Drought

Update

As of October 1, 2020, nearly all of Utah was in some stage of drought. Fire danger is high, native vegetation is sparse and streams are low. Total rainfall over the last 60 days is under 1” for the majority of the state, with much of this area seeing less than 0.5” and some seeing less than 0.1”. This year set a record for Utah’s hottest, driest August on record. That combination deepened the already existing drought conditions. 

Weather forecasts predict dry conditions will continue. Dry conditions in fall will reduce the benefit of winter snowpack. Snowmelt will first soak into the extremely dry soil before running off into streams and reservoirs. Drought conditions could potentially develop very rapidly in the spring and deepen throughout next summer. The Division of Water Resources will monitor conditions closely over the winter to be prepared to respond rapidly in the spring if conditions do not improve.

Drought Update October 2020 pdf

Reservoir Levels

What Is Drought?

Drought is a normal and recurring climate feature. Although it occurs in virtually all of the world’s climatic zones, its characteristics vary significantly from one region to another. Consequently, there is no universal drought definition. In general, drought is a result of a deficiency of precipitation over an extended period of time, resulting in a water shortage, which impacts normal water usage. The severity of a drought depends upon the degree of moisture deficiency, its duration, and the size of the affected area. Because it is so hard to develop a quantitative definition for drought, it is difficult to determine precisely when a drought starts and ends.

In the United States, droughts are among the most financially burdensome of all weather-related disasters. In fact, in the 20 years preceding hurricane Katrina, the single largest U.S. weather-related disaster was the drought of 1988, which resulted in over $40 billion in damages throughout the central and northeastern portions of the country. Unlike impacts from flood, hurricane, tornado or other weather-related disasters, drought impacts are not always immediate. Failed crops can impact food prices well into the future. Devastated domestic livestock and wildlife herds can also take many years to recover.

UT Drought Monitor

 

Managing Drought

Drought should not be viewed as merely a natural phenomenon or event. Its impact on society is often a result of the interplay between the natural event (reduced precipitation) and the way society responds with management of existing supplies. People often compound the impacts of drought through the mismanagement of available supplies. One example of this occurs when outdoor watering restrictions imposed by community leadership are actually perceived by the general public as being premature or unnecessary. Often in these instances, while people comply with the letter of the law, water use actually rises. Consequently, an informed and caring general public is an important ingredient to successful drought management.

Utah’s successful drought management will in large part be a function of leadership providing the necessary information to the public, and people, in turn, responding positively. Utah’s current Drought Response plan was written during the drought of the late ’80s and early ’90s. The plan uses the Surface Water Supply Index (SWSI) to describes five drought conditions. The SWSI is a relative scale with 0 representing average conditions. A positive number indicates that water supplies are above normal, while a negative number indicates that water supplies are below normal.

The first condition, Normal to wet, is really a non-drought condition and the plan merely calls for the periodic updating of SWSI data and maps. When the SWSI moves into the 0 to -1.0 range, conditions are still considered normal, with water supplies only slightly below average. Although this is not a true drought condition it is called “Emerging Drought” in the plan, primarily because of the potential for worsening conditions. During this phase, the plan merely calls for increased monitoring of data. When the SWSI moves below -1.0, the condition is a Phase I Drought. At this point, the state’s Water Supply and Availability Committee is activated and begins to closely monitor water supply data and initiates the dissemination of information to the media and general public. When the SWSI moves below -2.0, it is a Phase II drought condition. At this time, a Drought Review and Reporting Committee and Drought Task force are created with members of various state agencies to coordinate drought response actions and facilitate the timely dissemination of data and information. The Governor’s Proclamation of Drought Emergency, rather than a SWSI number, triggers drought Phase III. The Governor’s declaration of drought emergency is the initial and necessary step to make available many of the state and federal drought assistance programs.

Measuring Drought

The U.S. Drought Monitor is a broad-scale national drought map. It is updated weekly and communicates any unusually dry conditions with 4 drought categories (moderate, severe, extreme, and exceptional drought) and an “abnormally dry” category, indicating areas that may be moving into or out of drought. These categories correspond to percentiles of different data (exceptional 0-2, extreme 3-5, severe 5-10, moderate 11-20, abnormal dryness 21-30), with the lower percentile numbers meaning drier conditions.

Different data that account for precipitation over multiple time scales, streamflow, groundwater, soil moisture, and other meteorological and hydrological variables, are placed into percentiles for different locations. Often, the different data will not all indicate the same drought category for a particular location. The author of that week’s map looks at all of this information and assign a category to an area based on what percentile range the different indicators and indices converge on.

Since the U.S. Drought Monitor map is intended to show the entire nation, local conditions may vary from the categories shown on the map. Here in Utah, we rely upon snowmelt runoff stored in reservoirs to get through the hot summer irrigation season. If enough snow falls in the mountains during the winter months, dry summer weather conditions can be somewhat overcome in many areas of the state. While the U.S. Drought Monitor is a useful tool with many applications, the Surface Water Supply Index (SWSI) is used to monitor drought status. The SWSI compares gauged streamflow and current reservoir storage with average streamflow and reservoir storage conditions. This comparison provides us with a more accurate assessment of our ability to deal with the drought situation indicated by the U.S. Drought Monitor map.

Drought Webinars

Drought webinar logoDrought webinars are held on a regular basis to collect feedback on weather conditions around the state. The webinars are hosted by a committee headed by the Division of Water Resources and the Department of Agriculture and Food. For more information on drought webinars, email drought@utah.gov.

Webinar Schedule

The next webinar is scheduled for October 20, 2020. (Webinars are typically scheduled on Tuesdays and are held every two weeks.)

Past Utah Drought Webinar Presentations

October 6, 2020

September 22, 2020

September 8, 2020

August 25, 2020

August 11, 2020

July 28, 2020

July 14, 2020

June 30, 2020

June 18, 2020

June 4, 2020

May 21, 2020

May 7, 2020

April 23, 2020

Community Collaborative Rain, Hail and Snow Network

You can also participate in the Community Collaborative Rain, Hail and Snow Network. This group is a unique, non-profit, community-based network of volunteers of all ages and backgrounds working together to measure and map precipitation. CoCoRaHS is run by the Utah Climate Center. For more information visit www.cocorahs.org

Additional Resources

Drought Response Plan (Revised 2013)

United States Geological Survey

U.S. Drought Monitor

NOAA Drought Information Center

Colorado River Basin Forecast Center

Intermountain West Climate Dashboard