,
 

2004/07/18 Drought Report for the Agricultural Region of Alberta

 
 
Subscribe to our free E-Newsletter, "RTW This Week"Sign up for our
E-Newsletter
     Download 1,219K file ("y2004_m07_d18.pdf")Download pdf - 1,219K
 
 
 
 Summary | Current situation | Explanation of terms
.
Summary
.
Since the last report (July 04, 2004), a number of significant storm events have continued to bring precipitation to many areas of the province with total accumulations ranging from 0-140 mm. Much of the precipitation was delivered by severe thunderstorms accompanied by hail, funnel cloud sittings and few tornado touchdowns. As a result of these localized thunderstorms some areas may have received more precipitation while others may have received less than what has been reported here. Areas largely missed by recent storm activity include the already dry northern and extreme southwestern Peace region, parts of east central Alberta as well as much of southern Alberta. Most of the precipitation was centered around the Swan Hills (140 mm) with total amounts upwards of 40 mm extending into the south eastern Peace region, across most of the northern parts of the reporting area and much of the north west with a broad band extending through much of central Alberta, including Edmonton, Red Deer, and as far south as the County of Wheatland.

As a result of the recent precipitation, the areas classified as drought in the central and east central portions of the province have greatly decreased but still remain as small points on the map. In the south three pockets classified as Drought have also decreased in size since the July 04 report confined mostly to the M.D.'s of Pincher Creek and Cardston and the County of Forty Mile. The mapped as drought alert in the July 04 report have diminished greatly save for the northern part of the Peace region, which has increased slightly.

Precipitation during the past 90 days has resulted in a trend toward at least Normal, or low risk of drought, for most of the province, including all areas currently in Drought status. One exception applies to the northern Peace region where the 90-day trend is towards Drought Alert. If the 90-day trend towards Normal persists existing long-term Drought conditions will normalize in most areas within in a few months.

Soil moisture conditions were predicted to be Well Below Normal in much of west central, western and southern Alberta as well as the central part of southern Alberta. Within these areas several small pockets of Extreme Deficit can also be found suggesting many of the areas currently classified as Well Below normal may grade to Extreme Deficit if precipitation deficiencies occur. In the Peace region, all but the southeastern areas are predicted to have Well Below Normal soil moisture conditions with areas of extreme deficit found over much of the northern Peace and parts in the extreme southwest Peace region. There is still immediate need for moisture in these areas as there is not enough soil moisture reserve to carry a crop through the next two weeks in these areas.

Current Situation

Long term drought (Figure 1):
  • Since the last drought report the areas classified as Drought have decreased from 5% to just over 1% of the reporting area. Areas in this category in northern Alberta, include a small pocket in the M.D. of Lesser Slave River, one in western Alberta in the county of Yellow Head, and in central and southern Alberta, five other pockets exist, one in the county of Starland, one spanning the boarder between special areas 3 and 4, and one each in the counties of Forty Mile, Cardston, and Picher Creek. Of significant note is the fact that the Northern Peace region is not categorized as drought despite dire need of moisture here. The reason for this is that Much Below Normal precipitation began to fall at the onset of the growing season. Prior to this these areas received mostly Below Normal precipitation over winter and Normal precipitation through most of June, July, and August of last year.
  • Currently nearly 31% of the reporting area is in Drought Alert down from 52% reported in the July 04th, 2004 drought report. Recent rains have reduced the Drought Alert areas in much of northern and central and southern Alberta. Currently Drought Alert areas include west central Alberta, central Alberta and east central Alberta with some pockets remaining in southwestern and south central Alberta.
  • The areas classified as Normal have increased significantly and now are account for 68% of the reporting area up from 43% as reported 14 days ago in the last drought report. These areas include the most of the southern half of the Peace region, most of northern Alberta, about half of northeastern Alberta as well as much of southern Alberta.
Recent trends (Figure 2):
  • The area representing recent (90-day) trends toward Normal conditions decreased since the last report but still represent most of the mapped area. Since 52% of the province was in Drought Alert status, this represents a trend toward improvement in most of the affected areas
  • 90-day trends towards Drought Alert were found in two pockets in the Northern Peace region affecting the M.D.'s of Mackenzie, Northern Lights and Northern Sunrise. Of these areas, if current 90-day trends persist those areas currently in Drought Alert status are expected to stay in Drought Alert and those areas in Normal are expected to move into Drought Alert.
Precipitation (Figure 3, Figure 4 and Figure 5);
  • At least Above Normal precipitation over the last 90 days was recorded over most of the reporting areas with notable exceptions in the northern Peace region where Much Below Normal precipitation has been recorded in the M.D.'s of Mackenzie, Northern Lights and Northern Sunrise, as far south as Manning. The rest of the northern Peace Region is reporting Below Normal precipitation as far south as Peace River including M.D's of Fairview and Peace. Other relatively large areas reporting Below Normal include the M.D. of Lesser Slave river, a long north-south running corridor in east central Alberta that extends between the southern edge of Lake Land county down as far south as Starland county. In the south the same conditions are occurring in the counties of Forty mile and Cypress. Smaller pockets can be found in various areas around Alberta including the counties of Parkland, Lacombe, Starland, Special areas 3 and 4, Warner and Pincher Creek (Figure 3).
  • Since the last report (June 04th, 2004) a series of storm events coupled with thunder storm activity has continued to deliver varying amounts of precipitation 0-140 mm over much of central Alberta. The majority of the precipitation fell around the Swan Hills (140 mm) and beyond with total amounts between 40-90 mm extending into the southeastern Peace region. Greater than 50 mm fell across most of the northern parts of the reporting area and much of the north west, and in central Alberta a broad band of precipitation (>50 mm) extended through much of central Alberta, including Edmonton, Red Deer, and as far south as the county of Wheatland.
  • The northern Peace region remains in desperate need of precipitation as less then 10 mm has fallen over much of this area. The remainder of the northern half of the Peace region received between 10-20 mm of precipitation, barely enough to sustain crop growth. Much of southwestern and southeastern Alberta was also missed by the recent storm activity with total amounts in these areas ranging between 0 and 20 mm. The same is also true in parts of east central Alberta for parts of the counties of Wainwright, Flagstaff and Two Hills, which reported less than 20 mm of precipitation. All other locations within the reporting areas received between 20 to 40 mm, which is enough precipitation to supply the crop needs for the next week or so. (Figure 4).
  • July is historically a very important month for precipitation with 30-year normals that range between 30 mm in south central Alberta to 140 mm in the northwest (Figure 5). Given current soil moisture conditions a return to normal precipitation totals should result in adequate crop growth over most of the province with the exception of south central Alberta. Dry conditions here, in and around the county of Warner currently exist and as a result above normal precipitation will be needed to insure good crop growth.
Soil Moisture (Figure 6, Figure 7 and Figure 8)
  • Soil moisture levels were less than 50 mm of plant available water for most of south central Alberta and east central Alberta stretching as far north as the county of St. Paul with a few pockets appearing in central Alberta in the Counties of Ponoka and Lacombe as well as Special Areas 2, 3 and 4 and the M.D. of Acadia. Much of southeastern Alberta has soil moisture levels of less than 25 mm, a condition requiring immediate precipitation for continued crop development (Figure 6). However, for many of these areas, particularly in the south east and east central areas, soil moisture levels of below 50 mm represent an average condition which highlights the dependence of agriculture in these areas on regularly occurring timely rains fall events (Figure 7).
  • In the northern Peace River region soil moisture levels are below 50 mm in the counties of Fairview, Peace, Clear Hills, Northern Sunrise, Northern Lights and Mackenzie. Any remaining crops, permanent pasture, or hay land in this area are in desperate need of precipitation. In the rest of the northern and western Peace region, soil moisture levels are between 25-50 mm, which translates to soil moisture deficits of Extreme to Well Below Normal for this time of year.
  • Most of western Alberta, the southeast Peace region and the northeast have soil moisture levels ranging greater than 50mm and as high as 150 mm (Figure 6). These areas are currently not in a crop moisture deficit but again, continued rainfall is needed to keep crop growing as depending on soil moisture conditions a crop can use upwards of 30 mm of water in a week
  • Soil moisture levels are in Extreme Deficit for most the northern and the extreme southwest portions of Peace region a condition that has worsened since the last report (July 04th). In the northern part of the reporting area, soil moisture deficits continue to be Well Below Normal to Extreme Deficit but the areas affected have diminished in size and are not confined to the M.D.'s of Lesser Slave Lake, Opportunity and the County of Lake Land. Since the last report, the areas of extreme deficit in the northwest have disappeared, grading into Below Normal to Near Normal.
  • Since last report, areas of Well Below Normal soil moisture in west and west central Alberta have decreased but are still affecting the Counties of Woodlands, Wetaskiwin, Clear Water, Ponoka, Camrose, Lacombe Red Deer, Mountain View and Rocky View. In addition, one pocket of Extreme Deficit can be found in the county of Lacombe and one in the county of Clear Water. In southern Alberta, areas in the Well Below Normal category have expanded and now include most of the county of Forty Mile, Warner Cardston and parts of the M.D. of Pincer Creek. One isolated pocket of Extreme Deficit in the county of Cardston continues to intensify. At least Near Normal soil moisture conditions are predicted to occur in many parts of the south half of the Peace county in addition to east half of the reporting area and most of southern Alberta (Figure 8).
Explanation of Terms

Long term (hydrologic) drought
Long term, or hydrologic, drought is a result of the cumulative effect of several dry months. It primarily impacts livestock feed and water supply and may affect annual crops. Hydrologic drought is determined from precipitation totals over a 365-day period using the Standardized Precipitation Index (SPI). Long-term drought is rated as either Wet, Above Normal, Normal, Drought Alert, Drought or Exceptional Drought. The SPI is recommended for drought identification by the United States National Drought Mitigation Centre. The long-term drought conditions are reported year-round.

The trend in long-term drought is determined by comparing the 365-day SPI with the 90-day SPI. Where the 90-day SPI value is -1 to +1, then a trend toward moderating conditions is occurring, potentially resulting in Normal status. If the 365-day SPI values for that area are already Normal, then the trend is toward no change. If the 90-day SPI value is -1 to -2, then the area is trending toward Drought Alert status. This could be a deteriorating condition if the current 365-day value is Normal, however it could represent a continuing condition if the area is already in Drought Alert, or an improving condition if the area is already in Drought. Values of the 90-day SPI that are between of -2 to -3 and lower than -3 indicate a trend toward Drought and Extreme Drought respectively. Values of the 90-day SPI that are between +1 and +2, and greater than +2 represent a trend toward Above Average and Wet respectively.

Soil moisture (reported during the growing season months only)
The crop gets the moisture it requires from the reserve of soil moisture, which in turn is replenished by rainfall. Soil moisture is a valuable indicator of drought potential because it shows the reserve of water available to the crop at a given point in time. During peak growing periods, soil moisture reserves are consumed quickly and must be replenished frequently by rainfall. Low soil moisture reserves during these times indicate a high risk of immediate crop stress. Prolonged stress becomes drought, and results in significant unrecoverable yield loss.

Because the climate varies across Alberta, comparing current moisture levels to normal levels provides a valuable indicator of drought risk that can be applied to all localities and to all times of the season. Below average soil moisture levels, at any time, indicate a need for more rain or snow to restore reserves.

Soil moisture is measured as millimeters (mm) of plant available water. Plant available water is approximately half of the total water that can be measured in the soil. Soil moisture is monitored from May through October.

Report prepared by the Drought Reporting Team
Ralph Wright , Allan Howard, , Katherine Altman, and Kris Sabourin,
Conservation & Development Branch & Program
Alberta Agriculture, Food and Rural Development,
Edmonton, AB T6R 5T6
Contact: Ralph Wright; ph (780) 427-3556;

This report was created on July 07, 2004.

Drought analysis is currently scheduled at bi-weekly intervals between May 1 and October 30. This report was generated as a result of a widespread recent precipitation and updates the previous report of July 27, 2004.

Exent and severity of long-term Drought.
Figure 1. Extent and severity of long-term Drought in the agricultural region of Alberta, as of
July 18, 2004.

Recent (90 day) trends in Drought conditions.
Figure 2. Recent (90 day) trends in Drought status in the agricultural region of Alberta as of July 18, 2004.

Precipitation departures in the agricultural region of Alberta for the past 90 days as of July 18, 2004
Figure 3. Precipitation departures in the agricultural region of Alberta for the past 90 days as of July 18, 2004.

Precipitation (mm) sinced the last Drought report.
Figure 4. Precipitation (mm), since the last Drought report, as of July 18, 2004 in the agricultural region of Alberta. The last drought report was July 04, 2004.

Average precipitation for July in the agricultural region of Alberta.
Figure 5. Average precipitation for July in the agricultural region of Alberta based on thirty years of data (1971-2000).

Soil moisture in the agricultural region of Alberta as of July 18, 2004.
Figure 6. Soil moisture in the agricultural region of Alberta as of July 18, 2004.

Modeled 30-year average soil moisture conditions for July 18.
Figure 7. Modeled 30-year average soil moisture conditions for July 18.

Soil moisture departure in the agricultural region of Alberta from average modeled soil moisture for July 04, 2004.
Figure 8. Soil moisture departure in the agricultural region of Alberta from average modeled soil moisture for July 04, 2004.
 
 
 
 
For more information about the content of this document, contact Ralph Wright.
This document is maintained by Isabel Simons-Everett.
This information published to the web on August 17, 2004.