that Northwest folks were spoiled by all the sun and warmth, so they brought a weak front through last night. And the models suggest some rainy periods this week.  But today will be mainly dry as will tomorrow for most of the region.   

I have one of these in my office.


New Podcast: The Holiday Week Weather Forecast and the Inside Story on the Northeast Snowstorms

My new podcast is out and I provide a detailed forecast for this weekend and next week, including Christmas Day.  And then I turn to the gre...