6:25 AM. Altocumulus perlucidus. According to my cloud chart, informally known as “America’s Cloud Chart”, it could rain within 6 to 196 hours. Its quite useful.10:24 AM. Altocumulus opacus. Note the rumpled look of the sky. Indicates that the clouds are rather shallow and composed of droplets rather than a mix of ice crystals and droplets. However, if you strain your eyeballs and look to the horizon, you can see a smoothing and a little virga showing that the cloud tops are rising and they’ve gotten cold enough to produce ice. According to my cloud chart, when you see “Ac opacus” it could rain within 6 to 196 hours.1:44 PM. While the clouds are pretty much the same gray color as in the prior photo, they’re much thicker here and are “Altostratus opacus”. “opacus” because the sun’s position is not visible, though it wouldn’t be in this direction anyway, but to the right. The bottom of this is smooth due to widespread, light falling snow, though it not in a localized area enough to be called virga in this shot. The lack of bunched or heavy virga somewhere tells you that the cloud tops are pretty smooth, too, not a lot of variation in height. The base is really determined by the point that you descend out of this precip, in this case up around 10 kft above the ground over Catalina.4:12 PM. Altostratus opacus praecipitatio or Nimbostratus, either name will do. Recall the quirk in our cloud naming system that makes, “Nimbostratus” a middle-level cloud. The base of these clouds is the general level where the snow falling out has evaporated. Due to bulging tops, and stronger updrafts, a little of the precip was able to fall out because the snowflakes coming out the bottom had grown larger and were able to survive the dry air below cloud base.
Some rain fell about this time in Catalina. Not enough to darken the pavement completely at any time. The main thing to take away from that hour of very light rain is that it was not “drizzle” as even some errant meteorologists call such sprinkles.
You will be permanently banned from attending any future meetings of the cloud maven club if you refer to such rain as we had yesterday afternoon as “drizzle.” Drizzle is fine (200-500 micron in diameter drops that are very close together and practically float in the air. Because they fall so slowly, and are so small to begin with, you can’t have drizzle at the ground from clouds that are much more than a 1000 feet or so above the ground because as soon as they pop out the bottom, those drops start evaporating and fall slower and slower by the second, and in no time they can be gone even in moist conditions. That’ s why its somewhat hilarious and sad at the same time, when, in particular, military sites for some unknown reason, report ersatz “drizzle: (coded as L, or L-) in our hourly aviation reports from clouds that are based at 5000 feet or something CRAZY like that.
This band of Nimbostratus/Altostratus had a backside that approached as the sun went down, and as you know, that clearing let some sunlight enrich and dramatize the views of our beloved Catalina Mountains:
5:39 PM.5:41 PM.
Finally, dessert:
5:47 PM. Rainbow lands on the University of Arizona Wildcat’s Skycenter atop Ms. Mt. Sara Lemmon.5:48 PM.
The amazing rains ahead
Nothing that you don’t already know about, so no use me blabbing about it too much. But in case you haven’t seen it, The Return of Joe Low (after over-hydrating over the warm waters of the eastern Pacific), is expected over the next couple of days, with a little help from another disturbance, to bring colossal rains to eastern Arizona and especially New Mexico.
Below, from our friendly U of A Wildcat Weather Department a model run from yesterday’s 5 PM global data (the Wildcat’s downsize the US WRF-GFS model in this awesome depiction).
Check out the totals expected by the evening of October 23 rd. Stupendous. Usually these totals are a bit overdone, but even so…… Will take a nice bite out of drought.
Precipitation totals expected by 5 PM AST October 23rd. Looks something like a tie-dyed Tee.
Through deliberate deception, the title is likely to bring in quite a few football-centric people, since “jumbo package” is a term used when an offensive team bring in all the “Sumo wrestlers” they have, usually in attempts to score a touchdown from 6 inches outside the goal line.
The “jumbo package”, however, is about some weather, essentially at “mid-field” rather than on the goal line (i.e., just ahead):
A large and very strong upper low center is forecast to arrive on Sunday, October 25th, football day, the last reference to football in this blog. As it passes over Arizona, the first snow of the year would likely fall on the ‘Frisco Peaks by Flagstaff.
Tremendous rains, too, would occur here in AZ with this low, espepcially2 here the SE corner, should it happen. See WRF-GFS model outputs below, as rendered by IPS MeteoStar:
Valid on Sunday, October 25th at 5 PM AST.Valid on Sunday, football day, October 25th at 5 PM AST. The bluish regions denote especially heavu rains having fallen in the prior 12 h.
But does it happen?
Let’s check the spaghetti from NOAA for a hint about whether this weather happenstance has much chance of occurring:
Valid on Sunday, October 25th, at 5 PM AST.Same map as above, except annotated for those who found the first map geographically challenging.
You, too, as an expert on spaghetti now, are as crestfallen as I was to see this spag output from last night, showing that the espepcially strong low is, in fact, an outlier; a not impossible situation, but an unlikely one since we don’t have the bunched blue contours where the jet stream is strong, down thisaway. Rather, those blue lines are grouped over the Pac NW, and only one or two bluish contours are down here, ones that would be associated with that upper low on the 500 mb map above for Oct. 25th
Still, even when you know its an outlier, it brings hope for a bountiful rain, which is good. Will monitor this as the days go by, in case the outlier spaghetti output is an outlier.
The weather just ahead
Of course, as all weatherman know, we still have our boomerang friend Joe Low returning with rain; that’s in the bag, and has a little “friend” following behind him. These, combined, should bring substantial rains overall in AZ and in the Catalina area, in the form of scattered showers and TSTMs that persist over several days beginning later Thursday through Monday. Joe et al. are slowpokes, which is good.
Haze and smoke are up, if you’ve noticed that our skies have been not so blue, but whitish. Stuff is coming up from Mexico it appears; (Smoky) Joe will bring more of that before it gets here. So, look for a hazy patches of Altocu and/or Cirrus in the next couple of days. Maybe a small Cu off in the distance.
2:06 PM, October 11th. Shows the kind of hazy, smoky conditions we’ve been having lately. There is also some delicate Cirrus up there contributing to the whiteness.
The End
——————————-
2“Espepcially” is a word I made up via some inadvertent key strokes, but I kind of like it: “In particular, but with some energy.” BTW, Coke tastes better than Pepsi, if that new, unexpected word made you think of a soft drink.
Joe is pretty dried out after dumping so much rain on AZ and NM, and will be spinning around northern Mexico before heading back out to sea off Baja to re-hydrate before coming back with another round of rain for AZ and Catalina in a week or so, maybe as much as 10 days before he gets back.
In the meantime, let us remember the Columbus Day storm, whose anniversary is coming up. The remnant of Typhoon Freda (not Olga!), infused the westerlies with extra energy, to produce one of the greatest tempests of all time when it struck the West Coast and passed inland over the Willamette Valley on its way to Seattle. It kept an extremely intense center having winds well over 100 mph, some estimates to over 150 mph; in essence equivalent to a Category 4 or 5 hurricane passage sans the torrential rains.
Below, the National Weather Service Remembers, in a reminder that it can, and will, happen again.
Recently, the jet stream has swept up the remains of Typhoon Oho and that triggered a strong “extratropical” cyclone in the Pacific, though far from shore. More tropical cyclones are forecast to form and be swept up by the westerlies in the next two weeks…..
NOUS46 KSEW 091729 PNSSEW
PUBLIC INFORMATION STATEMENT NATIONAL WEATHER SERVICE SEATTLE WA 1030 AM PDT FRI OCT 9 2015
..COLUMBUS DAY STORM ANNIVERSARY IS MONDAY OCTOBER 12TH…
MONDAY OCTOBER 12TH IS THE 53RD ANNIVERSARY OF THE 1962 COLUMBUS DAY STORM…THE STRONGEST NON-TROPICAL WIND STORM EVER TO HIT THE LOWER 48 IN AMERICAN HISTORY. AS THE GRANDDADDY OF ALL WIND STORMS…ALL OTHER WIND STORMS ARE COMPARED TO IT.
THIS STORM WAS EXTRAORDINARY. WIND SPEEDS EXCEEDED 150 MPH ALONG THE OREGON AND WASHINGTON COASTS AND TOPPED 100 MPH IN THE WESTERN INTERIOR VALLEYS FROM EUGENE TO BELLINGHAM. SINCE EITHER MANY WIND INSTRUMENTS LOST POWER OR WERE DESTROYED BY THE STRONG WINDS…THE ACTUAL HIGHEST WIND SPEEDS WERE NOT MEASURED OR KNOWN.
THE STORM KILLED 46 PEOPLE FROM NORTHERN CALIFORNIA TO WASHINGTON AND INJURED HUNDREDS OF OTHERS. IT BLEW DOWN OR DESTROYED THOUSANDS OF BUILDINGS AND KNOCKED OUT POWER TO MILLIONS OF PEOPLE FROM SAN FRANCISCO TO SOUTHERN BRITISH COLUMBIA. THE WIND STORM BLEW DOWN 15 BILLION BOARD FEET OF TIMBER FROM THE COAST TO AS FAR EAST AS WESTERN MONTANA…ENOUGH LUMBER TO BUILD A MILLION HOMES.
COULD ANOTHER STORM LIKE THIS ONE OCCUR AGAIN? THE ANSWER IS YES. AND NOW MANY MORE PEOPLE LIVE IN THE REGION THAN BACK IN 1962 ALONG WITH ALL THE ACCOMPANYING INFRASTRUCTURE SUPPORT. FOR INSTANCE…THE 1962 POPULATION OF WESTERN WASHINGTON WAS ABOUT 1.5 MILLION. TODAY IT IS OVER 6 MILLION.
IMAGINE WHAT WOULD HAPPEN IF THAT STORM STRUCK AGAIN TODAY?
WIND STORMS OCCUR ALMOST EVERY YEAR IN THE PACIFIC NORTHWEST. SOME OF OUR REGIONS STRONGER ONES OCCUR ABOUT EVERY 10 YEARS SUCH AS THE HANUKKAH EVE WIND STORM OF DECEMBER 2006 THAT KNOCKED OUT POWER TO ABOUT 1.5 MILLION PEOPLE IN WESTERN WASHINGTON.
SO IT IS PRUDENT TO PREPARE NOW FOR WIND STORMS OR ANY OTHER HAZARDOUS WEATHER OR OTHER EVENTS THAT CAN OCCUR SUCH AS EARTHQUAKES…TSUNAMIS AND VOLCANIC ERUPTIONS. HERE ARE A FEW KEY RESOURCES TO HELP YOU GET READY AT HOME…AT WORK OR SCHOOL…OR IN YOUR VEHICLE. WHEN YOU ARE PREPARED…YOU ARE NOT SCARED.
I was a small child, but 21 years old, when the infamous Columbus Day storm of 1962 hit the upper West Coast. I hoped it would come down my way, there in Reseda, California. It didn’t, only got as far as ‘Frisco.
I wrote out the weather reports for this storm from Short Wave Radio (SWR) with my best fountain pen. Here they are, because I never throw anything out. These transcribed weather reports were broadcaset twice an hour, five after.
Weather text, in ink, for the October 12, 1962, “Columbus Day” storm as compiled from Oakland Radio via SWR. SFO-Frisco, S-T, SEattle Tacoma AP; POR=Portland, OR; STK=Stockton, CA; LAX=LAX; RSA=Reseda, CA. The last three digits is the altimeter setting, with the first digit missing. Note that at 6 PM PST October 12th, SFO is having near hurricane force gusts, and at 8 PM PST, Portland is reporting gusts to over 90 mph. The 9 PM PST ob for Portland was missing!12:23 PM. Cumulus mass over the Catalinas.1:47 PM. When I wasn’t watching, this broke out!1:48 PM. Looking SSW. Looked awesome, but only heard one rumble of thunder.1:48 PM also, looking SW. “Spin move” used to get sky shots from all quads pretty much all at once. Those shown are the best. It was clear to the NW-N.1:55 PM. Dark base to right begins to unload on some lucky person.2:06 PM. Told ya! Nice addition to the prior day’s storm. Raining here now, too.2:32 PM. Nice line of Cumulus humilis or mediocris trailing off the Tortolita Mountains W-NW of Catalina.
2:35 PM. A well-known, de facto livestock pond was enhanced by that afternoon’s rain on our country access road. “Do not enter when flooded”, but everyone does anyway.
in Sutherland Heights, that is. but 1.58 inches (!) over there by Tangerine and Oracle Road:
Personal weather station rainfall totals as of 7 AM AST this morning. All of these totals are for the period after midnight last night! The green and yellow regions are rain areas from the TUS radar.
Yesterday’s clouds; pretty spectacular stuff
2:42 PM. Out of focus hailstone. Thought you’d like to see that first.
The remainder of the photos were taken at various times during the day, except as noted:
2:49 PM. Dwarf rainbow due to the high altitude of the sun.2:49 PM. Dwarf rainbow with a larger view of backyard letting go to HELL, not doing anything with it, or, as we would say, is a “restoration of habitat combined with erosion control project in progress (Letting nettle grass takeover, too.) Its great being environmental and lazy at the same time! Hahahaha, sort of. Originally this recovering area was scrapped off for a new septic system. Is in recovery now. Yay!
Rarely do passing lows get a two chances to produce rain, but the low passing overhead today and tomorrow, does. Ten days from now, its overhead again! How funny izzat? And precipful, too.
Measurable rain will fall today in Catalina CDP (“Census Designated Place”, i.e., its not a city), and in about 10 days when the SAME low returns after a boomerang trip down Texico way, thence to Baja, thence to so Cal, and back over Arizona on the 10th-11th after picking up some juice over the east Pac.
Thinking, as you are now, of a minimum of 0.05 inches and top of 0.50 inches, the latter larger amount if projected afternoon thunderstorms land on us. Thus, best estimate, average of those two extremes, thinking Gaussian conceptual model modal value here, about 0.275 inches.
BTW, should be something in the way of an arcus cloud, or a batch of low scudding clouds underneath Cumulus and Cumulonimbus bases this afternoon as a windshift to the NW comes through in the afternoon or early evening hours, well in the next 18 h or so. That could be a dramatic sight, and with that windshift, the temperature will drop 5-10° F.
When the low trudges over us the second time around in mid-October, the estimated extreme amounts are a trace minimum, and 1.00 inch max, in other words, pretty clueless here about how much could fall the second time around ten days from now.
If you don’t believe me about all this, here are is the WRF-GFS prediction for this afternoon, followed by the WRF-GFS model prediction 10 days from now, today being October 6th, in case you don’t know what the date is today, maybe you’re retired and lose track of the days and dates because you don’t have a lot to do everyday, just kind of sit there:
5 PM AST, today, October 6th. Joe low goes by, heads toward Texas.5 AM AST, Friday, October 16th, the day before football day. Joe returns after visiting NM, TX, MEX, Baja, east Pac, then SC. Full cycle here, from IPS MeteoStar. Pretty humorous to watch this happen.
Yesterday’s clouds, punctuated by a large worm
6:57 AM. If you thought the clouds were fatter to the north most of the day yesterday, you were right. Many modest Cumulus passed overhead of Catalina and then fattened up to the north because the lifting mechanism aloft was stronger to the north of us. Quite a few moiuntainstations registered over an inch to the north of us.
However for a moment, we did have a shower threat move toward us from the south, this:
11:52 AM. Whilst on a hike up the Baby Jesus Trail, this appeared. Looked promising! But, vaporized into mere sprinkles. If you saw this, you almost immediately were thinking of ice forms like needles and sheaths, since the cloud was relatively shallow, and its still warm aloft. Needles and sheath (hollow columns) only form at temperatures above -10° C. Such an occurrence is rare in Arizona, so, quite an interesting bit of hand-waving here.10:57 AM. Hike up the Baby Jesus Trail was punctuated by seeing a very colorful worm of some kind. Not much else happened in weather or wildlife the rest of the way, Morning glory coverage was a little disappointing.4:17 PM. I am sure when you saw this Cumulus congestus that you, as I was, thinking you’d see a little ice emit out the right, aging and descending side of this cloud. In fact, no ice was visible. However, it was kind of neat to think how close we are now days in our cloud assessments, right or wrong.
The last data point is for 2014-15. These data are an amalgam of the Our Garden site on Pinto and Columbus, from the top of Wilds Road, and the last two years from Sutherland Heights.
OOPS. I was listening to a Southwest CLIMAS podcast, originating at the U of AZ, and realized I missed in the above graph what can only be termed an “ineffectual Niño” that which occurred in 1986-88 and did not produce a precipitation “signal” here. How lame was that?
So, while we are excited about the prospects of extra rain this winter due to the current, supersized El Niño, like all things weather, some doubt must be in place.
Rather than hiding the omission of the “ineffectual El Niño” period, I am inserting the corrected water year history plot here with slightly revised annotation so you can compare them both.
These data are mostly from Our Garden, 1977-78 through 2011-12, located at Columbus and Stallion. The data after that are from Sutherland Heights, Catalina, some 2 mi or so to the SE of that site, and about 300 feet higher in elevation. So there is a bit of what we would call a “heterogeneity” in the data.
The downward trend is misleading, since the Our Garden record began with extremely wet water years, due to a combination of a shift in the Pacific Decadal Oscillation that occurred in 1977-78 (a shift that squelched the then record West Coast drought) and a Niño or two.
That kind of downward trend shown for Catalina in cool season precip does not show up in the Statewide averages for the whole year, anyway, shown below.
Those annual data show the usual oscillations between drier and wetter epochs in Arizona. In the plot below, you can see that had the Catalina record started in 1950 or so, there would likely be little in the way of a trend since so many of those years were drier than average. You can also see the effect of the PDO change in the late 1970s where year after year was above for the State of Arizona as a whole.
The annual (Jan-Dec) state averaged rainfall for Arizona through 2014.
The weather ahead
Rain, tropical skywater, still appears headed our way around the 4-6th of October.
With these model outputs1 for early October. First, a tropical system barges into Arizona bringing copious rains:
Valid in only 10 days from now, sometime in October. Forget any rain chances in the rest of September. Temperature plummeting here now after hot night of foehn like wind from the north.
The exact same map shown above with annotation for helpless little weather babies that can’t see what’s going on.
But its gets even BETTER! In only two weeks, this tropical rampage:
A near hurricane strength tropical storm is about to smash into southern California/northern Baja bringing widespread rains to Cal and the whole SW, which once again, includes Arizony. Wow, wouldn’t that be something!
The End
———————————-
1These outputs, rendered by IPS MeteoStar, a great weather provider, are from the WRF-GFS model. You can’t find a better model than the WRF-GFS, unless you can access the European one (ECMWF), thought to have better “skill scores”.
So, combined with the giant El Niño in progress, which will spin off stronger tropical storms than usual (definitely), and the results of trillions of calculations from our best model that shows a lot of rain headed this way in TWO episodes in 10-15 days. The chances of this actually happening are way over 10%!
Spaghetti actually has a “weakness” in the upper level pattern that will allow that first system to creep toward us; not so much support for Hurricane “Giganta” that comes toward SC, or system number two.
Will get back to you when the drops start falling…
Might was well, since no rain will fall here through the end of September (ugh). Here it is:
The last data point, 18.33 inches, is for 2014-15. These data are an amalgam of the Our Garden site on Pinto and Columbus, from the top of Wilds Road, and the last two years from Sutherland Heights. Not much going on.
But lets look at a wider set of data to see what’s going on with the whole State of Arizona precip, through 2014, anyway. The plot below is the ANNUAL statewide average, January through December, the worst possible way to display 12 mos. of precip data. This is because it slices the cool season (October through May) in half, and whole cool seasons in particular can be impacted La Niñas and El Niños that usually only last one cool season. So those kinds of effects are muted in the presentation of annual averages in the plot below (from NOAA NCDC). Sure wish they would issue water year averages (October through September) or even the West Coast, July through June annual average; both of the latter two methods capture El Niños and La Niñas well.
The annual (Jan-Dec) state averaged rainfall for Arizona through 2014. You can see that lately we’ve been, as a State, drier than normal following the big wet years of the late 1970s and early 1990s, punctuated by the El Niños of 91-93 (a Pinatubo volcanic effect may be bound up with the early 90s wet spell, too). Its interesting to note that MOST of the years from the early 40s to late 70s were below average in ANNUAL statewide. Egad.
Gauge 15 1 3 6 24 Name Location ID# minutes hour hours hours hours —- —- —- —- —- —- —————– ——————— Catalina Area 1010 0.00 0.00 0.00 0.00 0.51 Golder Ranch Horseshoe Bend Rd in Saddlebrooke 1020 0.00 0.00 0.00 0.00 0.98 Oracle R S approximately 0.5 mi SW of Oracle 1040 0.00 0.00 0.00 0.00 0.83 Dodge Tank Edwin Rd 1.3 mi E of Lago Del Oro Pkw 1050 0.00 0.00 0.00 0.00 0.98 Cherry Spring approximately 1.5 mi W of Charouleau 1060 0.00 0.00 0.00 0.00 1.50 Pig Spring approximately 1.1 mi NE of Charouleau 1070 0.00 0.00 0.00 0.00 0.75 Cargodera Canyon NE corner of Catalina State Park 1080 0.00 0.00 0.00 0.00 0.55 CDO @ Rancho Solano CDO Wash NE of SaddleB 1100 0.00 0.00 0.00 0.00 0.63 CDO @ Golder Rd CDO Wash at Golder Ranch Rd
Santa Catalina Mountains 1030 0.00 0.00 0.00 0.04 2.56 Oracle Ridge Oracle Ridge, approximately 1.5 mi N of Rice Peak 1090 0.00 0.00 0.04 0.12 6.46 Mt. Lemmon 1110 0.00 0.00 0.00 0.00 1.73 CDO @ Coronado Camp CDO Wash 0.3 mi S of Coronado Camp 1130 0.00 0.00 0.00 0.00 2.05 Samaniego Peak Samaniego Peak on Sam Ridge 1140 0.00 0.00 0.00 0.00 4.92 Dan Saddle Dan Saddle on Oracle Ridge 2150 0.00 0.04 0.08 0.16 3.39 White Tail Catalina Hwy 0.8 mi W of Palisade RS 2280 0.00 0.00 0.00 0.08 3.82 Green Mountain 2290 0.04 0.04 0.04 0.08 2.05 Marshall Gulch Sabino Creek 0.6 mi SSE of Marshall Gulch
That seems like an appropriate description for Ms. Mt. Sara Lemmon after SIX inches of rain. Lemmon’s probably a little taller today than yesterday at this time, too. Should see the “glistening rocks” phenomenon now for a few weeks, as was the case after the several inches of rain at the end of last January. Will look to see if the Sutherland is flowing today.
Besides the stupendous amount of rain yesterday in the Catalinas, there were two other rare events.
1) an occurrence of the rarely seen cloud, Stratus (the cloud that resembles gray wall paper, not much going on inside it).
2) misty light rain and drizzle that fell from clouds having no ice (which means the tops could have been as cool as between -4 C to -10 C, nature’s highest ice-forming threshold temperatures in clouds, if you care.)
Below, the afternoon sounding, launched at Wildcat University at about 3:30 PM. Goes up at about a thousand feet a minute:
The TUS sounding for yesterday afternoon as rendered by the Cowboys of Wyoming.Same diagram, but with added value. Arrows point to region where tops were, rectangle highlights temperatures. With this diagram, called a “Skew-T”, you must tilt your head about 45 degrees to the left to get the correct view of the isotherms, those straight lines that in this view, slope upward to the right. The slightest drizzle that fell, likely fell from the warmest shallowest cloud tops, the heavier showers were deeper, likely extending to 0 C or slightly above.
Now, if you’re a real cloud maven person, you would have known that this was happening in Calalina/Oro Valley yesterday afternoon without looking at a sounding. It was the visibility reducing, fine, close together drops alternating between true drizzle1 When drops get bigger than that, we call those raindrops. But whose got a micrometer out there?
Much of the time the very lightest drizzle and rain fell on us without an indication of a radar echo, likely because the tops were below the beam from the radar site far to the SE of us. TEEVEE weathermen were flummoxed by this, reporting that rain was only falling in areas where there were echoes and that it wasn’t raining here. Woulda happened to me, making the big money on TEEVEE as a weatherman, too, had I not been here to observe this rare occurrence. But, instead I am here not making any money at all writing this. There must be a reason for it.
Now, what you’ve been waiting for, the shades of gray from yesterday:
Even those coupla of heavier showers later in the evening likely had no ice in them, though this is more of a guess based on the high concentration of raindrops smaller raindrops.
Next, let’s see if Hawai’i came to Arizona yesterday:
A couple of soundings from yesterday afternoon launched at Hilo and Lihue, HI.
In conclusion, based on nearly identical temperature and humidity profiles at TUS and in Hawai’i yesterday afternoon:
Hawai’i has come to Arizona!
There’ll be some more “climate substitution” today, too, before it all fades away into heat and dryness in the next coupla weeks.
Yes, your cloud day yesterday, starting with those STRANGE Stratus fractus clouds that churned and shot straight up the sides of Sam (Samaniego) Ridge just after the first bout of light rain. Estimating updrafts were something in the 10-20 kts straight up. Clueless about what exactly was causing that to happen, This phenomenon did not last long;
10:37 AM, after the lower air had been moistened by 0.09 inches of rain. No name for this strange sight, or maybe, Stratus floccus.OK, I’m talkin’ about that! Was shooting up like a rattler going for a horse’s belly. The higher cloud layer was Altostratus/Nimbostratus; you could use either name.10:37 AM also. More churning clouds over there.
After this, the intermittent light rain moved in again. If you don’t believe me that the rain was intermittent, here’s evidence from a tipping bucket record for the day, annotated for boredom after you questioned my statement:
Yesterday’s rain graph from a Davis Vantage Pro Plus Mark IV Extra Deluxe tipping bucket rain gauge in the Sutherland Heights area of Catalina, Arizona.
More clouds
11:29 AM. It starts raining again. Churning clouds briefly visible through cloud vault.2:23 PM. Looks like a view from Hilo to me except for the very different vegetation.4:25 PM. With southwest winds and lots of moisture, our familiar “crevice cloud” formed yesterday when the clouds lifted briefly showing how saturated air can be trapped in the lee of obstacles. When it occurs on a mountain top is called a “banner cloud.”5:15 PM. Stratus, a little ragged on the bottom, moves in and drizzle erupts along the Catalinas. A bird on a pole watches the drama.5:15 PM. In case you don’t believe me that there was a bird on a pole watching the drizzle drama unfold. I find I have to keep proving myself to my reader, even after all these years. Well, two years, anyway.5:56 PM. Finally, what you’ve been waiting for, as good an example of “pure Stratus” as has ever been seen, and it was right here in Catalina, Arizona, not along the northern California, Oregon or Washington coasts in summer where pure Stratus is usually seen every morning (if you’d like to see more Stratus, that’s where to go).
Wow, what a lot of information for you today! Hours of effort here! Well, maybe two. Maybe I could write a book about rain! Oops. Its already been done (“Rain2“). Cynthia Barnett, award winning science writer has just done it. That’s what happens when you procrastinate or don’t think of it in the first place.
Enjoy a last summer rain season day and those beautiful clouds we’ll have. Looks like drizzle/warm rain again on the mountains right now!
The End.
——————————-
1By definition, drizzle drops can’t be bigger than 500 microns in diameter, equivalent to about five human hairs; a fewer horse tail hairs. And, as you know from the many harangues on this subject, such small drops MUST be close together to be termed an occurrence of drizzle, as happened yesterday afternoon into the evening.
Had to come out of general hibernation to share this with you.From last night’s global data, this Canadian Global Environmental Model “solution”; a tropical storm center passes over Tucson!
Wow, what an interesting event that would be. Of course, wouldn’t be much of a wind thing, but could bring extra soaking rains with it. Size of font in figure below indicates level of personal excitement over this prediction.
As you know, good chances for significant rain have been predicted for most of AZ next week for a few days, but this would be a little icing on those predictions if we got a tropical low center passing over us.
Valid Monday afternoon. If this were too verify, there’d be a little wind with steady light to moderate rain over a period of hours, maybe would accum to an inch or two.
