Idaho Power Company’s Cloud Seeding Program

Slides:



Advertisements
Similar presentations
Unit 4 Weather and Climate
Advertisements

Cloud Development and Precipitation
Cloud Seeding in the Walker River Basin Arlen Huggins Desert Research Institute Scientific basis for wintertime cloud seeding Determining the potential.
Validation of WRF and WRF LES Simulations of the Dispersal of Ground-generated AgI Nuclei Xia Chu 1, Lulin Xue 2, Bart Geerts 1, Bruce Boe 3, Roy Rasmussen.
Moist Processes ENVI1400: Lecture 7. ENVI 1400 : Meteorology and Forecasting2 Water in the Atmosphere Almost all the water in the atmosphere is contained.
The Importance of Realistic Spatial Forcing in Understanding Hydroclimate Change-- Evaluation of Streamflow Changes in the Colorado River Basin Hydrology.
Welcome to Weather Science Jeopardy GeneralKnowledge Weather Factors I Weather Factors II ForecastingTools Final Jeopardy.
Climate and Weather CGC1P.
Meteorology Basics Lecture “Climate is what you expect, weather is what you get.”
Review of the 2009 Snowmelt and Rain Streamflow Forecasts & Snow Survey Advisory Team Ron Abramovich, Hydrologist Water Supply Specialist USDA Natural.
Numerical Simulations of Snowpack Augmentation for Drought Mitigation Studies in the Colorado Rocky Mountains William R. Cotton, Ray McAnelly, and Gustavo.
Cloud Seeding §Examples of man's desire to modify weather are as old as recorded history. § The modern era of weather modification began in the late 1940s.
Alan F. Hamlet Andy Wood Seethu Babu Marketa McGuire Dennis P. Lettenmaier JISAO Climate Impacts Group and the Department of Civil Engineering University.
Chapter 24 Section 4 Handout
Dew, Frost and Fog. RECAP Hydrological cycle: transport of water and energy. Humidity: absolute humidity, specific humidity, water mixing ratio, relative.
Cloud Seeding for Snowfall Enhancement: Concepts, Evidence of Effects and New Evaluation Techniques Arlen W. Huggins Desert Research Institute Reno, Nevada,
Section 4: Forecasting the Weather
Unit 4 Lesson 5 Weather Maps and Weather Prediction
CryosPheric responses to Anthropogenic PRessures in the HIndu Kush-Himalaya regions: impacts on water resources and society adaptation in Nepal DHM Centre.
Moisture and Clouds Weather Unit When you see this megaphone, Click it for audio information Weather Unit When you see this megaphone, Click it for audio.
The study of weather = METEROLOGY The study of weather = METEROLOGY Weather is the condition of the atmosphere at any given time or place Weather is the.
Water is the source of all life on earth
Slide 1 Impact of GPS-Based Water Vapor Fields on Mesoscale Model Forecasts (5th Symposium on Integrated Observing Systems, Albuquerque, NM) Jonathan L.
Ground Deicing Update Scott Landolt, Roy Rasmussen and Jenny Black.
Chapter 18 Review Place these notes into your Meteorology Notebook.
Chapter 5. The Formation of Dew & Frost  Dew forms on objects near the ground surface when they cool below the dew point temperature. More likely on.
Precipitation Hydrology (Spring 2013) Illinois State University Instructor: Eric Peterson.
Who Wants to be a Millionaire? A Weather Forecasting System Review Circle your answer as you go. Mark it right or wrong as you go.
Hydrologic Equation Inflow = outflow +/- Changes in storage Equation is simple statement of mass conservation.
The Santa Barbara County Regional Cloudseeding Program Food for Thought Lecture Series at Lake Cachuma Nature Center June 7, 2015 Dennis Gibbs, P.H., C.W.M.O.
Forecasting the weather Severe weather & fronts
►Weather forecasting dates back to 650 B.C. The Babylonians observed cloud patterns to predict weather. ►Aristotle described weather patterns in Meteorologica.
Water in the Atmosphere
Water in the Atmosphere Section 3 Section 3: Precipitation Preview Key Ideas Forms of Precipitation Causes of Precipitation Measuring Precipitation Weather.
Weather & Climate Chapter 6. Weather & Climate Weather:  Refers to the current, day-to-day, short term conditions of the atmosphere.
Weather Forecasting & Maps -Meteorologists make forecasts based on models that are produced by supercomputers which perform a large amount of calculations.
Weather 101 Brainstorm Why do we study the weather? Create a concept map with as many words you know about weather.
Climate  Climate is the average or usual weather pattern that occurs in a region over a long period of time.
Factors Affecting Climate
Unit 11 Lesson 2 Elements of Weather
Modelling and observations of droplet growth in clouds A Coals 1, A M Blyth 1, J-L Brenguier 2, A M Gadian 1 and W W Grabowski 3 Understanding the detailed.
Low Pressure Systems vs High Pressure Systems. Let’s Compare Low Pressure Systems (L) High Pressure Systems (H)
Section 1.2 The Causes of Weather
Weather Forecasting Subtitle.
Chapter 38 Weather.
Objective: Determine the humidity and temperature of air masses.
Weather in Atlantic Canada Chapter 3. Condensation Occurs when moist air rises and cools, forming clouds. Air rises because of being warmed from below.
Unit 4 Lesson 5 Notes Answer Key
Unit 4 Lesson 5 Weather Maps and Weather Prediction Copyright © Houghton Mifflin Harcourt Publishing Company.
Chapter 18.  Water vapor  Precipitation  Condensation  Latent heat  Heat is added but there is no temperature change because the heat is instead.
Aim: How do clouds form in the troposphere?. Russell the Boy Scout, describes the characteristics about cumulonimbus clouds but is ignored. How would.
Weather: the present state of the atmosphere and the current conditions Factors that effect the weather: air pressure, wind, temperature, and humidity.
Unit 4 Lesson 5 Weather Maps and Weather Prediction
2/6/12 Page 88 Which of these substances is a liquid form of precipitation? A. hail B. rain C. sleet D. snow.
WEATHER & THE ATMOSPHERE
What is Weather. Weather Meteorology
Chapter 16 Earth Science WEATHER.
Basis of Cloud Formation
Meteorology.
Introduction to Experiment 4: Clouds
Who Wants to be a Millionaire?
Weather in Atlantic Canada
Place these notes into your Meteorology Notebook
Water in the Hydrosphere
Long-Lead Streamflow Forecast for the Columbia River Basin for
Stability and Cloud Development
Do Now!!! What is weather?.
Weather and Climate.
Do Now Predict why weather could be different on the front side of a mountain (windward) than on the back side of the mountain (Leeward). Explain.
Presentation transcript:

Idaho Power Company’s Cloud Seeding Program @ IPC for over 20 years Worked on water resources and physical process projects for those 20 years Lead the cloud seeding group as well as river engineering group Have been involved with cloud seeding from the initial question a number of years ago Shaun Parkinson, PhD, P.E.

What is cloud seeding? The term cloud seeding has been used to describe: Fog suppression (airports) Hail suppression (reduce crop and property damage) Rainfall enhancement (water supply augmentation) Snowpack enhancement (snowpack augmentation) Our focus is snowpack enhancement In particular – IPC does winter orographic cloud seeding

Winter Orographic Cloud Seeding Cloud seeding provides additional ice nuclei that function at warmer temperatures, allowing ice formation to begin sooner. This occurs at temperatures as warm as -5oC (+23°F), though more effectively at -8oC (+17oF) or colder. (The majority of natural ice nuclei become effective between -15°C to -20°C (+5oF to -4oF).). Effectiveness is dependent upon limitation of natural ice nuclei, abundant SLW, and temperatures. . First Ice, not seeded . First Ice, seeding

Silver Iodide Distribution In commercial programs, silver iodide is burned to release silver iodide particles (ice nuclei) of an appropriate size to the atmosphere. Ground generators - Acetone – silver iodide solution is burned in a propane flame. Aircraft - silver iodide is incorporated into a flare, or solution is burned.

Cloud Seeding Programs

Idaho Power’s History with Cloud Seeding At the request of shareholders – began investigating cloud seeding in 1993 Literature review 1993 and 1994 Climatology study 1994-95 Contracted operational program in 1996-97 Planned to perform internal program in 1997-98 Reinstated in Feb 2003. Operational including assessment in fall of 2003 Completed second year of assessment and third year of operations in May 2005. In 2008 started working with HCRC&D and E Idaho Counties to enhance their program In 2010 started working with WWRC&D to evaluate cloud seeding opportunities in western Wyoming.

Idaho Power’s Cloud Seeding Projects Payette Upper Snake in cooperation with E. Idaho - HCRC&D

Manual Cloud Seeding Generator Remote Cloud Seeding Generator Generator Types Burn Head Temperature Probe Ignition Coil Valve Box Satellite Communication Tower Solar Panel Computer Box Nitrogen Solution Tanks Work Platform Batteries Manual Cloud Seeding Generator Propane Remote Cloud Seeding Generator

Aircraft Seeding

Rawinsonde Temperature Relative Humidity Pressure Wind Direction Wind Speed Up to 60,000’

Radiometrics M3000A Microwave Radiometer IPC’s

Target – Control Payette

Benefit Estimation Payette IPC has used 3 approaches to assess benefits in addition to DRI’s assessment: USBR Run-off regression equations Watershed modeling using IPCRFS forecasting model Weather Modeling using WRF

USBR Regression USBR Equations use precipitation and SWE as input to predict runoff at specific locations. Target control analysis indicates precipitation increases ranging from 5% to 16% (average over 6 years of 13%*). Assuming a precipitation increase of 10% from cloud seeding results in an average of approximately 120 KAF of additional April – July runoff at Horseshoe Bend. *dropped highs from dry years. Retaining all years is a 16%.

Streamflow Modeling IPC River Forecast System Additional runoff estimated using IPC’s river forecast system. Model uses mean aerial temperature and precipitation (MAT & MAP) by elevation Two scenarios…with and without cloud seeding Without seeding – adjusted MAP down by amounts indicated by target-control analysis (observed data includes seeding) With seeding – used MAP based on observed data Streamflow increase nearly 200 KAF / year Cost: less than $8.00/AF

Weather Model overview WRF v3.1 Domain: 420 x 300 grid pts 2 km horizontal resolution 60 vertical stretching levels Generator locations: Payette (black) Upper Snake (red) Proposed Wyoming (purple)

4-Year Comparison between average SNOTEL and PRISM observations and WRF Simulations Percent Difference : (model – obs)/obs NOV DEC JAN FEB MAR APR 6-mo. 2001-2002 13.7 -1.1 17.8 12.0 11.4 34.4 13.4 2003-2004 17.4 4.5 3.5 10.3 -3.7 8.2 8.4 2005-2006 -15.1 6.6 20.4 1.9 37.3 39.7 15.1 2007-2008 7.8 5.2 15.0 -1.6 6.1 -24.8 2.7

Upper Snake Potential Using the IPCRFS: Assumes 10% winter precipitation increase (Oct – Mar) Local unregulated flows Average increase in runoff over period ‘49 to ’09 DRAFT Results

Upper Snake Activities HCRC&D In addition to the 25 manual generators, In 2008 Idaho Power installed 3 remote generators, provided meteorological data and operations guidance In 2009 installed 6 additional remote generators (total of 9), meteorological data and operations guidance In 2010 installing 6 additional generators (total of 15), meteorological data and operations guidance 2011 replace old style generators with latest configuration. WWRC&D Installed radiometer, weather balloon, met station in Afton area. Currently working with NCAR on a Phase II feasibility study for a project to target the Salt and Greys River drainages (WRF modeling). With NCAR, modeling study to evaluate: Seeding opportunities Generator siting Aircraft Inversions

Questions?

Downwind Effects Research on the subject has shown there are neutral or positive effects (more precipitation) from a well run program. A poorly run program has the potential to reduce precipitation Snowy Hydro (AU) has conducted a cloud seeding trial since ‘04. Research by the AU Natural Resources Commission has not identified adverse downwind effects. http://www.nrc.nsw.gov.au/Workwedo/Cloudseeding.aspx To put quantities into context… Nature will condense about 20% of the water vapor as moist air rises over a mountain barrier (the remaining 80% remains uncondensed). Winter storms are typically about 30% efficient, meaning 30% of the 20%, or 6% of the total, reaches the ground. If cloud seeding increases precipitation 15%, that amounts to 15% of the 6%, or 0.9% of the total water vapor is the additional amount cloud seeding pulls from the atmosphere.

Silver Toxicity The WMA has issued a statement on toxicity of silver originating from cloud seeding http://weathermodification.org/AGI_toxicity.pdf In summary, “The published scientific literature clearly shows no environmentally harmful effects arising from cloud seeding with silver iodide aerosols have been observed; nor would they be expected to occur. Based on this work, the WMA finds that silver iodide is environmentally safe as it is currently being dispensed during cloud seeding programs.” Research by the AU Natural Resources Commission has not identified any adverse environmental impacts. http://www.nrc.nsw.gov.au/Workwedo/Cloudseeding.aspx

IDEQ Review IDEQ reviewed cloud seeding w.r.t. water and air quality. Water quality - it is unlikely that cloud seeding will cause a detectable increase in silver concentrations in target area or pose a chronic effect to sensitive aquatic organisms. Air quality permit not needed based on screening thresholds. http://www.idwr.idaho.gov/waterboard/WaterPlanning/CAMP/ESPA/WorkingGroups/PDF/WM//2010/02-09-10_MtgPresent.pdf Barry Burnell

Idaho Power’s Cloud Seeding Projects Payette Upper Snake in cooperation with E. Idaho - HCRC&D Salt and Wyoming Ranges