My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WMOD00439
CWCB
>
Weather Modification
>
DayForward
>
WMOD00439
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
7/28/2009 2:39:16 PM
Creation date
4/18/2008 10:02:21 AM
Metadata
Fields
Template:
Weather Modification
Title
HIPLEX-1: Experimental Design and Response Variables
Date
4/4/1984
Weather Modification - Doc Type
Report
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
16
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br />APRIL 1984 <br /> <br />S MIT. H ETA L. <br /> <br />501 <br /> <br />the region through which dry ice is dropped. A further <br />significant advantage of dry-ice seeding is the absence <br />of contamination effects and of even perceived envi- <br />ronmental effects. <br />The seeding aircraft carried two identical dry-ice <br />dispensers to provide a no-seed treatment (placebo) <br />mode that was indistinguishable to the aircraft crew <br />from the seed treatment (Dennis et al., 1980). Both <br />dispensers were loaded for takeoff, but a person who <br />took no further part in the operations disabled one <br />dispenser prior to each flight. A double blind procedure <br />was employed in which that person disabled one dis- <br />penser according to an unrestricted random selection, <br />but had no knowledge of which dispenser would be <br />activated in flight. Once the aircrews selected an ex- <br />perimental unit, separate instructions indicating which <br />dispenser to activate were relayed from the HIPLEX <br />radar site to the crew of the seeding aircraft. These <br />instructions appeared to the field participants to be a <br />random sequence, but were keyed to a master restricted <br />randomization sequence indicating whether or not the <br />experimental unit was to be seeded. None of the field <br />participants knew which dispenser was disabled, and <br />activating either one produced the same noises and <br />other indications in the aircraft. Activating the disabled <br />dispenser produced a no-seed case, while activating <br />the other one produced a seed case. The actual release <br />of dry ice was checked by examining data recorded <br />from temperature probes in the dispenser exit chutes <br />(these temperature data were not available in real time). <br />The procedure was carefully constructed in order <br />to avoid bias arising from knowledge of the treatment <br />becoming available to any of the field participants dur- <br />ing the operation. Thus the dispenser instructions were <br />transmitted in code so that successive experimental <br />units could be treated during the same flight without <br />the crew of the cloud physics aircraft (who may have <br />obtained indications of possible seeding from the ice <br />crystal concentrations observed in the test case clouds) <br />knowing which treatment was applied. A statistician <br />regularly monitored the execution of these procedures <br />to assure they were followed. <br />The restricted randomization procedure for se- <br />quentially allocating seeded and nonseeded treatments <br />to the experimental units was designed to maintain a <br />reasonably close sequential balance. No individual <br />should have been able to predict the next treatment, <br />at a rate better than chance, even if the entire history <br />of previous treatment was known. Randomization for <br />the first HIPLEX-I season (1979) was carried out by <br />pairs of test cases within each cloud category, using a <br />procedure quite similar to that discussed in the fol- <br />lowing paragraph. The major difference was that a <br />single block size of two experimental units was em- <br />ployed for the 1979 randomization so that the first <br />step in'the procedure was unnecessary. However, it <br />became evident that some project participants were <br />able to diagnose this procedure and guess (with better <br /> <br />I" <br /> <br />than chance success) whether the next case would be <br />seeded or not. To guard against any bias that might <br />have been introduced, the randomization was changed <br />for 1980. <br />A list of randomized allocations was constructed to <br />accomplish the goals of both balance and unpredict- <br />ability in the following manner. (Although this method <br />yielded an equal proportion of seeded and nonseeded <br />experimental units, a simple modification would yield <br />any desired proportion.) The first of two steps involved <br />constructing a sequential list of two block sizes; block <br />sizes of four and six experimental units were used in <br />1980. This first step was based on an unrestricted ran- <br />dom selection with equal probability for selecting either <br />block size. The second step then involved a restricted <br />random assignment of either seed or no-seed labels to <br />experimental units within a block, so that exactly half <br />of the units in each block received a seed label. For <br />example, each of the 20 possible permutations in- <br />volving the occurrence of three seeded and three non- <br />seeded experimental units in a block of size six had <br />an equal chance of being selected. Thus, the random- <br />ization sequence was pieced together from an unre- <br />stricted random arrangement of blocks of different <br />lengths, with random selection from the restricted set <br />of permutations of seed and no-seed treatments within <br />each block. A separate master randomization sequence <br />was prepared for each class of clouds. <br /> <br />5. Physical hypothesis and definition of response vari- . <br />abies <br /> <br />The exploratory studies prior to the development <br />of the specific design for HIPLEX -I led to the eluci- <br />dation of a detailed physical hypothesis regarding the <br />expected effects of seeding the Class A clouds with dry <br />ice (Table 2). Calculations using the observed concen- <br />trations of supercooled water suggested that any dy- <br />namic effects of seeding would be negligible in these <br />convective clouds, regardless of the .seeding rate. <br />Therefore the hypothesis as developed concerned only <br />the microphysical effects of seeding. Thus the objective <br />of the seeding was to increase the ice-crystal concen- <br />trations in the supercooled regions of the clouds, in <br />an effort to accelerate the formation of precipitation- <br />sized particles. To quote from the Dillon workshop <br />report (Bureau of Reclamation, 1977): <br /> <br />Because the clouds often begin to decay in the upper regions <br />. . . before precipitation develops through the cloud base, <br />the lifetime of the cloud provides a limitation on the pre- <br />cipitation development and an accelerated process should <br />have a significant advantage . . . the process should be <br />more efficient and should convert cloud water to precip- <br />itation that normally would simply evaporate as the cloud <br />decayed. <br /> <br />Thus the essential underlying concept was that clouds <br />which rain earlier should have a higher overall pre- <br />cipitation efficiency. The seeding was expected to in- <br />
The URL can be used to link to this page
Your browser does not support the video tag.