Category Archives: Weather & Sky

Blankets?

Cloud heat misconception (illustration from Dan Stterfield's Wild Wild Science Journal)

This morning it was extra cold (15 degrees F!).  It would have been cold anyway because an arctic air mass arrived over the weekend, but it was extra cold because the sky was mostly clear last night.  If we’d had lots of cloud cover we’d have been a little warmer.

The reason for this is not what you’d expect.  Traditionally we’ve heard that cloud cover acts like a blanket to hold the heat in.  The illustration above plays to that notion by showing heat arrows bouncing off the clouds.  But it ain’t exactly so.  Believe it or not this illustration is wrong.

The truth is that we’re warmer under cloud cover because the clouds radiate their own heat which warms the air below them.  You’ve seen this principle in action if you’ve parked your car under a leafy tree on a frosty night and found your windshield frost-free the next morning though the open ground has frost.  The tree radiated heat to keep your car just a little warmer than the open air.

I learned this from Dan Satterfield’s blog, Dan’s Wild Wild Science Journal, where I found this illustration.  In “Scientific Facts That Aren’t True” Dan writes:

The clouds do not “hold the heat in”. They absorb the heat, and radiate their own heat in all directions.  …If you’re camping, and you sleep under a tree, you will escape most of the dew compared to your buddies, who slept right out under the stars. The tree did not catch the dew, it just radiated energy to the ground around you, and kept it warmer. Warmer ground, less dew!

Click on the image to read more of Dan’s Scientific Facts That Aren’t True.

Clouds may blanket us but they aren’t blankets.

 

(traditional image of heat bouncing off clouds from Dan’s Wild Wild Science Journal: Scientific Facts That Aren’t True by Dan Satterfield)

Snow?

First snow in Schenley Park, 12 Nov 2013 (photo by Kate St. John)

As of this writing we know that very cold weather is on its way (18o Sunday night!) but the question of snowfall is still up in the air.  How much will actually stick?

On November 12 the first snow of the season was quite beautiful in Schenley Park.

By now all the leaves have fallen.  Even with snow, this scene would look different if photographed today.

 

(photo by Kate St. John)

 

Lawn Sprinkler In The Sky

Asteroid P/2013 P5 as seen on two days in September 2013 from the Hubble Space Telescope (photos courtesy of NASA)

Back in September an amazing asteroid flew by in outer space.

It first appeared as a fuzzy dot, seen by a PanSTARRS Survey telescope in Hawaii.  Wondering what it was, astronomers directed the Hubble Space Telescope to take a look.  Boy, were they surprised.  It has six tails!

This is not a normal asteroid.  Asteroids are very tiny planets and — until now — they don’t have tails.  This one is only 700 feet across and is traveling around the sun in the asteroid belt between Mars and Jupiter.  Like it’s traveling companions in the Flora asteroid family, its probably a chunk left over from a planetary collision.

So why does it have tails?  Comets have tails because they are made of ice, dust and small rocks.  When they get near the sun the ice evaporates, causing a long streamer of debris.  But this asteroid has no ice.  It must be streaming dust.  Lots of it.

Scientists named it P/2013 P5 and ran its behavior through modelling software at the Max Planck Institute for Solar System Research.  The model showed this asteroid is spinning so fast that anything loose on the surface (dust) is traveling toward its equator.  There it accumulates and episodically escapes the asteroid’s weak gravity, arcing into outer space. Yow!  Six tails!

Why is it spinning so fast?  Scientists theorize that the pressure of sunlight could have pushed P/2013 P5 into a tail spin.

Photos, above, from the Hubble Space Telescope show it spinning like a lawn sprinkler in the sky.

 

Read more here at NASA’s Hubble website.

 

(images of Asteroid P/2013 P5 from the Hubble Space Telescope, courtesy of NASA)

Mackerel Sky

Clouds, 20 Oct 2013 (photo by Kate St. John)

I love it when the sky does this.

These pretty clouds won’t rain … yet.  They drift by in thin shields with gaps between and when they thicken they look like buttermilk (click here to see).

These are altocumulus clouds that form in the mid-level of the cloud deck, between 6,500 and 20,000 feet.  Their thicker version is called a mackerel sky because the effect resembles the scales on a king mackerel.

Weather sayings confuse me about the message these clouds are bringing.  One poem says, “Mackerel sky, mackerel sky – never long wet, never long dry.”   Worst case:  These are overtaken six to eight hours later by different clouds that bring rain.

On the day I took this photo I was outdoors for six hours and yes, these happy clouds were followed by thick, potential rain clouds.

But it didn’t rain until I got home.

 

(photo by Kate St. John)

Bad News For Gyrfalcons

Gyrfalcon in western Greenland (photo form Wikimedia Commons)
Gyrfalcon in western Greenland (photo from Wikimedia Commons)

A new study on the future of climate change in arctic Alaska spells bad news for gyrfalcons in the U.S.

By 2050 the mean annual temperature in northernmost Alaska is expected to rise 3.10C (5.560F).  This will usher in a host of changes to ice, coastlines, tundra, plants and animals.  What will happen to the area’s breeding birds?

Scientists from the Wildlife Conservation Society, assisted by experts on each species, assessed the future of 54 of arctic Alaska’s breeding birds.  The goal was to prepare wildlife and land managers for climate change and ultimately develop plans to mitigate the effects if possible.

The study found that two species, gyrfalcons and common eiders, are highly vulnerable to the anticipated warming and likely to experience dangerous declines.  Seven others are moderately vulnerable: brant, Steller’s eider, pomerine jaeger, yellow-billed loon, buff-breasted sandpiper, red phalarope and ruddy turnstone.

Gyrfalcons are specialists and climate change is going to be rough on their niche.

  • They nest on coastal cliffs in microclimates that are a rare commodity in northern Alaska.  South-facing cliffs may become too hot, limiting the number of suitable nest sites.
  • At the start of breeding gyrfalcons eat ptarmigan almost exclusively.  When ptarmigan populations are low gyrfalcons won’t breed at all.  When climate change affects ptarmigans it will hurt gyrfalcons.
  • The gyrfalcon’s hunting style relies on open tundra but as the arctic warms shrubs will grow in formerly open land.
  • Spring storms are expected to increase. Unfortunately this will cause nest failure for gyrfalcons who require dry weather to hatch their eggs.

With all these cards stacked against them gyrfalcon numbers are expected to drop considerably from today’s 250 breeding pairs.

But the report has a silver lining.  There will be more seed eaters:  savannah sparrows, Lapland longspurs, white-crowned sparrows, American tree-sparrows and common redpolls.

Much as I like redpolls, I don’t want to trade them for gyrfalcons.

Read more about the report, Assessing Climate Change Vulnerability of Breeding Birds in Arctic Alaska, in this article in Science Daily or download it from this page on the WCS website (see the righthand column).

(photo from Wikimedia Commons.  Click on the caption to see the original.)

p.s. The report was careful to point out that the study only applies to arctic Alaska, not to all breeding ranges.  The photo above was taken in western Greenland.

Nature’s Mushroom Cloud

Sarychev Volcano, Matua Island, 12 June 2009 (photo from the International Space Station, NASA, via Wikimedia Commons)
Eruption of Sarychev volcano seen from the International Space Station, 12 June 2009 (photo from NASA)

3 April 2013

Imagine seeing this outside your window!

On June 12, 2009 the International Space Station was flying over the Kuril Island chain in the northwestern Pacific when they witnessed the eruption of Sarychev peak, an active volcano on Russia’s Matua Island.

Because the eruption had just begun, brown ash and steam was still rising in a mushroom cloud that had punched a hole in the cloud cover above it.  Meanwhile, dark brown ash rolled low to the ground, probably a pyroclastic flow of hot gas and rock up to 1,850oF (1000oC) and traveling at 450 mph!

The ash had just begun to spread out in the sky (light brown at top left and right).  Soon commercial air traffic was diverted to avoid engine failure from this abrasive particulate in the upper atmosphere.

The astronauts were lucky to see this eruption as it began.

Nature makes an impressive mushroom cloud.

(photo from the International Space Station, NASA)

Hold Onto Your Hats!

Chelyabinsk meteor trace, 15 February 2013 (photo by Nikita Plekhanov via Wikipedia)
Chelyabinsk meteor trace (photo by Nikita Plekhanov via Wikimedia Commons)

16 February 2013

There we were, focusing our attention on an asteroid that was going to miss the Earth when Bang!  A real live meteor zipped low over Russia yesterday morning, 15 February 2013.

The meteor taught me a lot more than the asteroid.  After it lit the sky, made an explosive boom, blew out windows, and injured more than 1,000 people I learned from NASA:

  • Its light was brighter than the sun.
  • Its contrail was 300 miles long. (That’s the distance from Pittsburgh to Philadelphia).
  • Eyewitnesses said the sonic boom lagged by three minutes … just long enough for everyone to go to their windows to watch.
  • The meteor was about the size of a bus (55 feet) but it weighed 10,000 tons –> 1,400 times heavier than a bus.
  • The atmosphere really did help after all.  When the meteor exploded it was still 12-15 miles up.  At least twice as high up as a jetliner.
  • If it was only the size of a bus and 2 to 4 times higher up than a jet, why did it cause such a problem?   Well, it was traveling at 40,000 mph!

So, hold onto your hats.  It’s the stuff we aren’t worried about that gets us.

This video from The Telegraph UK shows dashcam video and explains what happened.

p.s.  16 Feb 2013: The meteor also taught me two things about Russian culture:  (1) Russians have dashboard cameras in their cars to protect against corrupt policemen and disputed traffic accidents, and (2) They have already made a joke about it, quoted from the Houston Chronicle: “The meteorite was supposed to fall on Dec. 21, 2012 — when many believed the Mayan calendar predicted the end of the world — but was delivered late by Russia’s notoriously inefficient postal service.”

(photo of the Chelyabinsk meteor’s trace from Wikimedia Commons; click on the caption to see the original)

An Icy Parfait

Sea ice in the Arctic (photo courtesy Univeersity of Washington)

Even when scientists develop an answer to why something happened, they still test the idea to make sure they’re right.

That’s what happened with the Great Arctic Cyclone of August 2012.

Last August a rare, massive cyclone formed in Siberia and swirled out over the Arctic Ocean for days.  During its transit the sea ice disappeared faster than anyone had ever seen.  (See the swirl here.)

By September Arctic sea ice was at an all time low.  Some said the cyclone caused the lowest ice extent since record-keeping began.  Did it?  Or would the ice have melted anyway due to warm temperatures?

Scientists at the University of Washington’s Applied Physics Laboratory ran two computer simulations of last summer’s Arctic weather.  One matched the actual weather.  The other included everything except the cyclone.

The result showed that yes, “the effect is huge in the immediate aftermath of the cyclone, but after about two weeks the effect gets smaller.  By September, most of the ice that melted would have melted with or without the cyclone,” said lead author Jinlun Zhang.

Why?  Because of mixing.

Back in September most thought that the wind broke up the thin ice or pushed it into a warmer part of the ocean.  Since then scientists have learned that the ocean underneath the ice is like a layered parfait.  Just below thin ice is a layer of ice-cold fresh water.  About 65 feet down is a layer of salty water warmed by the sun.  The cyclone stirred the parfait.  The ice was exposed to the warm water beneath and it melted.

The cyclone did cause the ice to melt 10 days sooner, but in the end it made less than 5% difference in the ice extent.

So yes, the sea ice melted because it was hot last year.

Click on the photo to read more about the study in Science Daily.

(photo courtesy University of Washington)

Walking Down Vortex Street

I know almost nothing about fluid dynamics but my article about wingtip vortices piqued my interest in the subject.

Last weekend I learned about this amazing phenomenon, the von Kármán vortex street, animated above by Cesareo de La Rosa Siqueira.

Von Kármán vortex streets occur when a fluid flows past a stationary object and generates a long line of vortices that swirl in opposite directions.  The phenomenon was named for Theodore von Kármán, the man who described it, and is probably called a street because it looks like one.

We usually don’t see von Kármán vortex streets in the air but it’s important that engineers plan for them.  If a tall structure is uniformly straight or uniform structures are grouped too closely the vortices can make them fall down.  That’s what happened in November 1965 when three of the eight Ferrybridge cooling towers collapsed in high winds. They could individually withstand the wind speed but not the vortex.

On a small scale, von Kármán vortex streets make wires sing in the wind.  On a large scale they’re visible from outer space when clouds blow past a tall island.

Here’s a picture taken from the space shuttle that shows cloud cover blowing past Rishiri Island, Japan.  When the wind encounters Mt. Rishiri the clouds form a von Kármán vortex street on the downwind side.

There are more than twenty islands that reliably generate von Kármán vortex streets.  Click here to see more pictures from NASA.

(Vortex animation by Cesareo de La Rosa Siqueira via Wikimedia Commons.  Space shuttle photo from NASA via Wikimedia Commons. Click on the images to see the originals)

Open Water

Female buffelhead at Bosque del Apache (photo by Steve Valasek)

The long spate of cold weather froze all our ponds and lakes.  Even the rivers were beginning to freeze until Monday’s warmth reversed the trend.

Don’t expect to see a lot of birds at Lake Arthur right now.  Waterfowl who rely on open water for food or to get airborne have left for open water.  Some are at our rivers, most have left town completely.

This female bufflehead was on the other side of the U.S. — at Bosque del Apache, New Mexico — when Steve Valasek took her picture.

No, she didn’t leave Pittsburgh for New Mexico, but Steve did.

(photo by Steve Valasek)