Cloud Seeding in the Walker River Basin Arlen Huggins Desert Research Institute Scientific basis for wintertime cloud seeding Determining the potential.

Slides:



Advertisements
Similar presentations
THE WATER CYCLE The water cycle — the continuous exchange of water between Earth's surface and atmosphere — is Earth's natural mechanism for recycling.
Advertisements

Water in the Atmosphere
Chapter 7. Global Precipitation Climatology Project (GPCP) Most rain falls near the equator. Notice how dry it is on.
Potential Aerosol Impacts on Orographic Precipitation William R Cotton Dept of Atmospheric Science Colorado State University.
A Winter Season Physical Evaluation of the Effects of Cloud Seeding in the Colorado Mountains William R. Cotton, Ray McAnelly, and Gustavo Carrió Colorado.
Cloud Development and Precipitation
Precipitation Cloud particles are so small that they are easily kept afloat by even the weakest updrafts. This is why most clouds do not produce rain.
The ASCII 2012 campaign: overview and early results AgI Seeding Cloud Impact Investigation Bart Geerts presented by: Xia Chu contributions by: Katja Friedrich,
Cloud Seeding Shawn Trueman, Intern National Weather Service Forecast Office Phoenix, AZ.
Part 2. Water in the Atmosphere Chapter 7 Precipitation Processes.
Idaho Power Company’s Cloud Seeding Program
Earth’s Weather Weather Terms.
Family Homecoming Special Event "Can Climate Engineering Serve as a Complementary Step to Aggressive Mitigation?" Dr. Michael MacCracken, The Climate Institute,
Most collide on forward edge Some collide on backside About a million average sized droplets would be required to produce a raindrop! Terminal velocity:
Numerical Simulations of Snowpack Augmentation for Drought Mitigation Studies in the Colorado Rocky Mountains William R. Cotton, Ray McAnelly, and Gustavo.
Outline Background, climatology & variability Role of snow in the global climate system Indicators of climate change Future projections & implications.
Rain Sleet Snow Hail Types of Precipitation. Precipitation Starts With Different Air Masses Being Pushed Around by Global Winds High pressured air mass.
Chapter 23 Section 3 Handout
Precipitation. Precipitation Formation Requires Requires –condensation nuclei (solid particles) –saturation (air at dew point) Result is temperature dependent.
Chapter 23 Section 3 Review Page 590
Ice Storms. Why Study Ice Storms? Ice accumulation can: –cause extensive power outages –halt air and ground transportation –cause considerable property.
Chapter 7 – Precipitation Processes
Cloud Seeding for Snowfall Enhancement: Concepts, Evidence of Effects and New Evaluation Techniques Arlen W. Huggins Desert Research Institute Reno, Nevada,
HydrometJanuary AMS Short Course on Instrumentation1 HydrometeorologicalMeasurements Melanie A. Wetzel Desert Research Institute University of.
WINTER STORMS By: Hannah Winter Storms Moisture evaporates in the air. Snow falls into warm air and melts into rain. An ice storm is a type of winter.
Water in the Atmosphere 18.1 Humidity and condensation
Remote Sensing of Inflight Icing Conditions Dr. Charles C. Ryerson Cold Regions Research and Engineering Laboratory Engineering Research and Development.
Section 5: Precipitation
Water Cycle Breakout Session Attendees: June Wang, Julie Haggerty, Tammy Weckwerth, Steve Nesbitt, Carlos Welsh, Vivek, Kathy Sharpe, Brad Small Two objectives:
Ground Deicing Update Scott Landolt, Roy Rasmussen and Jenny Black.
 The movement of water through a cycle by phase changes: liquid, gas, and solid water.  Condensation- vapor cools and becomes liquid droplets  Evaporation-
1. Clouds are made up of: A.Liquid water droplets B.Ice Crystals C.Water Vapor D.A combination of liquid water, ice, and water vapor.
Precipitation Chapter 16 Section 5 Pages Chapter 16 Section 5 Pages
Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Section 3 Precipitation Chapter 23 Objectives Identify the four forms.
NASA Snow and Ice Products NASA Remote Sensing Training Geo Latin America and Caribbean Water Cycle capacity Building Workshop Colombia, November 28-December.
Unit 3 Lesson 3 How Do We Measure Weather?
Clouds Identify cloud types from photos
Chapter 9: Weather Factors Section 5: Precipitation clouds.
Water in the Atmosphere Section 3 Section 3: Precipitation Preview Key Ideas Forms of Precipitation Causes of Precipitation Measuring Precipitation Weather.
Chapter 24 Water in the Atmosphere Section 3 Precipitation Notes 24-4.
By Sam Belanger. Precipitation is water in solid or liquid form, that falls from the air to the Earth’s surface There are four main types: Snow, Rain,
Winter Weather Homeroom Read. Warm Up: Define WINTER WEATHER ADVISORIES WINTER STORM WATCH WINTER STORM WARNING FROST/FREEZE WARNING.
Ice in the Atmosphere W+H 6.5; S+P Ch. 17 Start with some terminology –Warm clouds = T > 0 ºC (= K) –Cold clouds = T < 0 ºC Cold clouds may or may.
18.3 Cloud types and Precipitation Clouds are classified on the basis of their form and height Clouds are classified on the basis of their form and height.
Why is our weather the way it is?.  Utah has four distinct seasons.  Summer days are hot, but nights are cooler.  Temperatures vary a lot from the.
Distribution of Liquid Water in Orographic Mixed-Phase Clouds Diana Thatcher Mentor: Linnea Avallone LASP REU 2011.
Northeast Winter C&V Program Roy Rasmussen NCAR Wes Wilson MIT/LL.
AMSR-E Vapor and Cloud Validation Atmospheric Water Vapor –In Situ Data Radiosondes –Calibration differences between different radiosonde manufactures.
Nov. 9 Artificial Modification of Clouds and Precip
Clouds Identify cloud types from photos Recognize and define prefixes and suffixes for cloud types Associate general weather conditions with cloud types.
Chapter 6 – Water Cycle and Weather 4 th Grade – Kristi Goggans Earth Science – Unit B.
High-Resolution Polarimetric Radar Observation of Snow- Generating Cells Karly Reimel May 10, 2016.
Water in the Atmosphere Section 3 Section 3: Precipitation Preview Key Ideas Forms of Precipitation Causes of Precipitation Measuring Precipitation Weather.
IEEE CS 70 th Anniversary Student Challenge Project Proposal entitled “ROBOT CONTROLLING WEATHER ” Submitted By: S.SEETHALAKSHMI E.VANISRI M.PRIYADHARSHINI.
Two Frigid 2014 Snow Storms – A Look at Snow to Liquid Ratios
Winter Storms By: Taylor and Maia.
Winter Storms By: Nolan and Tyler.
Structure of the general part
Class #25: Friday, March 6 Clouds, fronts, precipitation processes, upper-level waves, and the extratropical cyclone Class #25: Friday, March 6, 2009.
Climate change and adaptation planning on the Los Angeles Aqueduct
Precipitation Notes.
How do we measure Weather?
Group interests RICO data required
Water in the Hydrosphere
Precipitation Notes.
Precipitation Notes.
Winter Storms By: Taylor and Maia.
Forests, water & research in the Sierra Nevada
PRECIPITATION & WEATHER MODIFICATION
Group interests RICO data in support of studies
Presentation transcript:

Cloud Seeding in the Walker River Basin Arlen Huggins Desert Research Institute Scientific basis for wintertime cloud seeding Determining the potential for increased snowfall Seeding methods and materials Detecting the impact of cloud seeding Current activities in the Walker Basin Future directions

Cloud Seeding: A Brief History Cold Box Experiments: 1940’s Operational Projects: 1950’s to present Research Projects –Field Studies (1960’s ’s) –Statistical Experiments (1960’s and 1970’s) –Proof of Concept Experiments (1980’s- 1990’s) –New Evaluation Techniques (1980’s - ?)

Current Wintertime Seeding Projects

Concepts for Cold Cloud Seeding Winter clouds contain some water that has not been converted to ice crystals and snow Amount of supercooled liquid determines seeding potential –Ice forming particles (nuclei) required to produce ice –Natural ice “nuclei” are less numerous at warmer temperatures Artificial seeding either adds more ice nuclei or reduces the temperature so ice can form Seeded ice crystals grow and fall as snow

Sizes of Cloud Water and Ice Particles 1 mm

The Potential for Cloud Seeding Storm Frequency and Duration The Amount of Supercooled Liquid Water in a Storm Targeting Considerations

Seasonal Precipitation

Supercooled Liquid Water Remotely Sensed Microwave Radiometer Measures Cloud Liquid Depth and Water Vapor Depth

Supercooled Liquid Water: Integrated Effect

Conceptual Model for Cloud Seeding Seeding Generator

Modeling to Evaluate Generator Locations Seeding Simulation: Time = /14/94

Modeling: Plume after 30 minutes

Modeling: Plume after 1.5 hours

Modeling: Plume after 7 hours

Aircraft Cloud Seeding AgI Solution Burners AgI Flares in Aircraft Flare Rack Dry Ice from an Aircraft Hopper Nighttime Flare Test

Ground-based Cloud Seeding DRI Remotely-controlled cloud seeding generators. Left: Mobile Unit Above: Semi-permanent Unit

Generator Ice Crystal Production

Detecting the Effects of Cloud Seeding 1. Statistical Methods California 1969:AgI Seeding0.1 mm/h Colorado 1971:AgI Seeding mm/h Montana 1986:AgI Seeding0.3 mm/h

Detecting the Effects of Cloud Seeding 2. Direct Observation Washington 1975:AgI/CO mm/h Nevada 1987: CO mm/h Montana 1988:AgI mm/h Colorado 1988:AgI0.1 mm/h California 1988:AgI/CO mm/h Utah 1994:AgI mm/h 0.25 mm/h = 0.01 in/hr Over 35 sq. miles: Seeding effect = 18.7 acre-feet/hour For 8 storm hours = acre-feet For 20 storms = 2992 acre-feet

Seeding Effects: Detection Methods Aircraft or Vehicle-mounted Particle Probes

Seeding Effects: Detection Methods Short-wavelength Radar Snow profiling for chemical analysis

Seeding Effects: Some Results A 1-hour AgI Seeding Experiment in Utah Seeded Period

Seeding Effects: The Aerosol Plume

Seeding Effects: A Radar Plume

Seeding Effects: Precipitation Data

Walker Basin Seeding Program 6 ground-based generators for generators by Aircraft Seeding over Sierra Nevada

Future Directions Detailed Sub-basin Evaluation of Seeding Opportunities and Impacts –SLW climatology from radiometer data –Snow Core and Chemical Analysis of Snowpack Modeling Study to Evaluate Future Ground Generator Locations –Emphasis on targeting high SLW regions –Generator network expansion Observation/Modeling Study to Evaluate Runoff Impacts