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Further analysis of a snowfall enhancement project in the Snowy Mountains of Australia

The first phase of the Snowy Precipitation Enhancement Research Project (SPERP-1) was a confirmatory experiment on winter orographic cloud seeding (Manton et al., 2011). Analysis of the data (Manton and Warren, 2011) found that a statistically significant impact of seeding could be obtained by remov...

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Bibliographic Details
Published in:Atmospheric research 2017-09, Vol.193, p.192-203
Main Authors: Manton, Michael J., Peace, Andrew D., Kemsley, Karen, Kenyon, Suzanne, Speirs, Johanna C., Warren, Loredana, Denholm, John
Format: Article
Language:English
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Summary:The first phase of the Snowy Precipitation Enhancement Research Project (SPERP-1) was a confirmatory experiment on winter orographic cloud seeding (Manton et al., 2011). Analysis of the data (Manton and Warren, 2011) found that a statistically significant impact of seeding could be obtained by removing any 5-hour experimental units (EUs) for which the amount of released seeding material was below a specified minimum. Analysis of the SPERP-1 data is extended in the present work by first considering the uncertainties in the measurement of precipitation and in the methodology. It is found that the estimation of the natural precipitation in the target area, based solely on the precipitation in the designated control area, is a significant source of uncertainty. A systematic search for optimal predictors shows that both the Froude number of the low-level flow across the mountains and the control precipitation should be used to estimate the natural precipitation. Applying the optimal predictors for the natural precipitation, statistically significant impacts are found using all EUs. This approach also supports a novel analysis of the sensitivity of seeding impacts to environmental variables, such as wind speed and cloud top temperature. The spatial distribution of seeding impact across the target is investigated. Building on the results of SPERP-1, phase 2 of the experiment (SPERP-2) ran from 2010 to 2013 with the target area extended to the north along the mountain ridges. Using the revised methodology, the seeding impacts in SPERP-2 are found to be consistent with those in SPERP-1, provided that the natural precipitation is estimated accurately. •Accurate estimation of natural precipitation is important for accurate estimation of cloud seeding impact.•Sensitivity of cloud seeding impact to external factors identified•Spatial variability of cloud seeding impact identified•Consistent cloud seeding impacts found over two independent experiments
ISSN:0169-8095
1873-2895
DOI:10.1016/j.atmosres.2017.04.011