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Since 2008 – Progress Through Politics

Torrential Downpours Expected Over East Coast This Week, Flash Flooding Likely

Originally posted this in jaundice. Often forget that lots of you guys don’t go there anymore, so I figured I’d post it here. Oh, and hi! Long time no see.


A ribbon of deep tropical moisture is forecast to sweep across the east coast for the next week, leading to the potential for major rainfall totals and the potential for flash flooding for much of the east coast.

Precipitable water (PWAT) is a measure of how much rain would fall (in inches) if all the moisture in the atmosphere fell as rain all at once. The higher the PWAT value, the more moisture in the atmosphere, and the more rain would fall. PWAT values reaching 2.0″ is indicative of the presence of deep tropical moisture. These maps are a good way to predict how heavy rain will be in a thunderstorm. Higher PWAT values indicate the potential for torrential downpours, especially since the thunderstorms will be slow moving or stalled.

A deep ridge of high pressure over the Atlantic Ocean will serve as an atmospheric sump pump for Central America, sucking deep tropical moisture from near the Equator straight up to the northern Atlantic, as witnessed in the images below.

These are forecast precipitable water (PWAT) maps from this morning’s run of the GFS model, valid for later this afternoon and tomorrow afternoon, respectively. These maps will look pretty much the same straight through at least Wednesday.

This afternoon:

Tomorrow afternoon:

As the high over the Atlantic strengthens throughout the week, the ribbon of tropical moisture will tilt a bit, spreading into the Deep South and covering more of New England.

Here’s the forecast PWAT map for Friday morning:

Here’s a GFS forecast sounding from eastern North Carolina very early Tuesday morning. This is a SKEW-T/Log-P chart (a sounding) showing the temperature, dew point, and wind through a slice of the atmosphere. This is the same type of chart produced from the data collected by weather balloons, only this is a model forecast.

The red line is the air temperature, and the green line is the dew point. The fact that you can’t tell them apart (the dew point is more or less equal to the temperature) means that the atmosphere is 100% saturated — a testament to the amount of moisture in the atmosphere.

This deep tropical moisture mixed with the typical summertime pop-up thunderstorm regime will lead to potential flash flooding for everyone from Florida to Maine. The Weather Prediction Center/WPC (formerly the Hydrometeorological Prediction Center/HPC) issues quantitative precipitation forecasts (QPF) for up to a week out, showing how much rain they expect to fall across the country.

Their QPF (rainfall forecast) for the next 7 days reflects the deep tropical moisture — showing 8″ of rain in the Big Bend of Florida, with pockets of 5″ of rain over parts of the southeastern United States. The WPC mentions in their discussion that even these high rainfall totals could be a “conservative estimate” given the ample moisture in the region.

The National Weather Service uses flash flood guidance maps to determine the risk for flash flooding in each county/parish in the United States. By determining the moisture content of the soil in a certain area, the NWS can determine how much rain needs to fall over a 1, 3, 6, 12, or 24 hour period to create a flash flood. The more moisture present in the soil, the less rain will absorb into the ground, and the more will run off. If enough rain falls fast enough and runs off without absorbing, it could result in a flash flood.

Take the current flash flood guidance for the DC area (shown above) as an example. The colors in each county corresponds to the amount of rain that needs to fall in one hour to produce flash flooding. DC proper and Arlington County only need to see 1″/hour of rain to see flash flooding, mainly because they’re densely populated urban areas. They have more concrete/asphalt than soil, so it’s much easier for the rain to run off instead of absorb into the ground. Fairfax County needs to see 2.0″/hour for potential flash flooding. Prince William needs 2.25″/hour. Places like Fauquier and Culpeper Counties to the west of DC need extremely heavy rainfall — 2.75″/hour — since they’re relatively rural counties with extensive farmland and fields to absorb the rain.

If thunderstorms stall over an area or start training (one thunderstorm after the other moves over the same areas, like a train on tracks) over a longer period of time, it would require more rain to produce a potential flash flood. Thus, the 3 hour flash flood guidance is higher than the 1 hour, the 6 hour higher than the 3 hour, and so on.

Here’s a current example of thunderstorms training southwest of Charlottesville, VA.

It’s worth noting that it will require much less rainfall over places like Pennsylvania and New England to produce flash flooding due to the copious amounts of rain these areas have seen in recent days. For instance, in almost all of Vermont, it will only take about 1.5″ of rain falling in a 3 hour time frame to produce flash flooding.

You can check out flash flood guidance for every state in the country at this link.

Almost half of all flash flood deaths occur in vehicles. Cars can be swept away by less than two feet of moving flood water. People can be swept away by just 6 inches of moving water. You can’t tell how deep the water is, even if you think you know how deep it is. Heed the NWS’ saying: “turn around, don’t drown.” It’s your own damn fault if you do. Don’t risk the lives of the people who have to swim out there to rescue you.

It’s summer. Torrential summertime downpours are common. But this is expected to be a prolonged event with lots of very high rainfall totals. These storms will also be slow-moving or stalled over one area. Flash flooding is likely, especially where the storms set up and train or stall, and even more so in New England where the soil is already saturated from recent heavy rains. Pay attention to your local National Weather Service office for potential flash flood alerts.

UPDATE: The National Weather Service has issued flash flood watches for the counties shaded in green. Active flash flood warnings are the dark red polygons. Expect more of these watches to be issued as the week progresses.

Don’t Fall Into The Blizzard Hype

(Also posted to DailyKos)

OH MY GOD. IT’S THE BLIZZARD OF THE CENTURY. IT’LL  BE THE WORST THING TO HAVE EVER HAPPENED IN THE HISTORY OF RECORDED HISTORY. HOLY MOTHER OF JESUS RUN FOR YOUR LIVES. THE WHITE DEATH IS COMING. LOOK AT THIS MODEL. THE MODEL SAYS A BAZILLION INCHES OF SNOW. OH MY GODDDDDD. LIKE AND SHARE TO SPREAD THE WORD.

There. Now you’ve seen all the hype you need to see about the impending nor’easter in New England. Now here are some facts.

Dangerous Tornado Outbreak Likely Across Southern US Today

(Also posted to the orange fainting couch.)

A strong cold front that is currently moving through the Central Plains states will act as the proverbial spark in the powder keg this afternoon, firing off severe thunderstorms across parts of the southern United States. Given the upper-level dynamics associated with this system, there is a moderate (several magnitudes higher than normal) risk of significant, long-track, violent tornadoes over a large area of real estate this afternoon and evening.

The Threat

The main threats today will be significant, long-track, violent tornadoes, as well as violent straight-line winds.

The SPC has issued a moderate risk for severe weather (red) across a large chunk of the south. The yellow area is a slight risk, and the green area indicates a risk for general, non-severe thunderstorms.

Here’s the tornado probability chart. An area with a 15% chance of tornadoes means that there is a 15% chance that at least one tornado will touch down within 15 miles of any point in the shaded area. The black hatched area indicates the risk for significant (EF-2 or higher), long-track tornadoes.

Here’s the severe wind (greater than 60 MPH) map. Percentages work the same as they do with the tornadoes. The black hatched area indicates a risk for severe thunderstorm winds greater than 75 MPH.

The Setup

A strong cold front is moving across the Central Plains states into a very warm, very soupy airmass being pumped in straight off the Gulf of Mexico:



Dew point map as of around 1130AM Central. The greener, the moister.

A cold front ramming into this warm unstable air will wreak havoc for the areas outlined by the Storm Prediction Center above. Winds at 850 millibars (about 5500 feet off the ground) are screaming along in what’s called a low-level jet (LLJ), reaching speeds of almost 80 MPH. Winds at the jet stream level (30-35,000 feet off the ground) are moving along at almost 175 MPH.

This change in speed and direction with height is called wind shear, and along with the massive amounts of instability from the warm air, and the forced lift from the cold front, extremely strong storms are expected to develop this afternoon.

The storms are initially forming as individual supercells, which carry the greatest risk for tornadoes. Over time (probably later tonight) these supercells will start to merge with each other and create an intense squall line along the cold front as it heads into the southeastern and eastern parts of the United States.

CORRECTION: The supercells are forming out ahead of the main squall line along the cold front. The individual, more dangerous storms will come through first with the tornado threat, and be almost immediately followed by the damaging winds of the main squall line.

What we’re most concerned about are the supercells that form before the squall line. The shear I mentioned before creates a horizontal rolling motion in the atmosphere — think of a cardboard tube tilted on its side. This rolling tube of air can be tilted vertically by the strong updrafts in thunderstorms, making the entire storm begin to rotate.

This rotation is what facilitates the development of tornadoes. We measure this with something called “storm relative helicity.” Essentially, the higher the number, the more likely we are to see strong tornadoes. The threshold changes based on a number of factors, but in this type of setup we typically see tornadoes begin to form with SRH values of around 250.

SRH values are expected to climb up beyond 500, especially over Arkansas, this afternoon.

The supercells, by nature, will eventually form into a strong squall line and move east. When this occurs, the tornado threat will die down and the damaging wind threat will ramp up.

GET A WEATHER RADIO

National Weather Service Main Page

National Weather Service — Central Oklahoma

National Weather Service — Dallas/Ft Worth TX

National Weather Service — Tulsa OK

National Weather Service — Springfield MO

National Weather Service — Arkansas (whole state)

National Weather Service — Paducah KY

National Weather Service — Shreveport LA

National Weather Service — Memphis TN

National Weather Service — Jackson MS

National Weather Service — Huntsville AL

National Weather Service — Birmingham AL

Storm Prediction Center Main Page

Storm Prediction Center — Current Severe Weather Watches

Storm Prediction Center — Convective (Severe Weather) Outlooks

Storm Prediction Center — Mesoscale Discussions

Storm Prediction Center — Storm Reports

Storm Prediction Center — Mesoscale Analysis Pages

Wunderground’s Detailed Radar (click the + nearest to you to see your local radar)

NOAA Weather Models

TwisterData.com’s excellent GFS/NAM/RAP model website.

I’ll continuously post updates to my Facebook page on this and most other major severe weather outbreaks.

Fifty Meters of Doom — The Difficulty of Winter Weather Forecasts

Parts of the southeastern United States had a mild but nasty ice storm this past Friday. Ice storms in January in the southeastern United States are far from unheard of, but this one threw people for a spin because it was so cold that one would normally expect snow rather than rain.

“It’s 22 degrees. Why is it raining instead of snowing?”

One of the easiest things to forget for people who usually don’t track weather is that the atmosphere is alive and deep. In the United States, there’s usually between 7 or 8 miles of troposphere above you — the layer of the atmosphere in which the weather occurs. Subtle changes at any level within that layer means big differences in what kind of weather you’ll encounter at the surface.

IN YO FACE

For my second post at the Moose, I’d like to offer a detailed, thoughtful political treatise I hope you all will enjoy and carry near and dear to your heart as you fight the good fight over the years.

Hah! Yeah right.

To everyone who ever said that President Barack Obama simply would not win re-election without their sage political advice and ANGRY COMMENTS IN ALL CAPS, I offer the following:



In the immortal words of Nelson Muntz: HA HA.  

The Weather

Yo.

*No thunderstorms over the next 4-5 days.

*Snow confined to the far northern US where it’s supposed to snow in January.

*Snow showers are possible in/around DC on Inauguration Day, but it shouldn’t be anything apocalyptic.

*It’s going to be bitterly cold next week. Temperatures will struggle to break freezing during the day in most of the Mid-Atlantic and Midwest starting on Monday. Low temperatures will approach single digits and subzero levels in many places the first half of the week — the Washington DC area will see temperatures in the low- to mid-teens on Monday, Tuesday, and Wednesday nights.

*Auroras are possible tonight at far northern latitudes.

*An asteroid the size of a Boeing 757 will miss Earth by 21,000 miles (9% of the distance between the Earth and moon) on February 15th.