Three weeks ago I wrote about radiation fog and inversions. We had another inversion recently, this time without fog.
Here is the view last Sunday from the Allegheny Front Hawk Watch. It looks like a bad picture of beautiful scenery but it’s actually a good illustration of a hazy inversion. Notice how the near trees are colorful and Wills Mountain, 10.5 miles away, is bland and washed out. You can’t see the fire tower on Kinton Knob. The colors are cancelled by bad air.
This was a classic temperature inversion but the first time I was able to measure it. As I drove to the hawk watch my car’s outdoor thermometer registered 43o in the Laurel Highland valleys and 57o on top of the mountain. Normally the hawk watch site is far colder than anywhere else in western PA.
The weather was topsy-turvy. Warm air aloft trapped cold air below and with it pollutants that made the air smell bad in the cold zones.
Bad air was not limited to cities and industrial zones. On my way to the Allegheny Front I saw quite a few outdoor wood boilers creating thick white smoke that blanketed rural areas. These relatively new devices burn wood in backyard sheds to heat water for radiators in homes. Because outdoor wood boilers are small scale polluters they weren’t on the bad air radar at first, but their smoke is much worse than typical burning because the fire smolders when indoor heat demand is low. I saw valleys where wood smoke enveloped nearby homes and neighbors.
Nacreous clouds are named for their iridescence. Like nacre, the mother of pearl substance that lines oyster shells and pearls, they reflect all the colors of the rainbow.
They’re also called polar stratospheric clouds (PSCs) because they form in the lower stratosphere at 49,000 to 82,000 feet in the presence of super low temperatures, -108oF and colder. These conditions are only found in the polar regions during winter, mostly in Antarctica.
To give you an idea of how rare these clouds are, consider that they form in an extremely dry part of the earth’s atmosphere way above most human activity. Commercial jets fly at 23,000 to 41,000 feet; these clouds are much higher. It’s so dry up there it’s a wonder that they form at all.
The prettiest nacreous clouds contain only water droplets that glow profusely when the sun lights them from below. These clouds are benign but others are not. PSC clouds that form from nitric acid + water cause chemical reactions that deplete stratospheric ozone and make a hole in the ozone layer that protects Earth from the sun’s ultraviolet light.
As we head toward winter in the Northern Hemisphere, it’s summer in Antarctica so it will be many months before there are nacreous clouds again. These were photographed in August 2009.
(Nacreous clouds in Antarctica over the NASA Radome, photo by Alan Light on Wikimedia Commons. Click on the image to see the original)
How did we get such a strong hurricane so late in the season? Why did it hit New Jersey, a place that’s had only one hurricane make landfall in 161 years of hurricane records? (And that was in 1903.)
I learned the answers on WESA’s Allegheny Front on Saturday. Jeff Masters of the Weather Underground explained how hot ocean temperatures, prevailing winds, and high pressure centered over Greenland spawned the storm and steered it west. (Click here to listen to the podcast.)
And though this individual storm can’t be pinned on climate change, its causes can. The bottom line: The whole world is hotter.
I hadn’t realized how much hotter and how rapidly the heat has increased until I watched this NASA animation of global surface temperature anomalies from 1880 to 2011. Using the average global temperature in the mid-20th century as baseline, the map is colored blue when colder, orange when hotter.
Play the animation and see for yourself.
The train is rolling down the track. (Perhaps it’s naive of me to say…) we could do something if we worked together politically and individually. Meanwhile …
Last night as Hurricane Sandy approached Pittsburgh I thought about the birds. Where will they hide from the storm? I knew the answer but I wanted assurance.
Birds already know how to cope with bad weather. Each species uses its own strategy to survive.
Birds that live on cliffs or buildings, like the pigeons above, shelter out of the wind and find the driest possible place to wait out the storm. This doesn’t always keep them dry but it keeps them safe.
Birds that roost in cavities, such as woodpeckers, owls, house sparrows and starlings go indoors during bad weather. Sometimes more than 10 bluebirds will huddle together inside a bluebird box, using their communal body heat to stay warm.
Robins, sparrows and cardinals roost in thickets and hunker down close to the ground when it’s windy. If you have a brush pile, as Marcy Cunkelman does, the birds will hide there from bad weather and predators. The Coopers hawk happens to know this, too.
“Radiation fog” sounds scary but it’s actually the kind of fog we get in Pennsylvania at this time of year. We often see it in the early morning below our hawk watch sites. (Do you see the bird in this picture?)
It forms when winds are calm overnight while the land cools. The land’s thermal radiation lowers the air temperature and condenses moisture into fog that usually evaporates in the morning.
In hilly country it’s called “valley fog” and is more pronounced because the topography traps cold air in the valleys with warm air overlaying it in a temperature inversion.
Like fog, inversions are also common in southwestern Pennsylvania in fall and winter. They can be deadly when air pollution is involved. The famous Donora Smog occurred during a five day inversion in 1948, October 27 to 31. It killed 20 people and 800 animals immediately, sickened 7,000, raised the mortality rate in Donora for at least a decade, and lowered property values (who would want to live there after that!).
Inversions still occur but our air is cleaner.
Nowadays we take for granted that our laws will protect us from air pollution. Unfortunately the laws could be weakened because companies complain it costs money to avoid killing or sickening us.
Without protection from air pollution, the fog would be scary after all.
We’re in for some interesting weather though it probably won’t look as dramatic as the cold front pictured above.
Last night the National Weather Service Pittsburgh forecast discussion said, “Showers becoming likely daytime Thursday with the passage of a mature occluding cold front. NAM model profiles show the cold frontal passage can also be accompanied by wind gusts up to 30 mph.”
I had never heard of an occluding front let alone a mature one (obviously, I haven’t been paying attention), so I had to look it up.
Occluded means blocked or stopped up. An occluding cold front is one that overtakes a warm front, jamming it in a wedge between the cold air ahead of the warm front and the new cold air mass overtaking it. The warm air has nowhere to go but up. Cold air floods in and the warm air rides atop it like a cork on water.
It looks like this — before and after — as the cold front approaches from the left, catches up to the warm front and forces it up. (Technically this drawing shows a “cold occlusion.”)
The practical result is that we had cold air early this week, warm air today (the warm front), and cold air tomorrow. The weather map shows the actual occlusion will track north of us.
The forecast also said, “As what often occurs with these maturing systems there can be a dry slot passage Thursday night before the ensuing cold upper low passes eastward through the upper Ohio Valley Friday.” So it will be dry on Friday.
The cork will rise tomorrow.
(photo from Wikimedia Commons of a cold front moving rapidly along the Rappahannock River. Occlusion diagram from Wikimedia Commons. Click on the images to see the originals.)
p.s. 10/17, 6:23 pm, Thursday’s forecast more includes the possibility of a severe thunderstorm & Friday has a chance of showers. Things change all the time!
In fact they are breaking waves generated by the same fluid dynamics that creates wind-driven waves on water.
Both are caused by Kelvin-Helmholtz instability which occurs at the boundary where two fluids flow by each other at different speeds or densities. The air above these clouds is moving faster left-to-right than the air below them. The boundary is very turbulent and becomes more so when the waves break.
Kelvin-Helmholz instability can be described mathematically and its effect plotted over time. This silent video by VanjaZ shows a yellow fluid on top flowing faster than the black fluid on the bottom. Talk about turbulence!
We rarely see K-H clouds because the atmosphere has to be just right to make them stand alone. The curling waves disappear in seconds, wiped out by chaos as soon as they break.