KFVS12 News & Weather Cape Girardeau, Carbondale, Poplar BluffDrought Watch

Paducah, KY

Drought Watch

Drought Watch
By: Jason Lindsey

Paducah, KY - Although the StormTeam forecast is calling for rain, it won't soak up our drought-like conditions.

According to the United States Department of Agriculture drought monitor, the Heartland is abnormally dry with parts of southeast Missouri experiencing a moderate drought.

The dry weather has helped farmers especially when it comes to harvest, but McCracken County farmer, JW Goodwin says if we don't get rain soon there's going to be trouble. Goodwin says he hasn't seen any rain on his Kentucky farm since August.

According to National Weather Service meteorologist, Pat Spoden long term outlooks are showing indications of the dry weather continuing through the winter months. Spoden says rainfall deficits range from two inches near Farmington to nearly twelve inches short in Paducah and that it's going to take a lot more to catch up.

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Drought Basics
  • Drought is a weather-related natural disaster. It affects vast regions for months or years. It has an impact on food production and it reduces life expectancy and the economic performance of large regions or entire countries.
  • Drought is a recurrent feature of the climate. It occurs in virtually all climatic zones, and its characteristics vary significantly among regions. Drought differs from aridity in that drought is temporary; aridity is a permanent characteristic of regions with low rainfall.
  • Drought is an insidious hazard of nature. It is related to a deficiency of precipitation over an extended period of time, usually for a season or more. This deficiency results in a water shortage for some activity, group, or environmental sector. Drought is also related to the timing of precipitation. Other climatic factors such as high temperature, high wind, and low relative humidity are often associated with drought.
  • Drought is more than a physical phenomenon or natural event. Its impact results from the relation between a natural event and demands on the water supply, and it is often exacerbated by human activities. The experience from droughts has underscored the vulnerability of human societies to this natural hazard.
  • Types of Droughts

    • Meteorological drought

      Meteorological drought is defined on the basis of the degree of dryness, in comparison to a normal or average amount, and the duration of the dry period. Definitions of meteorological drought must be region-specific, since the atmospheric conditions that result in deficiencies of precipitation are highly region-specific.

      The variety of meteorological definitions in different countries illustrates why it is not possible to apply a definition of drought developed in one part of the world to another. For instance, the following definitions of drought have been reported:

      • United States (1942): Less than 2.5 mm of rainfall in 48 hours.
      • Great Britain (1936): Fifteen consecutive days with daily precipitation less than 0.25 mm.
      • Libya (1964): When annual rainfall is less than 180 mm.
      • Bali (1964): A period of six days without rain.

      Data sets required to assess meteorological drought are daily rainfall information, temperature, humidity, wind velocity and pressure, and evaporation.

    • Agricultural drought

      Agricultural drought links various characteristics of meteorological drought to agricultural impacts, focusing on precipitation shortages, differences between actual and potential evapotranspiration, soil-water deficits, reduced groundwater or reservoir levels, and so on. Plant water demand depends on prevailing weather conditions, biological characteristics of the specific plant, its stage of growth, and the physical and biological properties of the soil. A good definition of agricultural drought should account for the susceptibility of crops during different stages of crop development. Deficient topsoil moisture at planting may hinder germination, leading to low plant populations per hectare and a reduction of yield.

      Data sets required to assess agricultural drought are soil texture, fertility and soil moisture, crop type and area, crop water requirements, pests and climate.

    • Hydrological drought

      Hydrological drought refers to a persistently low discharge and/or volume of water in streams and reservoirs, lasting months or years. Hydrological drought is a natural phenomenon, but it may be exacerbated by human activities. Hydrological droughts are usually related to meteorological droughts, and their recurrence interval varies accordingly. Changes in land use and land degradation can affect the magnitude and frequency of hydrological droughts.

      Data sets required to assess hydrological drought are surface-water area and volume, surface runoff, streamflow measurements, infiltration, water-table fluctuations, and aquifer parameters.

    • Socioeconomic drought

      Socioeconomic definitions of drought associate the supply and demand of some economic good with elements of meteorological, hydrological, and agricultural drought. It differs from the other types of drought in that its occurrence depends on the processes of supply and demand. The supply of many economic goods, such as water, forage, food grains, fish, and hydroelectric power, depends on the weather. Due to the natural variability of climate, water supply is ample in some years, but insufficient to meet human and environmental needs in other years.

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