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SNOW!?

P80110If you do not know what it is, ‘snow’ is like frozen rain.

If you do not know what rain is, I wrote about it earlier for those of us who are native to the drier parts of California. If you notice strange drops of water falling from the sky tonight, that would be rain. There is no need to be alarmed. It is expected to happen here tonight, and a few times for the next few days. Contrary to former experience, it is normal for this time of year.

Anyway, getting back to snow. Unlike rain, which sometimes happens here, snow does not happen here.

Well, perhaps that is not entirely true. It might have happened as recently as 11,700 years ago, as the Ice Age ended, and again in more recent history, in February of 1976, when an epically humongous snowstorm deposited as much as half an inch of snow over the Santa Clara Valley!

It is difficult to imagine such a huge volume of snow! It must have been disastrous! It would be even more disastrous now, with more than a million people just in San Jose, and many of them driving cars!

In 1976, we third graders did not consider it to be disastrous. We were not old enough to drive. We were perplexed and mystified at first, but rather quickly discovered that snow had serious potential for being fun. Our parents wadded it up into something known as ‘snowballs’ and then threw these snowballs at each other and the neighbors. Yes, I know it sounds crazy. Nonetheless, it looked like fun, so we tried it. It really was fun. We also discovered that we could just as easily throw snowballs at cars driving by, but we were instructed to not do that. We could see that the Santa Cruz Mountains were discolored by snow. They were an almost white hue of very pale blue, speckled with the more typical darker blue.

On very rare occasion, when the ‘smog’* and smoke blew away on clear and cold wintry days, we could see snow on the tops of the highest peaks of the Diablo Range east of the Santa Clara Valley, particularly on Mount Hamilton where Lick Observatory is located. We did not know what it was. Before snow happened in our own neighborhood, we wondered what discolored the peaks like that.

Now that smog rarely obscures the view of the Diablo Range, snow is visible on the group of peaks around Mount Hamilton almost annually. If it gets cold enough, a slight blush of snow might be seen on the lower East Hills in front of the Diablo Range. It is quite scary to think of how close to home snow can be. There happens to be snow up there right now!

I am sorry that I do not have a picture of the snow on Mount Hamilton. I will just recycle this picture of Bill trying to escape snow south of Oklahoma City.

* Historical notation – The East Hills and Diablo Range to the east of the Santa Clara Valley were rarely visible in the olden days because of ‘smog’. If you do not know what smog is, you are fortunate. I have not written about smog yet because it is a part of our history that we would prefer to forget. To be brief, smog was a common form of air pollution. Although there was less smog in winter, there was more smoke from ‘fireplaces’ and burning ‘orchard’ stubble. A fireplace was a primitive heating device that warmed the interiors of homes and other buildings with the combustion of wood. An orchard was a grove of trees that were installed and maintained for the production of fruits, nuts and a few other horticultural commodities. Orchards once occupied vast areas of the Santa Clara Valley. Orchards that were removed to relinquish space for other development provided some of the wood for fireplaces. Perhaps I should write more about these later. I understand that the ancient history of the Santa Clara Valley can be rather baffling at times.

Posted on by tonytomeo · 10 Comments

The Weather Outside Is Frightful

P80110It is certainly not as cold as it is in other regions at or north of this latitude. Nor is it unusually cold for this time of year. It is not stormy. We got only a few heavy but brief rain showers with a bit of small hail. A slight bit of snow fell only on the Summit of the Santa Cruz Mountains

The problem is that the weather had been so mild earlier, and at times, downright warm. Many plants were coerced into premature bloom. Some started to generate new spring growth. When the weather suddenly became more seasonably cool, many of the flowers and new growth got frosted and ruined.

Fortunately, most of the deciduous fruiting trees seemed to know what they were being set up for, and abstained from bloom. So far, even the early blooming apricots, cherries, almonds prunes and plums are safe. The wild American plums bloomed, but not many of us use their fruit anyway. (I want some – both amber and red – for jelly, but there will be plenty of other fruit.)

Saucer magnolias were just beginning to bloom when the cool weather moved in. Now, some of the big pink flowers are spotting and melting before they open completely. Many of the camellias are succumbing to blight, and falling to the ground shortly after they open.

Weather is always risky, even in mild climates. Actually, our mild climate allows us to grow more of the plants that are sensitive to anomalies of the weather. Perhaps such anomalies would be less of a problem in harsher climates where the weather is naturally more variable. If so, it is probably a fair compromise. The problems with such a mild climate are still less significantly less than the advantages.

Posted on by tonytomeo · 18 Comments

The Coast Is Clear

P80218Between here and Hawaii, there is a whole lot of water. Between Hawaii and Australia, there is a whole lot more. Everywhere to the west and southwest of California, there is a lot of water. Unfortunately, none of this huge volume of water is useful for gardening. It is saline. It would kill plants.

Of course this is not just any water. It is the Pacific Ocean. Although the water within it is useless directly, it is what feeds the weather that provides the precipitation that becomes the water that makes gardening and everything else possible. Rain fills local aquifers. Snow in the Sierra Nevada fills reservoirs as it melts.

The weather that the Pacific Ocean feeds gets shared over a very large area. Weather that does not make rain here might make rain or snow in Nevada, or Oklahoma, or really anywhere the weather wants to go to. In fact all the oceans all over the world cooperate to make climate and weather what it is.

What is so special about the Pacific Ocean being right here off the coast is that it moderates our climate and weather. Places like Nevada and Oklahoma that are not on the coast get water from the Pacific Ocean because weather is mobilized. The moderating effect of all that saline water is not. It stays right here in coastal regions.

Water has a high specific heat. That means that it takes a lot of energy to change the temperature of water. Saline water has an even higher specific heat. The temperature of the Pacific Ocean therefore changes very slowly and very minimally.

This inhibits extremes of temperature in the air above all that saline water. Small batches of extremely cold weather tends to collect a bit of heat energy as they pass over the Pacific Ocean. Weather coming in over so much saline water can not get extremely hot without the water absorbing at least some of all that heat energy. Therefore, coastal weather is rarely extremely cold or extremely hot. Temperatures can be more pronounced a few miles inland from the Pacific Ocean, especially when the weather comes from inland. Farther inland cold and heat can get significantly more extreme.

A lack of cold weather in winter limits what can be grown here. Plants that require a good chill are not satisfied with our pathetic winters. That is why some bulbs that do well as perennials farther inland bloom only once here, and why some varieties of apple that perform well in central Washington are not grown here.

However, a lack of hard frost allows us to grow many plants that can not be grown where winters are more severe. Even if bougainvillea gets frosted every few years or so, it typically recovers. Avocados and lemons are likewise quite happy here. The weather may seem to be boring, but it certainly has its advantages.

Posted on by tonytomeo · 14 Comments

Weather To Die For

B80210KDon’t worry. He is not really deceased. He is just making good use of the lawn. The well foliated trees in the distance are a clue that this pictures was not taken recently, although it illustrates the current weather conditions accurately. We all want to be out in it, whether getting lazy in a local park, walking on the beach, or just staying home and working in the garden.

It seems that almost everyone else is contending with less pleasant weather. The summer in much of Australia had been historically hot. Much of Europe got some nasty storms. Parts of the Southeastern United States of America that get snow only on rare occasion got more than they have in recent memory.

We are certainly used to our share of pleasant weather through winter. We can only see snow in the distance on top of Mount Hamilton. Frost only happens a few times through winter. We often get a few consecutive days at of spring weather. What we are not accustomed to is this sort of duration of pleasant weather.

Many years ago, such a long duration of pleasant weather would have been bad for the orchards of the Santa Clara Valley. It would have prompted them to bloom prematurely, only to get the blossoms and developing fruit knocked off by subsequent rain. Although the orchards are gone, many of us still grow similar fruit trees in our home gardens. Apricots, cherries, nectarines, peaches, plums, prunes and almonds are all susceptible to premature bloom.

We really could use some wintry weather about now. Rain here with snow in the watersheds of the Sierra Nevada would be the best. Otherwise, cool weather to delay bloom of fruit trees until after the rain would be the second best option.

Posted on by tonytomeo · 9 Comments

Rain Is Necessary But Messy

10914Water is no more scarce in California than it has been in recorded history. The problem with it is that it is a limited resource that must be shared amongst too many people. Likewise, rainstorms are no more torrential than they have ever been. Floods, erosion and wind are only more destructive now because there is so much more infrastructure that can be damaged than ever before.

Rain and wind are perfectly natural. Furthermore, it is natural for the weather to knock down limbs or entire trees. It only seems unnatural when these limbs or trees fall on houses, cars or anything else that gets in their way. Plants actually enjoy rainy weather much more than we do. Some like to be rinsed of dust and debris left from former infestations of mites, aphid, scale or sooty mold.

What plants do not like about rain is erosion. It is bad enough that so many plants in refined gardens are deprived of their own litter to insulate the surface of the soil. It is even worse if the bare soil gets eroded away from fine feeder roots at the surface of the soil. This is something that the rest of us would agree on. We do not want gullies carved into slopes, or drains clogged with mud.

Trees, shrubs and some stout perennials with aggressive roots are useful where the potential for major erosion is a concern, but might not do much for annoying surface erosion. Sprawling and spreading plants that form dense networks of low branches and surface roots are more effective. They soften the splatter of rain, slow the flow of drainage, and catch much of any dislodged silt.

Groundcover plants like ivy, gazania and iceplant are probably the best option for controlling surface erosion. Dense and low shrubbery that spreads over the ground and holds its own debris probably work just as well. These include low junipers, trailing rosemary and dwarf coyote brush. Larger shrubbery can help if it can drag its lowest limbs on the ground, and no one rakes below it.

Mulching limits erosion while new plants grow. Although new mulch needs to be added annually as old mulch decomposes, less will be necessary as plants grow and cover more area. Mulch is also effective where no plants are desired. For large areas, especially where plants are not expected to fill in, landscape cloth below ornamental bark inhibits weeds. However, coarse bark slowly shifts downhill, so replaces one kind of erosion with another, and will eventually need to be raked back uphill.

Posted on by tonytomeo · 9 Comments

Snow

P80110It seems that almost all of us in the Northern Hemisphere are talking about it. Those of us who lack it can get to feeling somewhat deprived. It looks so pretty in pictures. It seems like such a natural part of winter. To many of us, it is a good excuse to take a break from gardening, stay inside, and write more compelling articles than the more technical sorts written when there is more activity in the garden.

In California, we get almost everything. Although most of the most densely populated ares lack snow, parts of the Sierra Nevada get more snow than anywhere else in the world. Californians can go to the snow to ski, hike, take pictures and do whatever people want to do in the snow; but we do not need to live with it at home like most people in other states do.

I grew up without snow. It snowed only once in 1976. It was only half an inch deep. The snow fell overnight while everyone slept, and it melted by early afternoon. Because the turf in the schoolyard was not resilient to snow, we were not allowed out there until the snow was gone. I later saw snow only when we went to where the snow was, in the Sierra Nevada. Snow only rarely fell at my home near the summit of the Santa Cruz Mountains above town, and it stayed for only a few hours.

I never had to live with snow until I went to Oklahoma at the end of 2012. Even then, it was minimal. The first snow fell only about three weeks before we left, and it never accumulated more than two inches or so. The difference from what I had experienced prior to that was that it lingered. It took a few days to melt. As minimal as it was, I could totally understand why people who live with snow dislike it so. I really can not imagine living with more accumulation of snow for months at a time.

First of all, snow is cold. It is very cold. It is, after all, frozen. That would not seem like much of a problem when the air is already cold, but snow is different. It sticks to the sides of boot and makes them cold inside. It seems to hold the cold on whatever it covers, including parked cars.

Also, snow is wet. Yes, as I already mentioned, it is is frozen, but it is frozen ‘water’, and it does not stay frozen when one is trying to get warm after being out in it. It gets clothing and everything else wet, just like a light rain. Frozen snow gets tracked in on boots and then melts just inside the doorway.

To go along with that, snow is messy. As cars drive through it, it becomes muddy, but does not necessarily melt right away. It becomes slushy mud that splatters onto otherwise clean cars.

There is actually quite a list of things to dislike about snow. It is dangerous on roadways. When it gets pushed off of roadways, it piles up around parked cars and on top of plants that happen to be in the way. I think that I prefer to see it in pictures of Switzerland, Minnesota, Ontario and Mount Hood as it looks from Portland.

Sometimes I think that it would be nice if we got a bit more of a chill here. We would be able to grow more varieties of apples, pears and other fruits. Perhaps peonies would do better, and autumn foliar color would be more spectacular. There are so many things that we can not grow or that do not perform as well as they want to in such a mild climate. However, all those frost sensitive plants that we can grow that others can not grow are nice too. Either way, I will pass on the snow.

Bill was mostly blind by the time we went to Oklahoma, but he could feel the snow on the ground well enough to determine that he did not like it either.P80110+.jpg

Posted on by tonytomeo · 4 Comments

The Molting Of The Chrysler

P80108+The old Chrysler looks different this time of year. Like dogs, cats, horses and deciduous plants, it adapted to the weather.

That tan canvas structure above the cab is known as a ‘roof’. It was there all along, but folded up behind the back seat. It was merely unfolded over the top of the cab. The ‘roof’ comes in handy this time of year, not only for keeping warmth within the cab, but also for keeping things out of the cab. Allow me to elaborate.

You may nave noticed that the Chrysler is wet. This is a direct result of mysterious droplets of moisture that fall from the sky. We discussed them earlier. They are known ‘rain’, and are falling from the sky presently. The ‘roof’ keeps the ‘rain’ out of the cab. Otherwise, the cab and everything in it would be as wet as the ‘roof’ is now.

The yellow, orange and reddish brown things strewn about are sweetgum leaves. You may not recognize them now because they are not green. They change color when the weather gets cool this time of year, and then get dislodged by meteorological events such as wind and the presently observed ‘rain’. The ‘roof’ excludes them from within the cab of the car.

The two devices at the bottom of the windshield are another adaptation to ‘rain’ known simply as ‘windshield wipers’. When in operation, they pivot from where they are affixed just below the windshield to literally wipe the the wet ‘rain’ away. They are a rather ingenious invention, since ‘rain’ on the windshield tends to inhibit visibility.

Just as a thick coat on a dog or horse can predict an unusually cool winter, the molting of the Chrysler is directly related to the weather. Although it can not predict ‘rain’ as early as dogs and horses can predict cold weather, it quite reliably happens immediately prior to ‘rain’. It is a good sign for the garden.

The ‘rain’ that falls immediately after the molting is composed of water, which is very important and useful to gardens and forests after such a long dry summer. As we discussed earlier, some of the water gets into the aquifer where it is stored for later use in and around our homes. We are very fortunate to have a Chrysler who is so proficient at predicting the delivery of the water that we need so much of.

Posted on by tonytomeo · 18 Comments

‘Rain’

P80103+Like something from an old fashioned science fiction movie, this anomaly appeared in a roadway overnight. There are several more in other roadways and elsewhere about town. They are quite wet. In fact, they are composed almost completely of water. What is even weirder is that the water that they are composed of actually fell mysteriously from the sky overnight as many countless droplets all over town! Many of these droplets migrated into low spots such as this one to form what we now see in this picture.

People in other climates where these mysterious droplets are not so rare might be familiar with this sort of phenomenon. The droplets of water are known as ‘rain’. They precipitate out of the atmosphere as it cools and can not contain as much water vapor as it did when it was warmer. As the droplets migrate into low spots in roadways and anywhere else, they accumulate into these collective herds of droplets known as ‘puddles’. Many of the droplets continue to migrate as huge herds known as ‘creeks’, and even bigger creeks known as ‘rivers’. Some of these creeks and rivers migrate into really big puddles known as ‘ponds’, and even bigger ponds known as ‘lakes’. Sadly, not all of the droplets can be accommodated in ponds and lakes, so many continue to migrate out into the ‘ocean’, which is that really big pond full of salty water to the west that we are all familiar with.

Hopefully, some of these droplets of rain will stay around for a while and provide water for the plants in our gardens and forests. Ideally, some will burrow into the ground and stay for a very long time, and maybe even migrate into the aquifer to hibernate. In our climate, particularly after such a long and dry summer and autumn, these strange droplets of rain are very welcome to stay as long as they want to.

Posted on by tonytomeo · 2 Comments

Unseasonable Weather Can Confuse Plants

70920thumbEven without any of the five senses that we are outfitted with, plants are remarkably perceptive of the weather and the changing seasons. They know precisely what time of year it is because they know how long the sun is up. Their calendar is just as accurate as ours is. They also know that the weather has been getting progressively cooler through autumn, and that it rained a bit earlier.

New Zealand tea tree, torch lily, euryops daisy and many other plants from other temperate climates do not seem to care that they should not be blooming at this time of the year, if the weather is telling them otherwise. If the weather is warm enough during the day, even if it gets cool at night, these plants will bloom right up until things get really cold, even if some of their bloom gets frosted.

Saucer magnolia, lilac, apple and the many other plants from climates with cooler winters should know better than to bloom this time of year. Many bloom only once annually, so whatever blooms now will not bloom when it should next spring. Besides, the flowers that try to bloom now will bloom slowly, and probably be ruined by cool or rainy weather before they can develop completely.

Roses had a particularly weird year. They bloomed well and on schedule last spring, but then idled through much of summer, only to express a new interest in blooming now that they should be going dormant for winter! No one wants to prune them while they have more buds than they did in August. Fortunately for them, they bloom more than once annually, so should recover by spring.

The colorful foliage of sweetgum and Chinese pistache, as well as the observable weather, indicate that everything is more or less in order for this time of year. Autumn might have started out mild, but it had been even warmer in past years. It is impossible to say why some magnolia, lilac and apple are trying to bloom already. They each have such distinct personalities, and respond to so many different variables besides the obvious; daylength, temperature and humidity.

Posted on by tonytomeo · 10 Comments

Frost!

P71208+K1Yes, we get it too. It took a while, but we finally got it just like most of everyone else in North America and the Northern part of the Norther Hemisphere. It is not much to brag about, but it is enough to melt the big feral pumpkin vine that I wrote about earlier ( https://tonytomeo.wordpress.com/2017/12/03/too-late-for-pie/ ). It has actually been frosting for a few nights. I just got around to getting this picture this morning.

Now that the foliage is melting and collapsing, a leak is now visible in the exposed valve manifold that was obscured in the previous picture. It did not get cold enough to freeze the pipe, so the water was dripping freely. This confirms the earlier theory about where the pumpkin vine was getting water from.

Two pumpkins are also exposed by the collapsing foliage. They were not visible earlier. Unfortunately, they are too under-developed to mature and ripen. A neighbor will likely take them and set them aside on the porch, just in case they are able to finish ripening. It would be nice if they did. The vine certainly put a lot of work into them!P71208+K2P71208+K3

While taking this picture, I was reminded why people who live with cooler weather dislike it so. First of all, and most obviously, it kills things. The season is over for pumpkin vines, which is not a problem. The problem is that so many of the citrus, avocados and other plants from mild climates that we grow so easily here get damaged or killed by frost in other climates.

The second reason to dislike cool weather is that it is too cool, maybe even cold. It is uncomfortable to be out in long enough to walk over and get these pictures of the pumpkin vine and pumpkins. I am glad that it does not get much colder here.