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Spatial precipitation trends and effects of climate change on the Hawai'ian Hualalai aquifer

dc.contributor.authorHendricks, Alyssa Danielle, author
dc.contributor.authorFassnacht, Steven, advisor
dc.contributor.authorLaituri, Melinda, committee member
dc.contributor.authorArabi, Mazdak, committee member
dc.date.accessioned2015-08-27T03:57:02Z
dc.date.available2015-08-27T03:57:02Z
dc.date.issued2015
dc.description.abstractWhile trends in temperature are well studied and understood spatially and temporally at a multitude of scales, trends in precipitation are less understood. As the predominant source of groundwater recharge in Western Hawai'i, precipitation plays a vital role in maintaining tourism and industry throughout the Kona Region. Kaloko-Honokohau National Historical Park was established in 1978 to perpetuate and maintain traditional native Hawai'ian culture and the surrounding ecosystem, which is dependent on freshwater from the surrounding Hualalai Aquifer. Precipitation increases with elevation from the coast to approximately 1500 meters up the slope of Hualalai Volcano and then decreases to approximately 2000 meters. Western Hawai'i has a dense rain gauge network and changes in precipitation in the last several decades have been observed, though the rate sand significance of change is unclear. This study introduces a new method of integrated spatial analysis aimed at representing spatial trends in more detail. Using the Rainfall Atlas of Hawai'i, produced by the University of Hawai'i at Manoa, spatial trends from 1978-2007 were studied by annually adjusting the 30-year climate normal and calculating residuals between adjusted and observed precipitation. The Mann-Kendall and Sen's Slope statistical tests were used spatially to determine the rate and significance of change. This method was then compared with spatial interpolation by inverse distance weighting (IDW) and ordinary kriging to assess the differences in methods. Results from the integrated spatial analysis show an annual decrease of -8.42 x 10⁶ m³/year across the entire study area and a decrease of -4.62 x 10⁶ m³/year when only significant areas are considered. This can be compared with -10.8 x 10⁶ m³/year total and -0.64 x 10⁶ m³/year in significant areas from IDW and -8.41 x 10⁶ m³/year and -1.31 x 10⁶ m³/year respectively from ordinary kriging. On a monthly basis, both the integrated spatial analysis and IDW yield similar trends regarding an increase or decrease in the net volume entering the aquifer, however IDW underestimates the overall magnitude. The introduced integrated spatial analysis method provides an improved assessment of spatial trends that, while not limited to precipitation, can assist in broadening the limited knowledge of spatial precipitation trends across the globe.
dc.format.mediumborn digital
dc.format.mediummasters theses
dc.identifierHendricks_colostate_0053N_12875.pdf
dc.identifier.urihttp://hdl.handle.net/10217/166915
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relation.ispartof2000-2019
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subjectHawaii
dc.subjectwater resources
dc.subjectprecipitation
dc.subjectclimate change
dc.titleSpatial precipitation trends and effects of climate change on the Hawai'ian Hualalai aquifer
dc.typeText
dcterms.rights.dplaThis Item is protected by copyright and/or related rights (https://rightsstatements.org/vocab/InC/1.0/). You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
thesis.degree.disciplineEcosystem Science and Sustainability
thesis.degree.grantorColorado State University
thesis.degree.levelMasters
thesis.degree.nameMaster of Science (M.S.)

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