A rainy, drizzly Catalina day; 0.69 inches in The Heights

Yesterday’s cold front packed a few more rain “calories” than expected….  Kind of wrecked my play on beer in yesterday’s blog title as a way of making fun of it, you know, “Front light”.    See rain amounts below.

—————

But before that, a heads up:  1) More rain on way next week, at least a 100% chance of measurable rain during the week, and more storms after that (people will be complaining before long);

2) there are some pretty cloud photos at the very bottom in case you’d like to skip over a lotta verbiage;  quite dull writing, hand-waving, that kind of thing about what happened yesterday.

=============

Personal weather station totals as of 2 PM AST yesterday as rain ended.
Personal weather station totals as of 2 PM AST yesterday as rain ended from the Weather Underground map.  The green and yellow areas are radar echoes, yellow the stronger ones.

The official totals are pretty amazing, too, considering our best model was predicting something like 0.01 to 0.10 inches here in Catalina just before the rain started1.  Note below the 2.20 inches at Mt. Lemmon.  BTW, we’re now just about at our average rainfall total for December here in Catalina of 1.86 inches and we’ve gotten 1.85 inches so far.

Here’s a truncated rain table for our area from the Pima ALERT gauges (its a rolling archive and so you’d better get there early if you want to see the full lineup of totals for yesterday’s storm):

Pima County Regional Flood Control District ALERT System:  Precipitation Report
                              
              Precipitation Report for the following time periods ending at: 04:14:00  12/14/14
                       (data updated every 15 minutes)      
              Data is preliminary and unedited.
              —- indicates missing data
                          
    Gauge    15         1           3          6            24         Name                        Location
    ID#      minutes    hour        hours      hours        hours
    —-     —-       —-        —-       —-         —-       —————–            ———————
Catalina Area
    1010     0.00       0.00       0.00        0.00         0.51      Golder Ranch                 Horseshoe Bend Rd in Saddlebrooke
    1020     0.00       0.00       0.00        0.00         0.55      Oracle Ranger Stati          approximately 0.5 mi SW of Oracle
    1040     0.00       0.00       0.00        0.00         0.63      Dodge Tank                   Edwin Rd 1.3 mi E of Lago Del Oro Parkway
    1050     0.00       0.00       0.00        0.00         0.55      Cherry Spring                approximately 1.5 mi W of Charouleau Gap
    1060     0.00       0.00       0.00        0.00         0.75      Pig Spring                   approximately 1.1 mi NE of Charouleau Gap
    1070     0.00       0.00       0.00        0.00         0.67      Cargodera Canyon             NE corner of Catalina State Park
    1080     0.00       0.00       0.00        0.00         0.59      CDO @ Rancho Solano          Cañada Del Oro Wash NE of Saddlebrooke
    1100     0.00       0.00       0.00        0.00         0.43      CDO @ Golder Rd              Cañada Del Oro Wash at Golder Ranch Rd

Santa Catalina Mountains
    1030     0.00       0.00       0.00        0.00         0.47      Oracle Ridge                 Oracle Ridge, approximately 1.5 mi N of Rice Peak
    1090     0.00       0.00       0.00        0.00         2.20      Mt. Lemmon                   Mount Lemmon
    1110     0.00       0.00       0.00        0.00         0.55      CDO @ Coronado Camp          Cañada Del Oro Wash 0.3 mi S of Coronado Camp
    1130     0.00       0.00       0.00        0.00         0.79      Samaniego Peak               Samaniego Peak on Samaniego Ridge
    1140     0.00       0.00       0.00        0.00         0.71      Dan Saddle                   Dan Saddle on Oracle Ridge
    2150     0.00       0.00       0.00        0.00         1.34      White Tail                   Catalina Hwy 0.8 mi W of Palisade Ranger Station
    2280     0.00       0.00       0.00        0.00         0.59      Green Mountain               Green Mountain
    2290     0.00       0.00       0.00        0.00         0.98      Marshall Gulch               Sabino Creek 0.6 mi SSE of Marshall Gulch

Hell, there wasn’t any rain in the cloud band west of us when I got up, and so I thought with some lifting, and that jet core at 500 mb slipping southward from southern Cal as the day went on, rain would develop farther south in the frontal cloud band.  It did, of course, but still thought it would blow through in 2 h or so, something akin to the models as well.   The rain fell for about 5 and half hours!  The clearing took place a little before sunset, not in the early afternoon as expected.

So what happened?

I think you and I  overlooked a disturbance aloft behind the frontal band.  It was sliding SEwd fast from Nevada, catching up to our little frontal band. When those things happen, clouds magically seem to be appearing on the backside of the frontal band, fattening it up, holding its progress back; and the rain areas get bigger.  The frontal band was MUCH fatter when it went by TUS than it had been just a 100 or so miles to the west at 4 AM AST yesterday morning.  Here are contrasting satellite and radar images for two periods yesterday, before the band fattened up and the second, when it was raining so much here:

Satellite and radar imagery for 4:30 AM yesterday. Sneaky backside disturbance is represented by those clouds near Vegas.
Satellite and radar imagery for 4:30 AM yesterday. Sneaky backside disturbance is represented by those clouds near Vegas.  No rain echoes west of Catalina, stop along the Pima County line making it look like rain will be marginal here.
BY 1:30 PM in this satellite image with radar, the band is twice as wide and there's rain all the way down to Mexico way.
BY 1:30 PM in this satellite image with radar, the band is twice as wide and there’s rain almost all the way down to Mexico way.  Look how those clouds and showers near Vegas have caught up with our front, almost attaching themselves to it in north central Arizona.  Lots of times this process of upper air disturbances catching up to a front generates a cyclone along the front as the front widens and begins to kink.  I think that’s what happened anyway.  Whatever.  It was a great confluence of events for us here in Catalina.  Think how the wildflower seeds are feeling right now with already an average amount of rain for December, and its not half over, and more is on the way, yay!

If you’re a true C-M disciple you noticed something else yesterday:  true DRIZZLE in the rain.  Drizzle may be even more rare than snow here.  And the thick low visibility rain consisting of smallish drops from drizzle sizes, 200-500 microns (a couple to a few human hairs in diameter)  and raindrops just above those sizes for much of the time the rain fell,  should have made you start thinking of a warm rain process day.  Maybe there was no bright band in the radar imagery during those times, something that happens when rain is ONLY formed by colliding drops that get big enough to fall out; no ice nowhere.  In the heavier rains, sometimes when visibility was improved, ice was very likely involved.

The TUS sounding really can’t shed light on this question since the morning was had shallow clouds that weren’t raining yet, tops barely below freezing, and the 5 PM AST sounding, with tops at -10 C (14 F), was a little too late, though that layer that was sampled did produce what appeared to be ice virga in the direction of TUS about the time of the sounding.    BTW, its well known that “warm” rain processes that don’t involve ice occur at temperatures below freezing, so the expression is a bit of an oxymoron.

So, without radar imagery over us during the time of the thick rain and drizzle, we can’t say for sure, but it sure looked like it to C-M, which is  what you should think as well I think.  Thanks in advance for thinking what I think.

Enough of my excuses2, let’s rock and roll with yesterday’s clouds

Your cloud day

7:35 AM.  Light rain, looking suspiciously like "warm" rain, spreads over the Catalinas.  Its only gonna get better from here and frontal band barrels in on Catalina.
7:35 AM. Light rain, looking suspiciously like “warm” rain, clouds not looking so deep, spreads over the Catalinas. Its only gonna get better from here as frontal band leading edge is just across the street over there on the Tortolitas.

 

 

8:09 AM.  "Oh, what a crummy front, things breaking up already", you were thinking.  Also, "Look at how shallow those clouds are!  Terrible."  Sometimes these brief thin spots or clearings are called, "sucker holes."
8:09 AM. “Oh, what a crummy front, things breaking up already”, you were thinking. Also, “Look at how shallow those clouds are! Terrible.” Sometimes these brief thin spots or clearings are called, “sucker holes.”  Hope you didn’t fall for it like I did.  (Just kidding.)
9:43 AM.  R--F (text for "very light rain and fog"), rain has piled up to 0.10 inches.  But you notice there's something different about the rain, its thicker, smaller drops, even drizzle drops in it.  You begin ask, "Could this be a solely warm rain event?"  I think so.
9:43 AM.  W0X1/2 R–F (text for “indefinite ceiling,  zero, sky obscured, visibility 1/2 statute mile in very light rain and fog”), rain has piled up to 0.10 inches by this time. But you notice there’s something different about the rain; , its thicker, small thick drops hardly making a splash in puddles, even drizzle drops in it. You begin ask, “Could this be a solely warm rain event?” I think so. Note disappearing telephone poles.
12:46 PM.  After several hours of rain, flood waters begin to appear.  Note mottled surface of this lake, showing that the drops were making good splashes at this time.  Rain intensity deemed R (moderate) then.
12:46 PM. After several hours of rain, flood waters begin to appear. Note mottled surface of this small rain-formed lake, showing that the drops were making good splashes at this time. Rain intensity deemed R (moderate) then.  Deemed not a warm process rain at this time due to those drop sizes and less bunching, fewer small drops in between the larger ones, visibility was about 2 miles in rain.

The best scenes of all were when the clouds began to part in the late afternoon and evening sun.  I hope you caught these beautiful scenes:

DSC_0405 DSC_0403 DSC_0387 DSC_0377

The End

—————————————————–
1Total rain prediction from our best model, the one from the U of AZ with the predicted totals through 3 PM AST yesterday. The model run was at 11 PM AST the evening just before the rain began:

Ann RaIN THROUGH 3 PM 12-13
The arrow points to our location, in which only a tiny amount of rain was predicted. Mod doesn’t miss very often by this much, but the earlier December storm had the same mod problem, too little in the model compared to what actually fell here. Gee, new thought… Could it be a poor representation of the warm rain process? Hmmmm.

 

2Your Catalina C-M did have a correct range of amounts that could fall in yesterday’s storm right up until the last minute.  For weeks he was predicting, and staying firm with, 0.15 inches on the bottom, and a voluptuous, if that’s the right word, 0.80 inches potential on the top.

 

 

April showers and why

From your Pima County ALERT gauges, these 24 h totals ending at 3 AM this morning (covers the whole storm):

Gauge                        24                Name                        Location
    ID#      minutes    hours      
    —-     —-       —-        —-       —-         —-       —————–            ———————
Catalina Area
    1010                   0.04      Golder Ranch                 Horseshoe Bend Road in Saddlebrooke
    1020                   0.20      Oracle Ranger Stati          approximately 0.5 mile southwest of Oracle
    1040                   0.08      Dodge Tank                   Edwin Road 1.3 miles east of Lago Del Oro Parkway
    1050                   0.20      Cherry Spring                approximately 1.5 miles west of Charouleau Gap
    1060                   0.55      Pig Spring                      approximately 1.1 miles northeast of Charouleau Gap
    1070                   0.08      Cargodera Canyon             northeast corner of Catalina State Park
    1080                   0.08      CDO @ Rancho Solano          Cañada Del Oro Wash northeast of Saddlebrooke
    1100                   0.04      CDO @ Golder Rd              Cañada Del Oro Wash at Golder Ranch Road

Santa Catalina Mountains
    1030                   0.75      Oracle Ridge                 Oracle Ridge, approximately 1.5 miles north of Rice Peak
    1090                   0.00      Mt. Lemmon                   Mount Lemmon
    1110                   0.75      CDO @ Coronado Camp          Cañada Del Oro Wash 0.3 miles south of Coronado Camp
    1130                   0.24      Samaniego Peak               Samaniego Peak on Samaniego Ridge
    1140                   0.83      Dan Saddle                   Dan Saddle on Oracle Ridge
    2150                  0.12      White Tail                       Catalina Highway 0.8 miles west of Palisade Ranger Station
    2280                  0.20      Green Mountain               Green Mountain
    2290                  0.24      Marshall Gulch               Sabino Creek 0.6 miles south southeast of Marshall Gulch

The absence of precip at Mt. Lemmon is not because the storm went around it, but rather because it fell as snow.

Here in the Heights, 0.08 inches fell between 1 PM and 3 PM.  Clouds accompanied the rain.

But what kind?  That’s why I am here for you.  See way below.

First, some techno-babble.   Rain was an on and off event for Catalina and environs in the models run after run.  A forecaster friend sent many e-mails that went from “looks good for rain” here, and just about as many that said,  “doesn’t look good for rain.”  In fact, the (WRF-GFS) model run for just 12 h before it rained, had no rain here, but just a bit to the north.  What happened?

Extra sag.

Here’s the amount of trough “sag” (“amplitude”, as we would say) over Arizona predicted just 14 h before it started raining in Catalina yesterday afternoon:

12 forecast valid for 11 AM yesterday morning.  Note that the wind maximum is NORTH of Catalina, and over central AZ.
12 forecast valid for 11 AM yesterday morning. Note that the wind maximum is NORTH of Catalina, and over central AZ.

 

Areas of rain forecast to fall in the 6 h ending at 11 AM AST yesterday morning.
Areas of rain forecast to fall in the 6 h ending at 11 AM AST yesterday morning.  Rain just a tad north of Catalina.
A computer analysis of the actual winds at 5 PM AST yesterday showing that the trough had more amplitude (sag, droop, etc.) as it crossed Arizona yesterday than was forecast just a day or so in advance.  That meant we in Catalina were more embedded in the deeper, and colder clouds with this trough.  The jet stream circumcribes those clouds during the cool season here in AZ and most of the SW US.
A computer analysis of the actual winds at 5 PM AST yesterday showing that the trough had more amplitude (sag, droop, etc.) as it crossed Arizona yesterday than was forecast just a day or so in advance. That meant we in Catalina were more embedded in the deeper, and colder clouds with this trough. The jet stream circumcribes those clouds during the cool season here in AZ and most of the SW US.  See rain totals at top of blog.

In case you think I am lying again, just because I am a meteorologist and say a lot of wrong things, below is the REAL map for last evening with wind data from rawinsonde balloons on it.

From the Huskies, this 500 mb map over satellite imagery.  Strongest winds in our trough run from San Diego, Tuscon, to El Paso, with the tightest spacing of contours and strongest winds at this level in extreme northern Mexico
From the Huskies, this 500 mb map over satellite imagery. Strongest winds in our trough run from San Diego, Tuscon, to El Paso, with the tightest spacing of contours and strongest winds at this level in extreme northern Mexico

I hope you’re happy now.

Here’s what the temperature did as the windshift and rain began, in case you missed it:

Yesterday's temperature trace for Sutherland Heights.
Yesterday’s temperature trace for Sutherland Heights.

 

Yesterday’s clouds

The sequence:  cloudy, sunny “sucker hole” (one of Biblical proportions), cloudy, raining, sunny, dusty.

6:06 AM.  Altostratus and Cirrus combine to produce a gray sky.
6:06 AM. Altostratus and Cirrus combine to produce a gray start to the day.
9:44 AM.  Lower level moisture layer produces an Altocumulus lenticularis just beyond Pusch Ridge.  Seems sky will cloud up real good at this point.
9:44 AM. Lower level moisture layer produces an Altocumulus lenticularis just beyond Pusch Ridge. Seems sky will cloud up real good at this point.
Also at 9:44 AM.  Looks real bad off to the N, too, in dense Altostratus and lower Sc or Ac.
Also at 9:44 AM. Looks real bad off to the N, too, in dense Altostratus and lower Sc or Ac.

 

 

10:57 AM.  Sucker hole!  Its real sunny, warming up.   You're thinking as you ride your horse as I was, "What a bad weatherman we have!  Said would be windy, cold, and might rain, and yet here is the sun and warmth.  What a bad weatherman we have!"
10:57 AM. Sucker hole! Its real sunny, warming up. You’re thinking as you ride your horse as I was, “What a bad weatherman we have! Said would be windy, cold, and might rain, and yet here is the sun and warmth. What a bad weatherman we have!” (Weatherman is laughing in the background.)
11:44 AM.  Sucker hole starts to fill in...  Haha!
11:44 AM. Sucker hole starts to fill in… Haha!  “Dreamer” is the horse there.
12:10 PM Sucker hole filling in!
12:10 PM Sucker hole filling in more and more!  You’re starting to feel real bad that you made fun of your weatherman, but he’s still laughing at you.

 

 

 

 

 

 

 

 

 

 

1:17 PM.  Rain showing up to west-southwest, upstream.  Wind shift hits and ten degree cool off begins.  You're glad you finished your horseback ride none too soon.
1:17 PM. Rain showing up to west-southwest, upstream. Wind shift hits and ten degree cool off begins. You’re glad you finished your horseback ride none too soon.
3:54 PM.  A remarkable thing is happening.  While there's plenty of dust in the air. it is also still raining slightly, almost from drizzle-sized drops.   Eyeballig the cloud depth of the backside of the raining clouds from which the drops MAY have fallen from, CM opines that these drops are comprised of melted aggregates of needle or sheath ice crystals that were, as single crystals before aggregating as they do when in high concentrations, were really in high concentrations in those clouds, implying a strong ice multiplication phenomenon was at work.  Was really a weird scene to have so much SUN and drops falling from clear sky overhead.  I would be very proud of you if you noticed this few minute event at the end of our little rain.
3:54 PM. A remarkable thing is happening. While there’s plenty of dust in the air. it is also still raining slightly, almost from drizzle-sized drops. Eyeballing the cloud depth at the backside of the rainband clouds from which the drops MAY have fallen from, your CM opined that these drops originated with melted aggregates of needle or sheath ice crystals that, as single crystals before aggregating,  were in high concentrations (10s to 100s per liter) in those clouds, implying that a strong ice multiplication phenomenon was at work inside them. Was really a weird scene to have so much SUN and drops falling from clear sky overhead. I would be very proud of you if you noticed this few-minute event at the end of our little rain.

 

 

Rawinsonde balloon temperature and dewpoint profile near the time that it rained in clear air from the backside of our rainband.  As you can see, cloud tops were around -10 C or a little cooler, pretty warm for raining clouds here.  The main part of the rainband likely had somewhat cooler cloud tops.  Thought you like to know.  This sounding supports the idea that an ice multiplication process was at work, at least on the back shelf of these clouds that rained.
Rawinsonde balloon temperature and dewpoint profile near the time that it rained in clear air from the backside of our rainband. As you can see, cloud tops were around -10 C or a little cooler, pretty warm for raining clouds here. The main part of the rainband likely had somewhat cooler cloud tops. Thought you like to know. This sounding supports the idea that an ice multiplication process was at work, at least on the back shelf of these clouds that rained. I wanted to confirm prior ground speculations with more speculations from the sounding at rain time, though it was launched around 3:30 PM AST way over there by Davis Monthan Airbase. Wondering now if I will finish this blog today….
4:34 PM.  Shelf of rainband exits the Catalinas.  Nice lighting, though.
4:34 PM. Shelf of rainband exits the Catalinas. Nice lighting, though.
6:32 PM.  While the rain may have washed a lot of dust out of the air, more dust invaded the area as soon as the rain ended.
6:32 PM. While the rain may have washed a lot of dust out of the air, more dust invaded the area as soon as the rain ended.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

The End, finally.