Graduate Student

Mery Apple 

Applicability of the HSPF Model for two Contasting Hawaii Watersheds

Project Objectives

The main objective of this research is to test applicability of the HSPF model for Hawaii watersheds. Hypotheses to be tested are (1) HSPF is applicable to Hawaiian watersheds for predicting annual and monthly streamflow and sediment; and (2) the precision associated with simulating daily streamflow and sediment is questionable. The model will be tested on two contrasting watersheds.  The specific objectives include:

·        Calibrate and validate the model using different datasets

·        Conduct a sensitivity analysis

·        Compare and analyze model results

·        Evaluate applicability of underlying equations and assumptions of the model

·        Identify strengths and limitation of the model

The results of this study will identify both the advantages and the deficiencies of applying HSPF and contribute to a better understanding of sedimentation in Hawaiian watersheds. The outcome of this study will also assist in assessing problems of Hawaii watersheds, developing remediation strategies, and progressing the mythologies and procedures for developing TMDLs and other regulatory concerns for the State of Hawaii.

 

Study Sites

      Two watersheds were selected for this research, Kaneohe on the island of Oahu and Kawela on the island of Molokai.  The two watersheds were selected based on their contrasting features considered include topology, climate, and land use. 

Kaneohe, Oahu

The Kaneohe watershed is located on the windward section of the island of Oahu, extending from the Koolau Mountain Range to the Pacific Ocean.  It is approximately 14.7 km2. The watershed population was greater than 15,000 people in the Census 2000.  The upper portion of the watershed consists of various land uses including the Pali Golf Course, Koolau Golf Course, a banana plantation, the Hoomaluhia Botanical Gardens, and part of the Kaneohe Forest Reserve, including sections of three major highways.  The lower portion of the watershed is primary residential and commercial urban land use.  The Hoomaluhia Reservoir is located in the central part of the watershed (Burr 2003).  Average annual precipitation varies from 1000 millimeter to 2000 millimeters (Hawaii Institute of Marine Biology 2007).   

Kawela, Molokai

The Kawela watershed is located on the southeast potion of the island of Molokai, extending from the East Molokai Mountains to the Pacific Ocean.  It is approximately 13.81 km2.  The watershed population was reported as 249 people in the Census 2000 (Hawaii Institute of Marine Biology 2007).  The land use is Evergreen Forest land in the upper and lower portions of the watershed.  The center portion of the watershed is rangeland.  Approximately 90% of the watershed was formerly owned by Molokai Ranch (USEPA 2004).  The two of the adjacent watersheds, Kamalo and Kamakou, are part of the East Molokai Watershed Partnership Conservation Project Sites (Nature Conservancy of Hawaii 2003).  Kawela watershed is part of the Hawaii’s Local Action Strategy to Address Land-Based Pollution Threats to Coral Reefs program conducted by the EPA and several other State and Federal agencies.  This project examines ways of reducing land based pollution from coastal watersheds in an effort to decrease the degradation of coral reef systems.  Many fencing projects have been conducted in Kawela watershed to protect the area from feral undulates.  In addition, invasive weed control projects have been implemented.  Average annual precipitation varies from 400 millimeter to 3000 millimeters (Hawaii Institute of Marine Biology 2007). 

Watershed Comparison

      These two watersheds have very different climate, topology, and land use.  Kawela has a greater spatial distribution of rainfall over the entire watershed, where as Kaneohe has greater rainfall even in low-lying areas.  Kawela’s landscape consists of deep valleys which were formed by perennial streams.  For Kaneohe, the watershed boundary is composed of extremely steep cliff, with more moderate slopes throughout the rest of the watershed.  The most significant contrast is the land use.  Kawela consists primarily of forest and rangeland, where as Kaneohe has a mix of many land uses, yet contains a significant portion of urban areas. 






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