Interesting Weather Information

Tuesday, August 11, 2020

Blitzkrieg Weather: The Derecho

 It may seem odd that the title this post contains two words from languages other than English. The German word blitzkrieg meaning "lightning war" and the Spanish derecho meaning "straight ahead" (pronounced day-RAY-cho). So first some history.

HISTORICAL BACKGROUND

In 1863 Dr. Gustavus Detlef Hinrichs joined the faculty of the University of Iowa and taught physical science. In 1875 he organized the Iowa Weather Service, the first state weather service in the United States. In 1877 he published Volume 1 No. 1 of the Iowa Weather Bulletin.



In 1888 Dr. Hinrichs coined the term "derecho" to describe a line of severe wind storms that crossed Iowa on July 31, 1877. Below is his map from that publication showing how the derecho crossed the entire state causing damage all the way.


As Dr. Hinrichs discovered in his research, a derecho is a strong line of thunderstorms. He used the Spanish word for  "straight ahead"  to describe the main cause of damage - straight line winds.  As the story goes he wanted to be consistent with the term tornado which is also rooted in the Spanish language.

Tornado is from the Spanish verb "tornar" meaning to turn. Because both words, derecho and tornado, are derived from Spanish the plural forms of both derecho and tornado do not use the letter "e" before the "s". So the plural is derechos NOT derechoes and tornados NOT tornadoes. However "tornadoes" is more commonly used.

The name derecho was soon forgotten but finally resurrected in 1987 by National Severe Storms Forecast Center meteorologists Robert Johns and William Hirt in their paper, "Derechos: Convectively Induced Windstorms" (Weather and Forecasting, Vol.2 page 32).

That other foreign word in the title, the  German term "Blitzkrieg", means "lightning war". During WWII it was a way of doing battle by striking fast and forcefully and quickly breaking through the defenses of the enemy.  It is also very descriptive of how a derecho causes damage.

WHAT IS A DERECHO

A derecho is a long, line of thunderstorms (to the meteorologist a linear mesoscale convective system or linear MCS) that can live 12 hours or more, travel hundreds of miles and all the while generate straight-line winds in excess of 100 mph. While straight-line winds are its main feature tornadoes can be spawned and flooding rains and large hail can occur.
 
The image below is a radar history of the costly derecho of June 29-30, 2012 that visited the FOX19 NOW viewing area. It was the deadliest and most destructive derecho in American history. As many as 28 people lost their lives and 4 million lost power (1 million in Ohio). The highest wind gust was 91 mph in Fort Wayne, IN and hail as large as 2.75" in diameter fell in Bismarck, IL. It traveled 600 miles and lasted 18 hours.



MORE THAN ONE TYPE OF DERECHO

Serial Derecho - Most of the time a serial derecho is composed of a series of linked bow echoes in the warm sector and straddling the warm or stationary front.



Progressive Derecho - The classic progressive derecho consists of a single big bow echo, but it can be multiple bow echoes, straddling a warm or stationary front and pushed to the east or southeast by strong winds in the lower and middle atmosphere.



Hybrid Derecho - It has characteristic of both progressive and serial derechos.

Low Dew Point Derecho - Mainly a late fall to early spring phenomenon when the humidity of summer has withdrawn into the deep south.  This is essentially a series of dry  thunderstorm downbursts and has not received much study.


PROGRESSIVE DERECHO OF AUGUST 10, 2020



Derecho Aug 10, 2020
Derecho of August 10, 2020
Animation generated at http://weather.rap.ucar.edu/radar/ 
then screen captured with Camtasia and rendered as a gif

Sunday, May 3, 2020

Ohio, Kentucky, Indiana Tornadoes 1950 through 2018

I am currently working on collecting and manually entering preliminary latitude and longitude coordinates along with other information from NWS Forecast Office tornado surveys to update the map through 2019 and into 2020.

The data here are from the official NOAA SPC database updated and quality controlled in September 2019 through the year 2018.

It may take some time to load the 23 columns of data for 3559 tornadoes that touched down in Ohio, Kentucky and Indiana from 01.01.1950 through 12.31.2018. Your system may also run a bit slow but I have tested both mobile and desktop versions and have found no other problems.

Made to Zoom and Search.
F/EF Scale Color Coded
Click on a pin for Tornado Info
Zoom way in for greatest visual accuracy
Click the links below to access the interactive map



For DESKTOP: 

CLICK HERE: OH, KY, IN Tornadoes 1950-2018 Interactive Map

For MOBILE:  

1. Install Google Earth first (it is Free)

2. Use the link below for the OK KY IN tornado .kmz file 

3. Download the OKI TORNADOES.kmz and open

iPhone and Android


Tap the 3-Dot Gadget
Scroll down to "Open In" and Tap

Android - Google Earth Opens

iPhone Swipe R to L to "More" and Tap
Scroll Down to "Copy to Google Earth"


Wednesday, April 15, 2020

19 Weak Tornadoes: April 8-9, 2020 Near Cincinnati, Ohio


Click on any image for a larger version
Current Through 12:20 am 04.17.2020







Touchdown locations of the 19 Tornadoes on April 8-9, 2020

Track Map #1 Versailles, IN, Ripley Co.
Link to NWS ILN Statement
Track Map #2 north of Friendship, IN, Ripley Co.
Link to NWS ILN Statement
Track Map #3 starts south of Dillsboro, IN in southern 
Dearborn Co. ends in rural Ohio County, IN
Link to NWS ILN Statement
Track Map #4 starts  in rural Ohio County, IN and 
ends just south of Rising Sun, IN
Link to NWS ILN Statement
Track Map #5 Just east of Warsaw, KY in Gallatin Co, KY
Link to NWS ILN Statement



Track Map #6 Northwest of Dry Ridge, KY in Grant Co.
Link to NWS ILN Statement
Track Map #7 Across southern Pendleton 
County, KY south of Falmouth
Link to NWS ILN Statement

Track Map #8 North of Mt. Olivet, Robertson County, KY
Link to NWS ILN Statement

Track Map #9 Near Mays Lick, soutern Mason County, KY
Link to NWS ILN Statement


Track Map #10 Near Edenton, OH, 
northern Clermont County, OH
Link to NWS ILN Statement
Track Map #11 From southeast of Blanchester in southern 
Clinton County Ohio into rural northern Brown County, Ohio.
Link to NWS ILN Statement

Track Map #12 Newtonsville, OH in northern Clermont 
County to Lake Lorelei, northern Brown County Ohio
Link to NWS ILN Statement


Track Map #13 From south of Lake Lorelei to 
south of Fayetteville, Ohio in Brown County.
Link to NWS ILN Statement

Track Map #14 From near Kenwood across 
Indian Hill in Hamilton County, Ohio.
Link to NWS ILN Statement



Track Map #15 From near Northgate Mall across 
Springfield Township and Mt. Healthy past 
Finneytown into Wyoming, Hamilton County, Ohio.

Track Map #16 Far southwestern Ohio County, IN.






Track Map #17 Cross Plains, Ripley County, IN.

Track Map #18 Between Farmers Retreat and Dillsboro, 
Dearborn County, IN

Track Map #19 North of Bracht, KY Kenton County, KY


Thursday, May 30, 2019

Radar Views of the Brookville to Trotwood to Dayton to Riverside EF4 Tornado May 27, 2019

I will annotate and caption the images as I get time. For now here are the frames.

Using GR2Analyst here are PPI and 3D images from the tornado just east of Trotwood, OH at 0257z  28 May 2019 (10:57 PM EDT 27 May 2019).




















Monday, October 30, 2017

Cold Weekend, Cold Winter?

COLD WEEKEND!

The weekend we just enjoyed was a cold one.

On Saturday (OCT 28) the high temperature was 41° tying the record Cold High Temperature set in 1910.

On Sunday (OCT 29) it was even colder. The high was only 39° but the record Cold High Temperature for that date is 34° set in 1925.

The last time we had a high temperature as cold as 39° was March 15, 2017 when the high was 33°.

Of course you have to have chilly air to have a high of 39° but chilly air can warm 20° with bright sunshine.




Thick Weekend Cloud Cover

The key to the weekend chill is thick cloud cover working with the chilly air. The cloud cover above us Saturday was 18,000 to 20,000 feet thick (or a bit more).  Enough sunshine gets through to brighten the night sky but not enough to warm the ground which warms the air.

Thick cloud cover  kept the air cold over the weekend.

The clouds were not as thick on Sunday, but thick enough that the weak, late October sunshine could not mix them out.

"Mixing out" means surface heating by the sun causes thermals of warm air to rise. If air rises it has to sink nearby to replace the rising air. This exchange mixes the moist air in the clouds with drier air and the cloud layer can thin or completely evaporate.

In summer clouds mix out much more easily because of the strong sunshine than in the other seasons.


COLD WINTER?

Now to answer the question from Steve Horstmeyer's What's It Mean Meme #2.

One weekend of cold weather is not evidence that an entire season will be cold.

Now if we see the pattern that caused the chilly weekend persist and cold days are becoming common it could signal a trend.

For now we have to watch the  La NiƱa that is strengthening in the Equatorial Pacific.

More on that and other winter trends as they develop.

-Steve Horstmeyer

Friday, October 27, 2017

Wooly Bear - or - Wooly Bull?


Does the Wooly Bear predict the severity of the coming winter?

The short answer is no!


Wooly Bear caterpillar at Otto Armleder Memorial Park October 27, 2017

FOLKLORE

Folklore tells us more black means a longer, colder snowier winter and the position of the black tells you what part of winter will be the biggest headache. The Wooly Bear in the photo is black at its head and tail-end so tradition tells us winter will have a harsh beginning and end but a  long, mild, uneventful middle.

The Wooly Bear's body has 13 segments which tradition tells us correspond to each of the 13 weeks of winter. 

FOLKLORE HISTORY

Wooly Bear folklore has a rich, long history and has it origins in Colonial America.  
The year 1938 was a banner year of the Wooly Bear myth. 

In that year Dr. Howard Curran, curator of entomology from the American Museum of Natural History, went to Bear Mountain State Park, up the Hudson River from New York City,  He counted the brown bands on 15 Wooly Bears and made the first winter prediction based on the caterpillars that eventually become Isabella Tiger Moths.  

The story was published by the New York Herald Tribune and picked up by the national press. 

NAMES

Wooly Bear - Northeast U.S.
Wooly Worm - Southeast U.S.
Hedgehog Catepillar - because it often curls up in a defensive position when touched

What's Really Going On?

The amount of black and orange-brown depends on the age and species of the Wooly Bear. If the eatin' has been good during autumn there is more black and less orange-brown.

The Wolly Bear is telling you something, but it is about the recent past not the future. Good-for-caterpillar conditions mean fat and healthy Wooly Bears and more black not a harsh winter.


Isabella Tiger Moth (Pyrrharctia isabella) - the second part of a Wooly Bear's life.