Let’s check in on the upcoming El Niño

Here’s the ENTIRE message I got  just last night from an El Niño expert:

“For your entertainment, see below… and in other news, looks to me like an El Niño is coming on fast – maybe you and I will get plenty of rain in winter 2014.”

My friend, with insider El Niño “trading” info,  lives in Monterrey, California, and is referring to the 2014-15 winter as a whole.  Pretty exciting I thought since we can put the current winter pretty much in the trash can and move on…

BTW, the first part of his message referred to a sci lecture at the U of AZ on Monday about global warming impacts (now repackaged as “climate change”, since its not really been warming anymore  for some time, well, since your teenaged son was born, for some reason).  I think you should go there and hear it.

But, in the meantime, let us look at the ocean temperature anomalies (way below) and see what this expert is talkin’ about when it comes to an upcoming El Nino.

Some Niño background

First of all, let us remember there are two kinds of El Ninos, “Classic El Niño” (aka, “Classic Niño”) and “The New El Niño” (aka, “The New Niño”).  Below, we’ll use the short versions.

“Classic Niño” is the one we talked about for hundreds of years, well, maybe not you and me, but the one Peruvian  fisherfolk got real worked up over when, suddenly, the ocean water along the extreme northern coast of Chile and all of Peru warmed up and changed what fish were out there it got so warm.

Not only that, it began to rain like HELL in areas that were total deserts because the warm water brought tropical air with huge Cumulonimbus clouds that rained like HELL, to repeat and emphasize a point, and also to add some colorful language to what might otherwise be a dull discourse.

And that rain and warm water extended westward all the way to the Galapagos Islands where the people who lived there, if any, also got worked up over sudden. gushing rains.  Well, who knows if anyone lived there, but certainly the totals (haha, I thought I was typing, “turtles” and it came out “totals”–how funny izzat?) got worked up; whole bio communities could get almost wiped out by those sudden, punishing rains.

Before the big Cu moved in, all they had in the Galapagos was Stratocumulus and small Cumulus (boring!)   Sometimes those kinds of clouds could drizzle a little, or produce light rainshowers, and that’s about it.  Those shallow clouds were topped by a temperature reversal with increasing height, so they could never grow up to be Cbs.  The relatively cool waters normally along the Equator in the eastern Pacific were responsible.

When Niños occur, they extended even farther westward than just the Galapagos along the Equator,  as the unusually warm water propagated into the mid-Pacific Ocean.  Other islands out there,  like the Galapagos, and normally very, very dry, would be ambushed by heavy rains from huge clouds they hadn’t seen in years when normally,  they only saw “cup cake” Cumulus” with passing occasional very light showers, like Johnston Island way out there somewhere south of Hawaii.

But, the “Classic Niño”, wasn’t really good enough for scientists.   So they made up a new formulation of Nino and introduced “The New Niño”, sometime in the 1990s or, as they called it, to be more technical with greater obfuscation for scientific purposes,  “Region 3.4”which is really a patch of the equatorial waters WAY offshore  along the Equator from where “Classic Niño” occurs (120 to 170 degrees W longitude).  You can read about it, get more details, here.

Why did scientists do this?

Because “The New Niño”, or “Region 3.4”, to return to jargon) did a better job with something we call “teleconnections.”  “Teleconnections” is not a new service by Verizon, but rather how weather in one locale is related to the weather in another region, usually thousands of miles away.  It was something that was noticed in the middle of the last century, how, say,  stormy weather in one area was associated with stormy weather in another.  Often, severe winters in the eastern US are associated with severe winters in Europe, as an example, though it did not happen this winter.

In the the case of El Niños overall, research in the area of teleconnections fournd that  “New Niño” was better associated with GLOBAL telenconnections than was the “Classic Niño.”  So, most of us have moved on and scrutinize “Region 3.4” water temperature anomalies.  To explain, in what has become a lecture (is anyone left? Elvis certainly would have “left the building” by now) I use arrows in the sea surface temperatures below to point out where Classic Niño occurs and where the “The New Niño” one does.  They usually, though not every time, occur at the same time.

El Niños, as you likely know, are associated with greater chances of rain in the whole Southwest, along the southern Gulf Coast, and even folks in Saudi Arabia have some evidence that more rain even falls there in the winter when a Niño occurs!  However, its best, for these teleconnections to work out, to have a big Niño, like the ones in 1982-832, or 1997-98.

Map of the latest sea surface temperature departures from normal, this from just yesterday!
Map of the latest sea surface temperature departures from normal, this from just yesterday!

I don’t see much going on as yet, but my friend has access to stuff I don’t, like water temperatures lurking just below the surface that are about to rise to the top if the winds along the Equator all the way to Australia and beyond cooperate.  Note its cold as HELL in the “Classic Niño” area right now, but has warmed up some over the winter in the “New Niño” patch which is a good sign.

Been derelict in cloud photos lately, got relatives visiting.  But as weak troughs move toward us, they will keep the supply of Cirrus, Cirrostratus, and maybe some Altocumulus streaming by overhead for the occasional spectacular sunrises and sunsets for the next several days.

The End.

—————————

1You wonder if the “New Coke” would have done better if it had been called, “Coke 3.4”?  Sounds more like an solid advance in coke formulations, something I might want to drink, with numbers attached like that.

2Had about 30 inches of rain here in Catalina during the 1982-83 water year!  Dream about that one if you weren’t here to see all the water flowing in just about every wash imaginable in those days.   However, there have been some Niño duds here, too, like 2004-05, or 1976-77, ones that were associated with below normal totals here during the water year.

Snowy day (overhead)

Cloud tops in those deeper Cu reached -30 C (-22 F) yesterday, plenty cold enough for lots of ice, with a few scattered very light showers reaching the ground, even a few drops here in Sutherland Heights a little before 5 PM, qualifying for a day with a trace of rain.    Imagine!  Rain!  What izzat?

Here is that day below (if you want the short version, go to the U of AZ time lapse film department, online here).

Day Summary: Sunny with Altocumulus castellanus/floccus virgae in the early morning, then in the late morning, Cumulus humilis and mediocris, the latter with virga;  Cu grew into shallow, but very cold Cumulonimbus capillatus (lots of “hair”-ice), with virga and RWU (rain showers of unknown intensity) in a couple of spots.   Sunny again in mid-afternoon, but Cumulus re-developed in mid-late afternoon with more virga and some Cu reaching the shallow Cb stage with sprinkles here and there.

That’s it, in kind of a jumbled form.   Hope you logged all these clouds and changes yesterday.

 

DSC_0085
9:55 AM. Altocumulus castellanus/floccus virgae
DSC_0092
11:06 AM. Cu developed rapidly over and downwind of the Catalinas. Lots of ice at far left, indicating how cold those clouds were, likely around -20 C (-4 F) at cloud top by this time. Bases, too, below freezing by this time.
DSC_0095
11:10 AM. A classic, gorgeous example of Ac castellanus and floccus (the latter has no base, just a turret).  No ice visible here.
DSC_0116
2:07 PM. Cold Cumulus and Stratocumulus filled in as trough apex was about to pass overhead (wind shift line, one you can see in the movie linked to above).
DSC_0117
2:08 PM. Rain showers reach the ground toward Marana whose city limit is pretty much everything you see in this photo I think…
DSC_0121
2:36 PM. Snow on The Lemmon!
DSC_0129
4:00 PM. Clearing developed for awhile in the mid-afternoon, but then Cu were quickly reforming. Lots of ice again in this one at left, the oldest portion of the cloud where droplets are evaporating, but the ice becomes visible because it doesn’t evaporate as fast as the droplets do. BTW, air flows THROUGH the cloud, youngest portions on the upwind side, oldest portions downwind.  You want to know that if you’re flying around with a research aircraft because if you’re only targeting the young portions, you’re not going to find the “correct” amount of ice that developed in that cloud.  Some researchers apparently did this and reported in journals anomalously low ice particle concentrations for the cloud top temperatures that they sampled.  For the sake of courtesy, I will not mention their names.  But this is why at Washington, we always found a LOT of ice because C-M /we knew where to go!1
DSC_0143
4:31 PM. This was probably the deepest cloud of the day, and there is some suggestion of soft hail (“graupel”) falling out as would be an indicator of some higher liquid water contents before it converted completely to ice. Graupel comes from ice crystals or snowflakes that have bumped into a lot of supercooled cloud droplets that then freeze instantly on the crystal, helping it fall faster and collide with more droplets on the way down, a process called “”riming.” Pilots know full well about riming.
DSC_0155
6:24 PM. Nice sunset color in clouds and on the mountains.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Don’t see any weather ahead that I like, and so not talkin’ about that today.

—————————————-
1One of the many pioneering innovations here at “cloud-maven” is the novella-sized figure caption.

Cumulus and ice

Today:

Virga here and there, chance of sprinkles through early afternoon, then blammo, clearing as wind shift aloft makes it way across Oro Valley/Catalina.  CLouds will consist of Cumulus mediocris virgae, small Cumulonimbus capillatus virgae.  Cloud bases will be below freezing and higher than Ms. Mt. Lemmon, so will be tough to get rain down to the lower elevations, though a virga trail may hit The Lemmon.  Tops of Cu, -15 C to -25 C, i.e., cold enough for ice formation, of course.  Crystals will be mostly stellars and dendrites with some clustering into aggregates we would normally call “snowflakes.”  Some of the very coldest tops will contain some solid columns, maybe some prisms and hexagonal plates.

If you’re having trouble here because you’ve forgotten a few things, you might well want to get your Magono and Lee (1996) ice crystal “bible” and review crystals types and the temperatures they form at.  Heck, maybe I’ll just put the first couple pages here for you…Magono and Lee (1966).  Everybody had one back then.  Very important to have that with you.  As a further challenge, I have not rotated two pages to the upright position to make it too easy for you.

I suppose, too, that you COULD hire an small aircraft to go up there and check on these predicted types using the old “black glove” technique of the early 1960s, where a scientist would stick out a black-gloved hand from the passenger side of the aircraft and then report/log the ice crystals he found.  Not making this up.

 Yesterday’s clouds (something’s “wrong”)

Day started out dusty; ended up dusty.

8:16 AM.  Dirt roads 'n' dust, that's who we are.  Got some Altocumulus, but they are so high and cold (-30 C) that they transformed into patches of Cirrus clouds almost immediately.  Pretty normal, even at temperatures that low for a liquid drop to form first, followed by freezing.  Weird.
8:16 AM. Dirt roads ‘n’ dust;  that’s who we are. Got some Altocumulus, but they are so high and cold (-30 C) that they transformed into patches of Cirrus (ice) clouds almost immediately. Pretty normal, even at temperatures that low, for a liquid drop to form first, followed by freezing. Weird.

 

8:23 AM.  Here, a real bird, not a fake one, begins to notice something extraordinary; the virga trails from the parent cloud are going the "wrong way", toward the northeast!
8:23 AM. Here, a real bird, not a fake one, begins to notice something extraordinary; the virga trails from the parent cloud are going the “wrong way”, toward the northeast!
8:35 AM.  "What's going on here?", the photo asks.  Well, the virga trail is going FASTER and leading the head or "generating cell" from which it issued, meaning the wind increases with velocity going down, not UP, as usual!  Incredible, really!  Hardly ever see this.  Is it due to global warming, the polar vortex has maybe turned upside down?  I think so.
8:35 AM. “What’s going on here?”, the photo asks. Well, the virga trail is going FASTER and leading the head or “generating cell” from which it issued, meaning the wind increases with velocity going down, not UP, as usual! Incredible, really! Hardly ever see this. Is it due to global warming/climate change, the polar vortex has maybe turned upside down? I think so.  Has annotations on it.

 

12:07 PM.  Then I saw this, a cloud with no name, but could be the silhouette of a polar bear, eyes and head at lower left.  Can't be Cu fractus, but a thermal has pushed a damp layer up here, causing a concave shape.  You don't want to fly that small plane in or below this cloud, looking for ice.  It would be real bumpy.
12:07 PM. Then I saw this, a cloud with no name above the Catalinas.  Could be the silhouette of a polar bear, eyes and head at lower left looking downard, asking what have we done to it? Its white, too.   Can’t be Cu fractus, though a thermal has pushed a damp layer up here, causing the concave shape.  You don’t want to fly that small plane in or below this cloud, looking for ice. It would be real bumpy.

DSC_0059Above, through the dust, for some perspective of our ghost  “bear.”  Pretty cool, huh?  I hope there are some left by the time I get done with this blog!  Maybe I should check….let’s see what the Canadians (well, one Canadian at U of Victoria) has to say about this dire sitiuation, get informed about stuff.  Here’s a link provided by the climate provocateur, and former WA State Climatologist, Mark Albright, who forwarded it to me for my own illumination.  I found that post interesting, unexpected…maybe you will, too.

12:39 PM.  Iridescence in Cirrocumulus patch.  Very pretty for a minute or two, then gone.
12:39 PM. Iridescence in Cirrocumulus patch. Very pretty for a minute or two, then gone.

 

 

3:24 PM.  Day ended up cloudy and dusty with some areas looking like sprinkles could have fallen out and reached the ground, but nothing here, and echoes on radar were awful weak when present.
3:24 PM. Day ended up cloudy and dusty with some areas looking like sprinkles could have fallen out and reached the ground, but nothing here, and echoes on radar were awful weak when present.

 

Rain continues to show up on the forecast horizon, which is about 8 days

Best chance of rain, 21st-23rd, mods fuzzy on which day has the best chance.  If you love spaghetti, you’ll love this one below.  The vast change in the pattern, indicated for almost two weeks now, is just about here.  Some mod runs have rain as this “trough bowl” develops, and a strong trough passes through from the west.  Seems more likely than not from here that rain will fall as that happens.

Valid for 5 PM AST March 22nd.
Valid for 5 PM AST March 22nd.

The End. (Nice sunrise, lots of Ac cas, Sc, virga around!)

Dusty Sunset..

..will be playing your favorite western tunes in the inimitable style of Johnny Cash at the Whistling Cactus Bar and Hitching Post this Friday and Saturday…  :}   (Hahahaha;  “inimitable style of Johnny Cash”; that means Cash’s style can’t be imitated!)1

6:37 AM: I see now that there’s a lot more dust than last evening! Wow. Dusty Sunrise!

DSC_0029
4:13 PM. Cumulus fractus. Dust is visible if you look hard on the horizon. The back scattering of sun light from dust aerosols makes them hard to detect looking away from the sun. But looking toward the sun, the sky has a whitish, gritty look as we had yesterday. When smoke aerosols are present, the sun can appear very orange or reddish, not white in the mid-day-afternoon hours.  See the photo below, taken in the forward scattering direction, that whitish look near the sun.  For those who want to go deeper, this.  Images here.
DSC_0026-1
4:12 PM. Whitish, gritty dust exits Tucson and envelopes  Mark Albright’s house in Marana/Continental Ranch, carried on a SE blast of wind from Texas and NM.

 

6:11 PM.  Same view as above but most of the sun's white light has been scattered out leaving the longer yellow and orange wavelengths to carry on.
6:11 PM. Same view as above but most of the sun’s white light has been scattered out leaving the longer yellow and orange wavelengths to carry on.
DSC_0036
6:20 PM. Classic appearance of a dusty sunset.

 

Satellite image of aerosol content as seen from above (:}.  Green area is the dust plume that appeared to originate in SW Texas and southern NM, then blew into Tucson town yesterday afternoon.
Satellite image of aerosol content as seen from above (:}. Green area is the dust plume that appeared to originate in SW Texas and southern NM, then blew into Tucson town yesterday afternoon.  Looks like its still here this morning.  Go here to see more jpegs of aerosols.

Today’s mix of clouds and dust

Cloud action today, likely some small Cu and Ac later today as a weak upper level trough approaches and passes over us.  Should be enough clouds around to pose a sprinkle threat.  Imagine.

Should be an especially interesting day for cloud watchers since the dust aerosol should get into the small Cu.  Sometimes that can lead to much larger cloud droplets in them because the dust particles are so much larger than the usual aerosol stuff that gets into our clouds.

What does that mean?

Will help those lower Cumulus clouds to form raindrops, since the larger the cloud droplet, the higher the temperatures at which ice forms.  Sometimes, even drizzle drops, formed from just droplet collisions can result in  Cu mediocris clouds with large dust particles in them (no ice involved).  Would sure like to have an instrumented aircraft in the clouds of today!

Normally, ice would be expected to form at temperatures below about -10 to -12 C here in AZ.  Today, it might be higher with virga falling from shallower clouds than usual.

 The weather ahead

Found some rain for ya…  March 21st.2014031300_CON_GFS_SFC_SLP_THK_PRECIP_WINDS_216  See those green areas in SE AZ?  Been quiet on rain lately.  Don’t like to talk about rain when there’s none indicated for two weeks at a time. The rain shown for us on the map above has been coming and going around this date in the model runs, mostly going, actually, but scored one here based on yesterday’s 5 PM AST global data and that has allowed me to take the rain muzzle off.

So….in sum, we can look forward to another chance of rain in March, one just ahead, and, of course, more of “Dusty Sunset” in the meantime leading up to this chance.

—————————

1Saw a vinyl record album with those EXACT words on it in the Durango Market  on Main Street, Durango, back in the ’70s when I lived there.  Pretty funny, because you KNEW that imitating Johnny Cash was exactly what that singer was going to do!

 

Cirrocumulus display

First, it behooves me1 to point out that there remains a considerable amount of uncertainty in the weather WAY ahead.  This is demonstrated below by the map from the NOAA spaghetti factory from last evening, one that  churned out a LOT of “spaghetti”, perhaps making the point about how chaotic weather is:

Valid at 5 PM, March 26th.  Doesn't matter where Arizona is.
Valid at 5 PM, March 26th, two weeks from now. Doesn’t matter where Arizona is;  although, although… when I look really close….I think I can see some rain for us.  The lines are selected contours of the height of the 500 mb surface, after slight errors have been introduced to the initial state of the forecast model.   The actual forecast of those contours is in their somewhere.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Yesterday’s Cirrocu

Late yesterday, a thin moist layer moved in and produced, where the air was lifted that bit more, a little patch of Cirrocumulus, our most delicate cloud.

5:09 PM.  Cirrocumulus.  No ice apparent.
5:09 PM. Cirrocumulus. No ice apparent, something that would blur the spaces between the tiny cloudlets.  Height was about 17 kft above the ground, temperature, -15 C.  So delicate!

 

6:28 PM.  Line of Altocumulus  enhances sunset.  Too thick, elements too large to be Cirrocu, though they were both at the same height yesterday.
6:28 PM. Line of Altocumulus enhances sunset. Too thick, elements too large to be Cirrocu, though they were both at the same height yesterday.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

I think that covers just about everything.

The End.

——————-
1What an odd expression, to “behoove oneself” in effect, as in becoming a perissodactyla, while doing something you feel you must do as a responsible person.  Imagine, before issuing a responsible statement, that it was normal for people to put on hooves, or to wear them when coming out to a news conference to announce something responsible, correct the record, etc.  Perhaps, if it wasn’t that bad, you would wear only one hoof…

High cold ones

Web crawlers:  This is not about Rocky Mountain Silver Bullet Beer1.

Lotta wind last night.  Gusts to 50 mph here in Sutherland Heights, stuff all over the yard.  I didn’t mention anything about excessive wind coming last night, and so there’s no point in mentioning it now.  I’m a cloud-maven, not a wind-maven….

Here’s yesterday afternoon’s sounding from Tucson, around the time we had all that ice pouring out of just about every Cumulus humilis and mediocris around:

The TUS vskkppm sounding, launched around 3:30 PM AST.  A quite fascinating finding just now, is that when you type letters on the keyboard, and miss by only letter, you get a quite different word. Above, the Polish word, "
The TUS vskkppm sounding, launched around 3:30 PM AST. A quite fascinating finding just now, is that when you type letters on the keyboard when you’re not looking at it, and miss by only ONE letter to the one you are targetting, you get a quite different word.  Above, the Polish word, “vskkppm”, which was meant to be “balloon” in English2.  The arrows denote bottoms and tops of those small Cumulus yesterday, -17 C and the deeper ones (a km or 3 Kft thick), tops maybe around -25 C,respectively;  the bottom temperature exceptionally low  for Arizona.

The high cold ones of yesterday afternoon

9:53 AM.   Reminescent of a summer's day, Cumulus begin taking shape over the Catalinas.
9:53 AM. Reminiscent of a summer’s day, Cumulus begin taking shape over the Catalinas.  At this time, tops are near freezing, too warm for ice.  As the day worn on, the bases and tops of the Cumulus clouds both rose, a pretty normal sequence.

 

1:47 PM.  Not much happening yet, though Cu are now reaching "mediocris" in size.
1:47 PM. Not much happening yet, though Cu are now reaching “mediocris” in size.  Nice lighting on mountains, though.

 

1:46 PM.  Even flatter Cu to the NW-N at that time.
1:46 PM. Even flatter Cu to the NW-N at that time.  I’m thinking, by this time “Where’s is the ice?”

 

2:40 PM, about an hour later, ice began appearing in just about every Cumulus.  Here in the distance (just above home), some sprinkles likely reached the ground.
2:40 PM, about an hour later, ice began to appear in several Cumulus clouds. Here in the distance (just above the house), some sprinkles likely reached the ground.

 

3:52 PM.  Hardly a cloud around without a veil of ice crystals around it.  Its likely that cloud tops (and bases) rose to temperature below -15 C during the mid-afternoon hours.  Here, even Cu humilis are emitting little, hazy-looking ice plumes!
3:52 PM. Hardly a cloud around without a veil of ice crystals around it. Its likely that cloud tops (and bases) rose to temperature below -15 C during the mid-afternoon hours. Here, even Cu humilis are emitting little, hazy-looking ice plumes!

 

5:25 PM.  A snow flurry even touched the Catalinas.
5:25 PM. A snow flurry even touched the Catalinas.

 

5:32 PM.  Iced out!  The little cloud that gave out the flurry on the Catalinas in its dying phase, no more liquid water in it, and so all of the ice crystals and snowflakes in it fall out or evaporate and in 20 min, it was gone.
5:32 PM. Iced out! The little cloud that gave out the flurry on the Catalinas in its dying phase, no more liquid water in it, and so all of the ice crystals and snowflakes in it fall out or evaporate and in 20 min, it was gone.
6:23 PM.  Its not windy at this time.  Wind hits just before 9 PM.   Here tiny shred clouds, remnants of somewhat larger clouds, show their ice.
6:23 PM. Its not windy at this time. Wind hits just before 9 PM. Here tiny shred clouds, remnants of somewhat larger clouds, show their ice (veil on the right).  BTW, its still windy this morning.  Should die out during the morning.

There are really no good names for the clouds we saw yesterday.  Maybe Cumulus humilis virgae?  Cumulus mediocris virgae praecipitatio (to keep the Latin discriminators)?  They have all the ingredients of miniature Cumulonimbus clouds, some vertical development, fall streaks and little shafts at times.  So, these kinds of clouds, that are COMMON in the interior of the West during the cooler half of the year, really don’t have a good place in our cloud atlases.  In fact, you won’t even find one in any cloud atlas! (Tell your friends how special yesterday was…)

 

The End.

 

 

 

 

 

 

 

 

 

 

————————-

1 In fact, a legendary beer from Colorado, sung about below by no less than John Denver, or someone who sounds an awful like him, while also describing some football coaching history at the University of Washington Huskies.

 

2You should try this and see what other languages might be recovered from your keyboard by making just the slightest of errors.

Cumulus humilis and distant icy tops

DSC_0113
3:05 PM. Classic Cumulus humilis (aka, “pancakeus”).  Its not a bad thing to be humilis.
DSC_0117
4:03 PM. Here you got yer corral, yer horse poop and pee (dark area of soil in foreground), and off on the NW-N horizon, glaciating Cumulus tops;  shallow Cbs most likely. Some rain up that way, of course.  Don’t needa radar once you detect that ice. You did detect it didn’t you?

In case you don’t believe me again, see below!  You can also find a few small amounts here in the USGS network.

24 h radar-derived precip totals for AZy.
24 h radar-derived precip totals for AZy (from WSI Intellicast)  denoted by bluish regions.  Not much more than a tenth was reported in USGS gauges,  which is what’s indicated here by radar.

Today

More bigger Cu, likely some ice/virga visible.  U of AZ mod thinks rain will be to the east and south of us.  Darn.  But, if you’re horny for rain, might be worth a family trip to, say, Douglas, take in a few drops.  Nice town, Douglas.

WAY ahead

Big changes still ahead, though lately mod runs haven’t had as big of a wet change here as I would like to see, so not reporting on that.

 

The End.

Perlucidus translucidus doesn’t get any better than this; neither does future weather

Let us begin today’s cloud lesson by examining the perfect example of Altocumulus perlucidus translucidus:

9:11 AM.  I am sure many of you were exulting over being able to add such a grand example to your ,perlucidus collection.  Quite satisfying.
9:11 AM. I am sure many of you were exulting over being able to add such a grand example to your perlucidus collection. Quite satisfying.
5:02 PM.  That Ac perlucidus got a little exuberant, thickened up to lines of Ac opacus (dense gray lines in the distance, topped by Altostratus and Cirrus.
5:02 PM. That Ac perlucidus got a little exuberant, thickened up to lines of Ac opacus (dense gray lines in the distance, topped by Altostratus and Cirrus to make the scene pretty gray.  Kind of amazing how many gray days we’ve had in the midst of drought.
6:27 PM.  The aforementioned clouds led to a nice pastel-ee sunset.
6:27 PM. The aforementioned clouds led to a nice pastel-ee sunset.

The rains of March

From NOAA’s WRF-GFS model run based on last evening’s global data, this beauty below.  A model cannot calculate more areas of rain and snow in, and west of the Rockies, than this one!  So, headin’ for a big change here in the West, as we deserve, after our AZ non-winter.  See caption for details.

Valid at 5 PM, March 22nd.  The colored regions are those in which the model has calculated precipitation during the PRIOR 12 h.
Valid at 5 PM, March 22nd. The colored regions are those in which the model has calculated precipitation during the PRIOR 12 h.  Its way out there, and could be “March Model Madness”, but, odds are we WILL be seeing rain here in Catalina after mid-month when the jet pattern changes.  Rain also indicated here overnight on the 16th-17th, and a few isolated light showers around tomorrow afternoon and evening! “Ch-ch-ch-ch-changes”, as David Bowie might say, or was it The Who1 or both? Oh, well.  I like to leave you with something to think about all day.

—————
BTW, Science mag, in their tradition of catchy, amusing titles in their plain-language summaries of peer-reviewed technical articles that appear later, ones that are generally not comprehensible, used this The Who song excerpt when titling an article about the Argentine “tawny crazy ant” (I did NOT make that name up!) invasion now affecting the southern US:  “Meet the New Boss, Same as the Old Boss”, a title cribbed from the great The Who song, “Won’t Get Fooled Again.”  Feb 28th issue, p974.

BTW, its hard to write a sentence that sounds grammatically fluid and correct when writing about the works of the great The Who band.

Speaking of ants, I used to collect big red ants when I was a kid and try to transplant them into my back yard; kind of start a local big red ant invasion.  I thought you would like to know that about me.

The End.

Signal in the spaghetti; updated with climate info from Science mag just now!

Here it is:

Valid two week from now, Thursday, 5 AM, March 20th.
Valid two weeks from now, Thursday, 5 AM, March 20th.  Massive trough, at last, settles into the West for awhile, more in keeping with climo.   Keep jackets at the ready.  Rain?  Dunno yet, but probably on the correct side of 50-50 beginning around the 17th.  Changes!  Warm and dry for a coupla days, followed by a parade of troughs, quite a few minor ones over the next week or so, before the Big One forms.  Above, this is a VERY strong signal in the spaghetti for two weeks out, and so got pretty excited when I saw it, as you are now, too.  So, when mid-March arrives, get ready!

Was going to close with this NWS forecast for Catalina (might be updated by the time you link to it), but then saw just now that Saturday, the day a cold, dry trough is over us, it’s predicted to be 76 F here in Catalina,  too warm.  I would prepare for upper 60s.

Canadian model has even had rain near us at times as this trough goes by on Saturday, but only here in the 11th hour (from yesterday’s 5 PM AST run) has the US model indicated that the core of the trough and rain near us on Saturday, as the Canadian one had for a few days before that.  Hmmm…

The fact that any trough is ending up stronger than it was predicted, as the one on Saturday,  is a good sign of being close to the bottom (farthest S lattitude) of the “trough bowl”, that location where troughs like to come and visit.   So, maybe this is a precursor for us, this unexpected little cool snap on Saturday.  Maybe climatology is beginning to work its wonders at last in the West.

Powerful storms begin affecting the interior of the West and Great Basin in 10 days, and that pretty much marks the time when the winds here start to pick up to gusty at times as strong low centers develop to the north of us, and the major jet stream subsides to the south toward us.

It will be the end of the warm winter era for us, too.  While cold settles in the West, it will mean very toasty weather back East from time to time, something those folks will greatly enjoy.

———————–Climate issue commentary; skip if you’re happy with the climate as it is now—————————-

As you likely know, much of the upper Midwest had one of its coldest winters ever, and just a few days ago Baltimore (locally, “Ballimore”, as in “Ballimore Orioles”) had its lowest measured temperature EVER in March, 4 F!

“RECORD EVENT REPORT
NATIONAL WEATHER SERVICE BALTIMORE MD/WASHINGTON DC
0930 AM EST TUE MAR 04 2014
…DAILY AND MONTHLY MINIMUM TEMPERATURE RECORDS SET AT BALTIMORE
MD…
A DAILY RECORD MINIMUM TEMPERATURE OF 4 DEGREES WAS SET AT BALTIMORE MD TODAY…BREAKING THE OLD RECORD OF 5 SET BACK IN 1873.
THE MINIMUM TEMPERATURE OF 4 DEGREES FROM TODAY WAS ALSO THE
LOWEST MINUMUM TEMPERATURE RECORDED ON ANY DAY IN MARCH FOR
BALTIMORE. THE PREVIOUS RECORD MINIMUM TEMPERATURE FOR MARCH WAS 5 DEGREES ON 4 MARCH 1873.

(Thanks to Mark Albright for this official statement; emphasis by author)

If you’ve followed some media reports, the exceptional cold of this winter has been attributed to global warming, a hypothesis that has been questioned by climo Big Whigs.  However, if it is right (which even lowly C-M doubts), parts of the upper Midwest may become uninhabitable due to cold in a warming world, quite a weather “oxymoron.”

Also, if you’ve been hearing about weather extremes and global warming (AKA, “climate change”) you really should read this by a scientist I admire, Roger Pielke, Jr., at Colorado State Univsersity, his rebuttal to a Whitehouse science adviser’s characterization of his testimony before Congress about weather extremes (they’re not increasing).

What seems to be happening in climate science is the opposite of what our ideals are.  Our conglomerate of climate models did not see the present “puzzling” halt to global warming over the past 15 years or so as CO2 concentrations have continued to rise.  However, instead of being chastened/humbled by this failure, some climate scientists seem emboldened and only are shouting louder about the danger ahead.   Presently we are struggling with a number of hypotheses about why the hiatus has occurred (e.g., drying of the stratosphere which allows more heat to escape the earth, more aerosols in the stratosphere in which incoming sunlight is dimmed some as it was due to the Pinatubo eruption in 1991, ocean take up of extra heat, the Atlantic Meridional Overturning Current slowing down, causing northern hemisphere continents to cool off.)

UPdating at 8:28 AM:  This from the “current”issue of Science (Feb 28th) about the Global Warming Hiatus (GWH):  It might be due to the cold waters of the eastern Pacific, now reigning year after year almost for the whole time of the “hiatus.” (BTW, you’ve heard of it, haven’t you, that hiatus in rising global temperatures?  If not, write to your local media sources about this.  Its pretty important.)  Science mag is $10 if you want to buy it off the newstand.

What ever the cause of the puzzling hiatus in warming, it was not accounted for in our best models right from the get go, and so, naturally there SHOULD be caution on everyone’s part until we know what happened and can get it right in those many climate models..dammitall!    Unless we know what done it, how else can we have confidence that they are going to be very accurate 100 years out????

———————————————end of climate issue/rant module————————–

Here are a couple of nice sunset scenes from March 4th, that same day it was SO COLD in Ballimore, these to help you cool off personally after I got you pretty worked up with climate issues.  Hope I didn’t spoil your day, and try not to be mad at work thinking about it.

DSC_0067
6:19 PM. Row of Cirrus lenticulars appears below CIrrus/Altostratus layer. I think they were too high to be Altocumulus lenticulars, and dissipated into ice puffs right after this shot.
DSC_0075
6:31 PM. Cirrus spissatus (thicker parts) with strands from Cirrus uncinus under lit by the sun.

 

The cloud streets of Oro Valley

3:53 PM.  Three little rows of clouds are emitted from the Tortolita Mountains to the west, drift over Oro Valley.
3:53 PM. Three little rows of clouds are emitted from the Tortolita Mountains to the west, drift over Oro Valley.  These kinds of “streets” are there, and usually emit form the same spots, every time we have a moist, but shallow layer of air, and there’s a bit of wind.  We met men would call this situation a “cloud-capped boundary layer” where air rising to form these clouds doesn’t get any higher, usually due to a stable layer like an inversion.  The visual divergence, where one of the streets looks to be going to the left, and the one on the right going to the right,  is due to perspective.  Cloud streets are virtually parallel to one another.  The flow at cloud level was toward the photographer, me.  You got Cirrostratus on top of these Cumulus/Stratocumulus clouds.  (Where clouds like these are more isolated, we call them, Cumulus, when the same clouds group together into masses, we start calling them Stratocumulus.   Its kind of a fuzzy area in our fuzzy classification system (see Catalina cloud maven’s cloud classification article in the Encyclopedia of the Atmospheric Sciences, 6 vols., yours for $2258.20, “only one left in stock”, Amazon says, and the great Judy Curry, is Ed.–better get it before its gone!

 

5:03 PM.  That little zone on the Tortolitas is still pumping out the clouds.  Compare the back edge of this larger mass (which now would be Stratocumulus) with the origin point of the previous photo.  The cloud street is the one on the left that goes off the screen.
5:03 PM. That little zone (center, here) on the Tortolitas is still pumping out the clouds. Compare the back edge of this larger mass (which now would be Stratocumulus) with the origin point of the previous photo. The cloud street is the one on the left that goes off the screen.
5:32 PM.  That Cirrostratus steadily thickened as the afternoon wore on, almost making it look like another storm was moving in.   Cumulus filled in, too, becoming large areas of Stratocumulus, adding to the anticipation of a rain.
5:32 PM. That high Cirrostratus layer steadily thickened, becoming Altostratus here,  as the afternoon wore on.  Seemed like another storm was moving in.  Those isolated Cumulus clouds and their “streets” filled in, too, becoming large, dark areas of Stratocumulus, adding to the false anticipation of a rain as a storm skirted Arizona.

The weather way ahead after the upcoming heat wave

I have been staring at this weather Rorschach test for a few hours now, and there’s not much to say about it, except that there seems to be two eyeballs near the North Pole, and maybe one of the yellow lines forming a jaw down there toward Greenland, possibly a tilted drivers cap toward Russia.

Clearly the global patterns are “unsettled”, to use one of our favorite forecasting words.  (“We will have ‘unsettled’ weather over the next few days”, as one might say in Seattle most of the year.)

Below, “troughing” is suggested in the SW, but not much.  The Asian trough, anchored along the coast of Asia, is shown moving offshore here as it should during the spring, and that in turns helps form a trough downwind in the SW US, as we see happen in the spring over the long term (in climatology).   So we can only hang our hat on climo, that these uncertain times shown below in the plot below will resolve into something better than more drought.

We can also ponder the larger question of, “How’s come we can put a man on the moon and various space junk on Mars and can’t forecast the weather beyond about a week?”  Its crazy.

Or even the vastly larger question concerning chaos theory, a theory that rests on the phenomenon that small perturbations in the initial state of unstable systems are able to make huge changes over time, thus:

“Will a space probe, going off into deep space, as is happening now, an artifact that’s not supposed to be there, unsettle the unstable Universe?”

Valid for 1700 AST, March 17, 2014.
Valid for 1700 AST, March 17, 2014.

Pretty thoughtful blog today, I thought.  Usually don’t go this deep, but it just kind of happened.

The End, or is it?