Celebrity endorsement

 

It seems that the Kaslo Chamber of Commerce has hired the ultimate celebrity endorsement: a Great Gray Owl has arrived to promote local businesses. It hardly gets any better than this. Yesterday, upon seeing this rare celebrity in town, Dirk Pidcock, an enthusiastic local fan exclaimed, “Indeed it is a very special day! … After years of longing and searching, … I see a Great Gray for the first time this morning….” 

Pidcock’s pictures of this celebrity owl were posted yesterday. Today, I went to see it myself, and it quickly became clear that this celebrated owl was in full endorsement mode as it drew attention to local businesses. 

I spotted the Great Gray promoting a business that I never did recognize. This is clearly the downside of going with a really big-name celebrity: the mere presence of the owl has eclipsed the endorsement it offers.

This was not the case when the Great Gray moved to endorsing the Kaslo Hotel; I have had a few meals there.
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Alas, the mere presence of a Great Gray Owl in Kaslo outshone the businesses it (seemingly) promoted.

This is, after all, the celebrity owl.

 

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Great Gray Owl

 

The Birds of British Columbia (Vol. 2, 1990) describes the Great Gray Owl as:

An uncommon resident in the northern interior and rare resident to the southern interior.

Few bird enthusiasts around here have seen one, but today in Kaslo, Lorraine Symmes spotted one and alerted Dirk Pidcock, who took these pictures. He kindly let me post them so some of the rest of us could enjoy this rarity.

Two views of the same Great Gray Owl

Dirk Pidcock’s pictures are used with permission.

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Kill, pose, limn

 

I was perusing a digital copy of John Fannin’s Checklist of the birds of British Columbia (1891), when I ran across an illustration of a Merlin (well, it was often called a Pigeon Hawk, at that time).  

The Merlin’s pose looked familiar. I had photographed a somewhat similar view a few years ago. So, I looked more closely at the description, which read:

Common east and west of Cascades, and ranging well up into the Rocky Mountain District, in which locality I have taken it in its most perfect plumage. 

“Taken”? That word clearly had a different meaning for birders in the nineteenth century. Indeed, Fannin had shot the Merlin! The dead bird was then presented to an illustrator who posed it in a lifelike manner, and sketched it. 

That is how it was done.

The renowned illustrator of birds in the United States, John James Audubon, would (as he said) harvest the birds he painted. His harvesting tool of choice was a rifle. In short: he shot them, then posed them, and then painted them. Curiously, he also then ate (or tried to eat) each of the birds he had harvested.

Audubon’s work predated photography and there were few other options open to him if he wished to limn birds. While Fannin’s work postdated photography, it probably wasn’t until a century later that camera technology would consistently outclass a rifle in the acquisition of good images of birds. We now have high-quality, long-focus, image-stabilized, lenses mounted on high-resolution cameras. Taking a bird in its most perfect plumage, now has a photographic meaning. 

Here are two Merlins recorded in British Columbia (with only slightly different poses). On the left is a bird I photographed a few years ago. It was unaware of my presence. On the right is the one Fannin had taken. It too was unaware of Fannin’s presence, but that is because at the time of the illustration, it was dead.

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Dipper’s Goldilocks

 

It has been cold (as my recent postings about ice on the Lake and creeks attest). Weather forecasts suggest that the air temperature is about to rise and is unlikely to plummet as low again this winter. This may be the last time this season to visit the freezing-weather travails of a dipper caught between the twin scourges of surface and anchor ice.

Surface ice and anchor ice form in different portions of a creek. Where the flow is gentle, such as near the creek mouth, ice will cover the water’s surface, but anchor ice will not form. Where the flow is turbulent, such as where the creek is steep, anchor ice covers the creek bottom, but surface ice is inhibited from bridging across the water. 

What is a poor dipper to do? It normally finds its food anywhere along the length of the creek bottom, whether the flow is smooth or turbulent. It is now blocked by twin barriers.

Curiously, at present temperatures, Kokanee Creek (where I make these observations) has a Goldilocks zone: one that is not so turbulent that anchor ice forms, and not so smooth that surface ice bridges across. That is where dippers go—where the turbulence and ice are just right. Would the dipper’s Goldilocks zone vanish with another 10C drop in temperature? We are unlikely to find out this winter.

Do other local creeks have a Goldilocks zone for dippers? I have no idea. But, the existence of such a zone may play a role in the long-term suitability of a creek for dippers.

Where the flow is turbulent, anchor ice covers the creek bottom, but surface ice has difficulty bridging the stream. Dipper foraging is out of the question here. 

This dipper has been foraging in the waters of Kokanee Creek’s Goldilocks zone: the flow is too calm for anchor ice, but too turbulent for ice to bridge the surface. It is just right for dippers.

After posting the material, above, I realized that I should show a picture near the creek mouth where the flow is so gentle that surface ice covers everything. So, I visited the creek again and took this panorama. The marks are from boots and skates. They certainly show that, under the dusting of snow, there is a solid cover of ice. No dippers can hunt here. Yet, when I walked past the Goldilocks zone again, three dippers were foraging.

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Frazil on waves

 

Frazil ice is a collection of loose, randomly oriented flakes of ice in water. Frazil resembles slush and has the appearance of being slightly oily when seen on the surface of water. 

In a recent posting, it was noted that frazil can consolidate to produce skim ice and subsequently border ice. Carlo commented on the picture of skim ice (a portion shown to the right) that,

The ice crystals in the … photo show a conspicuous preferred orientation with long elements left-right in the image. This indicates that forces at the water’s surface were not equal in all directions. When I mentioned this to Alistair, he suggested that there may have been a very gentle swell impinging on the shore. This would tend to orient the free-floating frazil with their long dimension parallel to the shore, accounting for the observed directed pattern. Neat!

Yesterday, I saw it happening. Frazil along the shore was becoming oriented by waves.

First, an overview. Waves with whitecaps (left) are washing into a bay. There is ice along the shore where the water has washed up from earlier waves and frozen. The frazil is in the centre.

A closer view shows the frazil to be grains of ice floating on the water and moving up and down with the waves.

This view, elsewhere along the shore, looks directly into the approaching frazil-carpeted waves. The frazil is becoming oriented in a manner consistent with Carlo’s suggestion.

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Keeping Warm?

 

Why would a Heron stand half submerged in the water on one of the coldest days of the winter? 20140205_0167

Note the pupil sizes in each eye. The one facing the sun is smaller.

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Border ice

 

Ice is endlessly fascinating; its various forms are a frequent topic for this blog in the winter.

As the air temperature now ranges between -15C and -10C, ice is making its appearance along the shoreline. It forms where the water is shallow, flow is minimal, and waves aren’t disruptive. Initially, it is frazil: individual crystals floating freely. These proliferate and consolidate to form skim ice, which now covers the water surface, but lacks strength. These are stages in the formation of the border ice that clings to the shoreline.

Frazil ice has consolidated to form some chaotic-looking skim ice.

Elsewhere, border ice has formed so slowly that it contains few bubbles and so is almost transparent. It looks dark because we are looking through it into the water below. The white crystals are frost growing atop the border ice.

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Four curious birds

 

The weather has turned cold and the temperature is expected to drop further. Yet, as the wind is gentle; walks are pleasant. What might one see along the lakeshore? My curiosity was peaked by the four birds shown here.

The first is curious for being unexpected: Black-billed Magpies along the West Arm of Kootenay Lake. These birds prefer open country with thickets and scattered trees, a description that does not fit the heavily forested West Arm. Certainly, it characterizes the Creston Flats (south end of the Main Lake), where I saw my last magpie. Yesterday, there were five of these frenetic birds roaming around Harrop; I only managed a modest shot of one of them. Yet, it is enough to show that the birds I saw were magpies.

Not far from the magpies was a solitary Bald Eagle. This was to be expected because a perennially active eagle’s nest was nearby, and the nesting season is approaching. The curious thing is that the nest has abruptly vanished! What happened to it? What will happen to the eagles? This story is unfolding.

Another curious observation for this time of year on the West Arm was a Red-tailed Hawk. It just seems to have turned up a month, or so, early.

This morning’s observation of a Northern Pygmy Owl is curious primarily because such sightings have become strangely tedious. The odd thing is that most winters I would get to see only one or two; this winter, I and others are seeing them with startling regularity. These birds don’t migrate from afar; they descend from the mountains. Why have so many of them visited the valleys this year?
  

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Cat’s paw prints

 

An ancient mariner’s term for a breath of air that lightly brushes the water is a cat’s paw. The name implies the gentleness of the touch; it is a zephyr, a gentle gust of wind. 

This would probably be unremarkable, except that cat’s paws are strikingly visible: you don’t just feel them; you see them. They usually take the form of a dark (occasionally lighter) patch moving across the surface of the water. This has caused some people to assign the name, cat’s paw, to the disturbed water, itself—and indeed to fabricate explanations of it based upon the character of the disturbance. I prefer the older terminology: a cat’s paw is a wind that gently disturbed the water’s surface, leaving a cat’s paw print

Yet, all who discuss it agree that the disturbance appears to result from ripples—that is, capillary waves—that have been excited by the gust of air. Indeed, this seems correct. The problem I faced was: Why do the ripples make the water’s surface appear dark?

Waves on water fall into two overlapping groups: gravity is the restoring force (think of a swing); surface tension is the restoring force (think of a spring). When the wavelength is greater than 1.7 centimetres, gravity dominates; when it is less, surface tension dominates. Now there are a few differences in behaviour across this divide (one was discussed at hoodie ripples), but the interesting one for cat’s paws is that while the slopes of gravity waves (λ > 1.7 cm.) never get large, the slopes of ripples (capillary waves, λ < 1.7 cm.) become quite steep.

To understand why the steepness of the waves makes a difference in the appearance, one can imagine a calm surface of water. The light coming from it is a mixture of light refracted from the depths and light reflected from above the surface. If the view is nearly horizontal, most of that light is reflected from a bright horizon; if the view is straight in, most of that light is refracted from dark depths. 

When the surface is irregular, what is seen depends upon the statistics of the surface tipping: gentle tipping, it still looks close to the brightness of a horizontal surface; steep tipping, it takes on some of the darkness of looking straight in. So, regular waves favour viewing light from the bright horizon, while ripples favour peering into stygian depths. 

Ok, the ripples created by the cat’s paw make the surface appear dark. Yet, another problem remains: Why does the print follow the paw (the gust)? Look at the issue this way: someone who is ski touring on virgin snow leaves a trail from the start to the finish. The cat’s paw only leaves a mark immediately below the paw—it leaves no trail. While a gravity wave can travel across oceans, a ripple (surface-tension restoration) decays rapidly. Remove the driving force of the wind gust and viscosity kills them within metres. 

There it is: cat’s paws are gentle gusts of wind that generate ripples on the water’s surface; the steepness of the ripples emphasizes stygian depths over horizon brilliance; the transience of ripples emphasizes tracks over trails.  

Dark patches move across the surface of the Lake. They are the prints from a wind called a cat’s paw.

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Northern Hawk Owl

 

Irruption of a natural population: to undergo a sudden upsurge in numbers especially when natural ecological balances and checks are disturbed

You may have heard the word irruption recently in connection with the Great Snowy Owl appearances in eastern Canada.

The appearance of Northern Hawk Owls in our area is described either as an irruption or a rare and irregular visitor. It’s nesting range is the boreal forests of Northern Canada, in forest fire clearings where there are rodents, open areas and perches. They are not uncommon here; recently they have been seen in the high country and in the Creston Valley. They hunt during the day primarily for voles. Their eyesight is exceptional, said to be able to detect prey at 800 meters. In flight they look remarkably like a hawk.

This owl was surveying a field adjacent to the highway near Salmo.

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