H31G-1506
Quantifying effects of humans and climate on groundwater resources through modeling of volcanic-rock aquifers of Hawaii
Wednesday, 16 December 2015
Poster Hall (Moscone South)
Kolja Rotzoll, University of Hawaii, Water Resources Research Center, Honolulu, HI, United States, Scot K Izuka, USGS Pacific Islands Water Science, Honolulu, HI, United States, Tracy Nishikawa, USGS California Water Science Center San Diego, San Diego, CA, United States, Michael N Fienen, USGS Wisconsin Water Science Center, Middleton, WI, United States and Aly I El-Kadi, University of Hawaii at Manoa, Honolulu, HI, United States
Abstract:
The volcanic-rock aquifers of Kauai, Oahu, and Maui are heavily developed, leading to concerns related to the effects of groundwater withdrawals on saltwater intrusion and streamflow. A numerical modeling analysis using the most recently available data (e.g., information on recharge, withdrawals, hydrogeologic framework, and conceptual models of groundwater flow) will substantially advance current understanding of groundwater flow and provide insight into the effects of human activity and climate change on Hawaii’s water resources. Three island-wide groundwater-flow models were constructed using MODFLOW 2005 coupled with the Seawater-Intrusion Package (SWI2), which simulates the transition between saltwater and freshwater in the aquifer as a sharp interface. This approach allowed relatively fast model run times without ignoring the freshwater-saltwater system at the regional scale. Model construction (FloPy3), automated-parameter estimation (PEST), and analysis of results were streamlined using Python scripts. Model simulations included pre-development (1870) and current (average of 2001-10) scenarios for each island. Additionally, scenarios for future withdrawals and climate change were simulated for Oahu. We present our streamlined approach and preliminary results showing estimated effects of human activity on the groundwater resource by quantifying decline in water levels, reduction in stream base flow, and rise of the freshwater-saltwater interface.