Update on Wintertime Snowfall Augmentation in the Western U. S.

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Update on Wintertime Snowfall Augmentation in the Western U. S. NWRA Annual Meeting Emerging Water Augmentation Strategies 7 March 2012 Arlen Huggins Associate Research Scientist Division of Atmospheric Sciences Desert Research Institute Reno, Nevada

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Update on Wintertime Snowfall Augmentation in the Western U. S. NWRA Annual Meeting Emerging Water Augmentation Strategies 7 March 2012. Arlen Huggins Associate Research Scientist Division of Atmospheric Sciences Desert Research Institute Reno, Nevada. - PowerPoint PPT Presentation

Transcript of Update on Wintertime Snowfall Augmentation in the Western U. S.

Page 1: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

Update on Wintertime Snowfall Augmentationin the Western U. S.

NWRA Annual MeetingEmerging Water Augmentation

Strategies7 March 2012

Arlen HugginsAssociate Research ScientistDivision of Atmospheric SciencesDesert Research InstituteReno, Nevada

Page 2: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

Winter Cloud Seeding for Snow/Water Augmentation

• Conceptual model for winter cloud seeding• Current research activities– Randomized experiments– Physical studies– Hydrologic modeling

• Operational projects in the western U.S.• Upper Colorado River Basin Projects– Colorado, Utah, and Wyoming– Upper and Lower Basin interaction

• Summary of snow augmentation status

Page 3: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

Ground-based seeding with silver iodide

-10C

-5C

Conceptual Diagram of Orographic Cloud Seeding

Page 4: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

Recent Research• Australian Snowy Mountain Project– Funded by Australian government and conducted

by Snowy Hydro– 5-year study with randomized seeding of a single

target– Published results showed a statistically significant

14% increase in target precipitation for “seeded” events

• U. of Wyoming airborne radar study– Radar signal increase noted during seeding

periods– Radar signal increase corresponds to a significant

precipitation rate increase

Page 5: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

Recent Research• WY Weather Modification Pilot Project

– Dual-target experiment: one target randomly seeded when cloud conditions are similar over both targets – 4-hour experimental units (EUs)

– 121 EUs to date; requesting funding for an additional two years – funded by state of WY

– Statistical evaluation of paired seed vs. no-seed precipitation values – 200+ EUs desired

– Targeting and environmental assessment using trace chemistry techniques

– Unique use of atmospheric modeling for forecasting and evaluation of seeding events

– Hydrologic modeling to assess impact of seeding on streamflow in the North Platte RB

• U. of WY airborne radar study being repeated– NSF funding (~$1M budget) with more ground based

instrumentation– Attempting to verify earlier findings

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UW Cloud Radar • 3 mm (95 GHz, W-band), dual-polarization• pulse width: 250-500 ns• max range: 3-10 km• volume resolution @ 3 km range: < 40 m• minimum detectable signal (@ 1 km): ~-30 dBZ• Cloud droplets are much smaller than ice crystals, thus

in a mixed-phase cloud, reflectivity is dominated by ice crystals.

UW Cloud Lidar • non-coherent eyesafe backscatter lidar• up & down (down only for 4 out of 7 flights)• backscatter power & depolarization ratio• attenuated by cloud layers• lidar & radar can be combined to estimate cloud

properties

Page 7: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

WWMPP model output of seeding plume trajectories, winds and cloud water content

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Page 9: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

Plume of ice crystals

Weather stationcontrols dispenser

Seeding materials & delivery methods

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Research on Wintertime Cloud Seeding in Mountainous Terrain

Has verified all the links in the chain of the cloud seeding conceptual model

Has verified ice crystal and precipitation enhancement through physical observations

Has shown evidence of precipitation enhancement through statistical evaluations

Has revealed situations when cloud seeding is ineffective Does not have all the answers to every meteorological

situation where cloud seeding is applied

Page 11: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

Operational Cloud Seeding Projects

Page 12: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

Nevada Cloud Seeding Projects Tahoe funded by TMWA and

WRWC Walker Basin funded by BOR

(Desert Terminal Lakes Project) NE Nevada funded by SNWA

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Utah Projects

Cost share between state and local water groups

Cost ~ $370K

Est. snow water increase> 150 AF

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Colorado Projects in WY2011 – Local Funding plus CWCB/LCRB grants

Page 15: Update on Wintertime  Snowfall  Augmentation in the Western U. S.

Areas with snowfall augmentation

potential in the UCRB

1967-1968 Runoff Augmentation Estimates

10% increase1.3 – 1.9 MAF

Hunter (USBR, 2005)2-year SNODAS w/+10%

0.6 – 1.1 MAF

Griffith/Solak (NAWC, 2006)NWS Runoff Model

5-15% increase0.6 – 1.6 MAF

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Collaboration between Upper and Lower CRB States in Snow Augmentation Projects

Cooperative agreement between (CO, UT and WY) and (AZ, CA and NV) – in place since 2006

LCRB funding to: Extend operations in existing projects in UT & CO Add new equipment (seeding and observing) in UT & CO Add additional research equipment (WY) Apply modeling, physical evaluations, etc. to ongoing

projects

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Summary of Water Augmentation by Wintertime Cloud Seeding

A reasonably healthy research component Steady number of operational projects

Funded mainly by state, regional and local water agencies + power companies

Augmentation strategy used for over 50 years Project evaluations indicate benefits justify costs Operations being enhanced by interstate/basin

cooperative agreements Instrumentation and modeling advances have improved

operational efficiency – room for further improvement Hydrologic modeling used more to assess water augmentation

aspect and its economic, political and environmental benefits