|
|
|
October brought us gardeners (and foresters) in the Mid-Atlantic area a welcome respite from the searingly hot and dry summer of 1999. Combined with the dearth of rainfall dating back to June of 1998, the summer of 1999 was one of the most stressful growing seasons experienced in the eastern U.S. and Canada since the dust bowl days of the early nineteen thirties. October brought several tropical storm origin rainfalls to the region that greatly relieved the immediate topsoil moisture deficits that had been prevalent since the growing season had begun. Upwards of 8 to 10 inches fell in October that brought to an end water restrictions in most areas.
However, I fear, the drought lives on. While it is not obvious to us now, since moisture demand on surface soils is light do to reduced evapo-transpiration demand of the dormant season, our weather patterns have, in fact, resumed the trend towards drought. November and December precipitation totals are again below normal, repeating the fall and early winter trend of 1998 in 1999. Our entire early winter in fact appears to be a near repeat of last year. In addition to lack of precipitation, very warm temperatures again predominated in November and December. And the US Weather Service tells us that the La Nina conditions continue in the southern Pacific Ocean- just like last winter. The forecast therefore is for a continued warm and relatively dry winter here in the eastern US. Now all this aberrant weather is good news for your heating expense but could have adverse impacts on your garden. First, let's look at the water regime in our soils. As our plants in temperate climes go dormant in late October and November the demand on soil moisture is greatly reduced. Most plants simply aren't drawing much moisture from the soil as life functions aren't active. Deciduous plants and herbaceous perennials that die back in fall go almost completely dormant and draw practically no moisture from the soil. Coniferous and broad-leaf evergreen trees and shrubs go dormant also, but do draw a reduced volume of moisture from the soil to maintain leaf turgor. This will occur as long as root zone is not frozen solid and adequate moisture is available. When the roots can't take up moisture either because it is not present or is unavailable due its being in a solid state, these plants are subject to injury. We often refer to this as wind burn, as it often becomes most apparent after a we have a hard cold wind event that arrives with a cold front in conjunction with one of those frigid Canadian high pressure systems. Brrrrrr. All that cold, low humidity air moving past the leaves sucks the moisture right out of them- quickly. The result is a browning of the foliage. Normally, a fully dormant and healthy plant properly acclimated to our zones can endure this weather with minimal permanent injury. Often, the foliage regreens when dormancy is broken. The native eastern red cedar (Juniperus Virginiana) is a prime example of this phenomenon.
The copyright of the article Silent Drought, Part 1- Is it Stealing Your Garden? in Plants & Trees is owned by . Permission to republish Silent Drought, Part 1- Is it Stealing Your Garden? in print or online must be granted by the author in writing.
|
|
|
|
|
|
|
|