Thursday, September 10, 2009

20 Years Ago On This Date

Twenty years ago on this date
On September 10, 1989, the strong tropical wave that had moved off the coast of Africa the previous day acquired an organized circulation at the surface and began building a concentrated area of heavy thunderstorms near its center. A new tropical depression, the eighth of the season, was born. Moving westward at 20 mph, the depression brought strong, gusty winds and heavy rain showers to the Cape Verdes Islands as it passed to the south. Forecasters at the National Hurricane Center predicted that the steadily organizing tropical depression would strengthen into a tropical storm within the next day or two. The next name on the list of Atlantic tropical storm names for 1989: Hugo.


AVHRR visible satellite image of Tropical Depression Eight taken on September 10, 1989. Image credit: Google Earth rendition of the NOAA HURSAT data base.

Wednesday, September 9, 2009

Tuesday, September 8, 2009

Fun Facts About Horses


The average horse weighs about a half a ton, its brain is the size of a baked potato.

A horse's hoof is analogous to the human fingernail. Horses stand on their middle fingers!

Some of the equine family's closest relatives are tapirs and the rhinoceros.

A horse can poop up to 14 times a day!

Horses cannot vomit.

Most of the time, a horse's ear points where the horse is looking.

Horses can lock the muscles in their legs so they can go to sleep standing up and not fall over.

One of the first horses was called a Hyracotherium. It lived about 50 million years ago and was as tall as a fox. It had toes!

Camargue horses are completely white as adults. Their babies are pure black when they are born.

There is a breed of horse from Russia called Akhal-Teke. It can go for days without food or water.

You measure a horse's height in hands. Each hand equals four inches. If you say a horse is 16.2 hands high, the 2 stands for 2 fingers.

You can tell how old a horse is by how many teeth it has. A horse gets all of its teeth by the time it is five years old. After that, they just get longer.

A female horse is called a mare. In the wild it is the mare that decides when the herd moves on to another spot to find food.

A male horse is called a stallion. Usually only one stallion will stay with a herd.

Any marking on a horse's forehead is called a star, even if it is not shaped like a star.

Horses and ponies feel safer when they are in a herd.

Mustangs are one of the few breeds of horses that live wild in North America. They are related to the horses that the Spanish explorers brought to North America 400 years ago.

Horses can communicate how they are feeling by their facial expressions. They use their ears, nostrils, and eyes to show their moods. Beware of a horse that has flared nostrils and their ears back. That means it might attack!

A hoof is like a fingernail. It is always growing and needs to be clipped so that it won't be uncomfortable for the horse.

A farrier is a person who makes horse shoes and fits them on your horse. They also clip hooves to keep them from getting overgrown.

A horse can move in four ways: walk, trot, canter, and gallop. A gallop is the fastest gait.

Friday, September 4, 2009

Topdressing the lawn

Top-Dressing to Improve the Soil in Your Lawn

A nice, thick lawn requires healthy soil as its base, but it’s difficult to make changes to the soil once grass has been established. Most gardening recommendations include “working” organic matter into the soil through digging or tilling prior to planting, but this can’t be done once the grass has grown. So what’s a homeowner to do with an established lawn that’s in need of some serious help?

If done properly, the technique of “top-dressing,” or adding a thin layer of soil over your lawn, can improve the soil without killing the existing turf. Top-dressing addresses some common lawn problems, including:

  • Low spots due to rotting tree roots, settling after underground pipe or cable installation, or erosion.
  • Uneven terrain caused by winter freezing and thawing, water runoff, tunneling critters, or general soil settling over time.
  • Compacted soil in high-traffic areas or low-lying places where water pools.
  • Bare spots from variations in soil texture and nutrients, heat, drought, or other environmental damage.
  • Depletion of nutrients due to leaching, neglect, or repeated use of chemical fertilizers.

Top-dressing gradually improves soil over time. As organic matter breaks down, it filters through the existing soil to improve texture and overall health. Top-dressing can:

  • Improve drainage and drought-resistance
  • Even out the terrain
  • Reduce the need for supplemental fertilizers
  • Transform your lawn into organic, low-maintenance, healthy turf

When to Top-Dress

Ideally, do it in early fall or spring since you’ll want to give your grass time to grow through 3-4 more mowings before severe heat or cold, especially if you are overseeding. It can be done all at once, or in stages. I know one meticulous gardener who top-dresses small patches as he finds them, whereas I brought in a truckload of top-dressing mixture and had an autumn marathon.

Top-dressing involves some physical labor, but the process is really just a few simple steps:

Step 1: Aerate

Lawns should be aerated every 2-3 years, and if yours is due, start with a nice core aeration. Core aeration removes plugs of soil from the ground and leaves channels for air, water, and our top-dressing mixture to penetrate the surface. For more information, see our article on Adventures in Aeration.

Step 2: Prepare Your Top-Dressing

You can make your own top-dressing using a mixture of:

  • Sharp sand (not sea sand which contains lime)
  • Loam or topsoil (a fine crumbly soil that is neither clay nor sandy)
  • Peat (or compost if your soil needs a nutritional punch, but be prepared for sprouting weeds!)

For average loamy soil, mix these three ingredients equally. For applications on clay soil, reduce or eliminate the loam/topsoil. For sandy soil, reduce the sand. Your ingredients need to be dry and sifted until there are no clumps larger than ¼”.

Another option is to purchase high-quality top-dressing mixture or bagged lawn soil. Check with your local landscape supply yard – they often have a blended topsoil mixture on hand. While you won’t be able to guarantee the proportions, it’s economical and sold in bulk.

Step 3: Apply Top-Dressing

Now you’re ready to get started. Working a few square feet at a time, shovel out a small mound (maybe 2-3 shovelfuls) of mixture onto your lawn.

Spread the soil using something flat, like the back side of a heavy garden rake, working it into aeration holes and covering low spots. Make sure the top-dressing is no more than 1” deep (preferably ½” or less) over the existing grass.

Keep working the mixture until your grass peeks through and the depth is even. I like to flip the garden rake back and forth from the flat side to the tine side, carefully combing the grass to get the top-dressing mixture settled on the soil surface.

For low spots requiring more than a couple of inches of top-dressing, first remove the existing sod to prevent underground decay that can damage new grass seedlings. After filling in the low spot, either replace the old sod or re-seed the area. You can also address deeper spots by adding a couple of inches of top-dressing each year, slowly building it up over time.

Step 4: Water and Adjust

At this point you’re technically finished, but in my experience a good top-dressing mixture does some settling. I would recommend watering the area well (or top-dressing before a nice rain), letting the mixture settle for a day or two, then go back with your rake and smooth out any little hollows or bumps that may develop.

Step 5: Plant Grass if Needed

Now you can replant grass in any bare spots. Existing grass should be able to grow through as much as an inch of top-dressing.

How Often to Top-Dress

Trouble spots may need repeat applications, but regular, uniform top-dressing does not need to be an annual tradition. Keep in mind that you’re adding soil, which over time will raise your grade and affect thatch breakdown and soil ecology, so don’t go overboard. Plan several light applications for troublesome yards, rather than one deep one. For overall organic soil amendment, a very light application of top-dressing brushed into aeration holes can improve the soil without raising the grade.

Thursday, September 3, 2009

United States Drought Information - September 1, 2009

The Atlantic Coast States: Rain was heavy enough to eliminate dryness (D0) from Florida and reduce coverage in Georgia. In contrast, persistent dryness in northwestern South Carolina resulted in a slight expansion of moderate drought (D1). In Greenville-Spartanburg, South Carolina, summer (June-August) rainfall totaled just 6.28 inches (50 percent of normal).

The Western and Central Gulf Coast Regions: Rainfall in the central Gulf Coast region resulted in the removal of abnormal dryness (D0) from much of southern Louisiana and southwestern Alabama. August rainfall totaled 8.01 inches (165 percent of normal) in Lake Charles, Louisiana, and 10.18 inches (164 percent) in Mobile, Alabama. At the same time, dry conditions developed across parts of central Louisiana and neighboring areas. In Alexandria, Louisiana, August rainfall totaled just 0.42 inch (10 percent of normal).

Farther west, only minor changes were necessary in the core drought area of Texas. However, enough rain fell in parts of Deep South Texas to result in an improvement from exceptional to extreme drought (D4 to D3). Brownsville’s August 30 – September 1 rainfall total of 1.14 inches surpassed its 0.76-inch sum during the preceding 93 days (May 29 – August 29). Elsewhere in southern Texas, summer records for average temperature were established in locations such as Victoria (86.6 degrees F; previously, 86.2 degrees F in 1998), Corpus Christi (86.8 degrees F; previously, 85.9 degrees F in 1998), San Antonio (87.8 degrees F; previously, 86.2 degrees F in 1980 and 1994), and Del Rio (88.8 degrees F; previously, 88.7 degrees F in August 1998). San Antonio also completed its driest two-year period on record, with precipitation totaling only 24.83 inches (38 percent of normal) from September 2007 – August 2009. San Antonio’s former standard of 30.23 inches was established from August 1954 – July 1956.

By August 30, the U.S. Department of Agriculture reported that 54 percent of the rangeland and pastures in Texas were rated in very poor to poor condition. The Texas drought was also having an adverse effect on crops such as corn (39 percent very poor to poor), sorghum (39 percent), cotton (31 percent), and rice (21 percent). In Louisiana, nearly one-quarter (22 percent) of the sorghum crop was rated in very poor to poor condition.

In southern Texas, storage in Lake Corpus Christi (Nueces River basin) fell below 75,000 acre-feet on September 1 for the first time since August 31, 2001. The lake’s storage was above 200,000 acre-feet as recently as September 2008. Elsewhere in Texas, September 1 water levels in the Colorado River basin near Austin were about 20 feet below the historic September average on Lake Buchanan and more than 33 feet below average on Lake Travis. However, the lakes’ average surface elevations, 632 feet above sea level on Lake Travis and 991 feet on Lake Buchanan, were still above the record lows (614.18 feet in August 1951 and 983.70 feet in September 1952, respectively).

The Midwest: Additional rain in the upper Great Lakes region’s core drought area helped to cut the remaining region of severe drought (D2) into two pieces. The area of dryness and moderate drought (D0 and D1) also decreased in coverage, especially in Wisconsin and Michigan. In fact, dryness (D0) was completely removed from Lower Michigan. Coverage of dryness (D0) was also reduced in western Ohio.

During the two-week period ending August 30, rain helped the percentage of rangeland and pastures rated in very poor to poor condition fall from 26 to 13 percent in Wisconsin and 23 to 15 percent in Minnesota.

The Plains: There were only minor changes to the depiction. Heavy rain reduced the size of the abnormally dry (D0) region in Kansas and Nebraska, and moderate drought (D1) was removed from the latter state. In northern Oklahoma, further analysis of previous rainfall resulted in the removal of moderate drought (D1). A small amount of dryness (D0) was added to south-central Oklahoma and north-central Texas due to continuing dryness.

The West: Monsoon activity remained disappointingly light across the Four Corners States, resulting in further expansion of abnormal dryness (D0). In southeastern Arizona, Tucson completed its second-hottest July-August period on record, with an average temperature of 89.4 degrees F. Only 1994, with a July-August average of 90.3 degrees F, was hotter. From June 15 – August 31, rainfall in southern Arizona totaled just 2.12 inches (46 percent of normal) in Tucson and 1.31 inches (38 percent) in Safford. More than three-quarters (80 percent) of Arizona’s rangeland and pastures were rated in very poor to poor condition on August 30. Rangeland and pastures in New Mexico were also suffering in some areas, with 39 percent rated very poor to poor.

In late August, there was a marked increase in Western wildfire activity, mainly in Utah, western Colorado, and the Pacific Coast States. By early September, the largest active blaze in Utah was the 11,000-acre Mill Flat fire near New Harmony. Meanwhile in southern California, Santa Ana (102 degrees F) posted a daily-record high on August 26, the same day that the Station fire started in the San Gabriel Mountains north of Los Angeles. By early September, the Station fire had consumed more than 125,000 acres of vegetation and nearly 100 structures. Other triple-digit, daily-record highs in southern California included 103 degrees F (on August 27) in Long Beach; 107 degrees F (on August 27) in Fullerton; and 117 degrees F (on August 28) in Palm Springs. On August 29, Santa Maria (104 degrees F) registered a monthly record high, previously established with a reading of 103 degrees F on August 28, 1962.

Farther north, some moderate to severe drought (D1 to D2) was added in northwestern California and southwestern Oregon, following a closer examination of streamflows and long-term precipitation deficits. Additional dryness (D0) was added in western portions of Washington and Oregon to better match with long-term precipitation shortfalls. Portland, in the abnormally dry (D0) area of western Oregon, received a precipitation total of 26.63 inches (75 percent of normal) from October 2008 – August 2009. In addition, Portland’s year-to-date total of 22 days with highs of 90 degrees F or greater was very close to its 1987 annual record of 23 days.

Hawaii, Alaska and Puerto Rico: Another week of generally quiet weather in Hawaii resulted in no change to the drought depiction. On Maui, a wildfire just north of Kaunakakai charred nearly 8,000 acres of timber, brush, and grass by early September. Farther north, heavy precipitation continued across southeastern Alaska and developed in east-central Alaska. Therefore, all remaining dryness (D0) was removed from southeastern Alaska and trimmed from the eastern portion of interior Alaska. In southeastern Alaska, Yakutat’s August rainfall reached 17.50 inches (132 percent of normal). Meanwhile, Puerto Rico remained free of dryness and drought.

Looking Ahead: During the next five days, moisture associated with the remnants of eastern Pacific Hurricane Jimena will spread northward into the Four Corners region, generating scattered showers. Farther east, showers and thunderstorms will gradually shift from the eastern Plains into the middle and lower Mississippi Valley, while rain will linger along and near the southern Atlantic Coast. Dry weather will continue for several more days across the North and the Far West, but rain will arrive across the Pacific Northwest.

The NWS 6- to 10-day outlook for September 8-12 calls for near- to above-normal precipitation nationwide, except in the Northeast. Wet weather will be most likely along the southern Atlantic Coast and in the nation’s mid-section. Above-normal temperatures can be expected along the Pacific Coast, in southern Texas, across Florida’s peninsula, and from the Great Lakes region into the Northeast.


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Wednesday, September 2, 2009

The Science of Dressage Arena Repair

How to water a dressage arena correctly to keep the footing from releasing dust

The most common complaint among dressage riders is dusty footing, great billowing clouds of the stuff. It's kicked up with every step. It hangs in the air for what seems like forever. It gets on your clothes, your tack, your horse. It makes its way into the lungs. Even an outdoor arena with a breeze doesn't offer much relief. And when the dust gets so bad that the arena requires frequent watering to hold it down, the footing compacts as it dries. Out comes the harrow to break up the compaction, but that releases dust. Out comes the hose, but that restarts the compaction process. And the cycle continues. Common causes for dust include interior stalls, old bedding, hay and the arena footing itself. In this Equisearch segment, Brian J. Fahey explains how to water a dressage arena correctly to keep the footing from releasing dust.

How to Water Your Dressage Arena--The Math Behind Moisture Content
It's possible to determine how much water an arena needs by utilizing a mathematical formula known as the "watering increment principle." Here's how it goes: For every 1,000 square feet of arena surface--where the footing is three inches deep--apply 19.5 gallons of water for a 1 percent increase in the moisture content. That's fine, you may say. But I want to reach 10 percent moisture content. How do I figure out how many watering increments to add?

For that, you first have to know the percentage of moisture content in your footing. Thankfully, it's easy to determine. You know those probes you use to measure the moisture content of hay bales? Stick one in the sand about halfway down, and read the result.

Perhaps your footing contains 3 percent moisture and you want to increase it to 10 percent. That's seven watering increments or 136.5 gallons per 1,000 square feet of surface area.

Since most folks don't have a flow meter on their hoses or sprinkler systems, you'll probably need to figure out how many minutes to water per watering increment. You can do that by setting up your hose the way you normally do to water the arena. Take a five-gallon bucket, turn on the hose to its normal flow rate for watering and count how many seconds it takes to fill the bucket to the brim. (For sprinkler systems, put the bucket in the arena and let it fill.) Now divide the result by five to determine seconds per gallon. Take the reciprocal of that number (the reciprocal is either of a pair of numbers whose product is one, example: 2/3 and 3/2) and divide it into one to find gallons per second. Now multiply by 60, and you have gallons per minute. Divide that number into 19.5, and you have watering increments per minute.

Once you know how many watering increments you want to add, divide that number of watering increments by the watering increments per minute and you have the number of minutes to water per 1,000 square feet. Divide the total square footage of your arena surface by 1,000, and multiply that by the number of minutes per 1,000 square feet you just calculated. And there you are. Whether by hose or with a sprinkler system, you now know the total watering time.

Knowing how to water your dressage arena is only one component in correcting footing problems. Some are easy to figure out and fix. Others are complicated and require a deeper understanding of how and why things happen to your arena. In the November 2001 issue of Dressage Today Brian J. Fahey gives hands-on strategies you can use to restore the footing in your dressage arena.


The Rapid Rain is the highest rate horse arena watering and dust control tools on the market. Stop by our website today.

www.rapidrain.com

Tuesday, September 1, 2009

Protect your home during wildfire season.


Steps You Can Take To Protect Your Home During Wildfire Season

The state of California is adopting new building and fire codes, effective January 2008, that will primarily affect new construction. But homeowners with existing homes to worry about can take independent action to safeguard their dwellings in the event of a wildfire — an eventuality that is, or ought to be, top-of-mind for those who own or live in housing vulnerable to such a catastrophe.

Homeowners can increase the chances that their houses will be left standing after a wildfire with the right information, some advance planning, and regular maintenance, says Steve Quarles, wood-durability adviser for UC Cooperative Extension and an affiliate of the Center for Fire Research and Outreach at Berkeley’s Richmond Field Station.

Quarles has identified six priority areas for making changes to existing homes in fire-hazard zones. He suggests homeowners start with the roof, the most vulnerable part of the house in a fire, and then continue in order with vents, vegetation, windows, decking, and siding.

First things first: Roofs and vents

Ignition-resistant “Class A” and non-combustible roofs — such as concrete tile and asphalt composition shingles — have become the norm in California since the late 1990s, when new laws passed requiring all new homes and all roof replacements in very high fire-hazard-severity zones to be Class A. Nevertheless, many older homes still do not have Class A roofs.

“The importance of the roof covering cannot be overstated,” says Quarles. “If you haven’t already done so, you should make an upgrade to a Class A roof your first priority.”

The East Bay’s hills are covered with flammable plants, as those who survived the 1991 firestorm (above) discovered. (Jonathan King photo)

But don’t stop there. Many homeowners realize a false sense of security after installing non-combustible roofs and siding simply because those are dominant features on any house. There’s much more to do, says Quarles, who specifies vents as the second item on his priority list.

Most building codes specify vents for crawl or attics to prevent a buildup of moisture, which can lead to mold growth and decay. But vents also offer embers and flames an easy entry point. “Embers that slip through attic vents can ignite debris and items stored there, and subsequently construction materials, setting the home ablaze from within,” Quarles points out.

In addition, most codes require that vents be covered with, at a minimum, quarter-inch mesh to minimize plugging and reduction in air movement. But that’s inadequate to keep flames away from the inside of your home, says Quarles. “This is an example of conflict in code preferences between building and fire officials. Quarter-inch mesh cannot stop embers and flames during wildfires. Smaller-mesh screens would do a better job of keeping them out, but they plug up more easily.”

The importance of vents in wildfire resistance is leading to such innovations as the development of vents specially designed to limit ember intrusion while still allowing sufficient air flow for ventilation, and construction designs and procedures that permit unvented attics to avoid moisture-related problems.

Quarles suggests homeowners frequently check their vents to make sure there is no buildup of debris, such as highly combustible dry leaves and pine needles. For added protection they can make vent covers out of plywood or another solid material that can be quickly installed over vents when wildfire approaches.

Leggy and succulent

Next, suggests Quarles, examine the vegetation on your site, with the understanding that it can be both harmful and helpful when it comes to home fire protection. Plants close to the home — under eaves, in inside corners, and near windows — can be major fire hazards, but trees and shrubs farther away can serve as buffers against radiation, convective heat, and flying embers. “Trees might have a bad reputation because of the potential to spread fire in the crown, but that is seldom a hazard to structures,” Quarles says.

In addition to noting where plants are located, Quarles suggests careful attention be paid to plants’ innate fire resistance. Bushy junipers and cedars, for example, can be a poor choice for those seeking to minimize fire hazards. For landscaping close to a dwelling, select leggy plants with succulent leaves — the smaller the plants the better, especially near windows and in the parts of the home designed to give the house architectural interest, such as inside corners, where heat builds up much faster than on open, flat sides.

Whatever plants you choose, they should always be well-maintained, says Quarles: “Any plants near a house should be pruned, regularly watered, and kept free of dead material within the branches and on the ground.”

Well-tempered windows

The next priority should be windows. Research has shown that by far the most important factor in determining the vulnerability of windows in a wildfire is the glass, not the frame.

“It’s a good idea to install dual-pane windows with tempered glass,” Quarles says. “With dual-pane windows, the outer pane protects the inner pane. The inner pane heats up more slowly and uniformly, and therefore may not break even though the outer pane does.”

Tempered glass is much stronger than regular glass, so it provides more protection against breaking. The relevant chapter in the building code going into effect in 2008 requires at least one pane to be tempered glass. Since the type of frame doesn’t make much difference in a fire, it can be selected based on cost, aesthetics, energy efficiency, or other factors.

As is the case with vents, homeowners can fabricate window covers out of half-inch plywood or another fire-resistant material. Cut them to size and mark them clearly so they can be installed quickly over windows before evacuating the home when a fire breaks out.

A backyard deck is not a top-of-mind hazard for many in wildfire country, even though an ignited deck is often adjacent to large windows or sliding glass doors, both of which can break from a fire’s heat, permitting flames to enter the house.

“In general, the thicker the deck boards the better,” advises Quarles. “Boards an inch or less thick release heat much faster, and are therefore a higher hazard. Be especially mindful of the gaps between the boards and the house and decking. Combustible debris can build up in the gaps and corners, and flying embers can get lodged there and begin smoldering.”

For replacement, consider any material — plastic, plastic-composite lumber, fire-retardant-treated lumber for exterior use, or lumber — that passes the state test procedure approved by the California State Fire Marshal’s office. Tests conducted a few years ago showed some composite-decking products capable of resisting fire as well as solid wood, though none were better; Quarles says he expects new decking products to come on the market when the 2008 building code goes into effect.

The sixth priority is siding. In research trials, good-quality sheathing — which is installed underneath the siding — was a key to protecting the home’s studs. Non-combustible siding, made of stucco or fiber-cement, can be installed over the sheathing. Combustible siding — such as wood panels and clapboard — should be inspected annually for gaps, making sure that any are filled with a high-quality caulk to prevent hot embers from taking up residence and beginning to burn.

Even beyond these six priority areas, other elements and structures in and near your home (e.g., fences, garages, and gutters) can be improved to keep it safer in a fire. For further information, consult the “Homeowners Wildfire Mitigation Guide,” co-written by Quarles and Frank Beall, a retired professor of environmental science, policy, and management at Berkeley, at groups.ucanr.org/HWMG/index.cfm.


THE RAPID RAIN WOULD BE A GREAT ADDITION TO A HOMEOWNER LIVING IN A WILDFIRE ZONE.

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