Clouds larger than expected; and a travelogue about areas where historic July rains fell

First, yesterday’s sunset:

7:14 PM. Residual Cumulus and Stratocumulus supply targets for fading sunlight.
7:14 PM. Residual Stratocumulus clouds supply targets for fading sunlight.

Some pie, H-pie: Whereas a modest push of moisture into Tucson and central Pima County was deemed insufficient to produce rain here yesterday, some drops DID fall here producing a trace late yesterday afternoon.

But some areas of the Catalinas got clobbered with White Tail, over there around Sabino Canyon, collecting 2.17 inches (!) and Samaniego Ridge over thisaway, 0.47 inches, the latter from a pile of Cumulus congestus clouds that blossomed into a Cb with a dense rain shaft right before the writer’s eyes. This after he had opined to his wife that he doubted those dark clouds would rain on the western side of the Catalinas…. Hmmmm.

They thundered and rained a plenty, and the wind that came out of that shaft dropped the temperature some 15 degrees here in Sutherland Heights with wind gusts to more than 35 mph. Furthermore, that outflow, spreading out across Oro Valley and parts NW, and went on to launch one new thunderstorm north of Saddlebrooke, which was very nice, of course. Didn’t think that would happen either as very dry air was working its way in already from the SW.

As the clouds massed over Catalina-Sutherland Heights, was returning from a fabulous tour “investigating” the results of 8-12 inches of rain in Jul of the area around Sierra Vista-Fort Huachuca along HWYs 90 and 92 then through Coronado National Memorial Park (about 10 inches fell at Visitor’s Center in July), then over Montezuma Pass (6575 ft) and on to Sonoita.

Holy Smokes was that gorgeous; highly recommended. Traveling down HWY 90, With Stratocumulus topping the green, forested Huachuca Mountains, and the green in the foreground, one thought of Hawaii. Some photos from that trip FYI. It’ll be a LONG time before this happens again! Also, some summer wildflowers are in display as well.

10:12 AM, Sierra Vista.
10:12 AM, Sierra Vista.
10:20 AM, Sierra Vista. Some kind of flower. I am a cloud maven, not a flower maven.
10:20 AM, Sierra Vista. Some kind of flower. I am a cloud maven, not a flower maven.
11:13 AM. Entrance sign to the Park, in case you didn't believe that I went there to see the effects of a lot of rain.
11:13 AM. Entrance sign to the Park, in case you didn’t believe that I went there to see the effects of a lot of rain.
11:13 AM. Another view going in, one from the viewpoint of driving on the wrong side of the road for the purpose of startling you, getting your attention here.
11:13 AM. Another view going in, one from the viewpoint of driving on the wrong side of the road for the purpose of startling you, getting your attention here.
11:22 AM. Raingauge at the CNP Vistior's Center. I thought you would like to see that. Looks a little too enclosed by vegetation unless the rain is falling straight down.
11:22 AM. Rain gauge at the CNMP Vistior’s Center. I thought you would like to see that. Looks a little too enclosed by vegetation, and unless the rain is falling straight down. If its windy, its likely to under catch the precip.  Should be in an opening twice the distance as the nearest high thing, something like that, quite an opening.
11:55 AM. View of small Cumulus from the top of Montezuma Pass in the CNMP.
11:55 AM. View of small Cumulus from the top of Montezuma Pass (elev. 6575 ft) in the CNMP.  Temp was 81 F is all.
12:07 PM. A view of the Pass environs, with moderate-sized Cumulus clouds.
12:07 PM. A view of the Pass environs, with moderate-sized Cumulus clouds.  So green.
12:24 PM. Another flower of some kind, who knows what? There were a lot of these things on the way down toward the west.
12:24 PM. Another flower of some kind, who knows what? There were a lot of these things on the way down the Pass toward the west.
12:56 PM. Hell, its beginning to look like KS here. What is with that? Also, it was disheartening not to see any cars for long stretches, cars containing people looking at the effects of an historic July rainfall.
12:56 PM. Hell, its beginning to look like KS here. What is with that? Also, it was disheartening not to see any cars for long stretches, cars likely containing people looking at the effects of historic July rains.
4:52 PM. Blast of wind came about ten minutes later.
4:52 PM. Got back just in time to see this thunderstorm develop.  The blast of wind came about ten minutes later.  A day doesn’t get better than this one.

 

5:45 PM. So pretty!
5:45 PM. So pretty, this Cumulonimbus northwest of Saddlebrooke resulting from the outflow from the rain shaft shown above.

Hot dry days ahead for awhile, as you know.  May have to generate some filler material….

The End.

Afternoon clouds smaller than expected

Yesterday at this time it appeared that we had a good chance of a few high-based Cumulonimbus clouds with some virga and the chance of a sprinkle making it down to the ground.  Well, the precipitating clouds were even higher than expected, but with some nomenclature razzle-dazzle, I think we can say that the forecast of Cumulonimbus clouds in our domain did, in fact,  verify.  Below, the first use of the cloud descriptor, “Nanocumulonimbus.”

6:57 PM. Zoomed view of Nanocumulonimbus capillatus producing snow flurry as it drifted toward Catalina.
6:57 PM. Zoomed view of “Nanocumulonimbus capillatus” or maybe “calvus” (center; too small to tell which species for sure) producing a snow flurry aloft (virga)  as it drifted toward Catalina.

The early morning clouds were spectacular full of promise for yesterday, promise that went mostly, well, entirely really, unfulfilled. Here are those sweet morning clouds, more like Altocumulus castellanus, though some reached sizes that they would have to be termed, Cumulus congestus and Cumulonimbus, the latter with some virga and light rainshowers to the ground.

5:51 AM. Distant Cumulus congestus or Cb calvus NNW of Catalina. Held a lot of promise for the remainder of the day. But was just too dry in the end.
5:51 AM. Distant Cumulus congestus or Cb calvus NNW of Catalina. Held a lot of promise for the remainder of the day. But was just too dry in the end.
SONY DSC
5:51 AM Tall, sunlit Altocumulus castellanus line SSW of Catalina.

 

6:04 AM. I thought this was a great scene because that little wedge of brilliant white tells you that one turret from this grouping has shot many thousands of feet higher into the thinner air where the sun's light has not been diminished by the passage through the lower denser atmosphere. Very pretty I thought.
6:04 AM. I thought this was a great scene because that little wedge of brilliant white, center, tells you that one turret from this grouping has shot many thousands of feet higher into the thinner air where the sun’s light has not been diminished by the passage through the lower denser atmosphere that results in the brownish colors of the surrounding clouds. Very pretty I thought.

Today’s clouds

U of AZ WRF-GFS mod thinks there’s a better chance of showers and thunderstorms here in Catalina today, but this is dependent on a easterly surge of moist air this morning. Don’t get your hopes up too much, since we’re kind of on the westerly edge of this surge, and then it goes away. SO, everything really has to come together, and right now, our dewpoints are really down (37 F here) and the moist air is still east of TUS. But, as you know, some of the fun of weather forecasting is weather watching and seeing what Nature is actually going to do.

The weather way ahead

Mod outputs, including spaghetti plots, not looking that great for a full resumption of our summer rain season.
But, with a trough tending to recur along the West Coast in these plots, there’s the chance of a tropical storm being steered this way late in the month. Hey, remember August 1951? Maybe that will happen again in AZ to make August a more respectable rain month after sputtering most of the month…. Dreaming, of course, of the unlikely.

The End.

Ice with them clouds

Not expected by this brain yesterday, but several of those many more Cumulus clouds than expected also fattened up to heights where ice began to form, also not expected.   As you know, that means precip fell out, at least up there.  As a weatherman-cloud person, there are always surprises every day (!) to delight and disappoint you. Its quite and exciting life we lead.

How cold were those tops?

Well, you know, colder than -10 C on a day with very high and COLD cloud bases1.   How high and cold were the cloud bottoms yesterday.  Oh, about 0 C (32 F, of course) at 14,000 feet above the ground, 5,000 fee above Ms. Mt. Lemmon, the taller tops extruding upward to between -15 C and -20 C (5 F to -4 F), about right for the amount of ice that developed, “eyeballed” concentrations of a few to 10s per liter of air in those clouds (for size, think of a liter size plastic bottle of Bud Light with some ice crystals in it).  (Remember, a LONG time ago in another area of the Universe2,3, Mr. Cloud-Maven Person flew into such clouds with instruments aboard his Cloud and Aerosol Research aircraft and can say things like this with what appears to be some authority.)

Here are those clouds from yesterday, which I am sure you logged with excitement in your weather diaries:

2:55 PM. While out plant shopping at DS (Desert Survivor) this. Can you find the dead completely glaciated turret remains?
2:55 PM. While out plant shopping at DS (Desert Survivors Nursery) this. Can you find the dead completely glaciated turret remains?

 

3:57 PM. OK, I'm making it easy on you here to find the ice. Wasn't there a song like that back in the 60s? "Make it easy on myself, oooo?"
3:57 PM. OK, I’m making it easy on you here to find the ice. Wasn’t there a song like that back in the 60s? “Make it easy on myself, oooo?”  I will look on the internet; it has everything!

 

4:59 PM. Largest of the the ice-producing Cumulus virgae, or are they, having precip, Cumulonimbus mediocris. I like the latter better.
4:59 PM. Largest of the the ice-producing,  “Cumulus virgae”, or are they, having precip, “Cumulonimbus mediocris.” I like the latter better, not that you would care that much.

 

7:18 PM. Nice sunset, though.
7:18 PM. Nice sunset, though.

Today the cloud bottoms are 1,000 feet lower than yesterday afternoon.  But is it a diurnal effect where bases are always lower in the cool mornig (“morning”;  intentionally spelled wrong to see if you’re paying attention) than in the afternoon? BTW, if you like soundings, go to the “Happy State of Wyoming, the nation’s happiest4, to see all the soundings you want at the University of Wyoming

But, we have a windshift in the middle levels traipsing over us late this afternoon (U of AZ TUS sounding forecast here), and that will be, we hope, something like a fork lift;  help to push cloud tops up just it goes by.  (However, I can find no evidence of such a windshift in larger scale models, so MAYBE I have mistaken a diurnal shift induced by our mountains as a “trough”.  A trough would be a lot better, a diurnal turning of the wind, not so great a weathermaker. Another one of those “surprises”; they can come from all quadrants.

SO, high based Cumulus, some growing into Cumulonimbus clouds here and there, with some sprinkles because the bases are too high for a really good rain.  But,  hey, if you want a really good forecast, not a crummy one like this, see Bob and the NWS.

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1Remember cloud bases can be cold, but NOT temperatures, which are high and low.  The AIR is warm and cold.)

2Remember the solar system is speeding along (45,000 mph or so) in the Universe around the Milky Way Galaxy to god knows where (the constellation Hercules, according to the Stanford Solar Center).

3Quite fond of footnotes; they add a scholarly aura to trashy writing like this.

4OBJECTIVE HAPPINESS BY STATE  We’re not THAT happy in AZ, BTW, but people are really happy in Wyoming, Montana, South Dakota.  Huh.

Distractions from disappointments; so many yesterday

Thought maybe a nice distraction from yesterday’s rain disappointment would be looking at some file boxes from the University of Washington’s Atmos. Sci. basement.  This shot taken a couple of days ago.

Enjoy thinking about what might be in these boxes, and what you would do with the contents.  Have some extra coffee, talk it over with friends, think about how much you might offer if one of these boxes was something on a quiz show, and you had one thing you knew what it was, but had to take your chances on what might be in one of these boxes1?  Or if saw them in storage locker you were bidding on.  How much?  Lots of possibilities to think about.

Taken a couple of days ago. They have stuff in them, unlike our clouds of late.

———weather part——

You started to get a bad feeling about yesterday, in spite of the juicy clouds on Samaniego Ridge, bases around 15 C, extremely warm for AZ, meaning full of extra condensed water compared to our normal clouds, when the north wind began to blow, and the temperature was struggling to go beyond 80 F.

Usually, when the cloud bases are low, it doesn’t take a LOT of heating to power them up into Cumulonimbus (Cbs) clouds because the condensation itself releases heat.  But struggling to reach 82-83 F here was just too little heat.

Late in the afternoon we did have a nice, if weak, Cb on the Cat Mountains (no thunder, of course, it was that weak).   They did get half an inch on top of Mt. Lemmon and a couple of other places, so at least SOME rain fell near us.

And, not only did we have the “juice”, high amounts of water in the atmosphere over us, but also a nice cyclonic swirl passed overhead yesterday, too, something we normally look to cluster Cumulonimbus clouds into large groupings with major rains.  From the U  of WA, you can see it go by here.

To finish off thoughts of yesterday, some mood music to go along with those thoughts, I would like you to now hear covers of “pretty songs” by the Circle Jerks.

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Here are your clouds from yesterday, I know you’ll want to see them again, mope around some more about what could have been.  We will begin our review of yesterday’s clouds with today’s morning rainbows:

6:00 AM.
6:00 AM.  Sloping rain shaft tells you that the drops are very large, rain not too heavy.
6:02 AM. Bow over the Oro.
6:02 AM. Bow over the Oro.
11:03 AM. Those oh so promising Cumulus congestus clouds lining the Catalinas!
11:03 AM. Those oh so promising Cumulus congestus clouds lining the Catalinas!
4:19 PM. Finally a Cumulus congestus that looked like it would exit the juvenile stage and mature into an adult (Cumulonimbus).
4:19 PM. Finally a Cumulus congestus that looked like it would exit the juvenile stage and mature into an adult (Cumulonimbus).
4:36 PM. And it did grow up. This is what produced the half inch on Ms. Lemmon.
4:36 PM. And it did grow up. This is what produced the half inch on Ms. Lemmon.

 

No real chance of rain now for a few days. Oh, me.

The End.

 

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STAR WARS AND rEAGAN
From 30 years ago or so…. Wonder what historians would say now?

1Example of a quiz show where you bit on a mystery box if you want, or take the thing that’s offered in front of you.

A little rain overnight! 0.09 inches!

Let us first begin first by NOT exulting too much over our own rain, but let us revel in that rain that has fallen in the Plains.  New Mexico, too.  From WSI Intellicast this beauty for the past 7 days:

A radar-derived sum of the rain that has fallen in the past seven days over the USA. Please observe the orangy areas in Kansas, indicating 8-12 inches!
A radar-derived sum of the rain that has fallen in the past seven days over the USA. Please observe the yellowish and orangy areas in Kansas, indicating  that between 8-16 inches has fallen!  Oh, my.  Let us remember, too, that July and August are supposed to be relatively dry months in these areas; the wetter times in May and June.

Below is our national drought status at the onset of the week above (for July 30, 2013), and indicates why so many of us should be thankful for this past weather week:

The national picture of drought as of July 30, 2013.
The national picture of drought as of July 30, 2013.  It will be updated later today.

 

Here are some area-wide 24 h totals, ending now,  from the Pima County Alert system.

Yesterday’s clouds

Well, they didn’t get so big, so soon over the Lemmon, as foretold by one model referred to yesterday, but there was something later in the afternoon near the top of Lemmon. Can you detect whether that the turret shown below is mostly “glaciated” or not? You know, that’s why I do this, to learn you up on clouds and when they got ice and therefore are precipitating out the bottom even though here you can’t see the bottom. It all for YOU. Its no problem for me, of course.

4:27 PM. A Cumulus turret has protruded above the others behind Ms. Lemmon. If it glaciated, it might be better be termed the head of a Cumulonimbus calvus ("bald") and would have rain underneath it.
5:04 PM. A Cumulus turret has protruded above the others behind Ms. Lemmon. If it’s glaciated, it might be better be termed the head of a Cumulonimbus calvus (“bald”) and would have rain underneath it.  What do you think?  Only the C-M knows for sure.  Sounds like something from a radio program I’ve heard somewhere.  But, you should try anyway.  Answer at the bottom if I remember to put it there.
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6:31 PM, Swan and Trotter, with metaphorical “Dead End” road sign, lower right.
While to the uninitiated this Cumulonimbus capillatus anvil may have appeared to be heralding a storm, overspreading the Catalina sky the way it was, the lack of cumuliform portions, the fraying edges, not hard ones, indicated it was in its dying phase.  Photo of anvil with metaphorical sign; yours for $2,000 (more than usual because some mental effort was expended).  Now that I am thinking about money, I think I will demand a million dollars to continue blogging, and see what happens.

 

SONY DSC
2:47 PM. RIght here you knew that the model run that had an echo by 3 PM on Ms. Lemmon was going to be off as we see but a Cumulus mediocris forming after the usual mid-day clearing.

 

Nice sunrise this morning….

5:48 AM today. Sunrise over the Charoleau Gap.
5:48 AM today. Sunrise over the Charoleau Gap.  Mulitple layers of Altocumulus, some fine virga.

 

Another morning of remnant rains moving through right now, rather than the full blast. As usual, these clouds and rain showers are likely to be dissipating in the later morning before doing much.

Looks like one last day of possible big showers here….check this out from the U of AZ, 11 PM run (WRF-GFS mod)..  Lets hope so, cuz its gonna be dry after this for a few days.

The End.

At the risk of repeating myself…

…says the sky on August 5th, referring to almost the exact same sky as on August 4th at this time.  Also, both days had OCNL LTG (texting “occasional lightning” here in weatherspeak) off the to distant NE, unusual for this time of day.   Even heard thunder this AM.

Below, which shot is from today, just now, and which boring shot of “stratiform” debris clouds from complexes of Cumulonimbus clouds that have dissipated instead of arriving here full strength boo-hoo is from yesterday?

7:02 AM, August 4th. Altocumulus castellanus deck with Altostratus cumulonimbogenitus (watch out how you pronounce this in mixed company).
6:07 AM, August 5th. Altocumulus floccus/castellanus deck with Altostratus cumulonimbogenitus (watch out how you pronounce this in mixed company).

 

7:00 AM, August 4th. Altocumulus castellanus deck under Altostratus cumulonimbogenitus.
7:00 AM, August 4th. Altocumulus castellanus deck under Altostratus cumulonimbogenitus.

So what’s the routine now? Gradual thinning with isolated showers, ones that also eventually disappear, followed by brighter skies, and growing of Cumulus clouds like desert weeds in July after the first rain. You’ll have noticed by this time that was a cloud scruff (Stratus fractus) on Ms. Lemmon today, indicating that the moisture is enhanced today over yesterday when the bases were appreciably above Ms. Lemmon. So, a better chance of rain, sans any model glimpses, but then since rain was very sparse yesterday, except for that 2 inches that fell in the mountains S of TUS yesterday afternoon (1.61 inches measured at the Florida Canyon Work Center), almost anything would be an enhancement of a rain chance here over yesterday so I have fudged some words here.

What happened to produce all these dense, morning clouds the past two days? Cloud gigantism in northern Mexico last evening and overnight. Must have had a TON of precip in these complexes that just exploded down there, inches of rain no doubt fell. Sure wish we had some reports under these magnificent blow ups. There are quite a few rain measuring stations in Mexico, but that data is not available from remote areas until they’re published. Here’s a view of last night’s Mexican eruption from IPS Meteostar.

!! PM AST U of AZ mod has rain “on the mountain” (the Catalina ones)  by 3 PM AST, and, like yesterday strong storms to the south of us heading this way.  But, like yesterday afternoons showers down thataway, they don’t make it here, the model reports.  You can do the loop for precip here in their rendition of the WRF-GFS mod.  Hoping Mr. Leuthold, our U of AZ expert, will shed further light on this when he reports here today between 10 and 11 AM.  In the meantime, I am sure convection expert, Bob (Maddox), will have something to say before then.

Not looking that great for a juicy August rain season here in Catalina Sutherland Heights….  Recall last year we had about 8 inches in July and August here, and at the end of August the mountains and grasses were SO green!

The End.

 

 

Pretty and tall Cumulus, early showers and thunder, but, alas, a rain dud here

“Alas”, now there’s a word to don’t see every day…probably a little stiff from laying around so long.

Those Cumulus that shot up over the Catalinas early yesterday morning were a magnificent sight, and so full of promise.  And while thunder was heard here just after 11 AM here in Sutherland Heights-Catalina, the showers just did not get off the mountains around here as hoped, though there were a few big boys (or “gals”, to be gender neutral) around to the NW-N and down to the S-SW during the afternoon.  Here are the Pima County ALERT totals for the past 24 h.  Lemmon had a good drop of 1.46 inches; that’ll surely keep those mountain streams going.  But as you will see, not much elsewhere.  Just a trace here, our mode for this summer in Sutherland Heights-Catalina area it seems.

BTW, all available model outputs (U of AZ 11 PM run not available at this time) show fewer showers than yesterday, though to CM, it looks like a very similar day to yesterday in sat imagery and such1.  So, it would seem we have a another day with a chance for a good rain in the afternoon or evening, about like yesterday when some showers did form off the mountains and could have landed on us.  Besides, even without rain, it was a pretty day anyway.  Its all great.

Here is yesterday’s cloud history with its early promise, ultimately only fulfilled only on the Catalinas around here:

6:35 AM. Our usual broken layer of Altocumulus clouds. But, being composed of droplets, are especially subject to dissipation as the sun comes up, irradiates them, and ground plumes begin rising to help finish the job off.
6:35 AM. Our usual broken layer of Altocumulus clouds. But, being composed of droplets, are especially subject to dissipation as the sun comes up, irradiates them, and ground plumes begin rising to help finish the job off.

 

10:32 AM. EVery single and married cloud-maven junior should have been EXTREMELY excited and filled with anticipation at the sight of these towering Cumulus clouds, these early risers (Cumulus congestus erectus). They demonstrate that that the atmosphere was "loaded" for action, that is was really unstable.
10:32 AM. EVery single and married cloud-maven junior should have been EXTREMELY excited and filled with anticipation at the sight of these towering Cumulus clouds, these early risers (Cumulus congestus erectus). They demonstrate that that the atmosphere was “loaded” for action, that is, was really unstable, ready to produce deep clouds and heavy showers.  Above the Cu, the remnant of the morning’s Altocumulus layer.

 

11:36 AM. Has been thundering on the Lemmon for about half an hour. These next two photos show the risk of being under a nice, darker cloud base with no sign of rain coming out, and then 3 min later (from a video I took), the mountains are obscured in blinding 1-2 inch rainrates per hour.
11:36 AM. Has been thundering on the Lemmon for about half an hour. These next two photos show the risk of being under a nice, darker cloud base with no sign of rain coming out, and then 3 min later (from a video I took), the mountains are obscured in blinding 1-2 inch rainrates per hour.
11:41 AM. A couple minutes after the shaft dropped down.
11:41 AM. A couple minutes after the shaft dropped down.  This was another really good sign about this day, the dark bases weren’t going to be “Chrissie Hynde and The Pretenders2” so-to-speak in terms of alternative music of the 1980s, but rather,  the “real deal”;  were shooting up to….the level of glaciation and precip formation!  I probably did not have to tell you that last thing when you saw shafts of precip coming out eventually, but suddenly,  out of every darkened base.

 

 

 

 

 

 

 

 

 

 

12:12 PM. "Twin towers" able to escape the mountains.
12:12 PM. “Twin towers”,  able to escape the mountains.

 

12:51 PM. These beauties. Topmost turret on the left is loaded with ice--can you tell? This is pretty hard to do at this stage. In a couple of minutes, the results of that ice began to show up at the base.
12:51 PM. These beauties. Topmost turret on the left is loaded with ice–can you tell? This is pretty hard to do at this stage. In a couple of minutes, the results of that ice began to show up at the base.

 

12:53 PM. Shaft beginning to appear below base. This is the most exciting place to be if you're under it, since the drops are huge, have made it through the now collapsing updraft. Lightning had already occurred by this time, so you have to watch out for these early stages of thunderstorm formation since, underneath it, you might not see the ice forming, and know that the electrification process is well underway.
12:53 PM. Shaft beginning to appear below base. This is the most exciting place to be if you’re under it, since the drops are huge, have made it through the now collapsing updraft. Lightning had already occurred by this time, so you have to watch out for these early stages of thunderstorm formation since, underneath it, you might not see the ice forming, and know that the electrification process is well underway.

 

12:57 PM. Puttin' the hammer all the way down.
12:57 PM. Puttin’ the hammer all the way down.

 

 

7:20 PM. Scattered Altocumulus with Altostratus above (a bit too thick to be just "Cirrus."
7:24 PM. Scattered Altocumulus with Altostratus above (a bit too thick to be just “Cirrus.”

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1BTW, if you want a really GREAT forecast by a true expert, rather than a “shoot from hip” kind of one that CM so often offers, you have to read what Bob has to say today when he posts it.  U of AZ experts also often refer to his careful analyses.

2Here they sing about something we probably don’t want to happen to Catalina, Arizona.

Thunderheads cross border, enter Arizona again

Its not a motorcycle gang, though it would be a good name for one comprised of meteorologists. Don’t think that’s gonna happen.

If you were watching carefully, and you had no radar capability on your smart phone, you could have still detected the presence of clouds producing rain. Here’s what they looked like, in a kind of a washed out, low-contrast view toward the southern horizon. AZ mod didn’t have them there, so it was a nice surprise to see them. It suggests that the chances of scattered rain today, and rumbles from the The Lemmon, are pretty good. Model output from yesterday DID have that for today; rain on The Lemmon this afternoon into this evening, drifting northwestward onto the valley. Yay! Waxing rain gauge so that the first drops don’t stick in the dust covered collector part, but zoom down into the inner cylinder (the part that magnifies the amount collected so you can read hundredths).  You don’t want any water molecules from those drops, “leaving the building” before they get in.

Here’s a photo of those thunderheads crossing the border yesterday afternoon:

2:58 PM. A surprise sight.
2:58 PM. A surprise sight.

Nice to see some Cumulus mediocris shading Mt. Lemmon, too.

2:51 PM. Mediocre Cumulus clouds hover over Lemmon.
2:51 PM. Mediocre Cumulus clouds hover over Lemmon.
7:18 PM. By this time, Altocumulus clouds, including some lenticular ones were invading the sky, Along with scattered Cirrus way above them, promised a great multi-colored sunset.
7:18 PM. By this time, Altocumulus clouds, including some lenticular ones were invading the sky, Along with scattered Cirrus way above them, promised a great multi-colored sunset.

And here it is, nine minutes later:

7:27 PM. Altocumulus and CIrrus clouds, due to their vastly different heights, provide contrasting sunset color.
7:27 PM. Altocumulus and CIrrus clouds, due to their vastly different heights, provide contrasting sunset color.

So, there are pretty much all of your clouds for yesterday. What more can I do?

The End

 

This just in:  just when you think you can’t possibly do anymore, this sunrise;

In case you missed it, today at 5:45 AM. Clouds: Altocumulus opacus.
In case you missed it, today at 5:45 AM. Clouds: Altocumulus opacus.

See below for title

“Hot ‘n’ pretty”

And it was yesterday.  But if I titled this blog page that, I would get people complaining that they weren’t looking for a cloud and weather report from the prior day.  Still, “hot and pretty” it was with those small Cumulus shadows drifting across our Catalina mountains, the shadows ever changing like the patterns in a kaleidoscope.  Can anyone tire of these views? I don’t see how.

SONY DSC SONY DSC SONY DSC

This last photo shows a “cloud street”, an intermittent line of small Cumulus clouds,generated by either the Tucson Mountains, or maybe even as far south as from Kitt Peak.  This line of clouds demonstrates that one of our best wind directions for rain is from the SW, as it was yesterday, and that was about the direction of movement for our those big rain cells on July 15-16th that drenched so much of the west slope of the Catalinas.  This direction brings air that is moving upward due to the increasing height of the terrain north and northeast of us, and storms are not compromised by downslope flow as they were the day before when the wind rushed out of the north.

Many of you will want to know if I saw any ice from these clouds yesterday, to compare with your own notes.  The answer is “no”, I did not see any.  The sounding below shows why.  Tops of the clouds were only about -5 C (23 F) and that’s too warm for ice to form in a cloud in Arizona–can happen over the oceans, or in clouds with real warm bases, but not here, not yesterday.  Yesterday’s cloud bases were up around 12,000 feet above sea level, highest tops about 15,000 feet, so the thickest clouds in these photos were maybe 3,000 feet thick (1 km).  See below.

Atmospheric sounding for Tucson from a balloon launched between 3:30 and 4 PM yesterday.
Atmospheric sounding for Tucson from a balloon launched between 3:30 and 4 PM yesterday.

 

July rain “factoid”:

Douglass, Arizona, has just passed the TEN inches mark for rain this month, a remarkable amount that is several inches over the prior record! Definitely have to get down there to see what TEN INCHES does to plant life there, maybe see some nice puddles, running streams, the whole great scenes of water in the desert.  I think you should, too; get out of the house, experience some summer life out there, stop watching so much TV…  :}

No rain likely here through the end of July.  Boo-hoo.