Yesterday, after an ordinary beginning,, finished in a spectacular, if likely artificial way. Let us work our way through yesterday’s cloudulations:
Later that morning…..
But let’s go zooming up to flight level and take a closer look for a second:
Now, where was I? Got mammatus on my mind again. I love mammatus so much… Oh, yeah, that sunset yesterday…..
And the sun did its job….producing one of the greatest sunset scenes we’ve seen in a long time, even if phony (haha):
Finally, let look at the TUS sounding for last evening, see how cold those Ac cloud were with the ice trail in them:
The astounding thing here, something that goes against everything I believe about clouds, is that it is indicated that the Altocumulus, lacking much natural ice, was at -30° C! Yikes! No wonder aircraft were producing ice trails and stuff yesterday afternoon.
You have to conclude there were almost no natural “ice nuclei” up there at, oh about 24,000 feet above sea level. This is not the first time for such an occurrence of liquid clouds sans much ice at low temperatures1, but they are rare IME. This would never occur in a boundary layer cloud, that is, one where material from the earth’s surface is getting into the clouds, like the omnipresent dust, or biogenic ice nuclei.
The weather ahead
Some “fantasy” storms with rain in them for Catalina, are now seen on the model predictions beyond a week. Spaghetti is favoring this new development now. So, something to keep an eye on.
The view from here? Precip here is “in the bag” because going on subjective feelings, I really want to see a good rain here!
1The famous John Hallett said he saw an Altocumulus lenticularis sans ice at -35°C in a conference preprint! Rangno and Hobbs (1986) claimed to have detected droplets in Altocumulus like clouds at the top of a storm on the Washington coast at -44°C. Their claim, first published in a conference preprint, was later rejected by the J. Atmos. Sci.
Not as good as a rain day with lightning, but yesterday did have its moments in the sky, enough to make the astrologers on Mt. Lemmon jealous with displays of parhelia (“sun dogs”, or “mock suns”), faint haloes, a rare parhelic circle, something you don’t see but once every year or two, and fallstreifen (fall streaks) from Cirrus uncinus clouds going in almost opposite directions, an extremely rare sight.
The rare “parhelic circle” is a local brightening often extending out from a parhelia (sun dog) at a sharp angle, which I just learned about here1. Usually you don’t see a whole circle, just part of one.
These optic displays are caused by ice crystals, of course, ones not too complex, but rather simple ones like prisms, short solid columns, bullets, and hexagonal plates. Some examples of these can be seen here.
The bottom of yesterday’s moist layer was just above 30,000 feet at a temperature of -35° C and extended all the way up to about 40,000 feet above sea level where the temperature were around -65° C.
Some photos documenting the excitement of yesterday
Below, examples of cold Cirrocumulus, ones that quickly transition to Cirrus clouds.
If you thought those high clouds were moving faster than usual, you were right. The winds were about 120 mph at that level, about 28,000 feet above sea level, and just over 150 mph a few thousand feet above that level.
You may have noticed two things, if you are good, that there were repeated formations of delicate Cirrocumulus clouds, likely starting as liquid drops, but quickly transitioned into Cirrus. Sometimes, it was just flocculent Cirrus the whole way to us from the west.
The second thing that you may have noticed was that there was always an upwind clearing zone that remained stationary until late afternoon when it finally passed overhead. Yesterday’s high clouds formed at that back edge.
How can you tell that the upwind edge of that sheet of clouds was initially composed of liquid droplets, but then froze naturally within a minute or three as it jetted downstream?
Perform an experiment to demonstrate the two phases.
In this case we will have an ice producing aircraft fly through both regions, the droplet region, and also the region where no droplets exist because they have frozen and are growing larger and larger as ice crystals.
What will be the predictable result of two ice-producing aircraft flying through these two different phases?
In the liquid cloud region, an ice canal will develop as the appearance of ice in a droplet cloud results in the evaporation of liquid droplets, the molecules of vapor from the evaporating droplets provide “food” for fattening ice crystals, where “deposition” takes place. Under a microscope you would see the crystals getting larger, growing extensions; you would not be able to see the molecules producing that, of course.
The result of our experiment, something you likely will never see again in my lifetime:
Was holding breath, thinking about that CV enhancement, waiting for the TUS sounding, which was already in the air when these last few photos were taken, and, more importantly, it was going up near where the clouds were forming, so the moist level intercepted and its temperature would be pretty accurate for this shots. Now, if its -40 C, oh man, we got a pub! -36 C, maybe. Temperature greater than about -35 C? No pub, well, except here, which is something. That’s because liquid drops at temperatures between -30 and -35 C have been reported by remote sensing and aircraft repeatedly. Nature abhors forming an ice crystal in clouds without going through the liquid phase first.
Within a couple of hours the TUS sounding was in, and here it is:
I wasn’t going to get a journal pub. I thought about that guy that thought he was going to win the Nobel Prize…..and I know now how he felt.
Now about those pretty patterns, by Simon and Garfunkel. Enjoy.
Jet core at 18,000 feet now passing overhead and DRIZZLE or very light rain from warm processes now (4:15 AM) evident on the Catalina Mountains. The passage of that jet core at that level (500 millibars) seems to be an almost black-white measurable rain or no rain discriminator in the Southwest US, so as that happens right now, chances of some measurable rain are good. Still not expected to be more than 0.25 inches, but will now at least be 0.01!
The low clouds are pretty shallow now, and, if they rain, shallow clouds with tops warmer than -5 C (23 F) have to be pretty clean for that to happen. Clean clouds is got bigger droplets, ones that reach the Hocking-Jonas threshold of between 30-40 microns in size and can collide and stick together forming still much larger drops that collect more and more tiny cloud droplets, kind of a chain reaction, as Nobel Laureate in chemistry Irving Langmuir described it back in 1948 after he got interested in clouds and rainmaking.
However, the “collision with coalescence process will be short-lived as cloud tops go up to well below freezing level this morning, and real rain falls (as is happening now (7:18 AM) down in TUS and to our NW.
Measurable rain should be just on the doorstep, and it will have to develop in upwind clouds as they approach us and the air begins to rise as it goes uphill from the lower deserts and encounters the Catalinas’ there isn’t much in the way of radar echoes upwind of us now.
The development of rain in clouds as they approach us in marginal rain situations like this one is not terribly unusual. Sometimes, as a friend pointed out, new echoes in deepening clouds can appear over and over again near where I-10 runs to the SW and W of us in a purely orographic situation.
This is what CMP is hoping for, and the result of that might be a tenth of an inch or more.
Well, fountains spray water, and storms spray water (and snow) on the ground, so quite an unexpected confluence in descriptions, comparing fountains and storms.
That’s right, three storms are shown in the model run from last night. They been kind of coming and going, the model generally clueless about what’s really going to happen here, especially with California gully washing rains from the lower latitudes, that then affect Arizona.
However, they’re BACK, those gully washing rains in southern Cal, beginning around the 6-7th of Jan. They used to be exceptionally ferocious and floody in the WRF-GFS and came in on Rose Bowl day, that day when we were all dreaming of Ducks floating around in Pasadena. California Dreamin’, as it turned out. The floods now showing up would only be ordinary ones, at least to start.
But, “hey.” enough said about California! What about us?
A little snow overnight or the following morning after the day after Christmas. That would be the 26th. Precip amounts have to be light, since the trajectory of this cold storm is completely over land, but then that helps keep it cold, though I am not in favor of cold.
Amounts, again; Since its marginal to begin with; 0 to 0.25 inches max in melted snow water, if it snows.
Next, on New Year’s Eve, the model, as rendered by IPS MeteoStar, erupted with this Arizona “fountain” number 2:
But, as you know, when a low is predicted to be by itself, as in this case, the prediction is “iffy”. But, lows like this one, should it verify, bring the longest duration of rains and snows to Arizona, i. e,. are fabulous drought-denting storms because they move very slowly when out of the main flow. In fact this one would take more than 24 h to go by! You’d be looking at somewhere in the neighborhood of a half inch to an inch of precip here in the Catalina area.
Below, “fountain” number 3 “in preparation” as we say about our manuscripts, sometimes ones that never materialize in a journal, as it is with some of these storms the model predicts.
Truly, I say to you1, this is what dreams are made of for a southern California precipophile; get the sandbags out! Years of below normal rain, rectified! Drought busted! Let’s see what drought bustin’, mutton bustin’, cow-punchin’, drought stompin’, calf ropin’, hornswaglin’, storm herdin’ map really looks like:
Don’t even need to show what happens after this, “Juicy” out there mixes it up with some Arctic air and is slammed into southern Cal with Hawaiian-like dewpoints and rain. Just like calf ropin’. That cold air and upper jet extruding offshore will “rope” Juicy in. Lotta “warm rain” involved, too, that type of rain that forms without the need for ice.
While Juicy loses some water and some punch after southern Cal, it would still be a big rain producer in Arizona, particularly the northern half. We would likely be just inside the edge of the southern edge of this. Still, we have to be glad for the State as a whole as our water situation would vastly improve with these storms, especially storm fountains 2 and 3.
Standing by for snow and rain…. Sincerely, standing by for rain, C-M.
Yesterday’s day in contrails
Pretty upset yesterday as contrail after contrail formed and floated over Catalina. I don’t mind contrails when I’m flying somewhere, never even think of them, but when they foul the natural sky, I am livid.
Fortunately, the air got drier up there and contrails were rare after 10 AM. I can hardly stand to post this, but will for the sake of documentation so that you may be outraged as well. NIMB!
We hope this barrage was mainly due to those exceptional jet streams winds rushing down from Canada into the interior of the Southwest toward New Mexico causing airway contrails to shift over us.
Some winds between 30,000 and 35,000 feet were clocked at over 200 mph! Great if you’re going from Seattle to Albuquerqueque, but not so great if you’re going the other way.
1I had a sudden urge to say, “hypocrites!” just then for some reason. Crazy.
2″Spaghetti tasters”…. Made me wonder what happened to that great underground/alternative music band, The Oil Tasters… Remember their big hit, “Slit Chapped Lips“? Great example of what the 80s underground music scene was all about, that raw, exploration of different sounds, the overall contempt for “pop” music, the kind that makes a lot of money, like that produced by the Four Aces, etc.
(Can’t find that song about chapped lips on YouTube, its that good!) ((Later, found it!!))
((Can’t believe that I have touched the entire extrema of music in one blog, from the Four Aces on the left, to the Oil Tasters on the right, and everything in between; i.e., The Doors, 1967!)) (((Just shows you how deep your music knowledge can go; can it get any broader3?)))
3I remind the reader that if humor like this is not your cup of tea, nor the personality I effect here is also not, that my offer to stop blogging for a million dollars is still on the table.
Due to some kind of server meltdown, the NOAA spaghetti plots, better, “Lorenz plots” in honor of “Dr. Chaos”, Edward N. Lorenz, the ones my fans1 like so much, have not been available.
But they’re back today!
But what are they telling us? Gander this for Christmas Day:
Don’t need to tell you that the weather looks like there’s a good chance of cold and threatening weather for Christmas Day. Big trough implanting itself in the West around then. Maybe those easterners who hogged all the cold air last winter will share some of it this winter. The warmth we had last winter made it bad for horsey with all the fly larvae that survived.
Kind of bored now with the rain immeidately ahead, but only because everybody else is talking about it, too. Its no fun when you don’t have a scoop and you’re just saying things that other people are already saying. Even my brother in North Carolina, who knows nothing about weather, told ME that it was going to rain here on Thursday! How lame is that? Of course, it is true that you won’t here anywhere else that the chance of measurable rain is more than 100% this week in Catalina ; at least I still have that. Tell your friends.
When does it fall? Sometime, maybe multiple times, between Tuesday afternoon and Friday morning. Hahaha, sort of.
Looks like the first trough and weather system will go over on Tuesday through Wednesday, chances of rain then, and yet another colder one on Wednesday night into Thursday. So, 100% chance of measurable rain falling sometime between Tuesday afternoon and Friday morning, probably in several periods of rain. Look for a frosty Lemmon Friday morning.
Predicted amounts from this keyboard? Think the bottom of this several day period of individual rain events will be only a quarter of an inch. Top, could be an inch, if everything falls into place. Canadian mod from 5 PM AST global data yesterday, for now has dried up one of the storms, that on Thursday, the day the USA! model thinks is our best chance for good rains based on the virtually same global data! Of note, the USA model based on 11 PM AST data, has begun to lessen our Thursday storm that bit.
This is the reason that the certainty of measurable rain here in Catalina is spread over such a several day period.
Your cloud day yesterday
Just various forms of Cirrus, most seemingly from old contrails that produced exceptional parhelias (sun dogs, mock suns).
Very contrail-ee sunset, too, as contrail lines advanced from the west. They were likely more than an hour old when they passed over Catalina yesterday.
1Why just recently C-M had a comment from a fan in Lebanon3, that country near Israel, not the one in Ohio2! Said it was warm there now, but normally it rains for days at time in the winter, and gets real cold. You see, the eastern Mediterranean is, climatologically speaking, a trough bowl. Troughs just hang out there a lot, creating something called the “Cypress Low.” Though it only rains in the cool season, October through May, as in Israel, places in Lebanon get 25 -40 inches of rain during that time, and its exciting rain because it almost all falls from Cumulonimbus clouds, many with lightning! C-M is getting pretty excited, since he’s on record as wanting to go Lebanon to study the clouds there! See Lingua Franca article from 1997! He loves those Mediterranean wintertime Cu. Hell, you probably threw it out, so here it is: Lingua Franca _1997. See last sentence. last page. Thanks.
2Speaking of Ohio, who can forget that great 1980s rant against urban sprawl in Ohio by Chrissie Hinds and the Pretenders! Will it happen to Catalina after the road project? An insurance agent told me that Catalina was to be absorbed by Oro Valley after it was completed. Oro Valley says they know nothing about that.
The loop above, generated by last evening’s global obs by the Enviro Can “GEM” model might be the best a numerical model can put out for Arizona. It might even be the best model day of my life ever here (which hasn’t been that long, but still…).
1. Trough races into the precip “Red Zone”, located immediately SW of AZ. Rain moves in on Friday into Catalina and environs.
2. Trough forms circular, spinning low aloft there, that wanders slightly in place. Cloud and precip rush into Arizona, and it just doesn’t quit as wave after wave of clouds and rain move up from Mexico, the Gulf of Cal-Sea of Cortez, and the Pacific off Baja while the low center dawdles.
3. Low crosses into AZ and departs AZ late Sunday after showery day.
In sum, showery rainy conditions beginning on Friday, continuing into Sunday.
Amounts should be several inches in the mountains of AZ. Here, sans the great U of AZ calcs for the whole storm period, will go with the same “seat-of-pants” estimates of the botttom and top amounts made a couple of days ago: at least 0.4 inches (even if things don’t work out so great; low doesn’t dawdle so long). But as much as 1.50 inches on the high end here in Catalina if it DOES dawdle as this model run from last night shows and we get nailed by recurring rain bands. Best estimate, “therefore” he sez, is the average of the two, or about an inch.
It would seem some thunder now and then would also be in the mix, and BTW, we remind our reader that snow and rain mixed together is NOT SLEET, dammitall! SLEET is frozen raindrops, ones that have frozen on the way down and usually requires two to three thousand feet of below-freezing air temperatures before that happens. Also, they BOUNCE when they hit, are usually clear, and often have spikes where the water was trying to get out since they mostly freeze from the outside inward, and because water expands when it freezes, a spike or ejection of ice splinters results as freezing takes place. Kind of neat really. But its NOT rain and snow mixed together! Sorry, getting into some “sleet rage” here; need to work on it; get it under control. I just don’t want my reader to sound ignorant when rain and snow are mixed together, but rather, “precipitationally erudite.”
Yesterday’s clouds5:20 PM. Jet’s ‘n’ Cirrus. The very short contrails, formed by moisture and carbonaceous crap, oops, black stuff, in the exhaust, are short here because the jets are flying ABOVE the Cirrus.
Here’s a nice little example of how the weather computing models start to go awry fast when a little flummoxed when little DELIBERATE errors are input into them as they start their northern hemisphere data crunch (below, from the global data ingested at 5 PM AST yesterday). Us folks here in Arizona and those in the Southwest US comprise one of two “centers” of the greatest uncertainty in all of the Northern Hemisphere, as shown below in the red and blue lines (selected height contours at 500 mb).
Model outputs and what they are predicting will go to HELL faster due to our “zone of uncertainty”. Chaos in action. Wiggle something here, and it falls apart over there and all over. This example is the contour forecasts for 5 PM tomorrow.
Does this epicenter of uncertainty hereabouts mean we have a chance to get some real rain in the next 36 h?
No, but its great that you know about this uncertaity and how it plays out in the NOAA “ensembles of spaghetti”; useless-in-some-ways-knowledge, absorbed just for the sake of knowledge.
The uncertainty illustrated above is associated with a upper level wiggle in the winds and exactly how that will play out as that wiggle moves toward us from the NW today. Its a little baby trough in the upper air flow that the model is uncertain about but it is too weak to have much affect on the big cloud mass that will be drifting over us today, that cloud mass originally from a location about halfway between the Galapagos and Hawaiian Islands. These are real tropical clouds over us today, and they’ll be piled in layers (Altostratus, Altocumulus, Cirrus, Cirrostratus) over us to more than 350,000 feet!
Range of amounts here in Catalina: ZERO on the bottom to 0.10 inches, tops.
Below is an example (full set here) of what the Beowulf Cluster from the U of AZ sees in the moisture overhead at 3 PM local time (in other words, during the 84th hour of the Superbowl pre-game show). I realize that many of you will not be able to go outside and look at the sky at any time today due to this historical sports emergency, and so I will tell you something now about what you likely would have seen had you gone outside, perhaps even missing an equally historic commercial break of some kind:
What does this mean?
Weird clouds, most likely. Scoop clouds, concave (downward) looking cloud bottoms. Some areas of the sky might look like ocean waves upside down, “undulatus” clouds (we had a short-lived Ac undulatus yesterday to the NW of Catalina). Clouds with waves on the bottom. The bases of our tropical clouds are likely going to be in a “stable layer”, one where the temperature remains the same as you go up. It would be located just above the top of Ms. Mt. Lemon. Along with that stable layer, and is always a part of them, is wind shear; the wind turning in direction and speed as you go upward from just below this stable layer to above it.
Stable layers and wind shear produce waves, not ones always seen since the air is often too dry for clouds, but in this case, they should be visible. Could make for some interesting cloud shots this afternoon and evening. Here’s a risky example of what I think is likely, though with too much virga falling from above, they won’t happen, hence, the risk in a cloud detailed forecast:
Lots of contrails overhead yesterday, an unusual number. Really, we are SO LUCKY not to have many days like this, kind of a sky pollution, though at present, an unavoidable one. Just be glad we don’t live right under a main, well-traveled airway (though, with predictions of a doubling of air traffic by 2020, we are likely doomed to more days like yesterday when Cirriform clouds are present).
Our deep blue sky, loaded with interesting Cirrus clouds yesterday, and generally low in contrail impact, makes southeast Arizona a haven for Cirrus cloud watchers. Though no one site is completely immune from them, a sky like this, so free of contrails, is impossible on most of the Atlantic Seaboard due to air traffic. It was just so pretty here yesterday with so few contrails! Here are a few shots:
The weather ahead: cold front’s a coming
Its been well predicted for 1-2 weeks that a cold front would pass through our area on Dec 9th-10th. At times the models had substantial rain here, but it’ll be a dry blast from the north Sunday night. What makes us here in Catalina a little different in experiencing this frontal passage is that the high pressure behind the front pushes air along the Catalina mountains from the north here, and we often get quite a windy episode, 15-30 mph likely Sunday night. But, because we have no official weather reporting stations, and the Catalina Mountains block that north wind from Tucson so that they don’t get it, so us here in Catalina are about the only folks that know its quite windy, with a chill in the air.
This cold front is part of a large scale pattern change in the jet stream that is taking place, one that will vastly increase our chances of rain in the weeks ahead as storms barge into the Pacfic Coast farther south than they have and head this way. No longer will we be in a stagnant condition where day after day the weather is almost exactly the same; not much wind, temperatures above normal. Instead there will be occasional windy episodes as storms get close, temperatures closer to normal, and we hope, one that gets far enough south for a good rain.
Some rain is showing up now overnight on the 13th-14th. In our rain frequency chart, the peak rain days in December were the 11th-13th, deemed a statistical fluke from this keyboard in the 35 year record.
But, here’s a rain threat materializing in the very window. Hmmmm. Further, if you look at the spaghetti plot for this time period, a trough is guaranteed in this region on the 13th-14th, though getting circumscribed by the jet stream that is, its south of us as the trough goes by is what’s marginal with this trough situation, a requirement for almost all winter rain here.
Usually when you get carried away and expect something unusual to happen, it doesn’t, like that girl I thought liked me but didn’t (there have been a number of those…) Yesterday, carried-away Mr. Cloud Maven person mentioned the possibility of tubes in Cal. Here’s the report in the Big Valley near Merced, CA, from yesterday. Big hail, too. I am pumped! Spiking fubball now!
0535 PM FUNNEL CLOUD ATWATER 37.35N 120.60W
04/12/2012 MERCED CA PUBLIC
3 DIFFERENT FUNNEL CLOUDS IN THE ATWATER AREA
0605 PM HAIL ATWATER 37.35N 120.60W
04/12/2012 M1.75 INCH MERCED CA AMATEUR RADIO
Official name of tube-producing clouds? Oh, something like, “Cumulonimbus capillatus incus (has an anvil) tuba.”
Actually, its not terribly unusual to have tubes in Cal when the air is extremely cold up top over Cal in April and May, and that’s what we have now. Take a look at this nice, compact map from San Francisco State Former US Hippiedom Capital Weather Department for last evening at 5 PM AST. At San Francisco, its -29 C at 500 mb, very unusual for mid-April. (Actually, they got some real nice maps there.) Combine that with the strong sun on land surfaces, and voila, Cumulonimbus galore!
Also, if you look carefully, you will see that where there is no data, over the Pacific Ocean, the 500 millibar pressure contours are nice and smooth . But notice how “nervous” they get once crossing the coastline where there is data. I think really it has something to do with the interpolation scheme that try to place the contours exactly at the right spot between the real data; that algorithm may be a little primitive. Kind of funny in a way.
That cold core of air is heading for Arizona, and no doubt some April low temperature records will be set, such as lowest maximum, and likely a few minimum temperatures before this passes on into the Plains, with no doubt true severe weather there the result of that. And we, too, will have some Cumulonimbus clouds, lightning here and there around the State.
Below the SFO State map is the forecast from IPS Meteostar showing where this mass of cold air will be later Saturday at 5 PM AST, northern AZ. U of WA WRF-GFS mod thinks rain will be occurring here just about ALL DAY on Saturday after beginning around dawn! That would be a heckuva cold day, winter-like, with temps in the 40s-50s here at 3,000 feet and we’d have those pretty white Catalina Mountains afterwards. Sure seems like 0.20 inches is in the bag for the bottom of this rain event, with maybe 0.50 inches being at the top here in Catalina.
Yesterday’s line of enhanced virga in As deck at sunset
Now here’s an odd feature. Looked at first that it might have been due to an aircraft passage in that streak of Altostratus, but then I rejected that thought, as I can do. I came to believe somewhat confidently, odd as it is, that it was natural. Natural linear features in clouds are fairly common. Here it is, in case you missed it:
Apparently the castellanus formations went over during the nighttime hours when we couldn’t see them…
But it was a fabulous day again of interesting high and middle cloud flecks anyway. Below, a reprise of yesterday’s clouds starting with that delicate patch of Cirrus passing over the Catalina Mountains with its tiny fibers of Cirrus uncinus embedded in it. I have also included two sinister crossing contrails. Who knows what evil lurks there? Perhaps they’re marking a target of some kind, or filling out a questionnaire with crosses instead of check marks. Oh, well.
Later, as the sheet clouds of various Cirrus, Cirrostratus, and even Altostratus with virga cleared off, we got into some scattered lenticulars, some of to the distant north, and with our usual friend downwind of the Catalinas, shown in the last two shots. It was able to hang on for several hours, right past sunset.
Again, for the whole day’s cloud excitement, a great place to go is to our very own U of AZ Wildcat time lapse movie. In the late afternoon of this movie, you can see some great Altocumulus lenticularis clouds hovering over and downwind of the Catalina Mountains, occasionally shooting upwind as the air moistens in the humped up airflow, and you can get a sense of how little the air is pushed up in lenticular clouds from this movie.
(Once again the caption function has quit in WP before I got to some of these. My apologies.)
The weather ahead
Gee, “dusty cold snap” is beginning to look more like “muddy waters” as the later model runs dip the jet stream farther and farther south over us on the 14th and 15th. Check this forecast of the precip hereabouts from the U of WA’s WRF-GFS model run from last night, showing a bit of rain HERE Saturday morning (colored areas of map). Sure hope so. Terribly cold air with this, too, for mid-April. Likely some low temperature records will be set in the State somewhere for this time of year with this.