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The Feasibility of Operational Cloud Seeding in the North Platte River Basin Headwaters to increase Mountain Snowfall
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The Feasibility of Operational Cloud Seeding in the North Platte River Basin Headwaters to increase Mountain Snowfall
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Last modified
3/5/2013 4:20:28 PM
Creation date
2/25/2013 4:12:57 PM
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Water Supply Protection
Description
related to the Platte River Endangered Species Partnership (aka Platte River Recovery Implementation Program or PRRIP)
State
WY
CO
Basin
North Platte
Water Division
6
Date
5/1/2000
Author
Jonnie G. Medina, Technical Service Center, Water Resources Services, River Stystems and Meteorology, Denver, CO
Title
The feasibility of Operational Cloud Seeding in the North Platte River Basin Headwaters to Increase Mountain Snowfall
Water Supply Pro - Doc Type
Report/Study
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equipment must test new field equipment and operational procedures on a limited -scale basis. The use of <br />propane release for seeding clouds has never been tested in the high altitude zones of the Headwaters <br />Region. Scaling from an initial deployment of several test propane dispensers to a desired number is <br />considered the proper approach. Prior to deployment of an entire seeding network, answers must be <br />determined regarding seeding mode, targeting and seeding equipment siting for various components of <br />the varying terrain of headwaters barriers. It is recommended that successful operations be achieved in a <br />' limited scale network consisting of two seeding zones before large -scale deployment is pursued. <br />The prototype seeding project studies should involve weather forecasting and cloud modeling. Field data <br />collection should include the monitoring of SLW at propane dispensers and AgI generators (if used), and <br />the measurements of ice crystal in the target areas with simultaneous monitoring of natural crystals, either <br />crosswind of the seeded ice crystal plumes or in established control areas. Some local wind <br />measurements should be made with heated sensors, and some accurate air temperature and dewpoint <br />temperature observations should be obtained at dispenser and crest line elevations. A network of high <br />resolution precipitation gages should be deployed with proper protection from wind effects in selected <br />' forest clearings (Brown and Peck 1962). These gauges will provide relatively accurate high - resolution <br />snow water equivalent observations in seeded and control areas. These measurements should provide the <br />basis for a useful physical evaluation of seeding effectiveness. <br />�J <br />Ll <br />1 <br />1 <br />d <br />1 <br />Because significant electrical power will be needed to operate some of the instrumentation, such as <br />heated wind sensors, it is recommended that a primary prototype testing site be located (via permission <br />and /or cooperative agreement) possibly at the Desert Research Institute's (University of Nevada at Reno) <br />Storm Peak Laboratory, that is equipped with electrical power and is accessible via Steamboat ski lifts <br />and by snowmobiles. The laboratory has shelters for instruments and data collection by technicians. A <br />second prototype site should be. selected and instrumented possibly at a somewhat lesser level, but must <br />also be accessible by 4 -wheel drive and /or oversnow vehicle. Currently, the Storm Peak Laboratory is <br />manned periodically during winters to collect cloud and aerosol data. Observations by aircraft mounted <br />instrumentation are not recommended as a necessary data collection component because aircraft can <br />rarely operate low enough in orographic clouds to provide desired observations. However, any agency <br />willing to supply an instrumented aircraft and personnel to collect data will be encouraged to do so. <br />Because natural snow showers will sometimes mask seeding effects, randomization should be used on <br />some test seeding trials of the design phase. The randomization scheme should be determined after some <br />modeling studies are conducted and the terrain has been surveyed and analyzed. Should the two -year <br />field testing have normal or above seeding opportunities, there may be an opportunity to collect adequate <br />treatment and control samples for a seeding effect statistical assessment on precipitation. Generally, <br />contamination of the control will not be a significant problem with the propane seeding approach because <br />topography will largely control the transport of seeded ice crystal plumes. Only a brief residual seeding <br />effect will occur downwind from the propane dispensers as seeded crystals are transported out of the <br />target area. Propane seeding will not have the long- distance ice nucleation "contamination" that may <br />occur with AgI releases in which nucleation may occur well downwind. However, it may be found that <br />certain zones of the Headwaters Region are best suited for AgI seeding. The seeding design should not <br />eliminate this possibility. <br />An appropriate "buffer zone" of at least 3 miles wide should separate the two prototype study zones. The <br />number of seeding devices per prototype site should be determined after some modeling studies and <br />terrain inspection have taken place. The areas downwind from each seeding equipment zone should have <br />similar instrumentation. Experimental units should be aimed at 1 -3 hours in duration to help minimize <br />natural temporal variations. Delays between experiments must be specified to allow for flushing of <br />previous seeding effects. The test seeding trials should gradually work toward automation that requires <br />13 <br />
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