Utah Water Supply Outlook Report April, 2015 Bryce Canyon Snow Course, March 27, 2015 Photo by Lynn Kitchen, NRCS Water Supply Outlook Reports and Federal - State - Private Cooperative Snow Surveys For more water supply and resource management information, contact: your local Natural Resources Conservation Service Office or: Snow Surveys 245 N Jimmy Doolittle Rd, SLC Utah, 84116. Phone (801)524-5213 Internet Address: http://www.ut.nrcs.usda.gov/snow/ How forecasts are made Most of the annual streamflow in the western United States originates as snowfall that has accumulated in the mountains during the winter and early spring. As the snowpack accumulates, hydrologists estimate the runoff that will occur when it melts. Measurements of snow water equivalent at selected manual snowcourses and automated SNOTEL sites, along with precipitation, antecedent streamflow, and indices of the El Niño / Southern Oscillation are used in statistical and simulation models to prepare runoff forecasts. Unless otherwise specified, all forecasts are for flows that would occur naturally without any upstream influences. Forecasts of any kind, of course, are not perfect. Streamflow forecast uncertainty arises from three primary sources: (1) uncertain knowledge of future weather conditions, (2) uncertainty in the forecasting procedure, and (3) errors in the data. The forecast, therefore, must be interpreted not as a single value but rather as a range of values with specific probabilities of occurrence. The middle of the range is expressed by the 50% exceedance probability forecast, for which there is a 50% chance that the actual flow will be above, and a 50% chance that the actual flow will be below, this value. To describe the expected range around this 50% value, four other forecasts are provided, two smaller values (90% and 70% exceedance probability) and two larger values (30%, and 10% exceedance probability). For example, there is a 90% chance that the actual flow will be more than the 90% exceedance probability forecast. The others can be interpreted similarly. The wider the spread among these values, the more uncertain the forecast. As the season progresses, forecasts become more accurate, primarily because a greater portion of the future weather conditions become known; this is reflected by a narrowing of the range around the 50% exceedance probability forecast. Users should take this uncertainty into consideration when making operational decisions by selecting forecasts corresponding to the level of risk they are willing to assume about the amount of water to be expected. If users anticipate receiving a lesser supply of water, or if they wish to increase their chances of having an adequate supply of water for their operations, they may want to base their decisions on the 90% or 70% exceedance probability forecasts, or something in between. On the other hand, if users are concerned about receiving too much water (for example, threat of flooding), they may want to base their decisions on the 30% or 10% exceedance probability forecasts, or something in between. Regardless of the forecast value users choose for operations, they should be prepared to deal with either more or less water. (Users should remember that even if the 90% exceedance probability forecast is used, there is still a 10% chance of receiving less than this amount.) By using the exceedance probability information, users can easily determine the chances of receiving more or less water. The U.S. Department of Agriculture (USDA) prohibits discrimination against its customers. If you believe you experienced discrimination when obtaining services from USDA, participating in a USDA program, or participating in a program that receives financial assistance from USDA, you may file a complaint with USDA. Information about how to file a discrimination complaint is available from the Office of the Assistant Secretary for Civil Rights. USDA prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex (including gender identity and expression), marital status, familial status, parental status, religion, sexual orientation, political beliefs, genetic information, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) To file a complaint of discrimination, complete, sign, and mail a program discrimination complaint form, available at any USDA office location or online at www.ascr.usda.gov, or write to: USDA Office of the Assistant Secretary for Civil Rights 1400 Independence Avenue, SW. Washington, DC 20250‐9410 Or call toll free at (866) 632‐9992 (voice) to obtain additional information, the appropriate office or to request documents. Individuals who are deaf, hard of hearing, or have speech disabilities may contact USDA through the Federal Relay service at (800) 877‐8339 or (800) 845‐6136 (in Spanish). USDA is an equal opportunity provider, employer, and lender. Persons with disabilities who require alternative means for communication of program information (e.g., Braille, large print, audiotape, etc.) should contact USDA's TARGET Center at (202) 720‐2600 (voice and TDD). STATE OF UTAH GENERAL OUTLOOK April 1, 2015 SUMMARY An exceptionally poor water supply year – 2015 will be one that water managers will compare as one of the worst like 2002, 1977 and 1934. Of the long term snow courses going back to the 1930’s, 2015 ranks somewhere between the worst year of record (4 sites) up to the 11th worst year. In the last 30 years, 2015 ranks as the lowest basin average on the Weber, Provo, Tooele, Duchesne, Price, San Rafael and the Sevier rivers. Suffice it to say – 2015 is a dead skunk. The remaining basins, while not the lowest of the past 30 years are very close to the worst. Being second or third lowest is pragmatically as bad as being number one. As of April 1 – the normal peak of snowpack accumulation, Utah watersheds stand at: Bear – 56%, Weber – 37%, Provo 32%, Tooele – 18%, Duchesne – 42%, Price -41%, Upper Sevier -47%, San Pitch -44%, and southwestern Utah -41% of normal. All low elevation sites have melted out. What little snowpack remains will melt quickly. With low snow packs, water managers can expect the following – 1) greatly reduced April-July flow, 2) much lower peak flows, 3) peak flows occurring about 1 to 4 weeks earlier and 4) the bulk of flow to come in April/May as opposed to May/June. March precipitation was below normal statewide ranging from 32% on the Provo to 68% in the southwest. The statewide average was 47% which brings the seasonal accumulation (Oct-Mar) to 62% of average. Current soil moisture saturation levels in runoff producing areas are well above normal due to early snow melt. Soil moisture may not have a significant impact on runoff this year simply due to the fact that there just isn’t much snow to contribute to stream flow. Reservoir storage is about the same as last year at 65% of capacity. General runoff conditions are much below average across the entire state. Surface Water Supply Indices range from 3% on the Weber, Eastern Uinta Basin and San Pitch to 42% on the Bear River. Water managers across the state should prepare for early, short duration stream flow, a longer irrigation season, and low stream flow volumes with low peak flows and poor runoff efficiency. SNOWPACK April first snow packs as measured by the NRCS SNOTEL system range from 18% of median in the Tooele area to 56% on the Bear River watersheds. Most areas have between 30% and 45% of normal. The entire state and indeed, west wide – have exceptionally poor snow packs. PRECIPITATION Mountain precipitation during March was 47% of average which brings the seasonal accumulation (Oct-Mar) 62% of normal. Precipitation ranged from 32% on the Provo to 65% over southeast Utah. SOIL MOISTURE Soil moisture is rising rapidly in response to melting snow packs but was above normal going into the melt season. Soil moisture at lower elevations is declining quickly. Given extremely poor snow packs across the state – above normal soil moisture may have little impact on runoff – there just isn’t sufficient snow to generate substantial stream flow. RESERVOIRS Storage in 46 of Utah’s key irrigation reservoirs is at 65% of capacity compared to 64% last year. STREAMFLOW Snowmelt stream flows are expected to be much below average for the entire state. Forecast stream flows range from 11% on Parleys Creek to 50% on the upper Weber. Most flows are forecast to be in the 15% to 40% range. SURFACE WATER SUPPLY INDEX Surface Water Supply indexes range from 3% for the Weber, East Uintah Basin and San Pitch to 42% for the Bear River. As this graph of the Logan River shows, in low snowpack and streamflow years, peak flows typically occur much earlier in the runoff season and the overall hydrograph is shifted earlier as well. In this graph of the Sevier River in 2002 – snowmelt for various SNOTEL sites and streamflow for the Sevier River at Hatch is shown. Note that there is basically no response to snowmelt and that the Sevier at Hatch is nearly a flat line for the entire period. This is a very likely scenario this year for not only the Sevier but many other streams across the state. Previous Year % Capacity Current % Capacity Statewide Utah 4/1/2015 Snowpack in Utah is much below normal at 41% of normal, compared to 92% last year. Precipitation in March was much below average at 47%, which brings the seasonal accumulation (Oct-Mar) to 62% of average. Soil moisture is at 80% compared to 62% last year. Reservoir storage is at 65% of capacity, compared to 64% last year. Forecast streamflow volumes range from 8% to 67% of average. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 140 Statewide 120 Southwestern Utah Percent of Average 100 Upper Sevier Lower Sevier 80 Price Basin 60 Duchesne Basin 40 Provo Basin Weber & Ogden… 20 Bear River Basin 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Utah SNOTEL Current Snow Water Equivalent (SWE) % of Normal Raft River Apr 01, 2015 98 Logan ! ! ! ! Snow Water Equivalent (SWE) Basin-wide Percent of 1981-2010 Median Ogden Great Salt Lake Bear River Weber Ogden Northeastern Uintahs 38 Salt Lake City 80 § ¦ ¨ 56 29 56 ^ _ ! ( Duchesne River 18 TooeleVernon 42 33 ! ! ! ! Roosevelt Provo unavailable * ProvoUtahJordan <50% 50 - 69% 70 - 89% Lower Sevier River 90 - 109% 41 San Pitch Price - San Rafael 44 41 110 - 129% 130 - 149% 70 § ¦ ¨ >=150% ! ! * Data unavailable at time of posting or measurement is not representative at this time of year 48 47 Beaver River Provisional Data Subject to Revision 15 § ¦ ¨ Southwestern Utah 23 70 Dirty Devil Upper Sevier River 42 74 Southeastern Utah Escalante River St. George ! ! 0 10 20 The snow water equivalent percent of normal represents the current snow water equivalent found at selected SNOTEL sites in or near the basin compared to the average value for those sites on this day. Data based on the first reading of the day (typically 00:00). Moab 40 60 80 Miles 100 Prepared by: USDA/NRCS National Water and Climate Center Portland, Oregon http://www.wcc.nrcs.usda.gov Utah SNOTEL Water Year (Oct 1) to Date Precipitation % of Normal Raft River Apr 01, 2015 96 Logan ! ! ! ! Water Year (Oct 1) to Date Precipitation Basin-wide Percent of 1981-2010 Average Ogden Great Salt Lake Bear River Weber Ogden Northeaster Uintahs 59 Salt Lake City 80 § ¦ ¨ 71 60 71 ^ _ ! ( Duchesne River 46 TooeleVernon unavailable * Lower Sevier River 70 - 89% Roosevelt Provo Price - San Rafael San Pitch 75 90 - 109% ! ! ProvoUtahJordan <50% 50 - 69% 56 59 ! ! 68 64 110 - 129% 130 - 149% 70 § ¦ ¨ >=150% ! ! * Data unavailable at time of posting or measurement is not representative at this time of year 55 Beaver River Provisional Data Subject to Revision 15 § ¦ ¨ 67 68 81 Upper Sevier River Moab Dirty Devil Southwestern Utah 59 75 Southeastern Utah Escalante River St. George ! ! 0 10 20 The water year to date precipitation percent of normal represents the accumulated precipitation found at selected SNOTEL sites in or near the basin compared to the average value for those sites on this day. Data based on the first reading of the day (typically 00:00). 40 60 80 Miles 100 Prepared by: USDA/NRCS National Water and Climate Center Portland, Oregon http://www.wcc.nrcs.usda.gov Utah streamflow and reservoir forecast points # * Percent normal # * # * # * # * # * # * # * # * < 50% # * Forecast points 50 - 69% 5 Cities 70 - 89% Rivers 90 - 109% Highways Ü 110 - 129% 130 - 149% 0 > 150% no % avail. 15 30 60 90 120 Miles SNOTEL Current Snow Water Equivalent (SWE) Records Apr 02, 2015 NOTE: Until further notice, record calculations are based on period of record through water year 2012; water years 2013 and 2014 are not analyzed. Current Snow Water (SWE) Equivalent Records New High Near High Non-Record New Low Near Low snow free Analysis includes sites with more than 20 years of historical data. "Near" record means that one other year of the period of record is more extreme. Provisional Data Subject to Revision Prepared by: USDA/NRCS National Water and Climate Center Portland, Oregon http://www.wcc.nrcs.usda.gov Previous Year % Capacity Current % Capacity Bear River Basin 4/1/2015 Snowpack in the Bear River Basin is much below normal at 56% of normal, compared to 120% last year. Precipitation in March was much below average at 50%, which brings the seasonal accumulation (Oct-Mar) to 71% of average. Soil moisture is at 88% compared to 67% last year. Reservoir storage is at 48% of capacity, compared to 46% last year. Forecast streamflow volumes range from 10% to 67% of average. The surface water supply index is 42% for the Bear River, 14% for the Woodruff Narrows, 4% for the Little Bear. Soil Moisture Snowpack 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 140 WOODRUFF CREEK 120 WOODRUFF NARROWS Percent of Average 100 80 PORCUPINE 60 40 HYRUM 20 BEAR LAKE 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Bear River * ^ 583.77 # KAF ^ 18.00 Storage + Forecast KAF ^ 601.77 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Bear River Surface Water Supply Index 1800 1600 Thousand Acre Feet 1400 1200 1000 800 600 400 200 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 42 -0.69 07, 10, 90, 14 Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Little Bear * ^ 14.10 # KAF ^ 8.00 Storage + Forecast KAF ^ 22.10 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Little Bear Surface Water Supply Index 140 Thousand Acre Feet 120 100 80 60 40 20 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 4 -3.82 13, 14, 03, 01 Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Woodruff Narrows * # ^ 50.93 KAF ^ 40.00 Storage + Forecast KAF ^ 90.93 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Woodruff Narrows Surface Water Supply Index 300 Thousand Acre Feet 250 200 150 100 50 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 14 -3.01 04, 13, 03, 90 Bear basin ! ( ! ( ! ( ! ( ! ( ! ( ! ( # *! ( # * § ¨ ¦ 15 ! ( ! ( ! ( ! (! (! ( § ¨ ¦ 84 ! ( 5# * Tremonton5 Logan # * # * # * ! ( ! ( ! ( § ¨ ¦ ! ( # * 15 Percent normal " ) " ) " ) " ) " ) " ) " ) " ) ! ( # * < 50% 5 Evanston 5 Ogden § ¨ ¦ 50 - 69% 84 § ¨ ¦ 80 70 - 89% ! ( # * 90 - 109% ! (! ( 110 - 129% ! ( 130 - 149% V U > 150% 150 ! ( no % avail. SNOTEL sites Forecast points Rivers Highways 5 Cities Ü 0 5 10 20 30 40 Miles Raft River Basin 4/1/2015 Snowpack in the Raft River Basin is near normal at 98% of normal, compared to 114% last year. Precipitation in March was much below average at 48%, which brings the seasonal accumulation (Oct-Mar) to 97% of average. Soil moisture is at 78% compared to 30% last year. The forecast streamflow volume for Dunn Creek is 28% of average. Snowpack Soil Moisture 120% Snow Water Equivalent Index Saturation, volume % 100% 80% 60% 40% 20% 0% Calculated using soil moisture content at 2, 8, and 20-inch depths. Max Min Avg WY 2015 2005-Current Precipitation 200 180 160 Percent of Average 140 120 100 80 60 40 20 0 Monthly Year-to-Date WY 2015 Avg Raft basin V U 16 V U 42 V U 30 ! ( # * 5 V U Park Valley 30 Percent normal " ) " ) " ) " ) " ) " ) " ) " ) < 50% 50 - 69% 70 - 89% ! ( # * SNOTEL sites Forecast points 90 - 109% Rivers 110 - 129% Highways 130 - 149% 5 Cities > 150% no % avail. Ü 0 1.5 3 6 9 12 Miles Weber & Ogden River Basins 4/1/2015 Snowpack in the Weber & Ogden River Basins is much below normal at 37% of normal, compared to 100% last year. Precipitation in March was much below average at 45%, which brings the seasonal accumulation (Oct-Mar) to 59% of average. Soil moisture is at 83% compared to 66% last year. Reservoir storage is at 57% of capacity, compared to 50% last year. Forecast streamflow volumes range from 14% to 50% of average. The surface water supply index is 11% for the Ogden River, 3% for the Weber River. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 2005-Current WY 2015 Avg Reservoir Storage Precipitation 120 SMITH AND MOREHOUSE 100 Percent of Average Calculated using soil moisture content at 2, 8, and 20-inch depths. ROCKPORT ECHO 80 LOST CREEK 60 EAST CANYON 40 CAUSEY PINEVIEW 20 WILLARD BAY 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Ogden River * ^ 77.94 # KAF ^ Storage + Forecast KAF 16.00 ^ 93.94 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Ogden River Surface Water Supply Index 400 350 Thousand Acre Feet 300 250 200 150 100 50 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 11 -3.24 88, 03, 13, 87 Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Weber River * ^ 232.33 # KAF Storage + Forecast ^ KAF 54.00 ^ 286.33 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Weber River Surface Water Supply Index 1200 Thousand Acre Feet 1000 800 600 400 200 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 3 -3.94 13, 04, 03, 07 Weber-Ogden basin ! ( ! ( ( !! ( ! ( ! ( 5 # * * # # * Ogden § ¨ ¦ ! ( 80 ! ( # * # * 5 Layton ! ( ! ( ! # * ( Percent normal " ) " ) " ) " ) " ) " ) " ) " ) ! ( # * # * ! ( < 50% ! ( ! ( 50 - 69% 70 - 89% § ¨ ¦ 80 90 - 109% ! ( # * 110 - 129% § ¨ ¦ 130 - 149% 15 ! ( > 150% no % avail. SNOTEL sites Forecast points Highways Cities Ü 0 2.5 5 10 15 ( # *! # * ! ( ! ( Rivers 5 # * * # # * 20 Miles ! ( Provo & Jordan River Basins 4/1/2015 Snowpack in the Provo & Jordan River Basins is much below normal at 32% of normal, compared to 88% last year. Precipitation in March was much below average at 41%, which brings the seasonal accumulation (Oct-Mar) to 59% of average. Soil moisture is at 86% compared to 70% last year. Reservoir storage is at 71% of capacity, compared to 73% last year. Forecast streamflow volumes range from 11% to 48% of average. The surface water supply index is 14% for the Provo River. Soil Moisture Snowpack 100% 40 35 80% Saturation, volume % 25 20 15 10 60% 40% 20% 5 0% 0 Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 140 UTAH LAKE 120 100 Percent of Average Snow Water Equivalent Index 30 JORDANELLE 80 DEER CREEK 60 40 UPPER STILLWATER 20 STRAWBERRY 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Provo River * ^ 920.40 # KAF ^ 28.00 Storage + Forecast KAF ^ 948.40 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Provo River Surface Water Supply Index 1600 1400 Thousand Acre Feet 1200 1000 800 600 400 200 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 14 -3.03 04, 03, 14, 02 ( ! (! # * # * ! ( * Salt Lake City 5 # # * # * § ¨ ¦ 80 ! ( # * ! ( ! ( # * 5 Heber City # * ( ! # * # * ! ( ! ( 5Provo ! ( # * § ¨ ¦ 15 ! ( ! ( ! ( # * 5 Nephi Percent normal " ) " ) " ) " ) " ) " ) " ) " ) < 50% 50 - 69% 70 - 89% ! ( # * SNOTEL sites Forecast points 90 - 109% Rivers 110 - 129% Highways 130 - 149% > 150% no % avail. 5 Cities Ü 0 2.5 5 ! ( ! ( ! ( # * # * ! ( Provo-Utah LakeJordan basin 10 15 20 Miles Tooele & Vernon Creek Basins 4/1/2015 Snowpack in the Tooele & Vernon Creek Basins is much below normal at 18% of normal, compared to 82% last year. Precipitation in March was much below average at 32%, which brings the seasonal accumulation (Oct-Mar) to 47% of average. Soil moisture is at 62% compared to 51% last year. Reservoir storage is at 50% of capacity, compared to 62% last year. Forecast streamflow volumes range from 16% to 22% of average. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 140 120 VERNON CREEK Percent of Average 100 80 SETTLEMENT CANYON 60 40 GRANTSVILLE 20 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Salt Lake City § ¨ ¦ 80 Tooele 5 § ¨ ¦ * ! (# 15 ! ( ! ( TooeleVernon basin Percent normal " ) " ) " ) " ) " ) " ) " ) " ) ! ( # * 50 - 69% # * 70 - 89% ! ( 90 - 109% 110 - 129% 130 - 149% > 150% no % avail. SNOTEL sites Rivers Highways 5 5 Vernon < 50% Forecast points Cities 0 2.5 5 Ü 5 10 15 20 Miles Northeastern Uintah Basin 4/1/2015 Snowpack in the Northeastern Uintah Basin is much below normal at 26% of normal, compared to 97% last year. Precipitation in March was much below average at 35%, which brings the seasonal accumulation (Oct-Mar) to 60% of average. Soil moisture is at 84% compared to 60% last year. Reservoir storage is at 84% of capacity, compared to 77% last year. Forecast streamflow volumes range from 51% to 63% of average. The surface water supply index is 24% for the Blacks Fork, 24% for the Smiths Creek. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 120 Percent of Average 100 MEEKS CABIN 80 60 STATELINE 40 20 FLAMING GORGE 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Blacks Fork * ^ 26.29 # KAF ^ 45.00 Storage + Forecast KAF ^ 71.29 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Blacks Fork Surface Water Supply Index 200 180 Thousand Acre Feet 160 140 120 100 80 60 40 20 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 24 -2.15 00, 12, 89, 13 Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Smiths Fork * ^ 8.86 # KAF Storage + Forecast ^ KAF 15.00 ^ 23.86 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Smiths Fork Surface Water Supply Index 80 70 Thousand Acre Feet 60 50 40 30 20 10 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 24 -2.21 07, 89, 03, 06 Northeastern Utah # * Manila5 # * ! ( ! ( ! ( ! ( ! ( ! ( ! ( ! ( # * V U 44 ! ( £ ¤ 191 Percent normal " ) " ) " ) " ) " ) " ) " ) " ) ! ( # * < 50% 50 - 69% 70 - 89% 90 - 109% 110 - 129% 130 - 149% > 150% no % avail. SNOTEL sites Forecast points Rivers Highways 5 Ü Cities 0 2.254.5 9 ! ( 13.5 18 Miles Duchesne River Basin 4/1/2015 Snowpack in the Duchesne River Basin is much below average at 40% of normal, compared to 91% last year. Precipitation in March was much below average at 45%, which brings the seasonal accumulation (Oct-Mar) to 56% of average. Soil moisture is at 76% compared to 44% last year. Reservoir storage is at 78% of capacity, compared to 76% last year. Forecast streamflow volumes range from 17% to 55% of average. The surface water supply index is 19% for the Western Uintahs, 3% for the Eastern Uintahs. Soil Moisture Snowpack 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 120 STRAWBERRY Percent of Average 100 CURRANT CREEK MOON LAKE 80 STARVATION 60 UPPER STILLWATER 40 BIG SAND WASH RED FLEET 20 STEINAKER 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Eastern Uintah * # ^ 31.00 KAF Storage + Forecast ^ KAF 22.90 ^ 53.90 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Eastern Uintah Surface Water Supply Index 200 180 Thousand Acre Feet 160 140 120 100 80 60 40 20 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 3 -3.94 14, 02, 13, 89 Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Western Uintah * # ^ 195.47 KAF Storage + Forecast ^ KAF 40.00 ^ 235.47 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Western Uintah Surface Water Supply Index 400 350 Thousand Acre Feet 300 250 200 150 100 50 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 19 -2.55 03, 12, 04, 07 Duchesne basin £ ¤ 191 ! ( ! ( ! ( ! ( ! ( ! ( # * ! ( £ ¤ * ! ( ! (# # ( * ! # * # * ! (# * ! ( # * 5 Duchesne ! ( £ ¤ 191 Percent normal < 50% ! ( # * 50 - 69% 70 - 89% SNOTEL sites Forecast points 90 - 109% Rivers 110 - 129% Highways 5 130 - 149% Cities > 150% no % avail. Ü 5 10 20 30 £ ¤ 5 # * * ## * 40 Miles # * Vernal 5 Roosevelt * !# ( 0 # * # * 40 " ) " ) " ) " ) " ) " ) " ) " ) ( # *! # * 40 * # Lower Sevier River Basin 4/1/2015 Snowpack in the Lower Sevier River Basin is much below normal at 41% of normal, compared to 71% last year. Precipitation in March was much below average at 38%, which brings the seasonal accumulation (Oct-Mar) to 75% of average. Soil moisture is at 74% compared to 59% last year. Reservoir storage is at 50% of capacity, compared to 59% last year. Forecast streamflow volumes range from 18% to 25% of average. The surface water supply index is 11% for the Lower Sevier. Soil Moisture Snowpack 120% Snow Water Equivalent Index Saturation, volume % 100% 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 220 200 180 Percent of Average 160 140 120 SEVIER BRIDGE 100 80 60 40 20 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Lower Sevier * ^ 117.10 # KAF ^ Storage + Forecast KAF 25.00 ^ 142.10 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Lower Sevier Surface Water Supply Index 900 800 Thousand Acre Feet 700 600 500 400 300 200 100 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 11 -3.24 03, 92, 02, 94 Lower Sevier basin § ¨ ¦ 15 5 Nephi # * ! ( *! # ( 5 Delta Fillmore 5 ! ( § ¨ ¦ 15 Percent normal " ) " ) " ) " ) " ) " ) " ) " ) < 50% 50 - 69% 70 - 89% ! ( # * SNOTEL sites Forecast points 90 - 109% Rivers 110 - 129% Highways 130 - 149% > 150% 5 Cities Ü 0 2.5 5 no % avail. 10 15 20 Miles Upper Sevier River Basin 4/1/2015 Snowpack in the Upper Sevier River Basin is much below normal at 47% of normal, compared to 69% last year. Precipitation in March was much below average at 58%, which brings the seasonal accumulation (Oct-Mar) to 67% of average. Soil moisture is at 78% compared to 65% last year. Reservoir storage is at 61% of capacity, compared to 82% last year. Forecast streamflow volumes range from 15% to 43% of average. The surface water supply index is 8% for the Upper Sevier. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 160 140 PANGUITCH LAKE Percent of Average 120 100 80 OTTER CREEK 60 40 PIUTE 20 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Upper Sevier * ^ 80.39 # KAF ^ Storage + Forecast KAF 26.00 ^ 106.39 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Upper Sevier Surface Water Supply Index 350 Thousand Acre Feet 300 250 200 150 100 50 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 8 -3.47 04, 91, 90, 92 Upper Sevier basin ! ( Fillmore 5 # * ! ( 70 ! ( ! ( ! ( 5 Richfield # * ! ( ! ( ! ( ! ( # * Beaver 5 Percent normal " ) " ) " ) " ) " ) " ) " ) " ) # *# * < 50% ! ( § ¨ ¦ 50 - 69% 15 ! ( 70 - 89% 90 - 109% ! ( 110 - 129% 130 - 149% ! ( > 150% # * ! ( no % avail. ! ( ! ( # * SNOTEL sites Forecast points Rivers Highways 5 Ü Cities 0 5 10 20 30 40 Miles ! ( § ¨ ¦ San Pitch River Basin 4/1/2015 Snowpack in the San Pitch River Basin is much below normal at 44% of normal, compared to 90% last year. Precipitation in March was much below average at 32%, which brings the seasonal accumulation (Oct-Mar) to 68% of average. Soil moisture is at 82% compared to 66% last year. Reservoir storage is at 11% of capacity, compared to 24% last year. The forecast streamflow volume for Manti Creek is 39% of average. The surface water supply index is 3% for the San Pitch. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 200 180 160 Percent of Average 140 120 GUNNISON RESERVOIR 100 80 60 40 20 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF San Pitch * ^ 2.28 # KAF Storage + Forecast ^ 6.50 KAF ^ 8.78 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. San Pitch Surface Water Supply Index 70 Thousand Acre Feet 60 50 40 30 20 10 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 3 -3.94 02, 13, 14, 03 San Pitch basin ! ( ! ( Mt. Pleasant 5 ! ( £ ¤ 89 Ephraim 5 Percent normal " ) " ) " ) " ) " ) " ) " ) " ) ! ( # * ! ( < 50% 50 - 69% * # ! ( 70 - 89% 90 - 109% 110 - 129% # * 130 - 149% 5 ! ( Gunnison > 150% no % avail. SNOTEL sites ! ( Forecast points Rivers Highways 5 Ü Cities 0 2.5 5 10 15 20 Miles ! ( ( ! (! Price & San Rafael Basins 4/1/2015 Snowpack in the Price & San Rafael Basins is much below normal at 41% of normal, compared to 88% last year. Precipitation in March was much below average at 45%, which brings the seasonal accumulation (Oct-Mar) to 64% of average. Soil moisture is at 83% compared to 63% last year. Reservoir storage is at 50% of capacity, compared to 45% last year. Forecast streamflow volumes range from 8% to 46% of average. The surface water supply index is 6% for the Price River, 8% for Joe's Valley, 6% for Ferron Creek. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 180 SCOFIELD 160 Percent of Average 140 MILLER FLAT 120 100 CLEVELAND LAKE 80 HUNTINGTON NORTH 60 MILLSITE 40 20 JOES VALLEY 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Price River * ^ 14.55 # KAF ^ 7.00 Storage + Forecast KAF ^ 21.55 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Price River Surface Water Supply Index 160 140 Thousand Acre Feet 120 100 80 60 40 20 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 6 -3.7 92, 04, 02, 94 Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Ferron Creek * ^ 10.84 # KAF ^ Storage + Forecast KAF 12.00 ^ 22.84 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Ferron Creek Surface Water Supply Index 120 Thousand Acre Feet 100 80 60 40 20 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 6 -3.7 13, 02, 90, 12 Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Joe's Valley * ^ 41.63 # KAF ^ 20.00 Storage + Forecast KAF ^ 61.63 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Joe's Valley Surface Water Supply Index 200 180 Thousand Acre Feet 160 140 120 100 80 60 40 20 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 8 -3.47 13, 02, 90, 03 Price-San Rafael ! ( basin # * # ! ( # * ! ( ! ( ! ( 5 Price ! ( ! ( ! ( # * # * Castle Dale 5 ! (! ( # * 5 # *Green River Percent normal " ) " ) " ) " ) " ) " ) " ) " ) ! ( # * < 50% § ¨ ¦ 70 50 - 69% 70 - 89% 90 - 109% 110 - 129% 130 - 149% > 150% no % avail. SNOTEL sites Forecast points Rivers Highways 5 Ü Cities 0 5 10 20 30 40 Miles Southeastern Utah Basin 4/1/2015 Snowpack in the Southeastern Utah Basin is much below normal at 22% of normal, compared to 55% last year. Precipitation in March was much below average at 65%, which brings the seasonal accumulation (Oct-Mar) to 68% of average. Soil moisture is at 79% compared to 75% last year. Reservoir storage is at 65% of capacity, compared to 53% last year. Forecast streamflow volumes range from 18% to 61% of average. The surface water supply index is 21% for Moab. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 140 120 Percent of Average 100 80 KEN'S LAKE 60 40 20 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Moab * ^ 1.50 # KAF Storage + Forecast ^ 2.00 KAF ^ 3.50 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Moab Surface Water Supply Index 14 Thousand Acre Feet 12 10 8 6 4 2 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 21 -2.44 12, 89, 04, 09 Vernal 5 Southeastern Utah 5 Price £ ¤ 6 ! ( Green River 5 § ¨ ¦ 70 # * Moab 5 # *! ! ( ( Percent normal " ) " ) " ) " ) " ) " ) " ) " ) < 50% 50 - 69% 70 - 89% 5 Monticello ! (* !# ( 90 - 109% 110 - 129% 130 - 149% > 150% no % avail. # * ! ( # * SNOTEL sites Forecast points Rivers Highways 5 Ü Cities 0 5 10 20 30 40 Miles Dirty Devil Basin 4/1/2015 Snowpack in the Dirty Devil Basin is below normal at 70% of normal, compared to 99% last year. Precipitation in March was much below average at 53%, which brings the seasonal accumulation (Oct-Mar) to 81% of average. Soil moisture is at 68% compared to 45% last year. Forecast streamflow volumes range from 44% to 48% of average. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current Precipitation 220 200 180 Percent of Average 160 140 120 100 80 60 40 20 0 Monthly Year-to-Date WY 2015 Avg Dirty Devil basin ! ( # * § ¨ ¦ 70 ! ( # * ! ( Hanksville Torrey 5 ! ( Percent normal " ) " ) " ) " ) " ) " ) " ) " ) ! ( # * < 50% 50 - 69% 70 - 89% 90 - 109% 110 - 129% 130 - 149% > 150% no % avail. SNOTEL sites Forecast points Rivers Highways 5 Ü Cities 0 5 10 20 30 40 Miles 5 Escalante River Basin 4/1/2015 Snowpack in the Escalante River Basin is below normal at 74% of normal, compared to 86% last year. Precipitation in March was much below average at 66%, which brings the seasonal accumulation (Oct-Mar) to 75% of average. Soil moisture is at 61% compared to 63% last year. The forecast streamflow volume for Pine Creek is 59% of average. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Calculated using soil moisture content at 2, 8, and 20-inch depths. Max Min Avg WY 2015 2005-Current Precipitation 160 140 Percent of Average 120 100 80 60 40 20 0 Monthly Year-to-Date WY 2015 Avg ! ( Escalante basin V U 12 ! ( 5 Boulder # * ! ( Escalante 5 £ ¤ 89 # * Percent normal " ) " ) " ) " ) " ) " ) " ) " ) < 50% 50 - 69% 70 - 89% ! ( # * SNOTEL sites Forecast points 90 - 109% Rivers 110 - 129% Highways 130 - 149% > 150% 5 Cities Ü 0 2.5 5 no % avail. 10 15 20 Miles Beaver River Basin 4/1/2015 Snowpack in the Beaver River Basin is much below normal at 48% of normal, compared to 85% last year. Precipitation in March was much below average at 56%, which brings the seasonal accumulation (Oct-Mar) to 55% of average. Soil moisture is at 46% compared to 42% last year. Reservoir storage is at 50% of capacity, compared to 57% last year. The forecast streamflow volume for the Beaver River is 30% of average. The surface water supply index is 6% for the Beaver River. Snowpack Soil Moisture 80% Snow Water Equivalent Index Saturation, volume % 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 120 Percent of Average 100 80 MINERSVILLE RESERVOIR 60 40 20 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Beaver River * ^ 11.72 # KAF ^ Storage + Forecast KAF 7.70 ^ 19.42 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Beaver River Surface Water Supply Index 100 90 Thousand Acre Feet 80 70 60 50 40 30 20 10 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 6 -3.7 02, 04, 90, 03 Beaver basin § ¨ ¦ 15 § ¨ ¦ 70 Milford 5 Beaver 5 Percent normal " ) " ) " ) " ) " ) " ) " ) " ) < 50% 50 - 69% 70 - 89% ! ( # * SNOTEL sites Forecast points 90 - 109% Rivers 110 - 129% Highways 130 - 149% > 150% no % avail. 5 Cities 0 1.5 3 Ü 6 9 12 Miles # * ! ( ! ( Previous Year % Capacity Current % Capacity Southwestern Utah Basin 4/1/2015 Snowpack in the Southwestern Utah Basin is much below normal at 41% of normal, compared to 46% last year. Precipitation in March was much below average at 68%, which brings the seasonal accumulation (Oct-Mar) to 59% of average. Soil moisture is at 69% compared to 63% last year. Reservoir storage is at 45% of capacity, compared to 39% last year. Forecast streamflow volumes range from 22% to 45% of average. The surface water supply index is 12% for the Virgin River. Snowpack Soil Moisture 100% Snow Water Equivalent Index Saturation, volume % 80% 60% 40% 20% 0% Max Min Avg WY 2015 Calculated using soil moisture content at 2, 8, and 20-inch depths. 2005-Current WY 2015 Avg Reservoir Storage Precipitation 120 QUAIL CREEK 100 Percent of Average SAND HOLLOW 80 GUNLOCK 60 KOLOB UPPER ENTERPRISE 40 LOWER ENTERPRISE 20 LAKE POWELL 0 Monthly Year-to-Date Previous Year % Capacity Current % Capacity Surface Water Supply Index April 1, 2015 Basin or Region Mar EOM* Storage APR-JUL Forecast KAF Virgin River * ^ 32.86 # KAF ^ 19.50 Storage + Forecast KAF ^ 52.36 ^ EOM, end of month; SWSI, Surface Water Supply Index; KAF, thousand acre-feet. Virgin River Surface Water Supply Index 300 Thousand Acre Feet 250 200 150 100 50 0 Water Year Storage (KAF) Streamflow (KAF) Percentile SWSI# Years with similiar SWSI % 12 -3.21 91, 03, 14, 13 Southwestern Utah § ¨ ¦ 15 ! ( Cedar City 5# * ! ( ! ( ! (! ( ! ( ! ( ! ( ! ( ! (! ( ( # *! # * 5 # * Hurricane St. George 5 Percent normal " ) " ) " ) " ) " ) " ) " ) " ) < 50% 50 - 69% 70 - 89% ! ( # * SNOTEL sites Forecast points 90 - 109% Rivers 110 - 129% Highways 130 - 149% > 150% no % avail. 5 Cities 0 2.5 5 Ü 10 15 20 Miles Surface Water Supply Index April 1, 2015 * Basin or Region Bear River Woodruff Narrows Little Bear Ogden River Weber River Provo River Western Uintah Eastern Uintah Blacks Fork Smiths Fork Price River Joe's Valley Ferron Creek Moab Upper Sevier San Pitch Lower Sevier Beaver River Virgin River Mar EOM Storage KAF ^ 583.8 50.9 14.1 77.9 232.3 920.4 195.5 31.0 26.3 8.9 14.6 41.6 10.8 1.5 80.4 2.3 117.1 11.7 32.9 APR-JUL Forecast Storage + Forecast Percentile KAF ^ KAF ^ % 18.0 40.0 8.0 16.0 54.0 28.0 40.0 22.9 45.0 15.0 7.0 20.0 12.0 2.0 26.0 6.5 25.0 7.7 19.5 601.8 90.9 22.1 93.9 286.3 948.4 235.5 53.9 71.3 23.9 21.6 61.6 22.8 3.5 106.4 8.8 142.1 19.4 52.4 42 14 4 11 3 14 19 3 24 24 6 8 6 21 8 3 11 6 12 SWSI # Years with similiar SWSI ‐0.69 ‐3.01 ‐3.82 ‐3.24 ‐3.94 ‐3.03 ‐2.55 ‐3.94 ‐2.15 ‐2.21 ‐3.7 ‐3.47 ‐3.7 ‐2.44 ‐3.47 ‐3.94 ‐3.24 ‐3.7 ‐3.21 07, 10, 90, 14 04, 13, 03, 90 13, 14, 03, 01 88, 03, 13, 87 13, 04, 03, 07 04, 03, 14, 02 03, 12, 04, 07 14, 02, 13, 89 00, 12, 89, 13 07, 89, 03, 06 92, 04, 02, 94 13, 02, 90, 03 13, 02, 90, 12 12, 89, 04, 09 04, 91, 90, 92 02, 13, 14, 03 03, 92, 02, 94 02, 04, 90, 03 91, 03, 14, 13 *EOM, end of month; # SWSI, surface water supply index; ^KAF, thousand acre‐feet. What is a Surface Water Supply Index? The Surface Water Supply Index (SWSI) is a predictive indicator of total surface water availability within a watershed for the spring and summer water use seasons. The index is calculated by combining pre‐runoff reservoir storage (carryover) with forecasts of spring and summer streamflow which are based on current snowpack and other hydrologic variables. SWSI values are scaled from +4.1 (abundant supply) to ‐4.1 (extremely dry) with a value of zero (0) indicating median water supply as compared to historical analysis. SWSI's are calculated in this fashion to be consistent with other hydroclimatic indicators such as the Palmer Drought Index and the Precipitation index. Utah Snow Surveys has also chosen to display the SWSI value as well as a PERCENT CHANCE OF NON‐EXCEEDANCE. While this is a cumbersome name, it has the simplest application. It can be best thought of as a scale of 1 to 99 with 1 being the drought of record (driest possible conditions) and 99 being the flood of record (wettest possible conditions) and a value of 50 representing average conditions. This rating scale is a percentile rating as well, for example a SWSI of 75% means that this years water supply is greater than 75% of all historical events and that only 25% of the time has it been exceeded. Conversely a SWSI of 10% means that 90% of historical events have been greater than this one and that only 10% have had less total water supply. This scale is comparable between basins: a SWSI of 50% means the same relative ranking on watershed A as it does on watershed B, which may not be strictly true of the +4 to ‐4 scale. For more information on the SWSI go to: www.ut.nrcs.usda.gov/snow/ on the water supply page. The entire period of historical record for reservoir storage and streamflow is available. Issued by Released by Jason Weller Chief Natural Resources Conservation Service U.S. Department of Agriculture David Brown State Conservationist Natural Resources Conservation Service Salt Lake City, Utah Prepared by Snow Survey Staff Randall Julander, Supervisor Troy Brosten, Assistant Supervisor Beau Uriona, Hydrologist Jordan Clayton, Hydrologist Jeffrey O’Connell, Hydrologist Bob Nault, Electronics Technician Kent Sutcliffe, Soil Scientist YOU MAY OBTAIN THIS PRODUCT AS WELL AS CURENT SNOW, PRECIPITATION, TEMPERATURE AND SOIL MOISTURE, RESERVOIR, SURFACE WATER SUPPLY INDEX, AND OTHER DATA BY VISITING OUR WEB SITE @: http://www.ut.nrcs.usda.gov/snow/ Snow Survey, NRCS, USDA 245 North Jimmy Doolittle Road Salt Lake City, UT 84116 (801) 524-5213 Utah Climate and Water Report Natural Resources Conservation Service Salt Lake City, UT
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