Cloud scenes from August 31, 2015, a big summer rain day

BTW, a little more than 4.5 inches has fallen on Mt. Lemmon in the past 24 h.   0.99 inches fell here in Sutherland Heights.  Maybe the Sutherland Wash will be running this morning.  That would be nice to see.

More rains ahead in the next few days.  Mushrooms coming…

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Rain water balloon about to hit ground.
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Rain water balloon hitting ground, shoving other rain shaft aside.
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Cumulus tribute to Pac Man.
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Electricity.
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Plein air painting by nature.
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Ditto on the Catalinas.
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Dramatic shot, film noir maybe.
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Marana gets wet, too.
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Pretty.
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An approaching complex array of clouds just before sunset led to evening/nighttime TSTMS (weather text for “thunderstorms”).  Often at this time of day, showers like this just fade away to just anvil debris. But not yesterday. Must have been, in this case, indicative of the approach  of an upper level “congregator” or disturbance that doesn’t care so much about day or night.

 

The End.

A day of cloud magnificence and error

Morning thunder, evening thunder; 0.84 inches of rain, 1-2 inches in the mountains, with some of the most dramatic skies and shocking cloud changes ever seen (by me).  “But,  hey, enough of ‘me’, lets get on with the ‘shockumentary'”,  as Rob Reiner might say.

Scene 1: Its morning.  A horsey ride has been planned with an important, published friend.   You’re thinking, “It will be good to be seen with someone important.”  No one’s paying attention to weather.  The weather is cloudy, quite nice really, but nothing threatening can be seen.

6:48 AM.  Nothing to worry about really.  Just a patch of Altocumulus castellanus.  Quite pretty.
6:48 AM. Nothing to worry about really. Just a patch of Altocumulus castellanus. Quite pretty.

Scene 2. Heading out.

7:20 AM.  Heading out.  Wonder what that is coming 'round the mountain.  Probably nothing, though it is kind of dark.  Cloud bases are lower, too.
7:20 AM.  Wonder what that is coming ’round the mountain. Probably nothing, though it is kind of dark over there. Cloud bases are lower, too. Desert’s turning a nice green now after the recent rains.  Too bad there isn’t more rain ahead.

Scene 3.  On the trails.

7:33 AM.  Been on the trails for more than 12 minutes...  Cloud bases lower still, but, its probably just harmless, non-precipitating Stratocumulus.   Nothing to be too concerned about, though the amount of water in the air must be prodigious today.
7:33 AM. Been on the trails for quite awhile, maybe more than 12 minutes… Cloud bases lower still, but, its probably just harmless, non-precipitating Stratocumulus.  Nothing to be too concerned about, though the amount of water in the air must be prodigious today.

Scene 4.  Ooops

7:43 AM.  Huh.  Rain and thunder approaching rapidly.  Note horse's rear pointing in the direction of the storm (lower center right).  As a horseman, you would know that this is a classic sign that a storm is approaching from that direction, though you can see it coming as well,
7:43 AM. Rain and thunder approached rapidly.  Note horse’s rear pointing in the direction of the storm (lower center right). As a horseman, you would know that horses often point there rear ends at storms, hard to say why,  but its a  classic sign that a storm is approaching from that direction, though you can see it yourself as well.  Actually, we were fleeing like mad, embarrassed galore that cloud maven person did not look at radar that morning to see what was over the hill.

Scene 5.  Dramatic skies and a few close strikes.

7:47 AM.  Just about back, but LTG strikes getting closer faster.
7:47 AM. Just about back, but LTG strikes getting closer faster.

The storm passed dropping 0.22 inches.  And, compounding error, as we know, when potent upper air disturbances bring morning thunder and rain, its pretty much always the case that the rest of the day will be dry as a subsiding couplet of air follows a rising one, the the strongly rising couplet of air that forced our morning clouds and storm.

So, was kind of looking ahead to a disappointing rest of the day , but was thankful for the unusual morning storm.

1:49 PM.  As expected, a large clearing occurred, followed by the development of a few harmless Cumulus over the Catalinas.
1:49 PM. As expected, a large clearing occurred following the morning rain, and a few harmless Cumulus developed over the Catalinas.
5:49 PM.  A thunderstorm passes NE of Catalina, but like the day before, will likely only bring on a mighty wind, though a rain-cooled one.  That will be nice.
5:49 PM. A thunderstorm passes NE of Catalina, but like the day before, will likely only bring on “a mighty wind”, to quote Rob Reiner again, though a rain-cooled one. That will be nice.
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5:59 PM.   Quite “histrionic”, but certainly won’t get here…..
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6:07 PM. Nice Cumulus congestus in foreground; giant anvil in back from the storm to the N-NE.
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6:10 PM. Nice scruff of Stratocumulus/Cumulus mediocris rides above the NE winds that blew out of the storm to the north. Certainly, these clouds won’t do anything. Bases disorganized, nothing congealing.
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6:17 PM. Huh. Bases looking a little better, especially back there over the mountains. Still, seems VERY unlikely anything will happen. Its late in the day, temperature falling…..
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6:31 PM. The larger base has crept closer to Catalina. But, as you can plainly see, its not doing anything, and hasn’t over the past 20 min or so, so you can pretty well forget that it will do anything. A few minutes later, thunder began to erupt from it. I could NOT believe it, as you were thinking as well.  No sign of an anvil, ice, or shaft!  Forecast of no rain going bad….very bad.
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6:34 PM. There it is, on the right, the emergence of the shaft from one of the smallest thundering clouds this writer has ever seen. Within a couple of minutes, Oro Valley below was not visible!
6:40 PM. Looking at Oro Valley!
6:41 PM.  Looking toward Catalina.  The visible sun shows that the intense rainshaft and cloud cover was quite narrow and limited.
6:41 PM. Looking toward Catalina, lower portion.  Its gone.   The visible sun shows that the intense rainshaft and cloud cover were quite narrow and limited.
6:54 PM.  Backside of first dump shown above.  Magnificent!
6:54 PM. Backside of first dump shown above. Magnificent!

But it wasn’t over by a long ways was it?

6:53 PM.  A new, much larger, firmer base has formed in the same spot as the previous storm.  And you KNOW its going to dump on us!
6:53 PM. A new, much larger, firmer base has formed in the same spot as the previous storm. And you KNOW its going to dump on us!
7:01 PM.  What a blast!  This one brought pea-sized hail.
7:01 PM. What a blast! This one brought pea-sized hail to the Sutherland Heights neighborhood.
7:02 PM.  Perhaps the shot of the day of the first evening blast as it moved off past Saddlebrook.
7:02 PM. Perhaps the shot of the day of the first evening blast as it moved over and past Saddlebrook.

 

The End, finally!

Some cloud photos from recent days

Have had little time lately, some problems, too, loading photos in WP, so that’s why.  Looks like the next best chance for rain is Friday into Saturday.  But you already know that from all the TEEVEE weather you watch.

The End.

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From three days ago. Marana/west Tucson got shafted pretty good. At least an inch fell in the core of this beauty. This was after it looked like it was going to be a quiet day west of the Catalinas.

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“Just another day”, pretty much like the day before

Just Another Day“, btw, one of the many great songs by Oingo Boingo, if you’ve ever heard of them.  We’re not just about clouds here.  Trying to broaden your pop cultural knowledge with distractions like this.

Yesterday was remarkable  in how exact it was to the day before in clouds, but ultimately disappoiting.1  There was supposed to be more cloud action, shafting around, that kind of thing, but there wasn’t.  It was virtually identical in every way, including having only two clouds that got high and cold enough to have ice in them. I am sure you recorded them in your cloud diary, and this will be a little tedious as a result, but….what the HECK.

Here is your cloud day for yesterday, focusing on the detection of ice in clouds:

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1:15 PM. Not much going on.
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1:17 PM. Not much going on.
2:44 PM.
2:44 PM.  Not much going on, but nice cloud street.
3:23 PM.  Suddenly,  a narrow erection of cloud shot out of the larger Cumulus mediocris/congestus.  Would it form ice?  I was thinking so, and with that, maybe a rain shaft that could disrupt the wind field and trigger more buildups.  "Here we go," I was thinking, as you were as well.
3:13 PM. Suddenly, an erection of cloud (center at top)  shot out of the larger Cumulus mediocris/congestus. Would it form ice? I was thinking so, and with that, maybe a rain shaft that could disrupt the wind field and trigger more buildups. “Here we go,” I was thinking, as you were as well.
3:14 PM,  Looks pretty firm yet.  No indication of ice.
3:14 PM, Looks pretty firm yet. No indication of ice.  But definitely a few thousand feet higher  and colder than the surrounding cloud.
3:15:30.  Beginning to soften and fall back!  No sign of ice.  Those ragged edges represent the intrusion of dry air into the cloud called "entrainment."  Entrainment is less as the cloud shoots upward and contains vortex rings.  Worried now that this turret was not as high as initially perceived.
3:15:30. Beginning to soften and fall back! No sign of ice. Those ragged edges represent the intrusion of dry air into the cloud called “entrainment.” Entrainment is less as the cloud shoots upward and contains vortex rings. Worried now that this turret was not as high as initially perceived.
3:17 PM.  Stepping back and looking at the whole cloud, the top has been disconnected from the bottom by very dry air between where the top is now, and the lower part of the cloud.  Entrainment has beheaded this cloud!  And, no sign of ice...yet.
3:17 PM. Stepping back and looking at the whole cloud, the top has been disconnected from the bottom by very dry air between where the top is now, and the lower part of the cloud. Entrainment has beheaded this cloud! And, no sign of ice…yet.
3:18 PM.  Not much good up there, with no body, but ice is now visible, and is likely forming, as more of the cloud head evaporates.
3:18 PM. Not much good up there, with no body, but ice is now visible, and is likely forming, as more of the cloud head evaporates.  See that faint ice  veil below the head?
3:21 PM.  I am sure you can see the wisps of ice that this turret contained quite easily now.  Won't do much good decapitated like that.  Huh?  "Decapitated."  Seem to be on a religious theme today.
3:21 PM. I am sure you can see the wisps of ice that this turret contained quite easily now. Ice won’t do much good being decapitated like that with no cloud body to fall through and grow.. “Decapitated.”  Huh?  Seem to be on a religious theme today.  Must be due to that article I read in the Atlantic recently.
3:30 PM.  Twin towers, but like the one over Catalina, it faded into oblivion.
3:30 PM. Twin towers, and like the one over Catalina, it faded into oblivion after getting a little higher than ours, forming more ice.
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4:13 PM. Ever hopeful, but no, never  saw no ice from this tall boy,  phrasing here mindful of that classic new  old folk song, “Never did no wanderin’ ” by The Folksmen.
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7:26 PM. Nice storms elsewhere. Here, looking NE-E.

Today is another day.  More hope for a shower late today or tomorrow, models say, then likely another dry spell as the summer rain season ebbs again for awhile until that possible super hurricane Dolores drags some moisture up this way.  (Dolores, now just a tropical storm, was just born off southern Mexico near the coast.  Will be interesting to see just how strong she gets.

The End

——————-

1Some fans  like to see misspelled words here.  Amyone see that criminal who was sentenced to “life in person” as described in the AZ Star?  That was pretty grate.

Localized trace of rain

Won something of a cloud lottery yesterday. A trace of rain might have fallen only on ME…as a single rain-producing cloud went over my house.   I felt pretty special.    Here’s the story in photos:

3:17 PM
3:17 PM.  Just a cloud, Cumulus one you know, no ice around so no hope for some rain.
3:23 PM.  Ice overhead!!  First ice of day!
3:23 PM. Ice overhead!! First ice of day!  Can you find it?  That’s why I am here, to learn you about seeing ice in clouds, my specialty.
3:23 PM.  Zooming on ice.
3:23 PM. Zooming on ice.
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3:24 PM. Going, going…..
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3:26 PM. Gone. All ice on the left.
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3:27 PM. Base and trunk of cloud approaching! Should be some drops any time! Note cloud street that this Cumulus is a part of, going over Pusch Ridge. This is a pretty common scene when the cloudy air is from the SSW.
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3:30 PM. Drops! Sparse large ones,  representing soft hail (graupel ) or hail that’s melted on the way down. They seem to be falling only on ME! Had just predicted to wife that the fall of large drops was imminent!  Remember, this kind of rain IS NOT DRIZZLE!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!  End of educational module.
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3:31 PM. Drops falling in sunlight here through the trunk of the cloud; you could see them falling from probably 50 feet or so above you. Those little white specks in this photo are those drops. Click on this, then click again to see drops.  Pretty cool, huh?

 Today

Looks like an active photogenic one with dense rainshafts around.  Lots of excitement for weather guys like me.   Hope we get shafted reel good here.

In unrelated matters, an extraordinarily strong hurricane still set to develop off Mexico in the next few days.  If nothing else, surf will be up along the coast of Mexico and southern Cal.   Will let you know when the winds in it have reached 140 mph or more.

The End

Some cloud scenes from yesterday; a forecast map gone awry?

0.07 inches here in Sutherland Heights yesterday afternoon. Much more SW-NW of us, as the photos below show.

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A predicted super hurricane?

I now direct your attention to the forecast maps below, produced by the WRF-GFS model last evening’s global data, courtesy of IPS MeteoStar, the usual.  The aforementioned extremely strong hurricane foretold in the models 24 hours ago, has acheived in this latest run, mythical strength, possibly a Category 6 or 7 (which don’t yet exist).

We presume the model went berserk, so its kind of fun to imagine how intense, how low the pressure in the center of such a goofy predicted hurricane could possibly be in the panels below.

First, the jaw-dropping -to-weather-nerds like the current writer, predicted height of 540 decameters height of the 500 millibar pressure level!  For the pressure of 500 millibars in the atmosphere to be reached at a level that LOW in warm tropical air means that the sea level pressure must be astoundingly LOW to begin with.  In warm air, the pressure doesn’t change as rapidly going up as it does in dense cold air.

I don’t believe, in viewing many weather maps with hurricanes that a height that low has ever occurred at 500 millibars.  Thus, the pressure at sea level, for whatever reason, must be incredible in this predicted hurricane SW of Cabo.  Surf will be up!

The record measured low pressure at sea level is 870 mb in one of the super typhoons (Typhoon Tip) in the Pacific some years ago where winds were estimated at about 200 mph.  It is thought that recent devastating Super Typhoon Haiyan, 2013, had a lower pressure, 858 mb, or the equivalent of the density of air at 5,000 feet elevation was thought to have occurred at sea level!

Valid at 5 AM AST, Sunday, July 19th.
The heights of the 500 millibar pressure level predicted for 5 AM AST, Sunday, July 19th.  The center of the hurricane SW of Baja  is shown to be 5400 meters (540 “decameters”).
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Valid at the time of the above map. The surface pressure lines are too packed to display, but the center pressure would certainly be less than 900 millibars, and in such a tight center, winds, maybe 200-300 mph, tornado-like. Kidding only slightly.

OK, enough fun with a crazy model prediction, though this hurricane will be extremely strong, and the models are still bringing its pathetic, but wet, remnant into California a couple of days later.  Many July rain records, though they are not much to begin with, will be broken if this remnant does make it to Cal.

What we really hope for is some aircraft reconnaissance reports during the life of this strong hurricane instead of satellite-derived estimates of strength (though the latter are quite good).

We still look quite wet during this period, too.

 

The End.

Another Catalina rain day for May 2015

We received 0.08 inches here in “The Heights” for a third day with measurable rain in May already.  0.12 inches fell at the Bridge on Golder Ranch Dr. , while Saddlebrooke got up to a quarter of an inch (as estimated by CMP) in a tiny streak of clouds that erupted into shallow Cumulonimbus clouds, anvils and all yesterday afternoon between 4:30 and 5:30 PM. It was pretty much all over by 6:00 PM,  those shower clouds passing off toward Mammoth.

No rain was reported at mountain sites, to give you an idea of how localized that was, localized practically to Basha’s Market parking lot,  Sutherland Heights’ Equestrian Trail Road,  and Saddlebrooke’s Acacia Drive, to exaggerate some.

The astounding aspect of a tiny line of showers that suddenly erupted over and a little downwind of Catalina was that it was EXACTLY predicted  in the University of Arizona’s 5 AM AST model run yesterday morning, one whose results are available by mid-morning!  So, there would have been a few hours notice of possible rain here in Catalina.

There is no rain predicted in that model run anywhere else except in extreme NW Arizona, just that tiny ribbon of rain right over us, and the U of AZ “Beowulf Cluster” weather calculator got it right.

However, unless you were in the right spot, you might not have even known that it rained, the shower streak was so narrow.

Below, the astoundingly accurate predictions for 3, 4, and 5 PM for that model run from yesterday morning.  No rain whatsoever is shown at 3 PM, as you will see.
3pm

Ann 4pm

Ann 5pmTo be “fair”, NO RAIN was predicted anywhere NEAR Catalina by that same model crunching the data from 5 PM AST the evening before our little rain event, leading CMP to be a little asleep at the wheel yesterday morning, no blog.

Some cloud shots before and as this predicted (or unpredicted, as the case may be) rain began to happen.  Of course, if you want to go to the movies and see this, go here, from the U of AZ:  Yesterday’s cloud movie

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3:23 PM. Looking upwind. Nada going on, clouds to shallow for ice.
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4:04 PM. Hmmmm. Clouds definitely fattening up upwind of us in a nice cloud street from upwind of and over Pusch Ridge to Catalina. Nice scene, anyway, even if nothing happens.
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4:12 PM. Cumulus clouds are looking to gather down there at the corner of Pusch Ridge and Oracle Road, Huh. And they’re heading in this direction. Can ice really form in these guys today?
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4:23 PM. Clouds over and downwind of Pusch Ridge continuing to gather while heading toward Catalina. Looking for ice now or virga, but don’t see any anywhere.
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4:33 PM. Ice begins to show up in even modest clouds! And it started to show up everywhere in the form of virga. But then then the virga became thin shafts all the way to the ground. Cloud Maven Person is beside himself, but must go indoors for a social engagement!  Those of you who fancy yourselves as Cloud Maven Juniors, should have recorded this sighting of “first ice” in your cloud diaries for yesterday.
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Also at 4:33 PM. Ice is now readily visible in that Cumulus mediocris massing upwind of Catalina and is not about over the south part of the Catalina CDP (“Census Designated Place” that might one day be absorbed by Oro Valley, rumour has it.)
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4:41 PM. Just minutes before the first drops fall in Saddlebrooke, and CMP’s last photo of this incoming masterpiece of weather forecasting and little rain band; he can no longer comfortably jump up from dining room table in mid-conversation to say he has to pee again whilst actually taking a photo. You can only say you have to pee so many times in 10 minutes and still have your credibility intact. But, how can you say repeatedly, “I have to go look at some clouds?”, so I can’t hear the rest of your quite interesting story……”  Really came down for a couple of minutes several times there in Saddlebrooke between a quarter of five and 6 PM as one little raining cloud formed after another in this cloud stream.

Below,  sat view of this cloud streamer with radar, from IPS MeteoStar.  The image below is at the same time as the last photo above:

Satellite and radar imagery for 4:40 PM AST.
Satellite and radar imagery for 4:40 PM AST.  Note the many lines of clouds running almost due south to north into SE AZ from Mexico.

Here some more cloud stuff from the sounding launched at the U of AZ around 3:30 PM AST.

The TUS balloon sounding ("rawinsonde") for yesterday afternoon.  Looks like most tops were dabbling with the ice forming temperature of -10 C, but the sounding suggests that somewhat deeper tops could easily have arisen (and did!).  Interestingly, the model "knows" when ice forms, and it must have "known" that the ice-forming temperature was going to be surpassed in that little cloud line coming off Pusch Ridge.  Astounding, for the Nth time.
The TUS balloon sounding (“rawinsonde”) for yesterday afternoon. Looks like most tops were dabbling with the ice forming temperature of -10 C, but the sounding suggests that somewhat deeper tops could easily have arisen (and did!). Interestingly, the model “knows” when ice forms, and it must have “known” that the ice-forming temperature was going to be surpassed in that little cloud line coming off Pusch Ridge. Astounding, for the Nth time.  Bases were pretty cold, 0 C (32 F).

Here’s a diagram of when ice forms in the type of clouds we mostly have in Arizona, “continental” ones with high droplet concentrations, and when ice should form in them.  As you can see, ice should form in them soon after the top temperature gets colder than 10 C WHEN the base temperature is about what it was yesterday.

 

From a survey of the onset of ice formation in continental clouds by Rangno and Hobbs (1995)1
From a survey of the onset of ice formation in continental clouds by Rangno and Hobbs (1995)1

 

“CMP” is not mentioning it at all, but yesterday was another kind of mucked up sky, not a Catalina postcard sky,  with lots of aerosols making the sky a whitish-blue, the lower aerosol stuff again from Mexico, but there was also a layer far above the cloud tops, likely a long-range transport event from thousands of miles away.

This higher haze layer still seems to be around if you look toward the horizons right now (5:59 AM).

We’ll be between two jet streams today, kind of a jet stream sandwich, and the stronger one is now approaching from the northwest with that mega upper low over Cal.  That means no rain today, subsidence rules, though we’ll have small, non-ice producing Cumulus, and likely some Altocumulus lenticulars, maybe a Cirrocumulus patch here and there.  Should be a pretty nice day for cloud photos, haze aside.

The best chance for rain is still after midnight tonight into mid-day tomorrow as the core of the stronger jet stream goes just about over us.  Still thinking a tenth of an inch will occur here, though mod run from the U of AZ at 5 PM completely dry.   A little snow likely on Ms. Mt. Lemmon, too!

The End, FINALLY!  Brain empty.

———————————-

1From “A New Look at the Israeli Cloud Seeding Experiments.”

 

 

 

Loud May rain totals 0.47 inches in Sutherland Heights, Catalina

After last evening’s surprisingly heavy rain, we have now met our average for May for Catalina, having received 0.47 inches of rain over the past 24 h, some 0.36 inches during some house-shaking thunderclaps last evening.

Below are the 24 h local totals, ending at 4 AM today from the Pima County ALERT gauges rolling archive , these totals pretty much capturing all of our beautiful storm:

    Gauge    Location
    ID#    
    —-     —-       —-        —-       —-         —-       —————–            ———————
Catalina Area
    1010     0.63      Golder Ranch                            Horseshoe Bend Rd in Saddlebrooke
    1020     0.83      Oracle Ranger Station          approximately 0.5 mi SW of Oracle
    1040     0.55      Dodge Tank                   Edwin Rd 1.3 mi E of Lago Del Oro Parkway
    1050     0.75      Cherry Spring                approximately 1.5 mi W of Charouleau Gap
    1060     0.79      Pig Spring                   approximately 1.1 mi NE of Charouleau Gap
    1070     0.39      Cargodera Canyon             NE corner of Catalina State Park
    1080     0.63      CDO @ Rancho Solano       CDO Wash NE of Saddlebrooke
    1100     0.35      CDO @ Golder Rd              CSO Wash at Golder Ranch Dr

Santa Catalina Mountains
    1030     1.18      Oracle Ridge                 Oracle Ridge,  1.5 mi N of Rice Peak
    1090      0.35      Mt. Lemmon                   Mount Lemmon
    1110      1.34      CDO @ Coronado Camp          CDO Wash 0.3 mi S of Coronado,       1130          0.83      Samaniego Peak               Samaniego Peak on Samaniego Ridge
    1140      0.79      Dan Saddle                   Dan Saddle on Oracle Ridge
    2150     0.24      White Tail                   Catalina Hwy 0.8 mi W of Palisade RS
    2280     0.24      Green Mountain               Green Mountain
    2290      0.12      Marshall Gulch               Sabino Creek 0.6 mi SSE of Marshall Gulch

For more rainfall info, go here and here.  And here to the USGS, too, not to mention the NWS rainfall tables.  Too bad they can’t all be in one gigantic table!

The clouds and weather just ahead

A little cold morning rain, and even snow on The Lemmon, is looking likely for Saturday morning.  Presently, the core of the jet stream at 500 millibars or around 18,000 feet associated with a  mighty upper cold low that sits on Arizona on Saturday is forecast to be south of us (as was yesterday’s jet), a pretty black and white discriminator for cool season (Oct-May) rain here.

However, if that jet core around the low does not circumscribe TUS, you can forget rain.  From IPS MeteoStar, this rendering of the upper level configuration for Saturday morning, showing that it WILL circumscribe TUS:

The 500 mb heights and winds predicted for 5 AM AST, Saturday morning, May 10th. Its gonna a cool Mom's Day, too.  One would expect rain here in Catalina with this configuration.  Note how max winds are in a band well south of us.  That banding circumscribes the deeper parts of the Pacific moisture that came in with this trough.
The 500 mb heights and winds predicted for 5 AM AST, Saturday morning, May 10th. Its gonna a cool Mom’s Day, too. One would expect rain here in Catalina with this configuration. Note how max winds are in a band well south of us. That banding circumscribes the deeper parts of the Pacific moisture that came in with this trough.  This rendering is from the global crunch of data taken at about 5 PM AST, yesterday evening.  These runs are updated every six hours.

In the meantime, “troughiness” today,  tomorrow and Thursday, with secondary jet stream to south of us,  will give us some more photogenic high-based  Cumulus, maybe with some with virga in the afternoons.    Today, as our upper low says goodbye, subsiding air is supposed to keep clouds from attaining tops high and cold enough to form ice.   So, no rain today.

Yesterday’s clouds (going deep, as in pedantically)

There were some great scenes yesterday, summer-like ones, odd for May here, with massive rainshafts as the cloud bases lowered, reflected a huge jump in surface dewpoints to summer-like values in the mid-50s.  Cloud bases yesterday morning, riding the tops of Samaniego Ridge, were near 7 C, compared with -5 C the afternoon before.

This warming of  cloud bases greases the precipitation “wheel” since clouds with warm bases are be able to rain easier than ones with cold bases (say, near or at below freezing temperatures).   Droplet sizes have to be larger at any given level above cloud base compared to the clouds of the day before since more moisture is forming in those updrafts at the higher base temperature.    And, oddly, the larger the droplets, the higher the temperature at which ice can begin forming in clouds.    And when ice forms, snow, then rain, come out the bottom.

To go on too long on this in covering all rain possibilities for yesterday,  a base temperature of 7 C here is on the edge of being able to produce droplets big enough so that some begin colliding with one another and sticking together so that drizzle, then raindrops can form, a couple to a few thousand feet above cloud base, and those sizes of drops can really accelerate the formation of ice and then rain out the bottom.  Are there any readers left?  I doubt it.

Let us go even deeper….  It was hazy, smoky looking yesterday most of the morning, even when some good thunderstorms formed.  So what?  Well, smoke is bad for storms.  Remember when it was reported by Warner and and the U of Arizona’s own Sean Twomey (1967) that sugarcane burning made it stop raining downwind from those fires in Australia?   That effect has been verified in satellite measurements by cloud seeding nemesis, Danny Rosenfeld2 of the HUJ in Science a few years ago.

Well, too much smoke can choke droplet sizes down and inhibit the formation of rain by collisions, and delay the formation of ice.   And so we had that counter effect of smoke from somewhere, maybe LA this time since it was in the boundary layer, not aloft like that smoke layer from Asia was a couple of weeks ago.

So, cloud microstructurally-spekaing, it was an especially interesting day, one, if he were cloud maven person, wishes he would have had an aircraft to sample them.

But let us look now and see what all the fuss is about:

5:40 AM.  Dewpoints in the 50s, Stratocumulus clouds top Samaniego Ridge!
5:40 AM. Dewpoints in the 50s;  Stratocumulus clouds top Samaniego Ridge!
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6:41 AM. Soft-serve Cumulonimbus forms over west Tucson, Oro Valley. Icy top looks like its comprised of needles and hollow sheaths to me, ice that forms at relatively high temperatures for ice formation, higher than -10 C.
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6:42 AM. In the meantime, drama over Oro Valley to the west and north of Catalina as a deeper cloud unloads. Thunder, too.
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7:19 AM. Haze and rain. This was a pretty astounding sight, so much haze/smoke in the rain as evidenced by these intense crepuscular rays.
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8:19 AM. A real summer-looking sky on a big rain day. Frequent lightning was emitted by this behemoth that went on to pound Saddlebrooke.
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8:37 AM. Unusually strong May thunderstorm pounds Saddlebrooke.

3:42 PM.  In spite of lots of convection and scattered Cumulonimbus clouds, the sky remained almost an eastern whitish due to smoke.
3:42 PM. In spite of lots of convection and scattered Cumulonimbus clouds, the sky remained almost an eastern whitish due to smoke, which I will blame on southern California, absent any facts or investigation.  No time.
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6:59 PM. Our major evening rain and thunderstorms were developing upstream.

The End

 

 

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1Warner, J. and S. Twomey, 1967: The Production of Cloud Nuclei by Cane Fires and the Effect on Cloud Droplet Concentration. J. Atmos Sci., 24, 704–706.

2Rosenfeld a “nemesis?”    See  the references and discussion below for kind of an interesting science story aside….

Rangno, A. L., and P. V. Hobbs, 1997a: Reply to Rosenfeld. J. Appl. Meteor., 36, 272-276, and…..

Rangno, A. L., and P. V. Hobbs, 1997b: Comprehensive Reply to Rosenfeld, Cloud and Aerosol Research Group, Department of Atmospheric Sciences, University of Washington, 25pp.

With the publication of voluminous (en toto) commentaries/critiques in 1997 by a few of our peers, but mainly by Danny Rosenfeld of the Hebrew University of Jerusalem, that concerned our 1995 paper reanalyzing the Israeli randomized experiments, yours truly and Peter V. Hobbs,  had attained, according the the Technical Editor of the Journal, the status of having become the most criticized meteorologists in the history of weather–well, in the history of the Amer. Meteor. Soc. journals, anyway!  How fun is that?  Its fun.

Our findings, that the two benchmark Israeli randomized cloud seeding experiments conducted in the 1960s and 1970s were largely misperceptions of cloud seeding effects due to storm biases on seeded days,  were independently verified in peer-reviewed publications by researchers at Tel Aviv University some many years later.

Operational cloud seeding has ended in Israel in favor of more fruitful avenues for obtaining the water they so badly need.

TSTMS overnight and this morning drop 0.11 inches

Well, it could have been more I suppose; some areas of central and northern Arizona have gotten between a half an inch and an inch of rain overnight.  Nevertheless,  it was great that a passing thunderstorms (“TSTMS” in weather texting) happened here in Sutherland Heights overnight, fabulous, really.    Dropped 0.28 inches on Mt. Lemmon, btw.

More scattered showers, and maybe a thunderstorm or two, should develop today.  Keep cameras well-oiled  for some great cloud scenes.

Yesterday’s clouds

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8:04 AM. In the beginning….. Unlike the day before, our shower clouds didn’t move in, but rather had to start from something akin to poppy seeds.   Still water highlights on Samaniego Ridge.
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12:06 PM. Cumulus increase in size and number. No ice yet.
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2:14 PM. First minute amount of ice begins to show up underneath downstream cloud portions. You’ll have to be awfully good to find it!
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3:37 PM. Ice, and now well-developed virga, is plentiful in many of these shallow clouds.
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4:00 PM. Numerous light rainshowers and glaciating shallow Cumulus clouds dot the horizon to the SW,
6:58 PM.  Shows the fine structure of virga, trails that can be only 5-20 feet wide as they drop out of a cloud.  Seems like a nice scene, too.
6:58 PM. Shows the fine structure of virga, trails that can be only 5-20 meters wide as they drop out of a cloud.  Strands like this are usually soft hail, or what we call “graupel.”   Snow virga like this tells you that cloud bases are well below freezing, and on a warm day are very high above the ground.  Yesterday’s late afternoon cloud bases were up around 14 thousand feet above sea level, at about -5 C (23 F).   The virga melted into raindrops behind the cloud below it.

 

7:04 PM.  A light rainshower advances on Catalina.
7:04 PM. A light rainshower advances on Catalina.  Where the pinkness disappears below the main cloud base is where the snow  virga is melting into less visible raindrops.
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7:06 PM. Another fiery sunset highlight involving a Cumulonimbus cloud. Cloud tops were beginning to deepen noticeably by this time.

The End

A cool May ahead?

Well, let us define “cool”….that is, cool for Catalina in May; that is #2, below normal temperatures.

What led to this thought?

I was gasping when I saw this from last night’s NOAA spaghetti factory, as you will as well, and decided I would have to say something about it.

Valid on the 17th of May, 5 PM AST. Wow! And with a persistent pattern like this (red lines dipping so far toward the Equator (which is that dashed line that goes through Hawaii and Mexico1), which we now seem to be in following our little warm up, now in gradual retreat, big flooding will occur in the central and southern Plains States, the kind that makes the 5 o'clock news (or is it 6 o'clock?). Wow.
Valid on the 17th of May, 5 PM AST. Wow! And with a persistent pattern like this (red lines dipping so far toward the Equator (which is that dashed line that goes through Hawaii and Mexico1), which we now seem to be in following our little warm up, now in gradual retreat, big flooding will occur in the central and southern Plains States, the kind that makes the 5 o’clock news (or is it 6 o’clock?). Wow.

Pretty unbelievable.

What does it mean for Catalinans: a personal view?

Oh, big windy episodes from time to time during the month, good chance for above normal rain for Catalina, and probably most interesting, the late spring ovenly weather that we like to brag about how we get through wherein so many of our Catalinans and “Tucsonians” flee to the high country,  or to Michigan, is held at bay by recurring puddles of cold air up top.

That’s my prediction for May, which has already been ludicrously posted in a prior post many days ago.  We might look back at May some day to see how this incredibly unprofessional forecast for a whole month based on one spaghetti run worked out.

If you want professionalism in medium range weather forecasting, then get the hell off this site now!  Maybe you’re the kind of person that would rather see a forecast from the NOAA Climate Prediction Center for Catalina and environs.  If so, you don’t belong here.

But lets see what they say, anyway for May, then for the whole of mid-April through July…..to add that bit of uncharacteristic professionalism to this site.  See maps below:

 

off15_temp
Looks like they’re pretty clueless about what the temperature’s going to be like here for May–“EC” means equal chances for below normal OR above normal.  So, they could be right no matter WHAT happens!  But not me.  I think Cal is goona be wrong, too; below normal, not above normal temps.  Its great when you can just type things like that!

off15_prcpThe Big Boys don’t really know what’s going to happen with the May rain here, either, since we are also in an “EC” area.  But boy, look at the May rain foretold for the Plains!  Looks like a great place to spend May!  OKC, maybe.   WCWS begins at the end of May, amateurism at its best.

But, at the same time, for the whole of mid-April through the end of July, the Big Boys at the CPC are expecting the drought in areas of the  central southern Plains States to persist or intensify–see dark brown areas below.

It will be interesting, being serious for the moment, to see how these predictions, seemingly in some conflict,  work out.  Note that in the longer view below, Catalina is in an area where drought “persists or intensifies”, even through JULY!  Egad.

Valid for May, issued in mid-April.

 Nice clouds yesterday….

 

6:00 AM.  Mamma to the S.
6:00 AM. Mamma to the S, pretty big mamma.  Indicates unstable conditions aloft, maybe some showers will reach the ground.
10:01 AM.  Heavy vIrga pummels air above Catalina/Saddlebrooke.
10:01 AM. Heavy vIrga pummels air above Catalina/Saddlebrooke.
4:20 PM.  High-based Cumulonimbus clouds approached from the south promising blasts of wind, maybe a few drops.  No drops here, though.
4:20 PM. High-based Cumulonimbus clouds approached from the south promising blasts of wind, maybe a few drops. No drops here, though.
6:47 PM.  Cumulonimbus and rain reaching the ground passed to the W-NW of Catalina.  Darn.
6:47 PM. Cumulonimbus and rain reaching the ground passed to the W-NW of Catalina. Darn.
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7:04 PM. The moon AND pink virga in the SAME photo! Yours today for $900. Trying to follow through on an Atlantic Mag article, “Blogging for Dollars.” That would be great, but it hasn’t happened yet.
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7:09 PM. Your Catalina sunset, May 2nd, 2015, Altocumulus castellanus with Cumulonimbus capillatus, along with a Cal palm silhouette.

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Yeah, I saw that report that America’s kids don’t know much about geography, so we’re just checking here to see how bad it really is by suggesting that the Equator goes over the Hawaian Islands (hahaha).  But, maybe, they’re really the Galapagos Islands…    Am I being too subtle?     Sam Cook once pointed out about himself,  “Don’t know much about geography”…in his song, “What a wonderful world it would be“.   it was a movement that apparently caught on.