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2019-09-25 Meeting Minutes (EMC)
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2019-09-25 Meeting Minutes (EMC)
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<br /> Dr. Romine introduced himself. He is with the University of Hawaiʻi Sea Grant College <br />Program and is a coastal geologist by training and background. He works out of UH-Mānoa and <br />has worked on coastal processes, beach erosion, and human impacts on the shoreline. He <br />works closely with the Department of Land and Natural Resources and actually worked there <br />for six years. At Mānoa his focus is on longer range projects, such as climate adaptation <br />initiatives, and he is involved with the Climate Change Mitigation and Adaptation Commission. <br /> <br /> Dr. Romine did a slide presentation entitled “Sea Level Rise Observations and Outlook <br />for Hawaiʻi Island.” A few of the highlights: <br /> <br />• The sea level at Hilo Bay has been increasing roughly 3 mm per year, which comes <br />to about 12 inches over a century. <br />• The rate of global mean sea level rise is increasing and has roughly doubled from <br />.6 mm per year in the early part of the century to 3.2 mm. Hilo’s rate is similar to <br />the global rate but somewhat higher due to the weight of the volcanoes pushing <br />into the earth’s crust. <br />• There are two contributors to the sea level rise: added water from melting <br />glaciers and ice sheets, and thermal expansion. <br />• Sea surface temperatures are increasing and contributing to the sea level rise. <br />• There are satellite missions that circle around the earth repeatedly, taking <br />measurements of ice mass changes. <br />• Greenland and the Antarctic ice mass are the two ice sheets of most concern. <br />Greenland is losing about 300 billion tons of ice per year, and Antarctica is losing <br />about 125 billion tons per year. <br />• Projections: it is very likely the sea level will rise 0.5 to 1.2 feet by 2050 and 1.0 to <br />4.3 feet by 2100, and extremely likely it will continue beyond 2100. <br />• The rise being experienced now is mainly from the past couple of decades’ worth <br />of greenhouse gas emissions, and projections show it will only continue to rise. <br />• NOAA forecasts a 1-foot rise by 2050 and 3-foot rise by 2100. <br />• King tide events will occur more frequently and severely. <br />• There are projections the ice mass loss may change the gravity field and possibly <br />the rotation of the planet. <br />• Scenario planning—how planners plan and engineers design, given the range of <br />possible scenarios—is ongoing. Higher scenarios should be considered for a major <br />CIP investment such as a wastewater treatment plant or power generation facility. <br />• Hawaiʻi became the first state to enact legisla?on that implements parts of the <br />Paris climate agreement. The Hawaiʻi Climate Change Mitigation and Adaptation <br />Commission has been established, and it is to provide direction, coordination, and <br />planning, develop strategies, and complete a Sea Level Rise Vulnerability and <br />Adaptation Report. <br />• There are websites that show the different types of sea level rise impacts. <br />• Because of the sea level rise, king tide events will get more severe, and there may <br />be flooding during regular high tides. <br />• Passive models can underestimate the effect waves may have, and it is expected <br />they will frequently overtop the coastal bench. <br /> <br /> <br />
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