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Sea Level Rise in West Hawai’i – (Anchialine Pools)

October 29, 2014
Menacing wave

A relatively small amount of sea level rise can make a huge difference. Photo – S. Lee

Global sea level will rise between 0.2 m and 1.9 m by 2100 according to the Intergovernmental Panel on Climate Change (IPCC). Sea level rise is caused by a combination of processes including the melting of polar ice caps and glaciers, thermal expansion of ocean water, mining of groundwater aquifers, and, in places like Hawaii Island, subsidence of land masses (the island is slowly sinking). Estimates of sea level rise vary depending on the trajectory of global greenhouse gas emissions, and are based on different scenarios established by the IPCC. The more extreme values of sea level rise (1.9 m) reflect a future emissions scenario in which global population growth is coupled with continued intensive fossil fuel use. In all scenarios, rates of sea level rise are accelerating and will continue to accelerate in the future.

Geospatial predictions of coastal change under sea level rise typically pair current coastal elevation data and future sea level scenarios. These models tend to be conservative because they often do not incorporate future tectonic uplift or subsidence, high wave events, or shoreline erosion which will exacerbate coastal inundation and change, especially during large episodic events (e.g. storms or tsunamis). In some coastal areas, groundwater floating on top of denser, more saline water, may also exacerbate flooding as sea levels rise. In all sea level rise models, predictions should be viewed with the understanding that there is considerable regional and local uncertainty in the future propagation of storms and waves, vertical land movement, and variation in basin wide processes such as the El Niño Southern Oscillation and the Pacific Decadal Oscillation.PUHO Tsunami Damage

Parks at Risk

Coastal erosion, tsunamis, and coastal inundation due to waves and sea level rise will have serious impacts on the future shorelines of all Pacific island national parks. Cultural and natural resources are already being altered by sea level rise. Incorporating detailed elevation data and sea level rise predictions in the early stages of resource protection planning will aid in long term management of park trails, resources, and infrastructure, and could lessen negative long-term impacts. Furthermore, scenario planning for habitat migration due to rising ocean levels and retreating groundwater is essential so that the predicted future locations of important habitats, like potentially nascent anchialine pools, can be factored in. This is one of the major components of the National Park Service’s Natural Resource Adaptation Strategy.

Predicting changes to anchialine pools

Anchialine pools are brackish coastal ecosystems without a surface connection to the ocean, where groundwater and ocean water (from underground) mix. In Hawai‘i, groundwater flows through these pools and out to wetlands and coral reefs making them valuable indicators of broad-scale groundwater recharge and contamination. The NPS Inventory & Monitoring Program takes regular measurements of the water quality and overall health of park pools, which are found no other place in the United States outside of Hawaii. Hawaiian anchialine pools are tidally influenced, range in size from less than 1 m² to over 3000 m² and support diverse endemic plants and animals, including seven species listed as Candidate Threatened or Endangered Species. Anchialine pool shrimp and mollusk species disperse throughout the ocean as larvae and through groundwater as larvae or adults.

3 models of sea level rise

Sea Level Rise Scenarios

A total of 193 anchialine pools have been mapped at Kaloko-Honokōhau National Historical Park, 15 at Puuhonua o Hōnaunau National Historical Park (PUHO), and 16 at Hawaii Volcanoes National Park. When the pool locations are overlain on maps depicting inundation scenarios, the extent of inundation can be calculated. At the 0.5 m sea level rise scenario at all three parks, current pools become larger but they are not generally inundated or connected overland to the ocean. In PUHO at a 1 m scenario, 50% of the pools are inundated and become connected to the ocean. For the 1.9 m scenario at the extreme tide, only a few pools continue to be isolated while 71% become inundated at PUHO.

Incorporating detailed elevation data and sea level rise predictions in coastal planning should aid in long-term management of both developed and natural areas. In particular, this project aims to identify key areas to preserve for maintaining environmental and cultural integrity in the future. For example, while some features such as individual anchialine pools will be inundated, anchialine pool, fishpond and wetland habitats will emerge or shift in the landscape, essentially fostering new habitats. Protecting future potential habitat from development will conserve valuable land, and will reduce the need to repair or relocate infrastructure placed in these areas.

The goal of this project is to share sea level rise inundation scenarios with NPS staff as well as public and private partners so that everyone can plan for the future condition of Hawai‘i’s shorelines.

This summary is just the tip of the melting iceberg. For a much more in-depth report, read the source article by Lisa Marrack and Patrick O’Grady from the University of California, Berkley: http://manoa.hawaii.edu/hpicesu/techr/188/v188.pdf

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