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Last modified
7/28/2009 2:39:27 PM
Creation date
4/23/2008 11:57:07 AM
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Template:
Weather Modification
Project Name
Park Range Atmospheric Water Resources Program
Title
Park Range Atmospheric Water Resources Program - Phase I
Date
1/1/1967
Weather Modification - Doc Type
Report
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<br />CONTENTS <br /> <br />IX <br /> <br />Figures-Continued <br /> <br />Number Page <br />43g. Plume Dimensions and Pibal <br />Soundings for 8 April 1965 37 <br />44. ZnS Concentrations in Snowmelt <br />Samples after Diffusion Runs of <br />25 March and 9 April 1965 .., 38 <br />45. 700 mb. Wind Direction Occur- <br />rence for Storm Period 1 <br />February to 1 May 1965 ...... 39 <br />46. Relation of Storm Precipitation <br />and Wind Group 2700-3000 .. 40 <br />47a-47c. Freezing Nuclei Count as Meas- <br />ured at Valley View Lodge. . . . 41 <br />48. Snowcrystal Replica from <br />28 January 1965 Storm. . . . . .., 43 <br />49. Skyfire Nuclei Generator Calibra- <br />tion Curve. .... ... .. .. . ... . . 43 <br />50. Background ZnS Concentrations <br />over Target Area-7 June <br /> <br />1965 ....................... 44 <br /> <br />51. Snowcourse Data Normalized <br />Water Content Values, 15' <br />January 1965 to 27 April 1965. . 46 <br />52. Average and Error Band of Snow- <br />course Data Normalized to <br />Buffalo Pass ................ 47 <br />53. Normalized Water Content <br />Values as a Function of Station <br />Altitude .................... 48 <br />54. Station Pairs Used in Phase I for <br />Computation of Coherence and <br />Interstation Precipitation <br /> <br />Ratios ..................... 49 <br />55. Typical Unity Energy Power <br />Spectrum ................... 50 <br />56. Maximum Record Length at Any <br />One Station vs. Analysis Period 50 <br />57a-57k. P'(f)f2 X 102 and Coherence by <br />700 mb. (millibar) Wind Group <br />(9-10 March 1965) ........... 51 <br />58a-58m. P'(f)f2 X 102 and Coherence by <br />700 mb. Wind Group (5 April <br /> <br />1965) .. . . . . . . . . . . . . . . . . . . . . 54 <br />59a. Original Steamboat Spectra-18 <br />March, 5 Apri11965 . .. ... ... . 58 <br />59b. Effect of Wind Speed Correction <br />on Spectra Comparison ...... 58 <br />59c. Original Long Lake Spectra- <br />18 March, 5 April 1965 ....... 59 <br /> <br />Number Page <br />59d. Effect of Wind Speed Correction <br />on Spectra Comparison ...... 59 <br />5ge. Original Steamboat-Long Lake' <br />Coherences-18 March, <br />5 April 1965 ................ 59 <br />59f. Effect of Wind Speed Correction <br />on Coherence Comparison.... 59 <br />60a. Contribution of Precipitation- <br />rate Intervals to Total Storm <br />Precipitation-Mt. Harris, 9-10 <br />March 1965 ................. 60 <br />60b. Contribution of Precipitation- <br />rate Intervals to Total <br />Storm Precipitation-Steamboat <br />Springs, 9-10 March 1965. . . . . 60 <br />60c. Contribution of Precipitation- <br />rate Intervals to Total Storm <br />Precipitation-Buffalo Pass, <br />9-10 March 1965 .. ...... .... 60 <br />60d. Contribution of Precipitation-rate <br />Intervals to Total Storm Pre- <br />cipitation-Base Camp, 9-10 <br />March 1965 ................ 60 <br />60e. Contribution of Precipitation- <br />rate Intervals to Total Storm <br />Precipitation-Buffalo Pass, <br />5 April f965 ................ 61 <br />60f. Contribution of Precipitation- <br />rate Intervals to Total Storm <br />Precipitation-Base Camp, 5 <br />April 1965 .................. 61 <br />60g. Contribution of Precipitation- <br />rate Intervals to Total <br />Storm Precipitation-Steam- <br />boat Springs, 5 April 1965. . . . . 61 <br />60h. Contribution of Precipitation- <br />rate Intervals to Total Storm <br />Precipitation-Mt. Harris, <br />5 April 1965 ................ 61 <br />61. Spectrum of all 2700-3000 Wind <br />Group Storms-Base Camp. . . . 62 <br />62. Spectrum of all Buffalo Pass <br /> <br />Storms ..................... 62 <br /> <br />63. Spectrum of Base Camp-same-as- <br />Buffalo Pass Storms .......... 62 <br />64. Base Camp 2700-3000 Storm <br />Spectrum With and Without <br />
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