Thursday, January 26, 2012

Snowfall in Kentucky - Winter 2012


Snow is a form of precipitation within the Earth's atmosphere in the form of crystalline water ice, consisting of a multitude of snowflakes that fall from clouds. Since snow is composed of small ice particles, it is a granular material. It has an open and therefore soft structure, unless packed by external pressure. Snowflakes come in a variety of sizes and shapes. Types which fall in the form of a ball due to melting and refreezing, rather than a flake, are known as graupel, ice pellets or snow grains. Snowfall amount and its related liquid equivalent precipitation amount are determined using a variety of differentrain gauges.
The process of precipitating snow is called snowfall. Snowfall tends to form within regions of upward motion of air around a type of low-pressure system known as an extratropical cyclone.

Snow can fall poleward of these systems' associated warm fronts and within their comma head precipitation patterns (called such due to the comma-like shape of the cloud and precipitation pattern around the poleward and west sides of extratropical cyclones). Where relatively warm water bodies are present, for example due to water evaporation from lakes, lake-effect snowfall becomes a concern downwind of the warm lakes within the cold cyclonic flow around the backside of extratropical cyclones. Lake-effect snowfall can be locally heavy. Thundersnow is possible within a cyclone's comma head and within lake effect precipitation bands.

In mountainous areas, heavy snow is possible where upslope flow is maximized within windward sides of the terrain at elevation, if the atmosphere is cold enough.

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Photo by M Smith

Wednesday, January 25, 2012

January 2012

      Still Waiting for the Snow

Sunday, January 22, 2012

Mourning Dove

The Mourning Dove is a member of the dove family. The bird is also called the Turtle Dove or the American Mourning Dove or Rain Dove, and formerly was known as the Carolina Pigeon or Carolina Turtledove. It is one of the most abundant and widespread of all North American birds. It is also the leading gamebird, with more than 20 million birds (up to 70 million in some years) shot annually in the U.S., both for sport and for meat. Its ability to sustain its population under such pressure stems from its prolific breeding: in warm areas, one pair may raise up to six broods a year. Its plaintive woo-OO-oo-oo-oo call gives the bird its name. The wings can make an unusual whistling sound upon take-off and landing. The bird is a strong flier, capable of speeds up to 88 km/h (55 mph).


Mourning Doves are light grey and brown and generally muted in color. Males and females are similar in appearance. The species is generally monogamous, with two squabs (young) per brood. Both parents incubate and care for the young. Mourning Doves eat almost exclusively seeds, but the young are fed crop milk by their parents.

Tuesday, January 17, 2012

Thursday, January 5, 2012

Kentucky Columbine

Several species are grown in gardens, including the European Columbine (A. vulgaris), a traditional garden flower in many parts of the world. Numerous cultivars and hybrids have also been developed as well. They are easy to propagate from seed.


Columbine is a perennial, which propagates by seed. It will grow to a height of 15 to 20 inches. It will grow in full sun, however, prefers growing in partial shade and well-drained soil, and is able to tolerate average soils and dry soil conditions. Columbine is rated hardiness of Zone 3 so does not require mulching or protection in the winter.

Large numbers of hybrids are now available for the garden, since the British A vulgaris was joined by other European and N American varieties. Aquilegia species are very interfertile, and will self sow.

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