Yesterday's wind storm is summarized in the cart below. Wind gusts ranged from 25 and 30 mph before noon.
These gusts are nothin' compared to what they experienced in Davis County
In comparison, a category one hurricane has sustained winds of 74 mph.
Wednesday, December 31, 2014
southern snow
Tuesday, December 30, 2014
A Blustery Day
source: KSL.com |
Still, winds in Spanish Fork are stronger today than normal on this downslope windstorm type of day. The ten minute averaged winds are around 15 mph and gusts nearing 30 mph.
However, winds are much stronger further north. At the University of Utah, on top of the William Browning Building, ten minute average wind speeds are 25 mph with stronger winds at the mouth of Red Butte Canyon. Gusts are over 55 mph.
And the temperature just keeps dropping, currently 10 degrees F. That's a cold wind. The wind chill makes it feel like -12 degrees F.
And a little further north, in Farmington, some of the strongest winds have been reported. This station currently is reporting sustained winds of 44 mph with gusts up to 77 mph! Surrounding stations measure similar wind speeds and gusts.
I remember being told that Lagoon's ferris wheel, the Sky Ride, was built to withstand a hurricane. We don't have hurricanes in Utah (obviously), but we definitely get hurricane strength winds.
Clearfield Traffic Camera with blowing snow. source: UDOT.utah.gov |
source: KSL.com |
These high winds will last most of the day and into the night. By this evening you may have new snow to shovel while you're neighbor will be lucky enough to have no more snow in their yard. It all depends on where those snow drifts settle.
From the National Weather Service:
High Wind Warning
URGENT - WEATHER MESSAGE NATIONAL WEATHER SERVICE SALT LAKE CITY UT 202 AM MST TUE DEC 30 2014 UTZ002-302300- /O.CON.KSLC.HW.W.0011.000000T0000Z-141231T1100Z/ NORTHERN WASATCH FRONT- INCLUDING THE CITIES OF...BRIGHAM CITY...OGDEN...BOUNTIFUL 202 AM MST TUE DEC 30 2014 ...HIGH WIND WARNING REMAINS IN EFFECT UNTIL 4 AM MST WEDNESDAY... * AFFECTED AREA...THE NORTHERN WASATCH FRONT FROM BRIGHAM CITY SOUTHWARD TO NORTH SALT LAKE. THE STRONGEST WINDS ARE OCCURRING BETWEEN LAYTON AND BOUNTIFUL...INCLUDING FARMINGTON AND CENTERVILLE. * WINDS...EAST WINDS GUSTING IN EXCESS OF 60 MPH...WITH LOCAL GUSTS IN EXCESS OF 75 MPH. * TIMING...THE STRONGEST WINDS ARE FORECAST TO OCCUR THIS MORNING...PEAKING MID TO LATE MORNING...BEFORE GRADUALLY DIMINISHING THROUGH TONIGHT. * IMPACTS...THIS IS A POTENTIALLY DANGEROUS SITUATION. STRONG CROSSWINDS ARE OCCURRING ALONG I-15...HIGHWAY 89 AND THE LEGACY PARKWAY THROUGH DAVIS AND WEBER COUNTIES WHICH WILL CREATE HAZARDOUS TRAVEL FOR HIGH PROFILE VEHICLES AND THOSE WITH TRAILERS. SIGNIFICANT BLOWING AND DRIFTING OF SNOW WILL ALSO CAUSE GREATLY REDUCED VISIBILITY AND SLICK ROADWAYS. VERY COLD WIND CHILLS CAN ALSO BE EXPECTED...WITH READINGS OF 20 TO 25 DEGREES BELOW ZERO. POWER OUTAGES ARE POSSIBLE... GIVEN THE VERY COLD TEMPERATURES HAVE A CONTINGENCY PLAN IN THE EVENT OF A LOSS OF HEAT. LOOSE OBJECTS SUCH AS TRASH CANS... TRAMPOLINES AND LAWN ORNAMENTS WILL BECOME AIRBORNE RESULTING IN POTENTIAL PROPERTY DAMAGE. WIND SENSITIVE OPERATIONS WILL BE AFFECTED. PRECAUTIONARY/PREPAREDNESS ACTIONS... A HIGH WIND WARNING MEANS A HAZARDOUS HIGH WIND EVENT IS EXPECTED OR IS OCCURRING. SUSTAINED WIND SPEEDS OF AT LEAST 40 MPH OR GUSTS OF 58 MPH OR MORE CAN LEAD TO PROPERTY DAMAGE. VEHICLES... ESPECIALLY HIGH PROFILE VEHICLES...CAN BE DIFFICULT TO CONTROL AT TIMES IN HIGH WINDS. MOTORISTS SHOULD TAKE EXTRA CAUTION... ESPECIALLY WHILE CROSSING BRIDGES...OVERPASSES AND UNSHELTERED AREAS.
Also be aware of the elevated avalanche danger today:
THIS AVALANCHE WARNING IS FOR CANYON MOUTHS AND FOOTHILLS OF CACHE...DAVIS...WEBER AND EASTERN SALT LAKE COUNTIES. STRONG WIND WILL CREATE POTENTIALLY DANGEROUS WIND SLAB AVALANCHE CONDITIONS IN LOW ELEVATION AREAS WHERE PEOPLE DO NOT NORMALLY SEE AVALANCHES. AVALANCHE DANGER IS EXPECTED TO INCREASE TODAY AND CONTINUE INTO WEDNESDAY. THIS WARNING DOES NOT INCLUDE SKI AREAS OR HIGHWAYS WHERE AVALANCHE CONTROL IS NORMALLY DONE.
Monday, December 29, 2014
Skiing :) New Snow and Rime
Before Christmas I went on a ski trip with my cousins to Brundage Mountain. Brundage is a ski resort near McCall, Idaho. They claim to have the "Best Snow in Idaho." The days we skied didn't have the best snow, but I'd say the view is one of the best!
The day before skiing the mountain received about of foot of new snow. After the first ride up the Bluebird lift it was apparent there was a lot more weather going on the night before than just snow. Everything at the top of the mountain was covered in thick rime. The wind sensor on top of the ski patrol hut was surely not working properly.
Rime is caused when the temperatures are below freezing, but the cloud droplets aren't quite frozen--the cloud is still liquid. Water doesn't necessarily freeze at 0 degrees Celsius. It needs something to freeze onto. For example, water will freeze onto dust particles (I suppose this is why as a kid I was always told that snow is dirty when it falls from the sky).
Liquid cloud droplets below freezing are called supercooled. Riming occurs when supercooled droplets hit something they can freeze onto. The droplets then freeze on contact. From all the riming on all the trees, chairlifts, towers, and buildings, it is apparent that the clouds last night were supercooled.
A general wind direction can also be inferred based on the side of the object the rime is located. You can see in the picture below that most of the rime is on one side of the post. That is the direction the wind was blowing. The wind blew the supercooled droplets onto one side of the post.
Also notice the detail in the rime. This isn't the same thing as snow. It's not made of flakes. Instead, it looks a lot like the frost build up you would see in an old freezer.
Snow flakes can also be rimed. Since the top parts of a cloud are much colder than the bottom, ice crystals are common at the top of a cloud while the bottom of the cloud can be made of supercooled droplets. As the snowflake falls through the cloud it collides with the supercooled droplets and we get graupel! Those soft, hail-like snow pellets.
Below are pictures of snow flakes taken by a multi-angle snow flake camera. On the left is a normal snowflake, the middle is a flake that is lightly covered in rime, and the right picture is a flake completely covered by rime, otherwise known as graupel.
On the way home from Idaho my cousin and I had to rent a car in Boise to drive to Salt Lake. We took rode the Frontrunner the rest of the way home. We looked like a pair of ski bums carrying all our gear and Christmas packages.
And just a few days after Christmas I took my younger brothers skiing at Sundance. It was the first time for two of them, and they caught on quick. I'll have to take them up again. Hopefully we'll have better snow this week. It was a really icy.
This is what it looked like on the University of Utah campus Monday morning. Probably wont get much more between now and next ski trip.
The day before skiing the mountain received about of foot of new snow. After the first ride up the Bluebird lift it was apparent there was a lot more weather going on the night before than just snow. Everything at the top of the mountain was covered in thick rime. The wind sensor on top of the ski patrol hut was surely not working properly.
Ski Patrol at the top of the mountain. |
Liquid cloud droplets below freezing are called supercooled. Riming occurs when supercooled droplets hit something they can freeze onto. The droplets then freeze on contact. From all the riming on all the trees, chairlifts, towers, and buildings, it is apparent that the clouds last night were supercooled.
A general wind direction can also be inferred based on the side of the object the rime is located. You can see in the picture below that most of the rime is on one side of the post. That is the direction the wind was blowing. The wind blew the supercooled droplets onto one side of the post.
Also notice the detail in the rime. This isn't the same thing as snow. It's not made of flakes. Instead, it looks a lot like the frost build up you would see in an old freezer.
Snow flakes can also be rimed. Since the top parts of a cloud are much colder than the bottom, ice crystals are common at the top of a cloud while the bottom of the cloud can be made of supercooled droplets. As the snowflake falls through the cloud it collides with the supercooled droplets and we get graupel! Those soft, hail-like snow pellets.
Below are pictures of snow flakes taken by a multi-angle snow flake camera. On the left is a normal snowflake, the middle is a flake that is lightly covered in rime, and the right picture is a flake completely covered by rime, otherwise known as graupel.
More pictures of skiing:
On the way home from Idaho my cousin and I had to rent a car in Boise to drive to Salt Lake. We took rode the Frontrunner the rest of the way home. We looked like a pair of ski bums carrying all our gear and Christmas packages.
And just a few days after Christmas I took my younger brothers skiing at Sundance. It was the first time for two of them, and they caught on quick. I'll have to take them up again. Hopefully we'll have better snow this week. It was a really icy.
This is what it looked like on the University of Utah campus Monday morning. Probably wont get much more between now and next ski trip.
Snow today, cold and windy tomorrow
It finally looks like winter with some snow on the ground, and tomorrow it will start to feel like winter. Today we'll have a high in the low 30s, tomorrow the high will be in the low 20s!
The fridged trough stretching over Utah will bring cold Candian air to our state until after the new year.
12 km NAM Forecast, Tuesday 11:00 AM Source: weather.utah.edu |
These synoptic conditions are the recipe for another downslope windstorm for areas north of Salt Lake. The high resolution NAM forecast shows sustained winds up to 15 meters per second (~30 MPH)
4 km NAM forecast, Tuesday 11:00 AM Source: weather.utah.edu |
The National Weather Service has issued a wind advisory for December 30-31
Source: NWS |
Wednesday, December 24, 2014
Friday, December 19, 2014
Meteorologist Robert Simpson dies at age 102
Robert Simpson, co-founder the of the Saffir-Simpson scale used to categorize hurricanes, died on December 18, 2014 at the age of 102.
Jeff Master's Blog
http://www.wunderground.com/blog/JeffMasters/comment.html?entrynum=2882
Wikipedia
http://en.wikipedia.org/wiki/Robert_Simpson_(meteorologist)
Jeff Master's Blog
http://www.wunderground.com/blog/JeffMasters/comment.html?entrynum=2882
Wikipedia
http://en.wikipedia.org/wiki/Robert_Simpson_(meteorologist)
Thursday, December 18, 2014
Last Weeks Pineapple Express
Last week California was hit hard by storm. The moisture transport is visible from GOES satellites (NASA).
It could be much worse
I've been asked many times in the last few weeks, "Hey! When is it going to snow?" Hopefully soon. I love a white Christmas, but I've enjoyed this unusually warm December. Not having snow has helped keep our air quality bearable. If we had an inch of snow covering the ground we would be in big trouble.
Below is the temperature trend this December shown in navy blue. The red shading represent record highs, the green shading is the average temperature range for each day, and the blue shading is the record cold temperature. Many days this month has been over 10 degrees above average! Some of our daily low temperatures were as warm as our average high. These warm temperatures mean the inversion we typically see this time of year isn't very strong. Two things have helped keep the inversion away. First, we don't have snow on the ground. Snow reflects the sun's radiation back to space and prevents day time heating. And second, we haven't had a mass of Canadian air come down and fill our valleys with their painfully cold air. Just because it hasn't happened yet doesn't mean it wont. We still have January and February to get through and weather can change quickly.
Below is the current PM 2.5 trend from the last few days. We're still below the"toxic" level of 35 ug/m3. With snow on the ground the inversion would be much stronger and we would definitely be in the orange and red.
So where is the snow? It's on it's way (hopefully.) It looks like the mountains will get some new snow this afternoon. If we get anything in the valley it will most likely be rain. It's still pretty warm out there today.
Below is the temperature trend this December shown in navy blue. The red shading represent record highs, the green shading is the average temperature range for each day, and the blue shading is the record cold temperature. Many days this month has been over 10 degrees above average! Some of our daily low temperatures were as warm as our average high. These warm temperatures mean the inversion we typically see this time of year isn't very strong. Two things have helped keep the inversion away. First, we don't have snow on the ground. Snow reflects the sun's radiation back to space and prevents day time heating. And second, we haven't had a mass of Canadian air come down and fill our valleys with their painfully cold air. Just because it hasn't happened yet doesn't mean it wont. We still have January and February to get through and weather can change quickly.
Below is the current PM 2.5 trend from the last few days. We're still below the"toxic" level of 35 ug/m3. With snow on the ground the inversion would be much stronger and we would definitely be in the orange and red.
airquality.utah.edu |
This Sunday the ski resorts could get dumped on :) We'll see if this plays out. Other models keep this storm a little drier, but we can hope this will play out.
You can check out utahskiweather.com for the latest forecasts of your favorite ski resorts.
Sunday, December 14, 2014
Saturday, December 13, 2014
Thursday, December 11, 2014
Lenticular Cloud
A classmate took this picture this morning...
Here are some time-lapse videos from the camera at the University of Utah and the Neil Armstrong Academy. The lenticular clouds are the stationary clouds. They kind of wiggle around a little.
Looking west, from the Neil Armstrong Academy: http://youtu.be/D5u4IuAveWY
Looking south, from the University of Utah: http://youtu.be/Ii9xhEoCDxw
Monday, December 8, 2014
FedEx Meteorology Team
Will your Christmas package come to your home in time? Meteorologists at FedEx can help!
(More Info)
washington post article
FedEx |
(More Info)
washington post article
Friday, December 5, 2014
Orion's First Flight
You may have heard of Orion, NASA's new spacecraft that will take astronauts beyond low-earth orbit again. Yesterday's launch was delayed due to wind and some malfunctioning valves, but the flight today was a success.
The test flight flew around the earth twice, up to 3,600 miles above earth, and up to 22,000 miles per hour. This is the furthest any capsule designed to transport humans this has flown since the last time man walked on the moon, almost 50 years ago.
Just how far away is 3,600 miles? We'll in comparison with the distance to the moon it isn't that far...
Orion's first flight was 4 hours long. It takes 3 days to get to the moon. Mars is even further way (obviously). Yeah, they didn't top off the fuel tank in those rockets engines for this test run. ATK, a Utah company, is building the heavy lift rocket system for future missions to the moon and beyond!
The test flight flew around the earth twice, up to 3,600 miles above earth, and up to 22,000 miles per hour. This is the furthest any capsule designed to transport humans this has flown since the last time man walked on the moon, almost 50 years ago.
Just how far away is 3,600 miles? We'll in comparison with the distance to the moon it isn't that far...
(C) KBKB |
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