All right, I exaggerate. But for several days earlier this month it felt like a distinct possibility. Or that at least some of the plants in the garden would take flight.
I don’t like strong winds, meaning more than 20 knots (37 km or 23 miles per hour). You would think that after thirty-two years I would be reconciled to them, because they’re not unusual here. I know the patterns by now: a low pressure weather system (which may or may not produce rain) is almost always followed by an episode of moderate to strong westerly winds. Such a wind blew from May 16th to 19th, almost without pause. It was the duration rather than the strength I found most trying.
The wind doesn’t really affect me personally, now that fifteen-kilometer (each way) bike rides are no longer part of my life, as they were when I was commuting to work. No, it’s the plants in my garden I worry about, especially when I see them swaying, thrashing, leaning, and occasionally breaking.
I provide stakes and string early in the season. I learned long ago it’s best to do that before supports are needed, rather than try to strap a leaning, disheveled plant to a pole after the damage is done. Not all plants can be staked and tied, however. Hellebores, for example, are clumps of big leaves, each on its own stem that sprouts from the ground. They’re self-supporting up to a point, but when the wind sways them back and forth, back and forth for three solid days, they splay out, and some are snapped off altogether.
Once things calm down, the garden looks battered and bruised. Pulped leaf fragments and twigs are everywhere, along with a few branches. Plants that were shapely and attractive before the blast have acquired an eastward list. Pots have fallen over and their occupants sustained some degree of injury. And if there has been no rain to accompany the wind, some plants may be limp and wilting.
The gardener, needless to say, is not happy, running around trying to set things to rights and cleaning up the debris, muttering curses the whole time.
I know winds aren’t malevolent forces intent on doing damage. They are natural phenomena caused by differences in atmospheric pressure of adjoining air masses, which create pressure gradients. In other words, areas of low pressure suck air from areas of high pressure. This is part of local weather, and it’s a fact that Victoria, British Columbia, is located in a place where weather systems trundle through and atmospheric pressure rises and falls. This produces winds. So suck it up (haha!)
As well as the post-frontal westerlies I’ve been complaining about here, we get icy north-easterlies at times in winter, like the ones that caused much damage in southern British Columbia last January. Meteorologists in Washington State refer to these as “Fraser outflow winds,” after the valley of the Fraser River, down which the cold air is funneled. Similar winds in high summer bring heat waves. In autumn, southeasterly gales precede our major rain events. As the air pressure rises after a cold front passes, the aforementioned westerlies kick in, blowing hard from the opposite direction.
The only wind I welcome is the westerly breeze that dispels our summer heat waves, as offshore air flow changes back to onshore, bringing the cooling effect of air from the Pacific Ocean. Those Washington State meteorologists call this a “marine push.”
Winds that happen at particular times in particular places are often given names. With a few exceptions, names are most often bestowed upon winds with unpleasant effects, such as cold, heat, or dust. I’m surprised there are so few named winds in Canada. On the east side of the Canadian Rockies we have Chinooks, that can suddenly raise winter temperatures by 20 degrees. Squamish winds funnel cold air through the fjord-like inlets on the north coast of BC, and, I suppose, the Fraser Valley as well. There is the famous Witch of November on the Great Lakes, but that’s about it for Canadian named winds, as far as I know.
I have my own names for these masses of moving air, some not printable. The post-frontal Westerly Whooper, which I’ve already described. The Thermal Trough Terror, a hot outflow from the interior of the province. The Arctic Blast or Fraser Freezer. The welcome westerly marine breezes that dispel our heat waves could be dubbed the Pacific Doctor, analogous to the Cape Doctor of South Africa and the Fremantle Doctor of Australia. But somehow these don’t sound as interesting as Mistral, Sirocco, or Simoom. Or Elephanta, Khamsin, and Williwaw.
Ah well, the winds can’t be argued with, and they do make me appreciate and treasure calm summer evenings, which are magical and lovely.
In case you’re wondering, yes it’s windy again today (May 25th). Twenty-three km WNW.
Featured image from Pexels.