Archive for the 'Weather & Sky' Category

Feb 17 2014

Intrepid Minnesotan

Gray jay in Minnesota (photo by Jessica Botzan)

I’m back in the ‘Burgh with a fond look back at my time in Minnesota at the Sax Zim Bog Birding Festival.

Though I never found a great gray owl I saw seven Life Birds(*) and learned a lot about cold and snow.

Cold… was not a problem.  I didn’t have to cope with the worst of this winter in Minnesota but -13F was a typical morning in the bog.  Three to four layers of clothes are indispensable. Toe warmer heat packets inside Sorel boots are the key to warm feet.  I was never cold.

Snow… is a way of life.  If you’re afraid to drive in snow in Minnesota you’re homebound for half the year.  So you just do it.

Minnesota snowplows are awesome, huge, coordinated.  I arrived during a Winter Weather Advisory (4”-6”) and left during a Winter Storm Warning (5”-7”).  No problem.  All the roads and parking lots were plowed, not to bare pavement but quite passable.  The Duluth airport was plowed down to bare pavement.  My flight home was delayed only by de-icing.  Check out this video of clearing the runway.

Birds … are intrepid in Minnesota’s winters.  The easiest to find are ravens and black-capped chickadees.  The rarest are Carolina wrens and robins.  The gray jay is the cutest and the most intrepid.

Gray jays (Perisoreus canadensis) look like oversized chickadees but have the typical corvid attitude.  They’re bold and curious and willing to eat anything including berries, insects, fungi, other species’ nestlings and small mammals.

Jess Botzan saw this one at Sax Zim Bog during the coldest of the cold weather last month and the bird wasn’t phased by it. Gray jays are so intrepid that they lay eggs in March while temperatures are still below freezing and snow is on the ground.  They don’t even bother to nest again in May and June when the weather is easy.

Like everyone else in Minnesota, the gray jay is intrepid in snow and cold.

 

(photo by Jessica Botzan)

(*) Life Birds seen:  Pine grosbeak, black-billed magpie, boreal chickadee, gray jay, northern hawk owl, black-backed woodpecker, Bohemian waxwing.

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Feb 17 2014

I Climbed Lake Superior

Published by under Travel,Weather & Sky

Walking on Lake Superior, 16 Feb 2014 (photo by Kate St. John)

Yesterday’s Sax-Zim-Festival field trip to Duluth held an unexpected surprise.  Every year the birding trip stops at Stoney Point to observe gulls and waterfowl in the open water on Lake Superior.  But there is no open water.  The lake is 95% frozen.  Locals say this hasn’t happened for 20 years.

In the absence of birds we walked down to the lake, and then on it — a moonscape experience.

The inshore ice was flat and walkable but the pressure of offshore ice and wind had left a landscape of broken plates stacked in piles and covered in snow.

Ice chards at Lake Superior (photo by Kate St. John)

Each piece was thick and clear like a pane of glass.
Man holding ice chard from Lake Superior (photo by Kate St. John)

Fifty yards out the pressure was orogenic, so strong that it created a mountain ridge of bluish, broken ice more than 15 feet tall, so high we couldn’t see the lake beyond it.

Blue ice on Lake Superior, 16 Feb 2014 (photo by Kate St. John)

 

In this video from my cell phone you can see how big and strange it is.

 

Inevitably, the ice mountain posed an irresistible challenge.  Two guys climbed it.  Eventually I climbed too.  Going up was like climbing a hill of shale but coming down was a butt-slide in an ice cube tray.

So now I have three “Life Lake” experiences:  I saw Lake Superior for the first time, I walked on it, and then I climbed it.

 

(photos and video by Kate St. John)

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Jan 29 2014

It’s Warm Everywhere But Here

Published by under Weather & Sky

Land and ocean temperature anomalies, Dec 2013 (image from NOAA National Climatic Data Center)

I don’t know about you but I tend to think everyone’s having the same weather I’m having.  So everywhere on earth is colder than normal now, right?

Wrong!  Much of North America is colder, but most of the world is quite the opposite.  Last week NOAA’s National Climatic Data Center published temperature anomalies for 2013 and they’re surprising if you think everyone’s weather is the same as ours.

Above, a snapshot of December 2013 shows red for hotter and blue for colder than normal temperatures, the deeper the color the deeper the variance.  The darkest color means a 5+ degree Celsius difference (that’s 9+ degrees Fahrenheit).  For visual impact I removed the explanatory text, so be sure to click on the image to see the details!

Notice that except for North America and eastern Turkey, in December 2013 almost everywhere on Earth was hotter than usual, sometimes a lot hotter.

Twelve months ago the story was quite different.  In January 2013 we were warmer than normal and Russia was colder.  Click here for January 2013’s map.

So if you don’t like the weather right now, just wait.  Things will change!

 

(Global temperature anomalies, December 2013, from NOAA’s National Climatic Data Center at Climate.gov. Click on the image to see the original)

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Jan 28 2014

Nature’s Snowballs

Published by under Weather & Sky

Large snow rollers, 27 Jan 2014, Dubois, PA (photo by Marianne Atkinson)

The weather was weird yesterday but it made something beautiful.

In Pennsylvania and Ohio people looked outdoors to find thousands of large snowballs dotting hillsides and open fields.  The snow rollers resembled hay bales, jellyrolls or the unstacked segments of snowmen and were so unusual that they became online sensations in social media.  They were made by the wind.

I didn’t know they’d happened until Marianne Atkinson sent me photos from her backyard in Clearfield County, PA.  I’d seen the wind make little snowballs in the Laurel Highlands so I thought I knew what she was talking about.  But no, these are special.  They’re a foot across!

Snow rollerabout a foot across (photo by Marianne Atkinson)

Snow rollers are pretty rare but yesterday morning produced the perfect weather mix…

  • With an icy layer on top of snow or the ground that new snow can’t stick to…
  • Wet, loose snow fell on the icy layer.
  • The temperature was near the melting point and…
  • The wind blew at just the right speed to start the balls rolling without destroying them.
  • The rollers stopped when they became too heavy for the wind to move.  Even so they’re often hollow and too fragile to pick up.

A quick search of the Internet found photos and video at WPXI Pittsburgh, Newsnet5 in Cleveland and NBC4 Columbus.

Thankfully the wind wasn’t strong enough to stack them into snowmen!

 

(photos by Marianne Atkinson)

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Jan 11 2014

No Snow

Snow buntings, Crawford County, Jan 2014 (photo by Shawn Collins)

Can you believe how warm it is today?

Shawn Collins found these snow buntings in Crawford County a week ago when the snow was melting.  Two days later we were in the sub-zero polar vortex.  Now it’s 60 degrees warmer and the snow is gone.

It’s a good thing snow buntings are white, brown and black. They’re camouflaged even when there’s no snow.

(photo by Shawn Collins)

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Jan 09 2014

Dowsing From Outer Space

Published by under Weather & Sky

GRACE satellite pair (drawing from NASA on Wikimedia Commons)

Here’s some old news to some of you… but new to me.

Launched in 2002, the twin Gravity Recovery and Climate Experiment (GRACE) satellites have collected data for 12 years and are already in a decaying orbit that will suck them down to Earth in 2015 or 2016.  During their run they’ve carefully measured Earth’s gravitational pull and contributed to our knowledge of aquifers, ice sheets, magma and earthquakes — all because of gravity.

Did you know that gravity is uneven around the world and can vary in the same location during the year?  Interestingly, water has a lot to do with it.  Gravity is determined by mass so an increase in groundwater causes a higher gravitational pull.  Since the GRACE satellites measure gravity, they find groundwater.  It’s as if they were dowsing (finding water using a forked stick).

George Casely dowsing for water on his Devon farm, 1942 (photo from Wikimedia Commons)

Here’s how it works.  Skimming like hockey pucks in their pole-to-pole orbit, the GRACE satellites maintain a 140-mile distance between each other which they measure constantly. Their microwave ranging system is so accurate it can record a 10 micrometre change in separation (1/10 the width of a human hair)!  When the lead satellite first encounters a stronger gravitational pull, gravity makes it speed ahead, increasing the distance between them.  When the second satellite encounters the same “bump” it speeds up too and their separation decreases.  When they’ve both passed the “bump” they both slow down.

Round and round since 2002 they measure the distance between themselves and report back to Earth.  NASA’s computers crunch the ebb and flow of gravity and create gravitational anomaly maps.  Click here to see a selection of them.

The maps help scientists understand changes in aquifers and improve groundwater management.  You can see the greatest anomalies in the tropics where there are dramatic wet and dry seasons.  On this map the Amazon basin is routinely blue (decreasing gravitational pull) in October at the end of the dry season and routinely red (higher gravity) in April at the end of the rainy season.  Bangladesh’s color cycle is the opposite because its wet-dry cycle occurs during the other half of the year.

Until gravity pulls them down and ends their mission the GRACE satellites travel above us, dowsing from outer space.

 

(image of the GRACE satellites and photo of George Casely dowsing on his farm from Wikimedia Commons. Click on the images to see the originals)

p.s.  Click here for more news from the GRACE satellites.

 

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Jan 07 2014

Polar Vortex

Published by under Weather & Sky

U.S. maximum temperature map for January 6, 2014 (graphic from NOAA)

If you’ve listened to the weather forecasters you know we’re in the grips of a polar vortex.

At first that name confused me.  I know about the single massive polar vortex that spins counterclockwise in the high northern latitudes in winter, covering 620 to 1,240 square miles and reaching into the stratosphere.  Is that vortex here now?

Not exactly.  We’re experiencing a polar vortex, not the northern polar vortex, though they’re related.

In the good old days before climate change, the winter polar vortex in the northern hemisphere was generally well behaved.  It was a persistent, strong, cold, low pressure zone surrounding the polar high at roughly the same latitude around the globe.  Its strong winds kept the jet stream in line.  Nobody got too hot or too cold.

In some years — and more frequently as the Earth gets hotter — hot air from the troposphere is forced into the stratosphere and disrupts the polar vortex.  The vortex becomes disorganized and may “collapse” into smaller pieces.  Its winds weaken and the jet stream flaps like a flag in the breeze, as shown below:

Jet stream Rossby waves (graphic from Wikimedia Commons)

(a) When the polar vortex is strong, the jet stream (pink band) circles the Earth in small amplitude Rossby waves. This keeps cold air in the north and warm air in the south.
(b) When the polar vortex weakens, the jet stream begins to wobble.
(c) A major wobble brings a tongue of polar air deep into the south, spawning a (smaller break-away) polar vortex that affects our weather.  Notice how the tongue of cold air resembles yesterday’s U.S. high temperature map above.

Disruption of the winter polar vortex used to be rare, but not any more.  Last winter the polar vortex completely collapsed because of hot air from the Himalayas. The vortex broke into pieces, one of which hovered over Siberia.  The jet stream went wobbly.  Europe had a very severe winter.

This year it’s our turn.

A lot of factors created today’s weather pattern but, yes, the weakening of the polar vortex can send us a polar vortex.

Right now only the snowy owls feel at home.  ;)

 

(images from NOAA and Wikimedia Commons. Click on each image to see it’s source)

 

 

UPDATE, 10 Jan 2014:  NOAA maps show the break-up of the polar vortex.  On the left, the 500mb pressure gradient on 5 Jan 2014 shows the polar vortex in bits and pieces.  On the right, the same pressure gradient on 14-16 Nov 2013 shows a nicely contained vortex.  Click on the image to see larger images and read the accompanying article at NOAA.

Polar vorrtex 500mb pressure comparison: Jan 5, 2014 to Nov 14-16, 2013 (maps by NOAA climate.gov)

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Dec 21 2013

Winter Solstice

Winter sunset over the Susquehanna at the Wrightsville Bridge (photo by John Beatty)

Today at 12:11pm the sun will stand still.

We call this the “winter” solstice but it’s more accurate to call it the southern solstice because the sun is going to stand still over the southern hemisphere.  The word “solstice” describes the event:  sol means sun and stice, from sistere, means to stand still.

You might be jealous of the southern hemisphere right now because they’re in the midst of summer but take heart in this: their spring and summer are shorter than ours.

That’s because the Earth doesn’t move at a constant speed in its elliptical orbit.  It takes the Earth 92.8 days to travel from the point of our vernal equinox to the location of the northern/summer solstice (March to June), 93.6 days from the summer solstice to the autumnal equinox (June to September), 89.8 days from the autumnal equinox to the winter solstice (September to December) and 89.0 days from winter solstice to vernal equinox (December to March).  Thus the seasons aren’t equal in length.

This means that in the northern hemisphere spring and summer together are 7.6 days longer than those seasons in the southern hemisphere.  We have a week’s more warmth than they do.

If this is confusing, check out the earth map and explanation at this link at timeanddate.com whose information I paraphrased above.

 

(photo of the sun setting over the Susquehanna at Wrightsville, PA by John Beatty)

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Dec 17 2013

Paintballs To The Rescue

Published by under Weather & Sky

When I wrote about the lawn sprinkler asteroid on November 11, I was intrigued by this sentence in the news article:

“The asteroid could possibly have been spun up if the pressure of sunlight exerted a torque on the body.”

The pressure of sunlight?

Apparently small bodies in outer space — from dust particles to 10km wide asteroids — are affected by the relentless though tiny touch of photons.  They reflect or absorb the photons’ energy and emit what they don’t retain.  The emissions become a tiny propulsion force. However, dust and asteroids have irregular shapes and surfaces so they reflect, absorb and emit unevenly.  This affects their rotation and flight path.

There’s a lot of fancy physics that predicts what a small irregular body will do under the pressure of sunlight.  I read about the Yarkovsky effect, the YORP effect and the Poynting-Robertson effect until I got confused.  Then I googled for a simple description and found …

The United Nations’ Space Generation Advisory Council holds an annual contest to solve the problem of deflecting a killer asteroid on a collision course with Earth.  In 2012 the winning solution of the Move an Asteroid Competition was to bombard it with white paintballs.

The reason this would work is due to the Yarkovsky effect (I think).  A dirt-colored rotating asteroid absorbs photons and heats up on its daylight side, then releases energy when that side turns to night.  In a steady state the asteroid would stay on course and hit the Earth but if it’s painted white it will absorb less and emit less — and this will alter its course.

All we need for deflecting a dangerous asteroid is a 20-year lead time, a rocket, a lot of white paintballs and very good aim.

Watch the video to see how we’d paint an asteroid.  Click here to read how it works in MIT News.

Paintballs to the rescue.

 

(video from MIT News on YouTube)

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Dec 11 2013

Iridescent

Published by under Weather & Sky

Iridescent cloud (photo by "not on your nelly," Creative Commons license on Flickr)

There are a lot of iridescent things in nature:  birds, beetles, seashells, fish, minerals and clouds.

Yesterday, after a snowy start (and really bad traffic!) the wind swung around to the west and the sky cleared with a few fast-moving clouds.  At lunchtime I looked up while standing in a building’s shadow and saw a thin, beautiful, iridescent cloud blowing past the sun.

Thin is important.  Iridescence occurs when sunlight diffracts through a thin layer of water droplets (or ice crystals) of uniform size and orientation.  The glowing colors are named for the Greek goddess Iris, the personification of rainbows.

Pittsburgh’s iridescent clouds aren’t nearly as cool as the nacreous clouds in Antarctica, but we don’t have the super-cold stratospheric temperatures that cause those clouds. For which I am grateful!

 

(photo by “not on your nelly” on Flickr, Creative Commons license. Click on the image to see the original)

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