I could literally hear the cameras clicking all over Catalina and Oro Valley as these patterns showed up, moving in from the southwest as the increasing numbers of cloud-centric folk lost control of themselves. Reflecting that general loss of control, which affected yours truly, too many photos will be posted here. Below holey clouds with icy centers, but not ones caused by aircraft:
And look closely at the fine patterns, lines and granulations in these shots! Truly mesmerizing.
But what’s missing in this photo above? There was no iridescence seen around the sun where we normally look for it suggesting that those Cirrocumulus clouds nearest the sun were composed of ice crystals, and not tiny droplets. Iridescence is rarely seen next to the sun due to ice crystals because they are usually the result of the freezing of existing droplets, that then grow rapidly as ice particles to sizes too large to produce diffraction phenomenon close to the sun. Where’s my Lear jet, so’s I can confirm these speculations?!! I would very much like to have one on “stand by”, in case I think of something. Below, a wonderful example of no iridescence even though newly formed clouds are by the sun:
A jet runs through it
Or so I thought. In this chapter of cloud-maven.com, we inspect the photos of a commercial jet flying at or near the level of these clouds and determine what happened. I was quite excited to see this happen because we would now determine whether there were any liquid droplets in what to the eye of the amateur cloud watching person would be a liquid droplet Altocumulus clouds. Here the size of the elements are just a bit too large to lump it into the Cirrocumulus category, if you care. So, with heart pounding, took this sequence of photos:
Let is go zooming:
By the way, if you caught it, there were a couple of standard, aircraft-produced, “hole punch” clouds at the very upwind, formative portion of this patch of clouds before it got here. These photos pretty much prove that the Cc at the formative end at that time was composed of highly supercooled droplets and that the passage of an aircraft produced ice, that caused a fall out hole.
In particular, those Altocumulus clouds, “cold” Cirrocumulus (ones that transform to ice immediately), and those “Altocumulocirrus” clouds combining with scenes of “regular” cirriform clouds. Lots of interesting sights to have seen yesterday. All these the result of marginal moisture aloft and strong winds, up around 100 mph at the highest Cirrus levels.
Let us begin as cloud maven folk by examining the late afternoon sounding launched from our Wildcat balloon launching machine at the University of Arizona, courtesy of IPS Meteostar:
The weather way ahead
Still looking for that chance of rain before July…. haha
Troughy conditions will actually recur aloft over us over the next few weeks it seems, which means slight chances of rain, but periodic cold fronts passing by, mostly dry ones. Best chance for rain still seems to be around the 20th, plus or minus a day or two, even though mod outputs have backed off that scene. But, we have our spaghetti that tells us the models will likely bring back that threat around the 20th, even if some individual runs show nothing at all or only close calls. We shall see if this interpretation has any credibility at all, won’t we?
Of note, Cal having big April in rain and snow after the gigantic January and February accumulations! Looks like they’ll continue to get slugged by unusually strong storms, off and on, for another couple of weeks. Water year totals are going to be truly gigantic.
I thought you’d like to read this (Peru’s Niño), forwarded to me by Niño expert, Nate M. Pretty incredible to read about what is happening down there in the wake of the Big Niño of 2015-16, which really turned out to be more of a couch potato in terms of weather production in the Great SW.
But, all this winter, along the Equator near the coast of South America, there has been something we used to call an “El Niño”, but is downplayed or ignored these days because of a new definition that seemed to explain more weather when it occurred, “Region 3.4” a large zone along the Equator WAY out in the Pacific rather than something near the South American coast (that zone now called, “Regions 1 and 2”), as nicely illustrated by NOAA here.
But what has been the effect of what we might call the “Classic Niño”, a warm strip of water along the South American coast, one that doesn’t extend too far into the Pacific? “Read all about it”, as they used to say. Its pretty remarkable.
And here’s what the SST field looks like. Its boiling down there off South America! (Speaking figuratively, of course):
Peru’s Niño can be thought of as a “classic Niño”, the ones written about in the decades before about 1990 or so when the definition of what constituted a NIño (or Niña) was expanded and delineated more sharply among several definitions that were floating around. We ended up focusing on a region WAY out in the Pacific Ocean called, “Region 3.4” that SEEMED to explain more over the prior years.
What’s so interesting about this is that the “Classic Niño” has been underway pretty much all this winter, and we’ve had, especially in California, a classic Niño response; that is, abnormally heavy precip farther down the West Coast that no one anticipated.
Well, the correlations with Cal precip and “classic Niño” occurrences will take a huge jump upward after THIS winter!
End of Statement (hand-waving) on Niñoes.
Local weather statement: for immediate release
Cooler, fluctuating weather foretold here for that latter part of March, I don’t know how many weeks ago, is on the doorstep after the long, anomalously hot dry spell. Poor wildflowers have been suffering, too, fading, looking a little stunted after a great beginning, one rivaling the great displays of 2010.
All of the local weatherfolk are on top of this now, and so no point recasting that stuff. HECK, you can go to Weather Underground1 and get as “good as can be” forecast for Catalina (Sutherland Heights) out to ten days! And, there’s nothing worse for a weather forecaster with forecasting in his blood, than to be excited about an “incoming” and when you mention it to a neighbor he replies, “Yeah, I heard about that already. Supposed to get a quarter of an inch.” There is no air whatsoever in the “balloon” after that. So, if you have a weather-centric friend who says something about the upcoming weather, pretend that you haven’t heard about it yet, “DON’T say something as hurtful, as “Yeah, I heard about that already.”
So, here, we go the long route because most weatherfolk are afraid to go too far into the future because its often WRONG. Our models tend to lie a lot after about even a week, so only the brave go out even ten days!
However, here, we go out as much as two weeks and more because its not a truly professional site but rather want to get something out there earlier than other people, sometimes called a “scoop” in the news and weather business. That’s why our motto here is, “Right or wrong, you heard it here first!” Furthermore, if a longer range forecast posted here is WRONG, you won’t hear about it anymore!
Cloud maven person will say this about the first incoming of several fronts: comes in early Thursday morning, its strong! Rainfall potential: 10% chance of less than 0.12 inches, 10% chance of more than 0.75 inches. Best of those is the average, or about 0.4350 inches in this one. It has great POTENTIAL to be a soaker, but mods have been all over the place; hence, the large range of potential amounts. At least some measurable rain seems to be in the bag, a paper one please, because plastic is insidious. Note, CMP’s forecast is more generous than that found in WU’s latest forecast for Catalinaland.
The weather WAY ahead, unprofessionally so
Let us look beyond the professional forecasting limits to April:
We know we got several storms/fronts zipping across AZ as March goes out like a lion, but what about April?
Looks like that pattern will continue into April with temperatures below normal for the first part. The end of the unprofessional forecasting portion of this blog, though we do have our NOAA spaghetti to hang our umbrella on…. Check it out for about two weeks ahead.
Some clouds recent clouds, including a couple from yesterday
———————– 1Although “Weather Underground” might sound like an org has a radical origin, maybe something left over from the late 1960s, this particular one was NOT formed by 60s “weatherman” terrorists like Bill Ayers and Bernadine Dohrn (the link is for those of you who may have set trash cans on fire, as happened at San Jose State to protest the Vietnam War, to look back at those days in horror or nostalgia; take your pick) , but rather by genuine weather geeks (haha, I count myself among them, those that can’t get enough of weather, there can never be too much, like the guys mentioned in this “Cloud City” article.)
I guess “billows” (“undulatus” in cloudspeak) two days ago in the late afternoon wasn’t enough of a sign that the weather was changing. Yesterday we had fast moving Cirrocumulus with rainbows in it, and as the sun was setting, “jet streak Cirrus”, a line of Cirrus clouds often seen in the very core of high altitude, powerful jet streams passed overhead.
How hard was the wind blowing up there in that Cirrus last evening? Oh, our Tuscon balloon sounding, lifting off around 3:30 PM, going up about a 1000 feet a minute to, indicates that the max wind up there at Cirrus level was 146 knots (just under 170 mph)! Yikes. Poor balloon. Must be in France by now.
The storm has been a bit of a disappointment in rain production. We’ve only logged 0.22 inches1. Not as much as foretold here, 0.33 inches, but that forecast was a better prediction than by “Weather Underground Robotics” (0.58 inches). Its great to beat a robot!
We had another sign yesterday in the fastest moving Cirrocumulus clouds I think you’ll ever see around here (about 100 mph), ones at just 18,000 feet above sea level, 15 kft above Catalina: rainbows of color near the sun called iridescence (also called “irisation”). Here, as is the norm here, are a few too many shots of the same thing2.
The colors themselves, of course, don’t warn of something about to happen, but the fast movement from the southwest did; a powerful jet stream is over you. That strong stream, the result of temperature gradients in the atmosphere, is dividing deep warm air from deep cold air, and steers the alternations of high and low pressure centers, and with those alternations of lows and highs along the jet stream, air is drawn from different latitude zones and the boundaries where those different masses of air meet at the surface, is called fronts. Here, such as last night, its nearly always cold ones.
The rest of the day was pretty exciting, the wind arising suddenly yesterday morning, along with our usual great visibility, and darker blue wintertime skies, made the clouds stand out more.
The sky at last, considering the power of the trough approaching, FINALLY began to fill in. Started looking around for the first sign of ice having formed in these clouds as the air aloft became cooler. Along with this filling in by Cumulus and Stratocumulus clouds, some sun highlights began to appear on our mountains, contrasted by the darkening skies above.
Eventually our jet streak Cirrus provided the background for another great sunset scene:
Today’s clouds and weather
From that map above, you’ll see that there’s a “tail-dragger” trough still to the west of us and about over Sandy Ego (haha). That’s going to keep the air over us extremely cold, and with some sun, the Cumulus clouds that arrive are expected to have tops colder than -15 to -20° C, plenty cold enough for the formation of ice.
Ice means precip, snow up there, rain down here in spots. So, we could still pick up a few more hundredths if a shower happens to drop by. The chance of isolated very light showers in the area is 100%, but no one can tell you if one will actually land on us. You’ll have to be watching, mostly after 12 noon. Look to the west toward the Tortolita Mountains, terrain that ought to spawn one or two of those.
Looks like a longer dry spell ahead; several days to a week, maybe more.
1CoCoRahs gauge, btw. NWS-style gauge had only 0.20 inches, likely due to enhanced wind loss associated with my collapsing prickly pear protector. 2 I was driving and had to park and jump out of car to get these. You only have seconds or maybe a minute or three to capture stuff like this.
We’re often confused with the California island, Catalina, and even places in Spain. Google “Catalina” and see if I am lying again. Oh, maybe that was Catalonia, SP…
Nevertheless, isn’t it time to think about a new name for our “Census Designated Place”, Catalina? In fact, at one time, each Catalina island and our Catalina, each had a marina to further confuse things by adding superficial similarities….
Think about it.
Some sunrise scenes among too many available to the writer from his camera card:
Now, for sunset color:
As you may know, there is some violent weather hitting the West Coast, California in particular. Let’s see what the Reno office of the NWS has to say about the incoming storm:
“…BLIZZARD WARNING IN EFFECT UNTIL 10 AM PST WEDNESDAY…
...WINTER STORM WARNING IN EFFECT FROM 10 AM WEDNESDAY TO 4 AM
THE NATIONAL WEATHER SERVICE IN RENO HAS ISSUED A BLIZZARD
WARNING, WHICH IS IN EFFECT UNTIL 10 AM PST WEDNESDAY. THE WINTER
STORM WARNING IS NOW IN EFFECT FROM 10 AM WEDNESDAY TO 4 AM PST
* TIMING: DANGEROUS BLIZZARD CONDITIONS DUE TO HEAVY SNOW AND
STRONG WINDS WILL CONTINUE TODAY THROUGH WEDNESDAY MORNING.
PERIODS OF MODERATE TO HEAVY SNOW WILL CONTINUE THROUGH
SNOW ACCUMULATIONS THROUGH THURSDAY MORNING: 5 TO 10 FEET ABOVE 7000 FEET WITH 3 TO 7 FEET AT LAKE TAHOE LEVEL.(Note: The large font size, the capitalization, suggest, as we know, that the writer is screaming, which I am.)
* WINDS: SOUTHWEST 20 TO 30 MPH WITH GUSTS TO 60 MPH THROUGH
WEDNESDAY MORNING. SIERRA RIDGE GUSTS OVER 100 MPH.
* SNOW LEVELS: BELOW LAKE LEVEL...MAY BRIEFLY RISE TO 6500 FEET
THIS AFTERNOON BEFORE FALLING AGAIN.
* IMPACTS: DANGEROUS LIFE THREATENING BLIZZARD CONDITIONS WITH
NEAR ZERO VISIBILITY WILL EXIST FOR TRAVEL AND OUTDOOR
ACTIVITIES WITH HEAVY SNOW ACCUMULATION ON ALL SIERRA ROADS.
THIS IS A LIFE THREATENING SITUATION. DO NOT ATTEMPT TO TRAVEL!
ROAD CREWS AND FIRST RESPONDERS MAY NOT BE ABLE TO RESCUE YOU.
STAY INDOORS UNTIL THE SNOW AND WIND SUBSIDE. EVEN A SHORT WALK
COULD BE DEADLY IF YOU BECOME DISORIENTED1."
As we know, extremely heavy snows in the Sierras can trigger cannabalism, It is our sincere wish that those affected by this severe storm curb his or her appetite for humans, i.e, that cannibalism does not break out in the Reno-Tahoe area, or ANYWHERE (capitalization for emphasis) in the Sierras during this terrible storm or its aftermath.
————————– 1Thanks to Prof. (emeritus) Roger Pielke, Sr., Colo State, for passing this warning along. His son, a great scientist as well, btw, has the exact same name, and that’s why THIS Roger goes by “senior.” Thought you’d like to know that.
Here are the latest 24 h totals, ending this morning the 23rd at 3 AM AST from your Pima County ALERT gauge network. Our own amount over this period is embedded for comparison purposes:
Gauge 24 Name Location ID# hours —- —- —- —- —- —- —————– ——————— Catalina Area 1010 0.71 Golder Ranch Horseshoe Bend Rd in Saddlebrooke 1020 0.83 Oracle Ranger Station approximately 0.5 mi SW of Oracle 1040 0.87 Dodge Tank Edwin Rd 1.3 mi E of Lago Del Oro Parkway 1050 0.59 Cherry Spring approximately 1.5 mi W of Charouleau Gap 1060 1.10 Pig Spring approximately 1.1 mi NE of Charouleau Gap 1070 0.79 Cargodera Canyon NE corner of Catalina State Park 1080 0.79 CDO @ Rancho Solano Cañada Del Oro Wash NE of Saddlebrooke 1100 0.67 CDO @ Golder Rd Cañada Del Oro Wash at Golder Ranch Rd
xxxx 0.58 Sutherland Heights, Catalina
Santa Catalina Mountains 1030 1.14 Oracle Ridge Oracle Ridge, approximately 1.5 mi N of Rice Peak 1090 1.34 Mt. Lemmon Mount Lemmon 1110 1.22 CDO @ Coronado Camp Cañada Del Oro Wash 0.3 mi S of Coronado Camp 1130 0.87 Samaniego Peak Samaniego Peak on Samaniego Ridge 1140 0.79 Dan Saddle Dan Saddle on Oracle Ridge 2150 0.71 White Tail Catalina Hwy 0.8 mi W of Palisade Ranger Station 2280 0.71 Green Mountain Green Mountain 2290 0.35 Marshall Gulch Sabino Creek 0.6 mi SSE of Marshall Gulch
Yesterday, with it many twists and turns, with that significant rain overnight providing a happy, moist beginning. Then, there was a sad middle of the day when two windshifts passed, the second a major, long-lived one one bringing a substantial drop in temperature and fronted by a dramatic arcus cloud, but there was no rain to speak of with either……at first.
Then the surprise, the unlikely resolution of the sad middle of the day just as a dismal clearing advanced from the west: a highly unusual thunderama and cloud burst beginning at 1 PM, one gushing a half an inch of rain in 18 min! This, just when it looked like a total dud was certain from the passage of that front. That “TRW++” (weather text for an extra heavy thunderstorm), provided the happy ending, thus making it a day truly out of Hallmark. The total rain was 0.58 inches, with the three day total at 1.03 inches! Yay, flower help! Rain table at bottom.
Though it was late December and at the winter solstice, the breezy 63° F damp air yesterday morning made it feel like you had awakened from your long vacation flight and found yourself in Hawaii or Miami. It was a truly remarkable, even a joyful feeling.
With that strong upper low WAY off to the southwest of us yesterday morning, and moving right this way, you KNEW that the rain wasn’t over, that thought adding to the joy of yesterday’s early morning. 0.34 inches had fallen mostly during the night before, adding to the humid feel.
Too, yesterday morning’s joy had a withering effect on all those dry weeks that had preceded these past few days with measurable rain, maybe even withering the hard feelings that remain in many of us about those disappointing Big Niño forecasts of a wet Southwest last year. You were finally beginning to feel that you could let go of those hard, grinding, grudge-holding feelings you had against weather forecasters, the ones that misled us so much last year about the Big Winter in the Southwest due to the Big Niño, a record Niño, they told us, indeed, a “Godzilla Niño.” Then, what followed was, “The Big Winter that Didn’t Happen.” And it will be years before we get another Big Niño!
But, let us move on from that tirade to current events; you can see that I am personally completely over the hard feelings of last year’s disappointing forecasts and have moved ahead, as we need to do in life…
Now, finally (!), for yesterday’s clouds, so fantastic in all their presentations and drama, that one really could finally forget the busted Big Niño forecasts of last year2:
Oh, yeah, the cloud diary for yesterday, probably more than you need to know, but, what the heck:
New storm marches toward Catalina! Due in tomorrow afternoon.
1Meteorologists, outside of Buffalo and Seattle, have inverted values regarding clear and cloudy.
2I hope we get 30 inches THIS water year, dammitall, busting this year’s seasonal forecasts of a dry Southwest.
Many strange1 and wonderful sights were seen yesterday; I could feel the excitement out there as one cloud microstructural mystery after another regaled our Catalina skies.
How cold are these clouds? Lets look at the TUS sounding, launched at about 3:30 AM yesterday morning.
That bank of Altocumulus was racing at more than 50 mph toward Catalina, and so it got here in a hurry. And, as it got closer, it was also getting more into some airways at that height, possibly descents into PHX since the height of those clouds was below normal jet cruising levels at 23,000 feet Above Sea Level.
Now for the aircraft effects. Hardly a few minutes go by before aircraft began marking up this cold Altocumulus layer. Notice that it doesn’t seem to be producing much or any ice on its own, making aircraft inadvertent seeding lines and holes where tremendous numbers of ice crystals are generated immediately present. Here’s the first of many:
Heading for Catalina, this:
Here’s the south end of that ice canal:
Looking straight up at the icy heart of a hole punch region caused by an aircraft. I am sure you have never done this before! This is gonna be a great blog with all these new things for you!
As the south end of the original ice canal began to enter the refraction zone for simple ice crystals around the sun, usually at the 22° degree halo position, things began to light up with a particularly bright circumzenithal arc (more often observed on a halo) or colorful (in this case) partial “reverse halo”. The colors (iridescence) due to the refracting of light within very small ice crystals. Normally iridescence is seen near the sun in Cirrocumulus clouds or the then edges of other droplet clouds. Very exciting.
Then this strange sight:
The day closed out with a lower layer of Altocumulus moving in, this layer, according to the TUS sounding, at “only’ -17° C, and little ice detected. Below, at 2:09 PM:
U of AZ mod thinks so light rain will develop around here in the mid-later afternoon.
1“stragne” above, originally an inadvertent typo, but left in place as another cheap trick to get draw the curiosity of readers who might wonder what stragne is.
Yesterday, whilst disappointingly dry, no rain fell here overnight was a day of rare cloud sightings, most of it involving the rarely seen, “Cumulo-cirrus1“, a cloud fakery situation where extremely cold (less that -40°Ç, -40° F)and clouds at Cirrus levels appear to be ordinary little Cumulus fractus clouds. I hope you weren’t fooled by those impersonators. You’d be pretty embarrassed at the next meeting when we go over yesterday… Yesterday was, in essence, a test for you, and I hope you passed.
Along with the rare “Cumulo-cirrus” sightings, there were intricate patterns in Cirrocumulus clouds that may have caught you’re eye. However, with the wind aloft being so strong (around 90-100 mph at 18,000 feet) you didn’t have a lot of time to enjoy them.
Explanatory figure below:
————— 1Though it fits, I made this cloud name up. Probably would be Cirrus floccus, maybe Cirrus castellanus in the humped up cases.
Not much else to talk about, no rain of course; what is that?
But with so many colorful scenes yesterday, we can be partially sated by the lives we lead here sans rain here. October ended with a puny 0.01 inches in Sutherland Heights.
Now, because I grew up in California and remain a little Cal-centric, this brief diversion from AZ:
But droughty Cal got nailed though, from about San Luis Obispo, so we can be happy about that I guess. One station, Gasquet RS, near the Duck border, got just under 28 inches in October; stations in the Santa Cruz Mountains, way down by Monterrey, got between 14-17 inches! From the California-Nevada River Forecast Center, this nice map of October rainfall anomalies in that domain. Red is real dry, and that’s the color we would be in if it was the California-Nevada-Arizona River Forecast Center:
But let us not dwell any more of generous rains that others got, but celebrate the color and clouds of Arizona. Here are yesterday’s glorious scenes, beginning with a spectacular Altocumulus lenticularis under some Cirrus at dawn:
Now, just some nice lighting and color:
In a further celebration of dryness here, let us examine the rainfall cumulative rainfall predictions calculated by the University of Arizona’s Dept Hydro and Atmos Sci computer the period ending at Midnight on November 5th. Says the coming rain in the State misses us here in SE AZ while falling just about everywhere else, of course. Dang. Let’s hope it one of the worst model predictions ever!
Not as good as a rain day with lightning, but yesterday did have its moments in the sky, enough to make the astrologers on Mt. Lemmon jealous with displays of parhelia (“sun dogs”, or “mock suns”), faint haloes, a rare parhelic circle, something you don’t see but once every year or two, and fallstreifen (fall streaks) from Cirrus uncinus clouds going in almost opposite directions, an extremely rare sight.
The rare “parhelic circle” is a local brightening often extending out from a parhelia (sun dog) at a sharp angle, which I just learned about here1. Usually you don’t see a whole circle, just part of one.
These optic displays are caused by ice crystals, of course, ones not too complex, but rather simple ones like prisms, short solid columns, bullets, and hexagonal plates. Some examples of these can be seen here.
The bottom of yesterday’s moist layer was just above 30,000 feet at a temperature of -35° C and extended all the way up to about 40,000 feet above sea level where the temperature were around -65° C.
Some photos documenting the excitement of yesterday
Below, examples of cold Cirrocumulus, ones that quickly transition to Cirrus clouds.