Severe weather pattern ahead for West and central US

Summary statement:  Begins in 5-6 days in the northern US, then expands southward; goes on and on, like the discussion below,  after that. Cloud pics WAY below the “novella” on spag plots.

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Our docile weather in the West for the past few months is about to end, as well as for those in the Rockies and Plains States.  Wasn’t gonna blog on TG day, but looking at mods, and realized that I am the SAME person that I was as a 6-year old in Reseda, California, on January 10, 1949,  that ran up and down Nestle Avenue knocking on doors to tell people it was starting to snow that afternoon (!), I realized that same “gotta tell ya” impulse lives on.

The trigger for THIS “gotta tell ya” is how bad the cold, snow, rain, and wind look for the western half of the US starting in about 5-6 days from now as cold air and storminess works its way south from the Pacific Northwest and Rockies at that time.  I am sure you have heard something about this developing pattern already from your favorite media weathercaster, but I’ll try to take it a bit farther out in time, and tell you why I think you can do that in this case.

I haven’t looked at the models per se with the exception of the Enviro Can one, one in which the lasted posted output is at the start of this episode, but rather the excitement for Mr. cloud maven person was triggered by those chaotic looking, “errorful” plots we call spaghetti plots, “Lorenz plots”, if you will, posted by NOAA that tell us how sensitive a pattern is to small errors.

It seemed, too,  like there was something to be learned from them, as well demonstrating a high confidence pattern of a severe weather pattern more than a week away.  Many forecaster, maybe most, shy away from forecasts beyond a week because we know how often they are faulty.   But there are exceptions and this is one coming up.

ann dec 4 5 pm spag_f192_nhbg
Valid at 5 PM AST, December 5th. This map shows a high confidence of a mammoth, cold trough at 500 millibars covering most of the US. Its “ginormous” as a friend used to say. You really don’t see anything like it, that is,  like that black “quiet” zone extending so far south anywhere in the whole northern hemisphere!

OK, here we go.

Above I have added boxes in this plot to show you where the forecast is highly reliable and in another one, where its not.   This is indicated by the bunching of those lines, height contours, the same ones, from many model runs starting with the introduction of slight errors.  At first in these plots, with errors being tiny, there is no difference in them in the first day or two.  But, as time goes on, the errors have greater impact.  A metaphor:  when you hit a ball off the tee, the error in the first inch of travel is nil in magnitude.  But 5 seconds later? Oh my.

Here, the bunching of lines in most of the US is what got me going.  Continuing the metaphor above, after 5 seconds and 300 yards of travel in this case, its analogous to 2 yards from the hole!  In other words, the were essentially no effect of errors in the model runs; you slugged that golf ball perfectly.

But what does it mean, in terms of weather?  That trough (the curved area where the “high confidence zone” is located, means a tremendous plunge of cold air into the West and Plains States.  Don’t need to look at future maps to know this.  You all know that a trough is a tongue, a wedge, of DEEP cold air that drags cold air at the surface southward on the west half of it, and drags warm air northward on the east side (in this case, toward the eastern US.  The size of this wedge indicates a gigantic area of high pressure from the Arctic will be pushing DEEP into the West and Plains States as this pattern develops in the few days before December 5th.

Once established this pattern lasts for several days, a huge, deep and cold trough dominating weather throughout the US.  And where the air masses clash at the ground presents ripe conditions for low centers to spin up, given a trigger aloft, like a traveling, much smaller wave in the jet stream where the lines are bunched.

Below, farther along in the sequence, these plots each one day later than the one above that illustrate how a confident pattern begins to erode.  In this case, “uncertainty” in the central and eastern Pacific begins to spread eastward into our confident pattern; the blue lines start to go goofy (highlighted by boxes):ann 2013120700_spag_f216_nhbg

ann 2013120800_spag_f240_nhbg

 

Last, here is the plot for 15 days (360 h) out in which those little errors have had their biggest effect, really done a number (haha) on the forecast confidence game, everything’s pretty unreliable except maybe in eastern Asia and the extreme western Pacific, and along the East Coast.

But, even with all of this chaos below, we can see that the model still thinks a trough (a bend in the contours to the south) will still be present in the mid and western sections of the US.  Since we know that weather, once changing into a new pattern likes to stay in that pattern for weeks at a time (with brief interruptions),  a reasonable forecast for December would be colder than normal in the Southwest and West overall, and in the central US, while its warmer than normal in the East, particularly the southeast US.

Precip?  Always more dicey than temperatures, but CM is going with above normal in the interior of the West and in the Southwest, near normal to above normal here in SE AZ.  Remember while reading this, Mr. Cloud Maven person is NOT an expert in long range forecasting, like for a month, and, he likes to see precipitation in the desert, and those wildflowers that follow.  (“Truth-in-packaging” clause.)

In a couple of days, the Big Boys at the CPC, that is, the NOAA Climate Prediction Center, will be issuing their temperature and precip forecasts for December.  It will be interesting to see what they make of these patterns, combined with other factors like sea surface temperature anomalies and northern hemisphere snow cover.

BTW, with a pattern like the one coming up, snow that falls during the storms is going to remain on the ground for long periods due to the lower than normal temperatures, those that snow cover helps to maintain (strong feedback loop, as we would say).

2013121300_spag_f360_nhbg

Your clouds of yesterday

If anyone is still with me, you had your Altostratus, your Altocumulus, and some Cirrus.  Here they are:


8:31 AM. Altostratus, an ice cloud consisting of single crystals and snowflakes.  Slight falls of snow (virga) can be seen at the bottom, that rumpled look.  WAY too high above the ground to reach it, estimating 18 kft here.

 

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3:41 PM. Altocumulus perlucidus (left), opacus center and right where they get solid. These clouds are comprised soley of liquid droplets; no virga is showing for one thing, and the greater detail, sharper edges goes with a droplet cloud composition. Droplets are almost always in far higher concentrations that are ice particles in clouds, thus, they have sharper edges.
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5:22 PM. Pretty nice sunset, Altocumulus overhead left; in the distance Altocumulus floccus with heavy, funnel-looking virga fall, and extreme distance, some following Altocumulus castellanus, no virga yet.

 

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5:24 PM. Close up of prior scene. Last row visible on the horizon is a nice little row of Ac castellanus.

 

Rain, and more of it

AZ Map of USGS gauges here (takes a couple of minutes to load); USGS AZ amounts here.

Pima County ALERT gauges here (Mt. Lemmon already at 0.67 inches at this hour!)

Rainlog.org here (best if used after 7 AM AST).

CoCoRahs here (best if used after 7 AM AST)

NWS rain totals here.

AZ agmet rain totals here.

I’m trying to keep you busy today. Maybe you’re retired and you don’t know what to do with yourself.  Well, today you can look at building precipitation totals in Arizona all day!  It will give you something to talk about.

In fact, occupying retirees with searches for precip data is why we have so many different sites that record precipitation.  We have a lot of retirees in AZ, low temperature refugees, and we need to keep them occupied and out of trouble.

Imagine how awful it would be if we had ALL of these rainfall amounts in ONE place and you could look at them all immediately, or have a map plot of all these sites and amounts?  Imagine just CoCoRahs and Rainlog.org being friends and cooperating together and just having one site for their rainfall collections?  It would be like the Berlin Wall coming down, precipitationally speaking.  Oh, well, that’s not gonna happen.

Oh, yeah, the Heights of Sutherland here in wonderful Catalina, AZ?

Got 0.17 inches overnight.  “Main bang” still ahead, quite a long ways ahead, considering the passing showers we have now.  Doesn’t look like the major band will get here until after midnight, then pound on us most of the day tomorrow.  This prediction from the Huskies of Washington’s Weather Department model seen here.

So being on the toasty side of the cold front, should be a pleasant, mostly  day with dry spells in between showers, and maybe, if the low clouds break a little, with fabulous middle and high cloud patterns associated with the powerful jet stream overhead (winds at Cirrus levels today and tomorrow should be over 100 mph!)  Have camera ready.

Range of amounts from this front, a little in the withering stage as it goes by tomorrow,  here in The Heights of Catalina, 0.4 to 1.5 inches, median guess 0.95 inches.  Just too cellular in nature to be sure you get hit with all that’s possible, so you fudge on the downside some.

HOWEVER, just viewed the accumulated precip from our great U of AZ mod and it shows about 1.5 to 2.5 inches here, with the model run ending at 1 PM tomorrow–with more still falling!  Wouldn’t that be fantastic!  Certainly we’d have water in the CDO.

Precip totals ending at 1 PM tomorrow!

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These mod forecasts do tend toward the high side, but I would be very pleased if more than my highest estimated amount (1.5 inches) fell.

So, what’s happening now?  Check this loop of radar-sat imagery combo map.

As you will see, rain’s piling up like mad in central AZ just to the west of us.  Amounts, according to radar,  already well over an inch just for the last few hours according to NWS storm total radar loops from PHX and Yuma.  Hah, Yuma!  How often does that radar see amounts over an inch in winter?

Below, the Intellicast 24 h radar-derived precip totals ending at 5 AM AST:

24 h rain from radar, ending at 5 AM AST.
24 h rain from radar, ending at 5 AM AST.

I suppose we’ll be complaining soon about too much rain….

 Yesterday’s clouds

So much was happening skyward yesterday!  So much so, its probably best seen through the U of AZ Weather Department’s time lapse movie here.  Its really great and shows all the complications of a day where clouds are moving in at different levels, and there are lots of wave clouds (lenticulars) over the Catalinas to marvel at.

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6:59 AM. Altocumulus patches and pastel Cirrus announce a new day.

 

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7:06 AM. A few minutes later, Altocumulus perlucidus join the color display.

 

11:07 AM.  Once again, the rarely seen Cirrus castellanus ("cumulus in a Cirrus) that I seem to notice every week here...
11:07 AM. Once again, the rarely seen Cirrus castellanus (“Cumulus in a Cirrus) that I seem to notice every week here…

 

11:44 AM. Hover clouds (Ac len) over the Catalina.
11:44 AM. Hover clouds (Ac len) over the Catalina, Altostratus above.

 

1:14 PM.  Barging in from the south, the next lower layer, Stratocumulus and Cumulus, bases touched Ms. Mt. Lemmon.
1:14 PM. Barging in from the south, the next lower layer, Stratocumulus and Cumulus;  bases touched Ms. Mt. Lemmon. Sky darkened rapidly and almost eerily right after this.
4:22 PM.  The occasionally seen Seattle June sky, overcast with threatening clouds that don't do anything, and with mild temperatures.   Tops 0f these clouds were right at the normal ice-forming level here, -10 C (14 F), and by evening, virga and light rain began to fall from them as they deepened up a bit more.
4:22 PM. The occasionally seen Seattle June sky, overcast with threatening clouds that don’t do anything, and with mild temperatures. Tops 0f these clouds were right at the normal ice-forming level here, -10 C (14 F), and by evening, virga and light rain began to fall from them as they deepened up a bit more.

The weather way ahead

More rain as month closes out.  If you don’t believe me, a theme here, check this image out:

Valid for 5 AM AST, November 30th.  Of course, I'm not going to show you the actual rain map, I want you to go from this as a bonafide Cloud Maven, Jr. (CMJ).  I've noticed that some of you have not yet ordered your "Dri-Fit" TM "I heart spaghetti" tee shirts...  What's up with that?
Valid for 5 AM AST, November 30th. Of course, I’m not going to show you the actual rain map, I want you to go from this as a bonafide Cloud Maven, Jr. (CMJ). I’ve noticed that some of you have not yet ordered your sophisticated “Dri-Fit” TM,  “I heart spaghetti” tee shirts… What’s up with that?

Clouds before the storm

First, let’s see how excited the NWS is about our upcoming major, drought-denting storm, now “in the bag”:

Tucson, here and a nice NWS YouTube presentation here.

Phoenix

Flagstaff

As you will see from these links, they’re getting pretty worked up, and have issued the SAME “Special Statement” for ALL of Arizona, that’s how big the storm is.  We’re all in this together.  BTW, the U of AZ model forecast from 11 PM AST last night had as much as 5-6 inches of rain indicated in the central mountains of AZ over the next 24-36 h! Will the washes flow here, eventually as the major rain moves east?  Hope so.

But, must point that the range of amounts that will fall here in Catalina has to be considered quite large; something from “just a nice rain” (0.4 inches total) to a gully washer (1.5 inches total) due to the fine-scale of the heaviest rainfall bands rotating around the dawdling low over the next couple of days.  Its really not possible to pin it down better than a large range of possible values in situations like this, but it does appear that most of it will fall on Friday night into Saturday.

In the meantime, more pretty skies today before the deeper clouds and rain get here overnight or tomorrow morning.  Very little rain is indicated here, though,  through tomorrow evening,in this latest U of AZ mod run. while inches pile up just to the west and in the AZ mountains.

Yesterday’s clouds

Had pretty skies all day yesterday, even saw some clouds that as far as I know, have no name, these ones below that LOOK like Altocumulus perlucidus but are all ice at Cirrus levels.   Could be called, to make up a name, “Cirrus perlucidus” I guess:

7:46 AM.  "Cirrus perlucidus."  It may be hard to tell for most folks, but these flocculent clouds are all ice.  There's a patch of Altostratus in distance.
7:46 AM. “Cirrus perlucidus.” It may be hard to tell for most folks, but these flocculent clouds are all ice. There is no WAY I would call an all ice cloud, “Altocumulus.”   There’s a patch of Altostratus in distance, and an Ac lenticular to left of pole on horizon.
9:49 AM.  Altocumulus virgae.  Great example of the "upside down" storm; droplet cloud at the top, ice and snow underneath as ice forms amid the droplet cloud, grows like mad and falls out.
9:49 AM. Altocumulus virgae. Great example of the “upside down” storm; droplet cloud at the top, ice and snow underneath as ice forms amid the droplet cloud, grows like mad and falls out.  This finding, first made in the 1950s was surprising because the clouds were liquid at the lowest temperatures.

12:04 PM. Cirrocumulus lenticularis, a bit too thin to be Ac lenticularis.

 

3:59 PM. Ac lenticular stack in lee of Catalina Mountains. Ac perlucidus in foreground.
3:59 PM. This view from atop horsey, an Ac lenticular stack beyond the Gap, in lee of Catalina Mountains. Ac perlucidus in the foreground.
4:00 PM. Looking S; buttermilk skies due to Ac perlucidus; lower layer of Ac opacus advancing from the the west below those mottled clouds.
4:00 PM. Looking S; buttermilk skies due to Ac perlucidus; lower layer of Ac opacus advancing from the the west below those mottled clouds.
5:31 PM.  Brief sunset "bloom" due to a small break in the overcast just over the horizon.
5:31 PM. Brief sunset “bloom” due to a small break in the overcast just over the horizon.

The weather way ahead

2013112100_CON_GFS_500_HGT_WINDS_276

Valid at 5 AM AST, December 2nd. A near twin of the upcoming situation.

Now showing up on mods, as November closes out, a low center that looks an awful like the situation we’ll have tomorrow and Saturday, another vortex aloft tracks S along the coast, settling in around San Diego, then moving along to the east very slowly. As you know, weather patterns like to get in a groove and repeat themselves for awhile. Could be we’re in that phase where the SW is a low “magnet” and that would mean above normal precip over a spell of a few weeks. Above, a map for December 2nd at 5 AM AST that looks a lot like what we have coming right up. For that reason, you tend to place a bit more credibility than you might otherwise in a forecast that far away.  The exact day this occurs will be most likely be off, but it is likely that a troughs/clouds and precip will   to affect the SW over the next couple of weeks or more.  Good bye dry spell!

If you don’t believe me, check this 10 day outlook from the NOAA spaghetti factory:

"Lorenz plot" from NOAA,  valid at 5 PM AST, November 30th.  Its pretty plain to see that there is a strong likelihood of a cutoff low in the extreme SW US.

“Lorenz plot” from NOAA,
valid at 5 PM AST, November 30th. Its pretty plain to see that there is a strong likelihood of a cutoff low in the extreme SW US, if you can find it.  (The vast number of contours is due to a software glitch today.  Usually only a few upper level contours are tracked.)

Cloud joy; all kinds of ’em; next rain chances on the 21st and again on the 29th

A couple of Pima County gauges reported measurable rain yesterday or overnight, but that was about it. But it was a fabulous cloud day yesterday.  Heavier spotty rains, one USGS station indicating over an inch, fell in the central and northern mountains, which is good.

Below, a rehash of yesterday’s great variety of clouds.

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7:48 AM.   Altocumulus lenticularis clouds beyond the mountains to the SE of Catalina. Lenticular clouds indicate a stable layer of air, one resisting being pushed up, the opposite of what the slender Cu below indicated.  So, an usual sky for us yesterday morning.
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8 AM. Towering Cumulus atop Ms. Lemmon indicated how unstable the air was just above mountain top level. Underexposed for dramatic silouhette look. The smooth top on the right would be Stratocumulus lenticularis, again an odd juxtaposition.

 

10:37 AM.  Then you had your Altostratus mammatus/testicularis.
10:37 AM. Then you had your Altostratus mammatus/testicularis.
3:08 PM.  Your Cumulus mediocris topping the Catalinas with a few Altocumulus above; nice shadows and sun quilting.
3:08 PM. Your Cumulus mediocris topping the Catalinas with a few Altocumulus above; nice shadows and sun quilting.

 

 

3:09 PM.  And you had your "weak" Cumulonimbus capillatus clouds to the north.
3:09 PM. And you had your “weak” Cumulonimbus capillatus clouds to the north.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

4:09 PM.  Dramatic scenes of banked up Stratocumulus over the Catalinas, Altocumulus top side.
4:19 PM. Here’s a better shot of the Altocumulus perlucidus (here) top side.

 

 

4:33 PM.  Nice example of glaciating smaller Cumulus remnant north over Saddlebrook.  Likely some sprinkles reached the ground under that ice plume.
4:33 PM. Nice example of glaciating smaller Cumulus remnant north over Saddlebrook. Likely some sprinkles reached the ground under that ice plume.  As you know, takes ice to get rain in AZ.
4:34 PM.  More sunlight and shadow drama due to Stratocumulus and Ac perlucidus above.  Was indoors socializing so didn't see sunset.  Hope it was a good one.
4:34 PM. More sunlight and shadow drama due to Stratocumulus and Ac perlucidus above. Was indoors socializing so didn’t see sunset. Hope it was a good one. I am beside myself thinking about how happy you were seeing all these kinds of clouds in one day!

 The weather ahead

Models beginning to act quite well now.  A little rain is foretold for Catalina and environs on the 21st of November, but Enviro Can make that storm look more significant and slower to move in, on the 22nd.  Still two mods, both having some precip?  Its all good.  First, for your viewing pleasure and because it portends more rain, from Canada, this:

Valid for 5 PM, November 21st.  Low and lots of rain shown banging into Cal.
Valid for 5 PM, November 21st. Low and lots of rain shown banging into Cal.  Would be here  about 24 h later, or on the 22nd.

 

Also valid for 5 PM AST, November 21st, this depiction of the flow at 500 mb.
Also valid for 5 PM AST, November 21st, this depiction of the flow at 500 mb.

 

An aside:   the Canadian model tends to have a westward bias, that is, a storm is foretold to be farther west a few days out than it turns out to be, something I’ve learned since becoming a forecaster yesterday (hahaha, just kidding,  if anyone’s reading this far).  So you have to figure the Enviro Can depiction of a trough off Frisco, Cal,  is really going to be inland that bit.  The US mod output shown above,  has this same trough going more overland before it gets to us than the Canadian one, and so there’s less cloud water in it by the time it gets here.  Root for the Canadian “solution”!

Farther down the road….more illusory water on the hot highway?

And, of course, a heavier rain is once again over Catalina and vicinity as November closes.  This model really likes Catalina and SE AZ!  Check it out:

Valid for 5 PM AST. November 29th.
Valid for 5 PM AST. November 29th.

Plenty of late November rain ahead…in model; a sunrise beauty

In case you missed it, yesterday’s sunrise:

6:52 AM.  Altostratus with mammatus underlit by rising sun.
6:52 AM. Altostratus with modest downward hanging mammatus1 bulges under lit by rising sun above the Catalina Mountains.  Altocumulus clouds are in the background.  Was a magnificent sight.
6:57 AM.  Mammatus protuberances more evident here, and quite lovely.
6:57 AM. Mammatus protuberances more evident here, and quite lovely I thought.  I seem drawn to mammatus formations.

 

 

 

 

 

 

 

 

 

 

 

The weather way ahead

Well, the WRF-GOOFUS model has lots of rain for us again as November closes out, with the model rain amounts foretold in November for Catalina now totaling over two inches, or about twice normal. Its been great model month of rain for us. Below the latest rains foretold, beginning on the 27th, continuing into the 29th.  Here from IPS MeteoStar, these renderings from our best model, based on last evening’s global obs taken at 5 PM AST:

27th 2013111400_CON_GFS_SFC_SLP_THK_PRECIP_WINDS_336
Valid at 5 PM, Wednesday, November 27th.
28th 2013111400_CON_GFS_SFC_SLP_THK_PRECIP_WINDS_348
Vallid on Thursday, November 28th at 5 AM AST.
28th 5 pm 2013111400_CON_GFS_SFC_SLP_THK_PRECIP_WINDS_360
Valid at 5 pm November 28th. Green areas denote areas where the model has calculated that rain has occurred during the prior 12 h.
27th 2013111400_CON_GFS_SFC_SLP_THK_PRECIP_WINDS_336
Valid at 5 AM AST Friday, November 29th.

There is some evidence from the NOAA spaghetti factory that churns out those spaghetti plots that a big change happens in the last week of November, so rain at the end of the month, two weeks from now,  is not out of the question.   This rain pattern results from a stagnant upper low SW of us which you can see here.

What about the weather immediately ahead?

Global pattern shifting like mad today due to what we call, “discontinuous retrogression” caused by low cutting off out of the jet stream in the central Pacific.  Troughs/ridges jump westward almost overnight when this happens.  Highs disappear overnight as is happening right now over the whole West!  Very exciting, except in this case, while a trough blossoms overnight replacing a ridge in the West, its amplitude (how far south the jet stream in the trough gets) doesn’t seem to be enough to provide us with rain here in Catalina now.  Remember that winter rain here is nearly ALWAYS associated with a jet (at 500 mb) to the south of us.

This drastic change in pattern often only lasts a couple of days, too, before reverting to “same old same old” as we had, fair and warm.  I wanna cuss here.

The foretold development of a trough in mid-month in the West was a huge, and strong signal, you may recall, in our “Lorenz  plots” (I am hoping this name catches on; he deserves it), those balls of yarn I show every so often.  So the trough and cold air getting here to SE AZ has been “in the bag” for more than 10 days in advance,  according to those strange plots.

However, the rain here in the actual model runs has come and gone in them as mid-month approaches, and lately, there ain’t been nothin’ here.  At most, a few hundredths it would now seem, and most likely, nil.

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1Gender-specific naming cloud variety convention: if male, as in the case of the writer, this cloud formation is deemed,  “Altostratus mammatus”;  if female, the proper name would be “Altostratus testicularis.”  Its part of an adjustment similar to the one when only female names were used for hurricanes, and doing that, it was felt,  lent a kind of stereotype to female behavior/character.  So, male names for hurricanes were introduced by NOAA in the 1970s to “even the score”.

An ordinary beautiful day in Catalina, Arizona

Yesterday was one of those ideal days for us here in Catalina, the kind that draws visitors from all over the country to be together with us.   It was also kind of like that space-age, relaxo-elevator music; goes nowhere in particular with a hook or melody, or if there is one, its been eviscerated by sleepy, sedated violin players.

But, going back to yesterday’s weather, you could have taken a nice snooze in the sun yesterday afternoon, with only zephyrs to brush up against you, and with temperatures in the upper 70s, it was perfect for being unconscious for a bit, not having to worry about missing an ice crystal, a patch of virga, or an interesting pattern in middle-level or high clouds that you should write about in your weather diary, or document with a photo.

BTW, tops of the small Cumulus (humilis) were warmer than -10 C (14 F) yesterday, and so not one ice crystal or snowflake fell out of them.

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6:52 AM. Residual Altocumulus castellanus from the little rainband that went through the night before last.

 

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2:00 PM, from along Equestrian Trail, these picaresque small to medium Cumulus clouds, hold the ice, with dramatic shadows on the Cat Mountains.

 

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Imagination going dry. I’ve talked about these kinds of days a lot. Will insert cow with cholla ornamentation here as a distraction. Might be best part of blog today.
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3:44 PM. Cumulus clouds wither to Cu fractus as temperature falls. These days are so clear that it seems the earth ends just over the horizon.

 

Today’s clouds (should be interesting)

Should see a band of Cirrus and thicker ice cloud, Altostratus, off to the NW horizon by about mid-day.  Some Altocumulus likely around, too.  That band (you can see it here, courtesy of the U of AZ Department of Weather).   should arrive here here during the mid to late afternoon, producing a fair amount of gray.  But also there should be thinner portions before the main icy mass gets here.  In those thinner portions and leading CIrrus, there could be some some great patterns, like Cirrus uncinus, hooked Cirrus (“Angel’s hair”).     Lower Cumulus clouds are likely to form over the mountains during the mid-late afternoon. Could be really pretty overall if you can get out of your windowless office for a moment to take a peak this afternoon.

Freezing level and the critical -10 Centigrade (14 F) level for ice formation in clouds here in AZ will be lowering especially during the evening and overnight hours, and should lead to ice formation/virga as the clouds fill in later in the day and overnight. This means a chance for measurable rain here. Noticed just now that yesterday morning’s U of AZ mod (available after about 10 AM) did have a few hundredths in Catalina overnight tonight.  You can also see this progression of clouds, more or less, in the U of AZ model output from that yesterday morning’s run here1.

 

Will write more about later happenings in November when the prior forecasted rain in the models returns; its gone for now!

The End.

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1The 11 PM AST model run from the U of AZ is not yet completed, so to HELL with it!  Hahaha, just kidding, but must move on to other chores, like digitizing old research flight videos from the University of Washington’s Cloud and Aerosol Research Group I was once a part of but now its over, plane gone, group gone.  Life changes, not always for the better, I can see that now.  I liked flying in clouds, hearing the graupel hit against the bubble where I had my head, standing on a little stool in the back.  BTW, here is what the bubble looks like.  I like to look at it even now and remember all the great cloud friends I got to know and write about.

The aircraft dome used by the Univserity of Washington on its research aircraft.  RIP.
The aircraft dome that was atop the fuselage of the University of Washington’s research aircraft. RIP. For awhile after retirement, I felt lost as many do. So, I would put this on my head, maybe while doing yard work in Seattle before coming here. It seemed to help the withdrawal I was feeling in those days. Great as a rain hat, too! It really didn’t look that bad.

Pretty cloud day

One of the best, really, never mind all that wind yesterday. No rain, of course, in our future, not even fantasy rain these days.

See usual rehash of yesterday’s clouds, the 60s, in case you forgot, below:

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8:49 AM. This Altocumulus perlucidus cloud behaved like a lenticular, holding in place for at least 2 h, but did not have the classic pancake or sliver look of lenticularis clouds. Air likely too unstable (temperature dropped with height rapidly) and allowed tiny cumuliform elements to form. Only on the very right edge where it first formed, did this cloud appear “lenticular” in any way with its smoothness

 

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10:15 AM. More classic looking, sliver Altocumulus lenticularis beyond the Catalinas. Cloud forms on the right edge, dissipates on the left as the air rises and falls slightly.

 

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11:58 AM. Cirrocumulus (delicate granulation) on the fringes of Altocumulus (larger elements on the right).
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12:01 PM. These clouds change by the second as the degree of moisture in the air jetting along up there ebbs and wanes.  Look how much larger that fine granulation on the left got in just a couple of minutes.
2:09 PM.  One of the many examples of iridescence seen yesterday in those Cirrocumulus clouds, or on the very thin upwind edge of Altocumulus lenticularis clouds.  Its due to the formation of extremely tiny droplets, a few microns in diameter, that cause the sun's light to go around them and in doing that the white light from the sun gets broken down into its colored components.  Do you remember that white light has the wavelengths of all the colors in it?  Here you can see some of them.

2:09 PM. One of the many examples of iridescence seen yesterday in those Cirrocumulus clouds, or on the very thin upwind edge of Altocumulus lenticularis clouds. Its due to the formation of extremely tiny droplets, a few microns in diameter, that cause diffraction in the sun’s rays (see link for a more complete explanation and nice examples). Do you remember that white light has the wavelengths of all the colors in it? Here you can see some of them, and photograph them by performing a replication of the Black Power salute of Tommy Smith and John Carlos from my alma mater, San Jose State, one that beat the Wyoming Cowboys recently in fubball.    I added a link in case you forgot and wanted to get worked up again. Yes I was at SJS when that happened down Mexico way, minding my own business doing weather forecasts with a political slant (left, of course, because that’s what made you popular during the rad lib days) for the college paper.  Suddenly, I feel like going to San Francisco, putting some flowers in my hair.

 

2:19 PM.

2:19 PM. Cirrocumulus and Ac lenticularis in the same layer. Recall Cc can’t have shading, not that it matters that much.

 

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4:39 PM. This dramatic scene amid the dust and wind. This would be an Altocumulus lenticularis, one that devolves into Altocumulus perlucidus (honeycomb pattern seen downwind from the distant leading edge).

The End.

Not likely to verify, but a wonderful map (but, “trending up” in twitter-speak)

This is definitely not the same title as was a few days ago for a similar map, one also valid for Nov 3rd-4th.  That title was quite different:  “Not likely, but a wonderful map.”  The  rainy Arizona map back then from our best model showed a tropical storm and moist plume being drawn northward into AZ.

Almost the exact map as that one a few days ago has shown up again out of the blue, if you can say that when you’re talking about clouds and precipitation.  There’s been nothing like that former map since that first time it showed up, and, in view of how odd it was, you tend to write it off as something you’ll not see again.  But there it was again, now only 10 days out.

Below, the happy, rainy AZ map churned out by last night’s model run based on global data taken around 5 PM AST yesterday ( from IPS MeteoStar):

MOdel outpur valid for 5 PM November 4th.  Shows tropical storm remnant being sucked up toward Arizona with lots of rain already here.
Model output valid for 5 PM AST, Monday,  November 4th. Shows tropical storm remnant being sucked up toward Arizona with lots of rain already here.  Green blobs denote where the model thinks rain has fallen in the prior 12 h, which here is the entire State of AZy!

Below is the pattern aloft that steers (hahaha) all that moisture into our water-challenged State, one that has a lot of steers.

HOWEVER, this rainy situation requires a lucky conjunction of a Pacific trough coming in out of the Pacific onto the southern California coastline, while a tropical storm/former hurricane is off Mazatlån at that same moment.  If these two features of interest are just about anywhere else than is shown here in these model projections, forget it.

The flow pattern in the middle of the troposphere, around 15,000 to 20,000 feet above sea level.  Yep, that's right, half the air is gone by the time you get to only about 17,500 feet!
The flow pattern in the middle of the troposphere, around 15,000 to 20,000 feet above sea level. Yep, that’s right, half the air is gone by the time you get to only about 17,500 feet!

The first time this rainy map was shown for Nov. 3-4th, back about five days ago, the chances of it actually happening were probably somewhere around 0.2 percent.  Just too much had to fall into place.  Coming up twice, however,  jacks the lucky numbers up to, oh, maybe to an 8 percent chance of actually happening as a wild guess.  Not a great chance, but one that’s trending upward.  You know, after the rainless October that’s about to finish up, we really deserve this storm in early November.  The NOAA spaghetti factory has good support for a trough along the California coast at this time, so its likely THAT ingredient will likely be in place on November 3rd-4th.

Yesterday’s clouds; yes, there were a couple, some patchy Cirrus and a little band of Altocumulus, some of the latter trending toward lenticularis-ee ones. later on.  Here they are.

2:37 PM.  Patches of Cirrus drift across the southeastern sky.
2:37 PM. Patches of Cirrus drift across the southeastern sky.
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3:51 PM. Lines of Ac perlucidus streaked across the sky in the afternoon, soon to disappear.
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4:52 PM. Ac len below a patch of Ac perlucidus.

 

The End

Weeds of Douglas 2013: a comprehensive pictoral survey following the record summer rains

You probably don’t believe that I went all the way to Douglas yesterday to see weeds from excessive, once-in-a -hundred years, record-breaking summer rains (16 plus inches).  I think you’ll find my activities in this matter quite interesting.  First, the documentation:

11:11 AM.  The Douglas Visitor's Center, Douglas,  Arizona.
11:11 AM. The Douglas Visitor’s Center, Douglas, Arizona, fronted with manicured, non-native plants and grasses.  Quite nice, really.

I thought I would do a comprehensive survey, radiating outward from the VC in all directions as far as I could go, even if it took several hours. But after that thought,  I decided to just go across the street into a vacant lot right there in front of me, and shoot some weeds there; maybe that would be enough.  It was getting pretty warm.

11:15 AM.  Weeds in a vacant lot across from the Douglas VC.  Took a few minutes after the prior photo.  But, while the weeds were nice, they didn't "pop" enough for a news and survey report about the effect of a lot of rain, so I looked around for better angles and bigger weeds.  I think you'll find I was successful.
11:15 AM. Weeds in a vacant lot across from the Douglas VC. Took a few minutes after the prior photo. But, while the weeds were nice, they didn’t “pop” enough for a news and survey report about the effect of a lot of rain, so I looked around for better angles and bigger weeds. I think you’ll find I was successful.  The plastic cup is for perspective.
Looking back at a sidewalk along the SAME vacant lot.  Much more dramatic.  However for the best/biggest weed displays, you need areas where the water puddles some.
Looking back at a sidewalk along the SAME vacant lot as above. Much more dramatic. However for the best/biggest weed displays, you need areas where the water puddles some. And I found that by going just a little farther.

 

11:18 AM.  A low spot at the end of the SAME street showing how the excessive rains led to massive weeds.  What appears to be oat or wheat stalks ten feet high with heads protrude in the background, maybe ten feet high!
11:18 AM. A low spot at the end of the SAME where the vacant lot was street showing how the excessive rains in Douglas led to massive weeds. What appears to be oat or wheat stalks ten feet high with heads protrude in the background. Where’s my camera crew?!  I could be standing in front of this scene giving a report!
11:27 AM.  The best is always last, it seems.  It finishing up my comprehensive survey of Douglas 2013 weeds, this metaphor for life and all the different pathways we could take, and perspective on how high the weeds were where the water collected some.  It doesn't get better than this.
11:27 AM. The best is always last, it seems. In finishing up my comprehensive survey of Douglas 2013 weeds, this metaphor for life and all the different pathways we could take, and at the same time, a perspective on how high the weeds were where the water collected some. It doesn’t get better than this. I stared at this sign for many minutes, wondering if I should have gone into weather after all, maybe done something else to the right. But what would it have been?

 

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On the way to Douglas from little Catalina, I passed through the tourist mecca of Old Bisbee. A sign called out as I approached it, “Scenic View”, and I am kind of a sucker for those. Thought I’d check it out.

10:34 AM.  Scenic view sign right next to Old Bisbee, in case you didn't believe me that there was one.
10:34 AM. Scenic view sign right next to Old Bisbee, in case you didn’t believe me that there was one.

 

 

 

 

 

 

 

 

 

 

 

 

I walked over to see what it was:

10:35 AM.  The "scenic view" was this giant hole, an old mine, that reached all the way down to the water table, and a small lake was forming.  Pretty interesting I guess, a lot of money was made here, but I'd be concerned about the water I was drinking if I was a Bisbee-ite.
10:35 AM. The “scenic view” was this giant hole, an old mine, that apparently reached all the way down to the water table, or maybe initially clean rainwater had formed a small lake.   Scenic?  I guess it shows we can dig huge holes, make a LOT of money, and leave a big mess.  Hmmmm.  Too, I’d be concerned about the water I was drinking if I was a Bisbee-ite. Of course, maybe this water flows underground and downstream from Bisbee, for others to drink…so maybe it’s OK for Bisbee-ans.  Sure glad we don’t do that anymore!

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Being a CM, I should report on the clouds of the day, Altocumulus ones:

12:08 PM.  On the way to Benson, this line of Altocumulus floccus with tiny Ac lenticulars around, too.  The shadows the clouds were causing made it a real nice scene.
12:08 PM. On the way to Benson, this line of Altocumulus floccus with tiny Ac lenticulars around, too. The shadows the clouds were causing made it a real nice scene.
2:24 PM, near the J-Six Ranch turnoff of I-10, this pretty "front row" of Altocumulus castellanus, in effect, miniature Cumulus clouds.
2:24 PM, near the J-Six Ranch turnoff of I-10, this pretty “front row” of Altocumulus castellanus, in effect, miniature Cumulus clouds.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Not much weather ahead except breezes and temperature changes, hardly anything for a CM. Maybe a lenticular with the winds aloft getting so trough with our incoming trough. Will be watching.

The End.

Updated Catalina water year rainfall; so much ice, so little rain yesterday

Updated water year rainfall through 2013

Add to text box, lower left, the words: “….unless you’re quite young.”
Looked like there was a leveling off during the past 15 years, along with the “puzzling 15-year hiatus1” in global warming, coincidentally, so I used a “poly” fit instead of a linear one that would reflect the “stabilization” of water year rainfall in these latter years. Those early wet years in our record are now associated with a big change in the positions where the lows and highs like to be in the Pacific, one that comes around every few decades called the “Pacific Decadal Oscillation” (PDO).  The change to a new regime occurred in 1977-78, just when the Catalina rainfall records started at Our Garden down on Stallion where you should buy some stuff.  There was also a gigantic El Nino in 1982-83 that contributed to that early wetness.  Remember all the flooding in September and October of 1983?
You may notice that I have posted this some ten days before the end of the water year.  I dare it to rain on this year’s data! (And I hope it does, given our meager total.)
Yesterday’s clouds
Many more and thunderstorms much closer than expected from this keyboard (heard thunder just after 12 Noon!)  Here’s our day in pictures:
8:15 AM.  Altocumulus perlucidus provides some nice lighting effects on the Catalinas.
8:15 AM. Altocumulus perlucidus provides some nice lighting effects on the Catalinas.
10:03 AM.  Early risers suggest tremendous instability up there.
10:03 AM. Early risers, like that middle one,  suggest tremendous instability up there.
10:31 AM.  See note.
10:31 AM. See excitement note.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

12:38 PM.  Cumulonimbus/thunderstorm forms NE of Catalina.
12:06 PM. Cumulonimbus/thunderstorm forms NE of Catalina.  Due to high and cold cloud bases (at and a little below freezing later) this cloud has a high preponderance of ice compared to our more tropical Cbs.
12:38 PM.  Eventually becomes the "Dump of the Day" over there by the town of Oracle.
12:38 PM. Eventually becomes the “Dump of the Day” over there by the town of Oracle as it recedes (boohoo).
3:44 PM.  As noted in the title, yesterday's clouds with their cold bases had a LOT of ice in them, and in most cases, not a lot of rain fell out.  Here, an example of a dissipating Cb that didn't produce much more even in its peak than what you see here.
3:44 PM. As noted in the title, yesterday’s clouds with their cold bases had a LOT of ice in them, and in most cases, not a lot of rain fell out. Here, an example of a dissipating Cb that didn’t produce much more even in its peak than what you see here, a VERY slight shaft.
6:24 PM.  Still, some nice color at sunset.  That's what this blog is mostly about, pretty pictures, in case you missed those scenes of the previous day..
6:24 PM. Still, some nice color at sunset. That’s what this blog is mostly about, pretty pictures, in case you missed those scenes of the previous day..

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Today….  Dewpoints are up from yesterday over much of southern Arizona, and mods suggest a similar day to yesterday, scattered to broken Cumulus clouds with an isolated Cumulonimbus, with more coverage in rain than yesterday.  Whoopee!  Rain is actually predicted here!  How fantastic would that be? And I would have to update my opening just graph just that bit, an enjoyable task, really.

Mods are also indicating that some rain may leak into tomorrow as our first tentative cool season-style trough and front pass by.  We’ll see.  In any event, should be a pretty day today and tomorrow.  Try not to be inside the WHOLE day watching football!

The End

 

 

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1From the news section of Science mag:  “Puzzling” 15-year hiatus in global warming