Tsunami Safety and Sea Level Rise
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Wind-Caused Waves Misleads Us Energy Is Transferred to the Wave
WAVES IN WATER is quite similar. Most waves are created by the frictional drag of wind blowing across the water surface. A wave begins as Tsunami can be the most overwhelming of all waves, but a tiny ripple. Once formed, the side of a ripple increases the their origins and behaviors differ from those of the every day waves we see at the seashore or lakeshore. The familiar surface area of water, allowing the wind to push the ripple into waves are caused by wind blowing over the water surface. a higher and higher wave. As a wave gets bigger, more wind Our experience with these wind-caused waves misleads us energy is transferred to the wave. How tall a wave becomes in understanding tsunami. Let us first understand everyday, depends on (1) the velocity of the wind, (2) the duration of wind-caused waves and then contrast them with tsunami. time the wind blows, (3) the length of water surface (fetch) the wind blows across, and (4) the consistency of wind direction. Once waves are formed, their energy pulses can travel thou Wind-Caused Waves sands of kilometers away from the winds that created them. Waves transfer energy away from some disturbance. Waves moving through a water mass cause water particles to rotate in WHY A WIND-BLOWN WAVE BREAKS place, similar to the passage of seismic waves (figure 8.5; see Waves undergo changes when they move into shallow water figure 3.18). You can feel the orbital motion within waves by water with depths less than one-half their wavelength. -
Tsunami, Seiches, and Tides Key Ideas Seiches
Tsunami, Seiches, And Tides Key Ideas l The wavelengths of tsunami, seiches and tides are so great that they always behave as shallow-water waves. l Because wave speed is proportional to wavelength, these waves move rapidly through the water. l A seiche is a pendulum-like rocking of water in a basin. l Tsunami are caused by displacement of water by forces that cause earthquakes, by landslides, by eruptions or by asteroid impacts. l Tides are caused by the gravitational attraction of the sun and the moon, by inertia, and by basin resonance. 1 Seiches What are the characteristics of a seiche? Water rocking back and forth at a specific resonant frequency in a confined area is a seiche. Seiches are also called standing waves. The node is the position in a standing wave where water moves sideways, but does not rise or fall. 2 1 Seiches A seiche in Lake Geneva. The blue line represents the hypothetical whole wave of which the seiche is a part. 3 Tsunami and Seismic Sea Waves Tsunami are long-wavelength, shallow-water, progressive waves caused by the rapid displacement of ocean water. Tsunami generated by the vertical movement of earth along faults are seismic sea waves. What else can generate tsunami? llandslides licebergs falling from glaciers lvolcanic eruptions lother direct displacements of the water surface 4 2 Tsunami and Seismic Sea Waves A tsunami, which occurred in 1946, was generated by a rupture along a submerged fault. The tsunami traveled at speeds of 212 meters per second. 5 Tsunami Speed How can the speed of a tsunami be calculated? Remember, because tsunami have extremely long wavelengths, they always behave as shallow water waves. -
Tsunamis in Alaska
Tsunami What is a Tsunami? A tsunami is a series of traveling waves in water that are generated by violent vertical displacement of the water surface. Tsunamis travel up to 500 mph across deep water away from their generation zone. Over the deep ocean, there may be very little displacement of the water surface; but since the wave encompasses the depth of the water column, wave amplitude will increase dramatically as it encounters shallow coastal waters. In many cases, a El Niño tsunami wave appears like an endlessly onrushing tide which forces its way around through any obstacle. The image on the left illustrates how the amplitude of a tsunami wave increases as it moves from the deep ocean water to the shallow coast. Over deep water, the wave length is long, and the wave velocity is very fast. By the time the wave reaches the coast, wave length decreases quickly and wave speed slows dramatically. As this takes place, wave height builds up as it prepares to inundate the shore. Why do Tsunamis occur in Alaska? Subduction-zone mega-thrust earthquakes, the most powerful earthquakes in the world, can produce tsunamis through fault boundary rupture, deformation of an overlying plate, and landslides induced by the earthquake (IRIS, 2016). Megathrust earthquakes occur along subduction zones, such as those found along the ring of fire (see image to the right). The ring of fire extends northward along the coast of western North America, then arcs westward along the southern side of the Aleutians, before curving southwest along the coast of Asia. -
2018 NOAA Science Report National Oceanic and Atmospheric Administration U.S
2018 NOAA Science Report National Oceanic and Atmospheric Administration U.S. Department of Commerce NOAA Technical Memorandum NOAA Research Council-001 2018 NOAA Science Report Harry Cikanek, Ned Cyr, Ming Ji, Gary Matlock, Steve Thur NOAA Silver Spring, Maryland February 2019 NATIONAL OCEANIC AND NOAA Research Council noaa ATMOSPHERIC ADMINISTRATION 2018 NOAA Science Report Harry Cikanek, Ned Cyr, Ming Ji, Gary Matlock, Steve Thur NOAA Silver Spring, Maryland February 2019 UNITED STATES NATIONAL OCEANIC National Oceanic and DEPARTMENT OF AND ATMOSPHERIC Atmospheric Administration COMMERCE ADMINISTRATION Research Council Wilbur Ross RDML Tim Gallaudet, Ph.D., Craig N. McLean Secretary USN Ret., Acting NOAA NOAA Research Council Chair Administrator Francisco Werner, Ph.D. NOAA Research Council Vice Chair NOTICE This document was prepared as an account of work sponsored by an agency of the United States Government. The views and opinions of the authors expressed herein do not necessarily state or reflect those of the United States Government or any agency or Contractor thereof. Neither the United States Government, nor Contractor, nor any of their employees, make any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, product, or process disclosed, or represents that its use would not infringe privately owned rights. Mention of a commercial company or product does not constitute an endorsement by the National Oceanic and Atmospheric Administration. -
What to Expect When You're Expecting: a Tsunami
WHAT TO EXPECT WHEN YOU’RE EXPECTING Tsunami Hazards in Washington State Maximilian Dixon – Washington Emergency Management Division Geological Hazards in Washington WA has the 2nd highest earthquake risk in the US We also have… • Tsunamis - local and distant M9 recurrence 300-600 years • 5 active volcanoes M7 recurrence 30-50 years • Landslides Cascadia Subduction Zone • 700 miles long (1,130 km) • Breaks 300 – 600 years (~500 years on average) • Last great rupture in 1700 (320 years ago) • 10-20% chance within next 50 years Juan North • Magnitude 8.0-9.0+ de America • Shaking felt region-wide for 3–6 minutes plate • Shaking intensity is greatest along coast & Fuca where local conditions amplify seismic waves plate • Earthquake followed by a major tsunami hitting WA’s outer coast in 15-20 min • Many large aftershocks will follow main quake Distant vs Local Tsunamis Distant Local • No earthquake felt • Event will typically be felt • > 3 hours until first wave arrives • < 3 hours until first wave arrives • Warning must be distributed • Earthquake is primary warning • Less inundation/slower currents • More inundation/faster currents • Less severe impact to coast • Significant impact to coast Local Tsunamis THE SHAKING IS YOUR WARNING! The first waves arrive within seconds to minutes Devils Mountain Fault South Whidbey Island Fault Cascadia Seattle Fault Subduction Zone Tacoma Fault Know the Natural Tsunami Warning Signs 1. Feel a long or strong ground shaking at the coast 2. See a sudden rise or fall of the ocean 3. Hear a loud roaring sound -
Atlantic Hurricane Activity During the Last Millennium
www.nature.com/scientificreports OPEN Atlantic hurricane activity during the last millennium Michael J. Burn1 & Suzanne E. Palmer2 Received: 13 February 2015 Hurricanes are a persistent socio-economic hazard for countries situated in and around the Accepted: 10 July 2015 Main Development Region (MDR) of Atlantic tropical cyclones. Climate-model simulations have Published: 05 August 2015 attributed their interdecadal variability to changes in solar and volcanic activity, Saharan dust flux, anthropogenic greenhouse gas and aerosol emissions and heat transport within the global ocean conveyor belt. However, the attribution of hurricane activity to specific forcing factors is hampered by the short observational record of Atlantic storms. Here, we present the Extended Hurricane Activity (EHA) index, the first empirical reconstruction of Atlantic tropical cyclone activity for the last millennium, derived from a high-resolution lake sediment geochemical record from Jamaica. The EHA correlates significantly with decadal changes in tropical Atlantic sea surface temperatures (SSTs; r = 0.68; 1854–2008), the Accumulated Cyclone Energy index (ACE; r = 0.90; 1851–2010), and two annually-resolved coral-based SST reconstructions (1773–2008) from within the MDR. Our results corroborate evidence for the increasing trend of hurricane activity during the Industrial Era; however, we show that contemporary activity has not exceeded the range of natural climate variability exhibited during the last millennium. The extent to which the climate dynamics of the Main Development Region (MDR) of Atlantic tropical cyclone activity are controlled by natural or anthropogenic climatic forcing factors remains unclear1,2. This uncertainty has arisen because of the reliance on historical meteorological records, which are too short to capture the natural long-term variability of climatic phenomena as well as a lack of understand- ing of the physical link between tropical Atlantic SSTs and tropical cyclone variability3,4. -
Meeting Agenda Special City Council
416 N Franklin Street City of Fort Bragg Fort Bragg, CA 95437 Phone: (707) 961-2823 Fax: (707) 961-2802 Meeting Agenda Special City Council THE FORT BRAGG CITY COUNCIL MEETS CONCURRENTLY AS THE FORT BRAGG MUNICIPAL IMPROVEMENT DISTRICT NO. 1 AND THE FORT BRAGG REDEVELOPMENT SUCCESSOR AGENCY Tuesday, February 26, 2019 6:00 PM Town Hall, 363 N Main Street Special Joint City Council/Planning Commission Meeting CALL TO ORDER ROLL CALL 1. CONDUCT OF BUSINESS 1A. 19-091 Receive Report and Provide Direction Regarding Mill Site Reuse Plan Local Coastal Program (LCP) Amendment Including: 1) Recommended Policy Changes from the Fort Bragg Sea Level Rise Study and the Tsunami Study; and 2) Recommended Policy Changes to the Safety Element of the Coastal General Plan Attachments: 02262018 Mill Site Reuse Plan - Safety Element Att 1 - Safety Element Att 2 - Sea Level Rise Report 2019 Att 3 - Tsunami Study 2007 Att 4 - RESO 4052-2017 Mill Pond ADJOURNMENT STATE OF CALIFORNIA ) )ss. COUNTY OF MENDOCINO ) I declare, under penalty of perjury, that I am employed by the City of Fort Bragg and that I caused this agenda to be posted in the City Hall notice case on February 21, 2019. _______________________________________________ Brenda Jourdain, Administrative Assistant NOTICE TO THE PUBLIC: City of Fort Bragg Page 1 Printed on 2/21/2019 Special City Council Meeting Agenda February 26, 2019 DISTRIBUTION OF ADDITIONAL INFORMATION FOLLOWING AGENDA PACKET DISTRIBUTION: • Materials related to an item on this Agenda submitted to the Council/District/Agency after distribution of the agenda packet are available for public inspection in the lobby of City Hall at 416 N. -
EARTH SCIENCE ACTIVITY #1 Tsunami in a Bottle
EARTH SCIENCE ACTIVITY #1 Grades 3 and Up Tsunami in a Bottle This activity is one of several in a basic curriculum designed to increase student knowledge about earthquake science and preparedness. The activities can be done at any time in the weeks leading up to the ShakeOut drill. Each activity can be used in classrooms, museums, and other educational settings. They are not sequence-bound, but when used together they provide an overview of earthquake information for children and students of various ages. All activities can be found at www.shakeout.org/schools/resources/. Please review the content background (page 3) to gain a full understanding of the material conducted in this activity. OBJECTIVE: For students to learn that tsunamis can be caused by earthquakes and to understand the effects of tsunamis on the shoreline MATERIALS/RESOURCES NEEDED: 2-liter plastic soda bottles Small gravel (fish tank gravel) Water source Empty water bottle (16 oz) Overhead projector Transparency of Tsunami Facts “What Do I See?” handout PRIOR KNOWLEDGE: In order to conduct this activity, students need to know how fault slippage can generate earthquakes. ACTIVITY: Set-Up (Time varies) Collect as many 2-liter soda bottles as possible or ask students to bring in bottles for this activity (3 students can share one bottle). Obtain an empty water bottle (about 16 oz). Remove labels from all bottles. Purchase or gather enough small gravel to fit through the mouth of the soda bottles. Students will fill up their soda bottles with gravel to create at least a 2 inch layer on the bottom of the bottle. -
King Tide Hike for Newsletter 1 21 19
RISING TIDES AT CHINA CAMP: A Reflection on the 1/21/19 King Tide Walk with the National Estuarine Research Reserve What is a King Tide? If you are a resident of Peacock Gap or Santa Venetia neighborhoods, you are well aware of this coastal phenomenon. Several times a year, residents find their daily commute interrupted by roads partially inundated with water. Some even risk the well-being of their vehicles by fording the flooded areas. For many, king tides are merely a nuisance, but at China Camp, they are a point of fascination for those who are captivated by the dynamic rhythms of the natural world. Sarah Ferner leading a King tide hike. On a brisk January morning this year, 25 nature-seekers gathered at Turtleback Trailhead to experience the annual King Tide on a hike expertly led by the National Estuarine Research Reserve Education Coordinator Sarah Ferner. King Tides are a peculiar natural phenomenon. They occur several times a year when both the sun and the moon align so that their gravity “pulls” the earth’s oceans creating a “bulge”. The pull is most acute when the full or new moon is closest to the earth in its elliptical orbit. Along coastlines, this creates extremely high tides and flooding of varying degrees. Image from higher-tides.com This cosmic event makes for a birding bonanza along marshland areas because animals evacuate the pickleweed and salt grass in search of higher ground, escaping the rising sea water. Birds from all over Marin County coalesce at China Camp’s marshes to feast upon lizards, mice, insects, and other creatures. -
King Tide Floods in Tuvalu
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Open Access Open Access Nat. Hazards Earth Syst. Sci. Discuss.,Natural 1, 1943–1964, Hazards 2013 Natural Hazards www.nat-hazards-earth-syst-sci-discuss.net/1/1943/2013/ and Earth System doi:10.5194/nhessd-1-1943-2013and Earth System NHESSD Sciences Sciences © Author(s) 2013. CC Attribution 3.0 License. 1, 1943–1964, 2013 Discussions Open Access Open Access Atmospheric Atmospheric This discussion paper is/has been under review for the journal Natural Hazards and Earth Chemistry Chemistry King Tide floods in System Sciences (NHESS). Please refer to the corresponding final paper in NHESS if available. and Physics and Physics Tuvalu Discussions Open Access Open Access C.-C. Lin et al. Atmospheric Atmospheric Measurement Measurement Techniques Techniques Title Page Discussions Open Access King Tide floods in Tuvalu Open Access Abstract Introduction Biogeosciences C.-C. Lin, C.-R. Ho, andBiogeosciences Y.-H. Cheng Discussions Conclusions References Department of Marine Environmental Informatics, National Taiwan Ocean University, Open Access Open Access Tables Figures Keelung, Taiwan Climate Climate Received: 16 March 2013 – Accepted: 25 April 2013 – Published: 17 Mayof 2013 the Past of the Past J I Discussions Correspondence to: C.-R. Ho ([email protected]) J I Open Access Open Access Published by Copernicus Publications on behalf -
Santa Rosa County Tsunami/Rogue Wave
SANTA ROSA COUNTY TSUNAMI/ROGUE WAVE EVACUATION PLAN Banda Aceh, Indonesia, December 2004, before/after tsunami photos 1 Table of Contents Introduction …………………………………………………………………………………….. 3 Purpose…………………………………………………………………………………………. 3 Definitions………………………………………………………………………………………… 3 Assumptions……………………………………………………………. ……………………….. 4 Participants……………………………………………………………………………………….. 4 Tsunami Characteristics………………………………………………………………………….. 4 Tsunami Warning Procedure…………………………………………………………………….. 6 National Weather Service Tsunami Warning Procedures…………………………………….. 7 Basic Plan………………………………………………………………………………………….. 10 Concept of Operations……………………………………………………………………………. 12 Public Awareness Campaign……………………………………………………………………. 10 Resuming Normal Operations…………………………………………………………………….13 Tsunami Evacuation Warning Notice…………………………………………………………….14 2 INTRODUCTION: Santa Rosa County Emergency Management developed a Santa Rosa County-specific Tsunami/Rogue wave Evacuation Plan. In the event a Tsunami1 threatens Santa Rosa County, the activation of this plan will guide the actions of the responsible agencies in the coordination and evacuation of Navarre Beach residents and visitors from the beach and other threatened areas. The goal of this plan is to provide for the timely evacuation of the Navarre Beach area in the event of a Tsunami Warning. An alternative to evacuating Navarre Beach residents off of the barrier island involves vertical evacuation. Vertical evacuation consists of the evacuation of persons from an entire area, floor, or wing of a building -
Re-Mapping the 2004 Boxing Day Tsunami Inundation in the Banda Aceh Region with Attention to Probable Sea Level Rise
Re-mapping the 2004 Boxing Day Tsunami Inundation in the Banda Aceh Region with Attention to Probable Sea Level Rise Elizabeth E. Webb Senior Integrative Exercise April 21, 2009 Submitted in partial fulfillment of the requirements for a Bachelor of Arts degree from Carleton College, Northfield, Minnesota. TABLE OF CONTENTS Abstract Introduction …………………………………………………………………… 1 Tectonic Background …………………………………………………………. 2 Geologic Background ……………………………………………………...…. 4 Tsunami Models ……………………………………………………………… 5 Sea Level Rise ………………………………………………………………... 8 Astronomical Tides Subsidence Climate Change Mechanisms Data Collection Models Sea Level Rise in the 20th and 21st Centuries Globally Regionally Data …………………………………………………………………………. 14 Methods ……………………………………………………………………... 16 Results ………………..……………………………………………………… 19 Linear Model Exponential Model Discussion …………………………………………………………………… 21 Conclusion ………………………………………………………………….. 23 Acknowledgements …………………………………………………………. 23 References …………………………………………………………………... 24 Re-mapping the 2004 Boxing Day Tsunami Inundation in the Banda Aceh Region with Attention to Probable Sea Level Rise Elizabeth Webb Senior Integrative Exercise, March 2009 Carleton College Advisors: Mary Savina, Carleton College Susan Sakimoto, University of Notre Dame ABSTRACT The effects of the Great Sumatra-Andaman Earthquake and the resulting tsunami on December 26, 2004 were greatest in the Banda Aceh region of northern Sumatra, where wave heights reached between 9 and 12 meters. Studies of the Sumatra-Andaman fault indicate that