Tracey day

Two maybe three sprinkles occurred in the early afternoon between 1:30 and 2:40 PM for a total accumulation of “trace.”  The first from our very own Catalina cloud street off Ms. Lemon.  Here it is in mid-afternoon when it was was still right over us, but the clouds in it not tall enough, as earlier, to have something in them that causes precipitation to fall out.   (What is it? Hint:  Think of the Beatles’ anthem about something that is, “all you need1.”)

3:11 PM.  Cloud street off Ms. Lemon Mt.
3:11 PM. Landscape version to show how isolated this cloud street was.

 

 

 

 

 

 

 

 

 

 

Bubble Cu drifts away, later becoming a “quarter pounder”… Watch the sequence below.

3:40 PM. Clouds still streaming in shallow line off Ms. Lemon.  But take a look at the oval base left of the line.  Its going to do something, be productive as we all should be.
3:51 PM.  I think I will keep an eye on this.

 

 

 

 

 

 

 

 

3:51 PM. Cumulus congestus now, top clearly sprouting, will reach the height where something forms and causes fallout.
4:06 PM.  After a skit by Damon Wayans et al from
“In Living Color,” sung at ball parks, “Bloop, der it is!” Something is evident in the top that now means rain will fall!  This cloud is becoming a…Cumulonimbus!
4:06 PM. Checking out the bottom…precipitation begins to emerge. Can you see it in the patch of clear sky at right? Can you see it streaming down, upper right?

 

 

 

 

 

 

 

 

 

4:17 PM. Our little cloud is becoming “quarter pounder” Cb, just enough of a Cumulonimbus to drop a quarter of an inch in the absolute heaviest core on some unsuspecting soul who wasn’t watching.
4:19 PM. Coming out fast, reaching peak productivity right here, right near Pusch Ridge and Oracle Road.
4:23 PM. Only FOUR minutes later and its just about all over. This cloud will drift off and just be a hardly noticeable remnant in a few more minutes after its little dump.

 

 

 

 

 

 

 

 

 

So, what did we get out of this sequence?

Even small clouds, really modest ones at the start, can boil upward and produce a useful amount of rain, albeit in a short-lived life.  Between the time it began to rain from this cloud and the end of it from this little cloud was barely more than six minutes, maybe ten.  But don’t overlook them; they can still get you wet.

And with that happy ending, let me leave you with this happy ending to our day; yesterday’s sunset Cumulonimbus cloud, and the thought of more of them today!  (The weather service says so…here.)

 

1ice

 

 

 

 

 

Rainbow? Or, after THAT storm, was it the “‘Arc’ of the Convenant”?

What an amazing, Biblical sight1 that came across the Catalina Mountains yesterday evening, that shaft of intense rain and attendant rainbow!  After a day where it looked like rain might not happen here, those earlier Cumulus clouds being pretty lazy really, this behemoth powered across Tucson and the Catalina Mountains dropping 0.56 inches in momentarily blinding rain blown on 60-70 mph gusts, with numerous cloud-to-ground lightning strikes, taking down power lines, and causing a 6 h plus power outage in Catalina.  0.51 inches fell here in 10 minutes!

Oops, forgot to remind you:  Don’t forget to go to the movies.  Shows the backside of what hit us just as the day ends.

How great this rain will be, too,  for our stressed desert-thornscrub vegetation after almost a week of dry conditions. (Only 0.17 inches at Sutherland Heights, though.)

For me, yesterday evening produced the most dramatic sights I’ve seen here in four years in Catalina.  I hope you caught it, but if you didn’t, here are a few of the most dramatic ones.  The first, penultimate shot was from the front porch about three minutes before bedlam hit Sutherland Heights.  Below this, those shots leading up to it.

7:04 PM. The Arc! Woulda been outside, gotten a better shot, but just there was a cloud-to-ground strike about 100 yards away a little before this “whilst” I was being a dummy outside grabbing the shots below.
6:34 PM. Storm hitting Tucson. TEEVEE weather presenters very excited. Its heading this way, but will it survive passage over the Catalinas?  A successful passage will require the renewal by new rising turrets.
6:50 PM. Looks like it will make it over the Catalinas.  Note cloud base AHEAD of the rain shafts.  This is looking pretty darn spectacular with the sun going down.
6:54 PM. 100 photos later, “executive override brain function” for controlling impulsive actions failing. Taking too many photos; agog at what I am seeing.  New cloud base holding up.
6:58 PM. “Whoa, Nelly”, as Keith Jackson might say.  An astounding sight; doesn’t look real.  But note clearing just behind shaft. So its not a wide storm at all.  Maybe it will miss us, as they have done lately. The “Arc” is just developing at left of the shaft.  More importantly, the base now overhead has held up and promises a new dump will emerge.  Each of these shafts only lasts a few minutes, and so you have new ones if you are going to get ROYALLY shafted (to use terminology appropriate for Olympics now in progress in Her Royal Majesty’s Britain).

 

 

 

 

 

 

 

 

 

 A repeat of yesterday today?  Not bloody likely.

Oh, well, any rain will be great, but drier air is moving in.  Check it out here from the University of Washington Huskies’ (some former of whom, if that is correct english which I doubt, are in the Olympics, for example, women’s volleyball, but not in beach volleyball which I seem to be watching a lot of) Weather Department here.

Note the drier air moving in from New Mexico and west Texas in this loop.   Just the same, it can still rain here some because while drier, it’s not dessicated air and so the usual isolated Cb should be around.  So, keep watching,  keep cameras ready and charged.

The End.

 

————————————————————————————————————————————————————-1Biblical allusion is to the “ARK of the Covenant” whose activity was demonstrated in a movie with Harrison Ford some years.

“Feint” rainbow

For a few minutes yesterday afternoon, it looked like some unexpected rain was trucking over the Cat Mountains from the east-northeast late yesterday afternoon.  No one could blame you for getting your hopes up and misleading your neighborhood by saying it might rain in half an hour.  Those clouds rolling in from the Catalinas (shown below) were great sights for soaring eyes, ones that look to the skies all the time for rain.

5:16 PM. What’s this! Looks like the old Charoleau Gap storm is coming.
5:16 PM. Good base all along the Catalinas, nice and solid-looking
5:57 PM. Bottom of those weak Cumulonimbus clouds have evaporated, leaving moslty virga, and a sprinkle that reaches the ground over there by those mountains but not here.

 

 

 

 

 

 

 

But within the hour, the clouds had broken up, and the shower they produced was reflected by a faint rainbow. Rainbows to the east and northeast are often precursors of rain and wind moving into Catalina. Here is the sad remnants of those albeit weak, Cumulonimbus clouds with their feint rainbow, one that was not followed by one drop of rain here.

A big patch of Cirrus kept the temperature down some during the first half of the day, and so our Cumulus were behind in development compared to areas around us.  Here is that bad Cirrus spissatus in case you missed it, that which hung over us so long.

It was quite visible even in the visible satellite image all morning.  When it shows up there, you can bet that the Cirrus in that image is thick enough to produce shading and mess up the development of Cumulus under and around it, particularly on marginal rain days like yesterday.

Much Cirrus is virtually invisible in visible satellite imagery; get it?  You can see it from the ground (i.e., its visible), those thin wisps of Cirrus, but try to find it in a visible satellite image!  This whole line of reasoning and befuddled exposition here reminds me of that Science knee-slapper of a few years ago; that article entitled, “Where are the invisible galaxies?”

1:49 PM. Cirrus spissatus, sitting there doing nothing, but wrecking out Cumulus clouds.

Today?

Raining lightly now at 5:25 AM! Yay. A night stalker mass of rain is moving into TUS now as I write. They don’t usually like the daytime and fade as the sun rises in the sky. Sprinkles, very light rain showers (and as always pointed out here, quite emphatically I might add, “sprinkles is not DRIZZLE, dammitall”, to be a little colloquial there!).

Let’s hope this heavy cloud cover we have now (5:30 AM), which you could call, Altocumulus opacus and castellanus due to its height above the ground (its at about 11-12,000 feet above the ground and has turrets here and there). But, to get a little pedalogical you could label it in your log book as Stratocumulus, perhaps with the appendage, castellanus, since turrets are present–those are what’s causing the sprinkles/light showers.

Sunset was nice….

U of AZ mod shows this is our best day for a significant rain, some of that this morning, and some arises later with those afternoon and evening giants we get around here. Hoping so.  Tomorrow is supposed to be drier.

The End.

Long distance Cumulonimbus top; cloud review for yesterday, and, big day tomorrow?

The only good Cumulonimbus (Cb) clouds seem to be occurring north of Golder Ranch Drive, about a 100 miles north. which of course, astronomically speaking is actually quite close.  Yesterday, with no intervening clouds, it was another chance to see how far can you see the top of a Cb, then use the NWS radar to place it.  The Cb top, with an arrow pointing to it in the first photo, is followed by a zoomed shot.  The radar indicates that lone, very tall cell was about 10 miles SE of Kingman, or more than 150 miles away!  It was common in South Dakota, working with radar in Mitchell and Parkston, to see Cb tops and anvils on the horizon that the radar was unable to see, partly because the radar beam is pointed slightly upward to minimize “ground clutter” as seen in the radar image below around PHX.

7:12 PM
7:12 PM
7:20 PM NWS radar mosaic rendered by the U of AZ.

Review of yesterday; another quiet day (Ed. Note: Getting tired of quiet days)

Yesterday was almost exactly like the day before, with a brief period of glaciating cloud in the same spot beyond the Charoleau Gap from Catalina as the day before. Here are a few representative shots of yesterday.

Can you pick out the icy top in that one little glaciating Cb? Its a little harder to detect this time compared with yesterday.

6:51 Cirrus for breakfast.
10:31 AM. Small Cumulus over the Catalinas by brunch time.
2:48 PM. Cumulus are really kind of in a post-lunch nap; inactive, not doing anything. It was pretty disappointing to watch all of this inactivity, lack of sprouts, into mid-afternoon.

 

4:03 PM. What’s this? Some bulk. Is that ice in those tops? I know, but do YOU?  Means some rain fell out the bottom.

 

 

 

 

 

 

 

I feel uncomfortable labeling this little mush of cloud a “Cumulonimbus”, maybe “Cb calvus”,  because the fibrous nature of the ice is not yet obvious.

Still it has the attributes of a Cumulonimbus, glaciating top, precip out the bottom, though we can’t see it here.  It will produce a radar echo like the little Cb the day before. What we really need, to editorialize some, are categories for these situations like “Cumulonimbus humilis”, “Cumulonimbus mediocris” so that we know that we have miniature versions of those clouds.

We do have, though I avoid it, a category of “Cumulus congestus praecipitatio”, because visual examples, as shown in the last (1987) World Meteorological Atlas, cannot be differentiated from Cumulonimbus clouds, at least, not by me!

 

The weather ahead

“Quiet time” is coming to an end, not today so much, the computers say, but tomorrow, oh my, could be huge!

Check it out here, courtesy of our U of AZ weather program and their massive Beowulf Cluster of computers.

The End

Official climatologist blasts “educated fools” for mischaracterizing “Arizony”

This just in!  Well….I didn’t see it until just now, so its kind of “just in”, the input domain smaller than one usually thinks of when you hear the phrase, “this just in!”

Please begin reading at the second paragraph, which discusses prejudice.  It seems some people were carelessly calling Arizona a desert!

Checking your cloud log book for yesterday

My attention began to drift toward a fattening Cumulus cloud beyond Charoleau Gap.  After days of Cumulus humilis and mediocris, I was buoyed by the sight of a real congestus cloud there.  Would it, could it, GLACIATE, get cold enough on top to form ice crystals and snow?

As you know, and I think the Beatles said it best (a boy group from Britain in the 1960s), in their famous anthem, ” All You Need is Ice”:

“All you need is ice, dah-ta-dah-ta-dah, all you need is ice, dah-ta-dah-ta-dah, all you need is ice, ice, , all you need is ice, etc, etc., etc. (it was a very repetitive song)  Furthermore they claimed, “it’s easy.”

It was going to be a great song, scientifically speaking, in many ways, though we know that rain can form without ice at times.   However, and I think the boys realized later,  that its not always THAT easy (to make ice) when the freezing level is at 15,000 friggin’ feet, and the tops have to reach -10 to -15 C, or about 24,000 feet, as we had here yesterday.

Later, the “Beatles” (BTW, the British spelling of “beetles”, which I doubt many of the Ancient Ones out there knew before I posted that information here) realized, having long been interested in precipitation in their homeland, that the original lyrics were misleading.   They decided to update the lyrics to something more accessible and commercially viable, changing “ice” to “love” soon after the first production.  You can hear the revised song here.

However, If you replace “love” with the origiinal word, “ice”, it will help you understand the precipitation process here in “Arizony” better.

Where was I?

Oh, yeah, I began to see a ruffle in a Cumulus congestus cloud top that looked like it might be converting from supercooled water (water at below freezing temperatures that aircraft like to avoid) that MIGHT be converting to ice.  Then after a few more minutes, much of the time having to talk with another human and missing the important transitional photo stage, it was completely iced-out, this meaning rain was falling out the bottom!  Somebody got wet!

Now this was NOT a large Cumulonimbus cloud, but rather, for us, a “mediocris” but here it is.  I wondered, in view of its small size and brief lifetime,  how many of you logged this cloud?  It could have easily been missed.

I am posting photos to help you fill in the correct and complete cloud observations for yesterday in your log books.  There were also several forms of Cirrus above the small Cumulus clouds that were prevalent.    I figure you were “all over” the Cirrus, but likely missed our little, and brief, Cb.

Here are a couple of cloud photos from yesterday, to check against your log of cloud observations, to help you make sure you got them all.  I’ve added some “excitement captions” as well, ones with exclamation marks to kind of get you going.

3:29 PM. A shot of the hum-drum Cumulus fractus and humilis, typical of yesterday, with a little Cirrus above.  Why waste camera memory on shots like this?
Also, at 3:29 PM, spinning rapidly to catch this shot, an honest-to-goodness Cumulus congestus!
3:34 PM. What’s this? I looks like the older turret on the left is converting to ice!
Its actually going to rain somewhere near here today!
3:53 PM. The original turret has completely iced out (left side white region, as has the turret that came up on the right behind it, now forming the main mass. Yep, somebody got measurable rain over there, though it looks like a 0.10 of an inch Cb to me.

July 2012: 15 days with measurable rain (with three traces); adds up to 4.45 inches!

And we were one of the drier areas!  Many places around us were between 5-10 inches this July making it a pretty memorable one and the 6th wettest July in Catalina since 1977.  Here’s the list of those wettest for Catalina:

1.  July 2006    7.22 inches   11 days with measurable rain

2.  July 1984    6.54 inches   17 days with measurable rain

3.  July 1990    5.25 inches   12 days with measurable rain

4.  July 1983    4.94 inches     9 days with measurable rain

5.  July 20081   4.73 inches   12 days with measurable rain

6.  July 2012    4.45 inches   15 days with measurable rain

1The record begins in 1977 down at Our Garden garden on Stallion Ave and in July 2008, is a mix of their records for the first half of the month, and here on East Wilds Road for the second half, and from East Wilds Road thereafter.

Here is the NOAA 30-day radar-derived rainfall map, ending July 31st, for Arizona to provide an overall picture of how well our State did this July.  Also shown is the percentage of normal map.  You can find these maps here.

De-briefing for yesterday

A disappointment for sure, since the day before, the models had indicated a pulse of rain moving through in the afternoon.  But then they changed by yesterday morning.  The rain pulse was gone.  That’s what weather computer models do;  they say they like you and then they say they don’t, in a sense.

However,  if one looked far enough to the south in the evening, there was a Cumulonimbus way off in Mexico, maybe a 100 miles or so,  that was exactly headed this way. It lasted about 20 minutes and never crossed the border.  Oh, well.  Rain hope springs eternal.

7:14 PM  Down Mexico way, a Cb!

Closer ones suddenly popped up to the NE and ENE, quite pretty, but they weren’t moving this way.

7:12 PM.  A closer Cb but may as well have been in New Mexico because it wasn’t moving this way.

There was too much haze yesterday, too.

7:03 PM.  “Deliquesced” (fattened up by humidity) smog aerosols show up as the cloud-free whitish areas at cloud base.  Really looks awful from an aircraft flying at that level since you’re looking at that layer on its “side.”

 The Weather Ahead

Seem to have entered a break in the showers now.  U of AZ mod (here), crunching data from 11 PM last night, doesn’t think the rain will be back until the 3rd.

We can hope its WRONG again!

Another big day; scattered amounts around us of more than THREE inches again; we only got 0.18 inches!


Trying to be excited for those around us who got all that rain yesterday while we received a paltry 0.18 inches here in the upper reaches of Catalina.  Still it was another good little rain for our local desert.

The 24 h rolling archive from Pima County rainfall gages is here.  Most seen here?  2.01 inches at Finger Rock and Skyline, Tucson.  You’ll see that storm in the movies.

Also, check the more comprehensive U of AZ rainfall network here.  In fact, you might as well join up, too.  It would get you out of your rut.  Think how exciting it would be to go out in the morning and see how much rain fell in your gage in the previous 24 hours!  Maybe someday you might win the “rain lottery” and have the biggest amount anywhere in the State!  The most reported so far this morning is a deluge of 3.17 inches over by Picture Rocks again.  Good grief, have they been getting hammered.

What a July this is turning out to be!

Here we are in Catalina, its late afternoon, it has just rained again, the temperature is a chilly 70 F, dewpoint 68 F (almost saturated), with Stratus fractus just above eyeball level lining the hillsides!  Its an amazing scene for an afternoon in Catalina and vicinity in July.  And so DARK!  Here is that odd scene from yesterday afternoon:

4:42 PM Stratus fractus is that low bar of clouds in the foreground just behind the tree.  Makes you want to run over there and play hide and seek in it.

Relive yesterday, as though you were in the city of Tucson shopping possibly, here in this movie, courtesy of the U of AZ Weather Department.  The movie is rated “R”, for violence since the sky goes WILD in the afternoon, winds going every which way.

Also, in this time lapse you will get a sense of how rapidly moist air is flowing across us from the east to east-southeast.  This movie, comprised of  still shots taken every 10 s shows movement, like the day before, that is phenomenal for summer, more like a winter scene when winds are normally strong.  There are even Altocumulus lenticular clouds (almond shaped ones) hovering over and just downwind of the Cat Mountains!  Amazing.

But check the CHAOS in the mid and later afternoon.  Unbelievable.  Areas toward the Catalina foothills, during this chaos, got another 1-2 inches again yesterday.

In contrast, let us now look at the very same day in a time lapse film in Seattle, Washington, where Mr. Cloud-Maven person spent 32 years, most with the U of Washington Huskies Weather Department.  Here it is.  I sum up the totality of that movie for July 29th below:

Bor-ring!

Those Seattle skies, for the most part, were like eating plain, cooked oatmeal everyday, all day.

Below, the start of our exciting day, the middle, and the end has already been shown above.  Lots of nice rain shafts SUDDENLY collapsing down out of clouds.   A sequence of the big northwest Tucson storm early in the afternoon that moved off toward Marana is included as part of the middle.  That shaft really fell out fast, and how you could detect the icey tops BEFORE the shaft appeared.  I try to point out how you might have been able to do that in this sequence, and thus, and quite importantly, impress your friends and gain status and some kind of weather sage.

Today?

Just looked at the latest AZ mod output, as you can here (forgot to past link until now, 8:08 AM).  Colored splotches are where it is supposed to have rained that HOUR.  That model has a much less active day today, but much more active tomorrow.  Cumulonimbus clouds in sight today?  Oh, yeah!  But, none are SUPPOSED to get us today.  But these mods are always slightly inaccurate, so keep watching this afternoon.  Should be another photogenic day, if nothing else.

10:03 AM. What a pretty start!
1:29 PM. Cumulus congestus converts into a Cumulonimbus calvus. While no rain is falling out the bottom, check the top peaking through above in the next shot.
Also at 1:29 PM. Annotated. Icey tops barely visible, but reveal that this cloud is LOADED with precip, certainly would have a radar echo aloft now. In a perfect world, the flash flood warnings would go out NOW, even though it hasn’t gone out the bottom yet.

 

1:32 PM. The first fibers of rain are just starting to be visible at cloud base as the updraft collapses, too much weight up there in rain, hail, and snow.
1:36 PM. There it comes! Close up of the main dump.
1:48 PM. What was interesting was how huge this got in just a few minutes, how the initial outflow winds kicked off other cells around the first dump shown above.

Every which way but here

Of course, alluding today in the title to the great western movie with John Wayne…

Every which way you looked yesterday afternoon, there was a great rainshaft.  1.85 inches fell in one hour at Picture Rocks Community Center yesterday afternoon,  2.01 inches total.  Several stations around the county had another 1-2 inches yesterday.  You can see the Pima County rain lineup here.  Seems the great amount in the Catalinas was about half an inch in a gage at Samaniego Peak.  Probably twice that between gages up there in the hot spots, where the best columns of rain fell.  Also, it would be good to examine our U of A rainfall network today, too, for some jumbo totals.  Values are being added during the morning hours as a rule.

Catalina?  Well, a measly 0.05 inches fell here after 7 AM until this morning from side-swiping Cumulonimbus clouds, though Sutherland Heights did receive a more respectable 0.28 inches–just measured it. .  So, if you were outside yesterday, you saw heavy shafts of rain all around, but none developed over us (the best kind), or moved in here.

But, then, 1.85 inches in an hour,  probably most in a shorter time than that, might be “counter-productive”; might make Catalina into a news story, and not a good one…  So, I’d better watch what I wish for.

Here are some views of yesterday’s “clouds and columns” of rain yesterday.  And, as has been the case, the day started with heavy layer clouds, Stratocumulus and Altocumulus, and a nice, but very brief sunrise “bloom” shown below:

Once these clouds thinned by late morning, Cumulus began to surge upward over the Catalina’s, and reflected an usually strong east-southeast wind just above mountain top levels by trailing over Catalina from Mt. Lemmón.  These reached the ice-forming level (read, began to produce rain at the ground) in a series of showers and thunderstorms by 11:30 AM (2nd photo).

Looked, too, like another tube (funnel cloud) at 3:48 PM yesterday off in the direction of Marana, but I’ve posted so many of late I thought I would just post it at the bottom of these more interesting photos.

11:03 AM.  Cloud “street” off the Catalinas.
11:31 AM. From Mt. Lemmon to us, straight overhead!
1:01 PM. Repeated showers STILL trailing off the Catalinas! But not over us.

 

 

 

 

 

 

 

1:01 PM. First major-colossal dump occurring N of Park Links Road.  Note bit of rain falling from overhang cloud from the prior photo.  Tops shearing off; rain-producing part (top of photo) has no underlying cloud for the drops to grow in as they fall, so no collosal-major dump.  Did start thundering about then, though

 

1:16 PM. This is so pretty! Now, one of those turrets has leaped upward, more or less straight above the bottom of the cloud, and now, though a small one, a major-colossal dump on the Cats. I love these scenes here!

 

 

 

 

 

 

 


 2:36 PM. Its gonna miss Catalinans, BUT, this is where you want to be under. Look at that downspout! That whole cloud is loaded with precip, and the Big Boys are dropping out now, and just before this, the largest ones able to overcome the updraft so its especially great and exciting to be under a cloud like this just as those strands of rain/hail drop out.  Also about the time such clouds get “plugged in” and send light daggers to the ground, as in this case.

 

 

2:41 PM. Its just FIVE minutes later! You probably haven’t even gotten in your car yet to try to get over there. Its too late.  This was a one dumper and gone.  Faded away into just a residual ice cloud.

 

 

 

2:57 PM. Done, cooked, fried. Without the flanking clouds piling up into new turrets that reach the ice-forming level, all you have after just 20 min or so, is this sad sight of a dying, once proud Cumulonimbus cloud. Rain here likely due to aggregates of ice crystals called snowflakes if you up there flying in them.

 

 

 

3:04 PM. What was truly remarkable about yesterday was that those smallish Cumulonimbus clouds just kept on generating over and over again off the Catalinas. Very unusual, and was a measure of how unstable, how easy it was, for the clouds to surge upward yesterday.

 

3:47 PM. Another one! Unbelievable. Like the bunny, going and going and going.
4:01 PM. Its practically nighttime, cool, overcast, not good for Cumulus, and yet look how this little group was trying so hard to be a rain cloud. Sadly, they didn’t make it.  Have never seen such tall thin clouds like this here in this kind of environment, that’s why I posted it.
3:38 PM. Likely funnel cloud just above bright spot, the longer filament, not the nub from the cloud base in the foreground, but from the next base farther away.

Moisture continues to revolve into Arizona from the southeast and so it would appear a similar day is in store for us.  Oh, goody.

Rainy days and Saturdays

Nice sunset yesterday….as some Stratocumulus spread over the sky underneath a pesky Cirrus cloud cover, clouds that announced the beginning of our next rain spell, now underway.

Light rain is falling this morning at 4:07 AM, and has been for hours, amounting to 0.01 inches.  However, some places in Pima Land have gotten much nicer rains, around a third of an inch in the Cat Mountains overnight, for example; check here.

Progress of the real monsoon, since June 1st, can be checked back there at the beginning of this sentence.  The coastal state of Karnataka has an average rainfall of about 70 inches since June 1st, a below normal amount, believe it or not.  However, being a statewide average, that 70 inches doesn’t reflect the hill stations in the western Ghats, surely to have about twice that amount.

Now, as a further aside, Karnataka, Kerala, two Indian west coastal states  would be a great place to go for a vacation now!  There you could REALLY absorb a REAL monsoon, where passing rains, heavy, pounding, thick with drops, visibility down to less than a mile, go on hour after hour with brief interruptions.  Its really pretty amazing and worth experiencing, at least once.

But, not much lightning there, like we have, because the rain develops mainly through a process not requiring ice, much like the rains in Hawaii where lightning is also rare.  The rain develops largely through the collisions of drops, ones that stick together after they collide, and get bigger on the way down through the cloud, sometimes called the “warm rain process” because ice is not involved, and that causes most of the rain in that Indian coastal region.  Cloud bases are right on the deck, and are typically 20-25 deg C, very, very warm.

In contrast, to continue a pedantic stream, “warm rain” is rare here in Arizony because cloud bases are relatively cool (less than 10 deg C in the summer as a rule), and droplet concentration are moderate to high (hundreds per cc).  Higher cloud droplet concentrations make it harder to grow cloud droplets big enough to collide and stick together inside our clouds.

But, we do get that kind of rain, “warm rain” here once in a great while in Arizona as part of the rain that forms in our Cumulonimbus clouds when their bottoms are especially warm, higher than 10 deg C.  Seems to happen about once or twice a summer in my experience so far.

What’s ahead?

Now that afternoon and evening rains around the area are back for the foreseeable future (5 days), what’s way ahead, beyond the foreseeable future?

There, as you know, when we start thinking about beyond the foreseeable future we start thinking about spaghetti! What do those crazy northern hemisphere-wide plots produced by NOAA with their dizzying numbers of lines mean for us here in Arizona?

First, I present a map of the 500 millibar contours as produced in the Haight-Asbury hippie district by San Francisco State–I mention this because the lines on this 500 mb map look a little nervous and maybe it has something to do with that map origin, being from a cultural area whose norms are “anomalous.”  I have pointed out  on this map, “Our Big Fat Anticyclone”, one whose position is critical for decent summer rains here.  In this map, as you can see, its not really OUR “BFA”, but rather belongs to Amarillo, TX, as of last evening.

Nevertheless, it is well positioned to fan humid air from the southeast into Arizona, as is happening now.  Remember, the circulation around a big fat anticyclone is clockwise.  When it sits on top of us, things are not so good; upper level temperatures are high, humidities are low up there, stifling convection and preventing tall Cumulus clouds.

But when the high is away on holiday, temperatures are lower above us, its more humid up there, and those factors allow for deep convection; huge Cumulonimbus clouds.  It only takes a few degrees difference to go from those dry days we just had with their Cumulus pancakus, to the kinds of days ahead for us now, where clouds stand tall!

Continuing, finally, Here’s is today’s plot for 15 days from now, the afternoon of August 11th, based on global data taken at 5 PM AST yesterday.  What do you see?  You see an arrow pointing to something of a void in all the “spaghetti.”  That void represents the most likely position of our BFA some two weeks from now, and that position is pretty darn good for summer rains here.  And it is in that region, to the north of us, almost the whole time from now!

So, based on this “most likely” position, one would venture that the rich summer rain season we have had thus far, will continue to be active.  Of course, this doesn’t mean rain everyday, but that breaks will likely be short through almost the first two weeks of August.

Can you imagine how tall those desert grasses and weeds will be by then if this is the case?

The last couple of photos document our fabulous re-greening now in progress.  If you haven’t been out in the desert, you should get out there and experience this wonderful event.  Doesn’t happen every year, as we know!

On a clear day you can see Flagstaff

Of course, you can’t see the TOWN of Flagstaff, you silly person, the title was just a hook to get you here to read about clouds!  The earth curves too much for you to see Flagstaff, for Pete’s Sake. How could you even imagine that such a title could be true?

But, you CAN see the tops of Cumulonimbus clouds boiling upward OVER Flagstaff, maybe there is someone you know there and you could call them about it, find out how much it has rained.  Those Cumulonimbus tops stick up above the horizon in that direction about a quarter of an inch if you were to take a ruler out and hold it out in front of you.  Thought you’d like to know this.

Here’s the scene I am describing from yesterday afternoon.  In case you wouldn’t know what to say to your Flagstaff friend, I’ve tried to help you out in the caption for the second photo.  Maybe its your mom you haven’t called in a while….  Who knows who it might be that you know up there?

1:27 PM. The scene. Cumulonimbus tops, likely above 40,000 feet above sea level, lined the higher terrain of the Rim to the NW-NE from Catalina yesterday afternoon.  BTW, I really like Catalina.  Who would have dreamed I would end up HERE coming from Seattle!
1:27 PM. Arrow points to a top right by Flagstaff!  If you have a friend or a relative up there because its too hot here, you could have called from Catalina yesterday and said, “Hi, I see its raining up there.  Are you getting much?  Friend:  “How do you know its raining? Did you look at some radar?”  You reply, “No, I can see the cloud over you from here, I really didn’t need to look at the radar.”


Finishing off today’s lesson: The tops you see are ALMOST always completely composed of ICE crystals and snowflakes because they too damn cold at 40,000 feet or so (temperature less than -40 C, less than -40 F; they are the same numeric at that temperature, yet another piece of knowledge for you) for anything but ice we think.

Some embarrassed people have reported liquid water at temperatures below -50 C such as Robert H. Simpson, former head of the National Hurricane Center and also husband of the late Joanne Simpson, famed Cumulus researcher and FIRST WOMAN TO EVER RECEIVE A PH. D. in meteorology1.  Must’ve have been an especially great marriage because they both loved weather and clouds and hurricanes and probably talked about ’em all day.

Continuing with something relevant, once when Bob (Simpson) was in Seattle giving a talk, after the talk I said to him, smiling, “You must be pretty embarrassed about reporting liquid water at -62 C”, as he did in 1962 in a conference paper, and again in 1963 in the peer-reviewed journal, the Monthly Weather Review.

He smiled and said, “The theoreticians don’t think its there, but its there.”

Hmmmph.

The weather today and the next few days into August?

Scattered rains, lightning thunder EVERY day into August! I am so happy. More rain is on the doorstep.  Take a look below at what this extra rain we’ve had so far in July has already done to our desert as of three days ago, July 25th.  Its incredible, isn’t it?  I call it, the “re-jungle-ation” of Arizona accompanied by the appearance of new life forms; see last photo.

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1Joanne Simpson, after reviewing my grades, advised me to give up meteorology. She was a professor at UCLA then (1963), and I wanted to “walk on” as a met student in their program. In effect, though I didn’t realize it then, she saved me from myself since UCLA was WAY too theoretical for me in the approach to weather. Later I attended San Jose State2, a program much more suited to me with my weak math skills.  (Can you put a footnote in a footnote?)”

2While at SJS in the later 1960s, I was forecasting weather for the college paper, forecasts that devolved into silly, juvenile, lame topical humor, much like the “humor” here.  To drop another name in this blog, I loved what KRLA-AM, a top 40 station in Los Angeles, where I grew up,  was doing in those turbulent days of the late 1960s. They had dared to start a news parody program, recreating news events that they would first report in a serious manner.  It was bold and courageous for a mainstream media station; they dared to offend. I wanted to be a part of it, and went down to apply for summer work there in 1968.

My interviewer?  A young Harry Shearer.  The “Credibility Gap“,  the KRLA news parody team in those days, consisted mainly of Harry, Richard Beebe, and David L. Lander.  An example of their work, “Dawn of New Era for Man”,  KRLA’s 1969 Apollo 11 counter coverage to the major networks; its 8 min long, Arizona’s Papago Indians mentioned.  You can’t find this on the internet!

Back to the interview:  Harry briefly examined my topical forecasts for the SJS paper, ones I presented to him pasted on a blank sheet of paper.  After just a minute or two, he said, “I don’t think they’re that funny.”   It was painful to hear, but upon later reflection, oh, so true!  I left immediately.

I had some low moments in the 1960s, but here I am!