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Planting Should Not Be Complicated

Soil amendment should not be excessive.

Autumn and winter are generally the best seasons for planting. Most vegetation is either less active than during other seasons, or dormant. It is therefore more complaisant to the distress of planting procedures. Weather is cooler and wetter than during other seasons. It is therefore less stressful to vulnerable vegetation recovering from planting procedures.

Nonetheless, planting continues throughout the year. Seasonal vegetables and annuals are seasonal at various times. Planting after any lingering chill or potential frost of winter is safer for several species. Also, planting commonly happens whenever it is convenient for whomever does it. Many species are most tempting whenever they happen to bloom.

Generally, this is no problem. Planting while vegetation is active during warm weather is riskier but feasible. It should preferably happen after the warmest time of day. Weather is likely cooler after three in the afternoon. Unusually hot weather justifies delay for another day. Once planted, thorough soaking settles comforting wet soil around vulnerable roots.

Realistically, most planting techniques and concerns are the same regardless of season. The processes only have more potential to be more stressful now than during dormancy. A few species are actually dormant during summer or even spring. Several spring bulbs, such as narcissi, are now ready for division or relocation. Bearded iris rhizomes are also.

Soil amendment helps new plants to feel more comfortable within their new situations. It encourages them to extend roots from their original media into surrounding soil. It should not be excessive though. Contrary to overly popular belief, it is unnecessary below roots. New plants can sink detrimentally below grade if amendment or loose soil below settles.

Stakes for trees that need them must extend past roots and into solid soil below. Binding nursery stakes should be loosened or removed if possible. Binding, which initially keeps trunks straight, can later interfere with trunk development. All new plants need systematic watering through dry seasons until they disperse roots. Most appreciate a layer of mulch, to retain moisture and insulate.

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Aridity Is Opposite Of Humidity

The sky is bluer with aridity.

Aridity is a measure of humidity. Humidity is a measure of aridity. Although opposite, they are similar. Humidity is the quantity of water vapor that is suspended within the air. Aridity is a deficiency of humidity. They are components of weather that are more likely felt than seen. Although, aridity clarifies the air, which typically causes the sky to seem more blue.

Of all components of weather, only atmospheric pressure is less tangible than aridity. It is measurable with instrumentation, but perceptible to very few. Except for its clarification of the sky, aridity is just as invisible. It is more perceptible, though. Just as humidity inhibits dissipation of heat, aridity promotes it. Therefore, arid heat feels cooler than humid heat.

That is why the West Coast is famous for its delightfully arid weather with sunsets. Even when the weather here is warmer than elsewhere, it may be more comfortable. Although undesirable, smog and smoke from forest fires provide color for clear sunsets. Temperate arid weather is more conducive to gardening. However, some vegetation might disagree.

Fragrant flowers can not disperse their fragrance quite as effectively during arid weather. Nor can aromatic foliage disperse its aroma quite as effectively. A few varieties of colorful foliage and flowers may fade a bit faster with minimal humidity. After all, most vegetation within home gardens is originally from more humid climates. It naturally enjoys humidity.

More importantly, most vegetation needs more water through arid weather. It loses much more moisture from its foliar surfaces at such times. Any breeze, which people might like, exacerbates loss of moisture. Obviously, warmth does also. Automatic irrigation requires appropriate adjustment as weather changes. Manual irrigation may become demanding.

Irrigation is less demanding for species that actually prefer local Mediterranean climates. Many of such species are native. Most are native to other regions with similar climates. A few are native to climates that are more arid, but tolerate a bit of extra moisture. Weather and climate do not adapt to a garden. It is best to cooperate with climate than not.

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In The Zone

Climate is regional.

We all know how excellent the local climate is for gardening. As we travel around the area though, we also realize that there is more than one climate. Locally, there are at least three of the standardized ‘Sunset’ garden zones, with several more within only a few miles. There are countless microclimates too.

Elevation, terrain, latitude and the proximity of the ocean or large bodies of water all influence the climate. Even though the Santa Cruz Mountains are not very high, they sometimes get snow on top because higher elevations are a bit cooler. When the Summit and Santa Clara Valley floor are cold in winter, the slopes in between are not quite as cold because cold air drains away downhill. The areas closest to the San Francisco Bay stay much cooler through summer because of the insulating quality of the water. 

More localized variables like forests, lakes, direction of slopes and infrastructure affect microclimates. Older neighborhoods with mature trees are shadier and cooler than newer neighborhoods with smaller trees. The west facing slopes to the east get warmer than the east facing slopes to the west. In Downtown San Jose, tall buildings create cool and shady microclimates to the north; and some reflect enough solar radiation to significantly warm areas to the south and west.

It is important to know what climate zone any particular garden is in to be able to select appropriate plants. Besides that, it is important to know the microclimates within the garden to know where each plant will be happiest. Tropical plants that would be happy in Los Angeles might succumb to even mild local frosts. However, plants that might succumb to frost if too exposed may be safe in sheltered microclimates.

Generally, Campbell, most of San Jose, southern Sunnyvale, northeastern Cupertino, northeastern Los Gatos and Union City are all within Sunset Zone 15. Most of Saratoga, southwestern Los Gatos, southwestern Cupertino and Mission San Jose are in Zone 16. Santa Clara, Alviso, Milpitas, northern Sunnyvale and western Fremont are in Zone 17.

None of these zones are too severe. Because of the marine influence of the San Francisco Bay, Zone 17 can actually be relatively boring and not so great for plants that want winter chill or summer warmth. Zone 16 is very similar to Zone 15, but comprises hillside thermal belts where cold air drains away in winter, and also gets a bit warmer in summer. Above and below Zone 16, Zone 15 gets cool enough for plants that want winter chill, but may not get warm enough in summer for plants that crave heat. The Sunset Western Garden Book not only describes the climate zones in detail, but also specifies what zones every plant is adaptable to.

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Microclimates Are Distinct From Climates

Larger buildings inevitably produce larger microclimates.

Climates and geology are why cinema and television industries are so established here. Cinema evolved in Niles before relocating, with the evolution of television, to Hollywood. The diversity of local climates, geology and associated scenery was the primary appeal. Farmers of all sorts had already been exploiting such climates as well as microclimates.

Climate is a regionally prevalent pattern of weather. Mediterranean or chaparral climates are prominent locally. Coastal, desert and alpine climates occupy other relatively nearby regions of California. Variations of geology influence weather, which determines climate. This comprises mountains, valleys, various altitudes and proximity to the Pacific Ocean.

Microclimates, as their designation suggests, are small climates within big climates. With such a mix of climates here, microclimates might be difficult to distinguish. Some climate zones of steep coastal hillsides are very narrow, for example. Yet, if they are distinct from those for higher and lower elevations, they are climates. Microclimates are even smaller.

For microclimates, exposure is as relevant as endemic climates. Such exposure can not change climate, but modifies its influence. For example, large eaves and warm walls can provide localized shelter from frost. Southern slopes of hilly terrain are likely a bit sunnier and warmer than northern slopes. Buildings and fences shade garden area to their north.

Many microclimates, such as those that involve terrain or forest shade, are natural. They are generally less dynamic than unnatural microclimates. Forest shade changes only as fast as associated trees grow or die. Only major disruption, such as fire or timber harvest, accelerates such slow change. Terrain may not change significantly for millions of years.

Unnatural microclimates are more dynamic and unpredictable. Taller modern homes and fences shade more within adjacent gardens. Skyscrapers can extend their shadows into gardens a few blocks away. Conversely, some can reflect sunlight to adversely increase heat and glare. Expansive and unshaded pavement likewise increases ambient warmth.

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Environmental Factors Silently Influence Bloom

California poppy dramatizes favorable weather conditions.

Superbloom occurs only about once every decade or so. It is very unpredictable though. It can happen for two or even three consecutive springs. Alternatively, it may not happen for two decades. It can be as early as late February, or as late as late May. It can last one or a few weeks. Superbloom is as variable as the environmental factors that influence it.

Actually, all bloom relies on influence from variable environmental factors. That is how it knows how and when to bloom. It is also why many species are so irregular about doing so. Various species prioritize reliance on various environmental factors. Therefore, some may bloom early or late while others adhere to stricter schedules. It can get complicated.

Warmth is undeniably the most significant of environmental factors that influence bloom. Cool weather inhibits bloom, even as growth resumes at the end of winter. Then, warmth accelerates bloom, mostly during spring, but also into summer. Many species continue to bloom as long as the weather stays warm. Very few prefer to bloom during cool weather.

As mentioned, the influence of environmental factors can get complicated. Many species actually require sustained winter chill, or vernalization, to bloom well. It is how they reset their growth seasons to begin in winter. Peony is unreliable here because of inadequate chill. After unusually cool winter weather though, flowering cherry and lilac bloom better.

Humidity is another important environmental factor. Although it does not stimulate bloom for more than a few species, it can prolong bloom. Some flowers, particularly from humid climates, can desiccate with aridity. Conversely, even flowers from desert climates retain hydration better with humidity. Also, rain provides water for areas that lack any irrigation.

Species from mild but not tropical climates might rely more on photoperiod than weather. Poinsettia in the wild does not experience sufficient chill to distinguish winter. It monitors the photoperiod, which is the duration of daylight, instead. It knows to bloom when nights are longer than days. A few species use the same very consistent technique to bloom for other seasons.

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There’s No Place Like Home.

Desert ecosystems are fascinating, but so are local ecosystems.

Vacation was excellent! I do not get out much, but when I do, I feel as if I enjoy it more than those who travel regularly. The simplicity of my travel allows me to enjoy it more intimately than those who travel more elaborately and put more effort into enjoying what they should probably just enjoy more effortlessly. Anyway, I went to the Pacific Northwest for two weeks, returned for two weeks, and went to the Southwest for two weeks. Actually though, my trip to the Pacific Northwest was limited to Western Oregon and Western Washington, and my trip to the Southwest was limited to the area between Los Angeles and Phoenix. Regardless, it was excellent, and I encountered several climates and ecosystems that are very different from what I am accustomed to. I drove through dense rainforests dominated by massive Douglas firs as well as sparsely forested deserts dominated by sporadic saguaro cacti. Winters are much cooler in some regions than here. Summers are much warmer in some regions than here. It was all so fascinating. I encountered so much vegetation that I would like to grow here, and brought a bit of it back, but can not grow everything that I find intriguing within other regions. However, as excellent as it all was, it also reminds me that I prefer to be here, within the climates and ecosystems that I am most comfortable with. Winters do not get too cool. Summers do not get too warm. I may not be able to grow all the cultivars of apples that prefer a bit more chill in Washington, or all the cacti that prefer more arid warmth in Arizona, but realistically, even if I could work in the garden constantly, I could not possibly grow everything that performs well here.

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Timeout

A moment before sunrise over Phoenix.

Apologies for my absence.

Perhaps no one noticed. Most of my posts were automated prior to my departure, and I managed to compose a few brief articles for what was not automated; so ultimately, there was no lapse of posting. I may have only been negligent with response to comments for the last two weeks.

Realistically though, I have been intending to discontinue blogging and recycling old articles, and to post only my weekly gardening column, in two parts, on Mondays and Tuesdays. I merely have not done so yet.

Anyway, my trip, although very different from how it was planned, was totally excellent! Just a short distance from the turnoff for the southbound San Diego Freeway towards my primary destination in Los Angeles, I was diverted to my secondary destination northwest of Phoenix. I missed the desert scenery as I drove all night to arrive shortly before four in the morning, and began my vacation exhausted. Although I missed out on some of my plans in Los Angeles, I got more time in Arizona. The weather was weirdly excellent, with a weirdly torrential thunderstorm right in the middle of it. It was too early in the year to collect the seed that I wanted, but I really was not expecting to find any anyway. I did happen to procure a hedgehog cactus of some sort. I decided that, since my return was already delayed by a day, that I may as well delay it for two days. (I had brought some of my work with me, so was able to tend to it prior to my return rather than after.) Therefore, I came to my original primary destination in Los Angeles secondarily, stayed to help Brent with the View Park Garden Tour on Sunday, and returned home on Monday.

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Mediterranean Climate Is Quite Californian

New Zealand natives perform well here.

“Mediterranean” translates from Latin to “middle of land”. The Mediterranean Sea is in the middle of the land of those who named it. Other regions were either unimportant or unknown to them until the Sixteenth Century. Nowadays, most people of the World are aware of many other regions. A few of such regions also enjoy a Mediterranean climate.

Such climates are obviously not confined to the regions of the Mediterranean Sea. They merely resemble such climates. Some extend eastward into Western Asia. Others are in eastern and southern Africa, southwestern South America and Columbia. Larger regions of such climate are in southern Australia. The closest are here in western North America.

Even these limiting regional designations are debatable. Many horticulturists consider climates of New Zealand to be typical Mediterranean. Such climates are mostly between thirty and forty five degrees north and south. However, some might exist within northern India and southern China. Ultimately, climate is meteorological rather than geographical.

Mediterranean climates receive almost all of their rain during winter. Rain is very minimal through summer. Even if it is twice as abundant in other similar climates, it conforms to a similar schedule. Although winter chill is adequate for many species that need it, frost is mostly minor. Locally, summer weather does not often become too uncomfortably warm.

Native species know what to expect from local climate. So do exotic species from similar climates. Some may prefer more or less winter rain, summer heat or winter chill. Almost all can tolerate warm summers without rain, though. Such weather conditions are normal for them. Therefore, the most adaptable exotic species locally are from similar climates.

This includes species of Eucalyptus, Pittosporum and Callistemon from Australia. Aloe, Agapanthus and Morea are from South Africa. Phormium and Leptospermum are from New Zealand. Oleander and the various species of Lavandula are truly Mediterranean. In the past, a few exotic species adapted too efficiently to become invasively naturalized. Horticulturists are now careful to not import such potentially aggressive species.

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Irrigation Resumes With Drier Weather

Spring gets progressively drier and warmer.

Spring, in several regards, is like autumn in reverse, or vice versa. Bloom increases for spring but decreases for autumn. Foliage increases for spring but decreases for autumn. The two seasons are in opposition. In this chaparral climate, the rainy season that began last autumn ends now. Irrigation that became redundant then becomes necessary now.

Diminishing rain is not the only reason that irrigation becomes more important for spring. Spring weather also becomes warmer and more arid, or less humid. Warmth and aridity increase evaporation of moisture that rain deposited not long ago. Increasing day length, intensifying sunlight and warmth accelerate plant growth. Such growth consumes water.

This need for moisture is progressive, though. Vegetation certainly requires more water as the weather becomes warmer and drier. However, it does not yet require as much as it will require later during summer. By then, the weather will be even warmer and drier, and the days will be even longer. Irrigation should increase accordingly in regard to weather.

Unfortunately, there are no simple formulas to determine how much irrigation is needed. Some vegetation with shallow roots may require frequent but moderate irrigation. Some vegetation with deep roots may prefer less frequent but more copious irrigation. Rain is possible at any time. It can briefly interfere with the most efficient of irrigation schedules.

Soil also affects irrigation. Sandy soils drain efficiently, but do not retain much moisture. This may not be a problem for some species that tolerate occasionally dry soil. It may be more of a concern for species that prefer more regularly moist soil, though. Dense soils retain more moisture, but do not drain as efficiently. Soil amendments can improve soils.

Manual irrigation is easier to monitor than automated irrigation, but can be tedious. That is why most irrigation is automated nowadays. Automation is more likely to be excessive than insufficient. Desiccation, wilting and other symptoms of insufficiency of irrigation are obvious. Symptoms of saturation may not become obvious until too late for remediation.

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Wind Is Messy And Hazardous

Trees lose limbs to strong wind.

Arborists become more popular after storms. That is when consequences of negligent tree maintenance become more apparent. Wind dislodges limbs and destabilizes whole trees. Unfortunately, the most diligent of tree maintenance can not prevent all damage. Trees and other vegetation are naturally vulnerable to frequently stormy winter weather.

Deciduous trees try to be less vulnerable to wind by defoliating prior to winter. Without foliage, they are less resistant to wind. In other words, they are more aerodynamic. Wind blows through them rather than against them. Some unfortunately defoliate slowly within the mild climate here. With such minor chill, some retain foliage until spring replacement.

For example, some sweetgum still retain much of their foliage. That is an advantage for the display of their autumn foliar color. It is a major disadvantage for their aerodynamics though. As a deciduous species, it does not expect to be so vulnerable to wind through wintry weather. What is worse is that sweetgum trees are innately structurally deficient.

Evergreen trees and other vegetation seem to be less concerned about wind. Actually, they merely employ different defensive tactics. Most cypress and some spruce are too dense and sturdy for wind to penetrate. Many pines develop sparse canopies that wind blows through. On the coast, coast live oak stays low and broad for wind to blow over.

Regardless of their efforts, trees of all sorts are vulnerable to damage from wind. Falling limbs or entire trees are very hazardous. Also, they can damage or destroy what they fall onto. That is why timely maintenance of trees is so very important. Any tree that becomes too hazardous to salvage necessitates removal. All trees eventually age and deteriorate.

Also, all trees, as well as all other vegetation, are messy. Some are messier than others; and many get messier as a result of wind. Some of such mess clogs eavestroughs and downspouts when they are most helpful. Detritus fills curbside gutters also. Actually, it gets everywhere. Its removal will be easier between the windy storms that generate it.