 Nawiliwili  Honolulu  Hilo

Slides:



Advertisements
Similar presentations
Climate Change and Sea Level Rise in the Pacific Islands
Advertisements

Tidal Datum Computation January 8, 2009 Center for Operational Oceanographic Products and Services.
Animation of Tidal Elevations in the Pacific
1.Gravitational pull of the moon and sun 2.Centripetal force of the rotating Earth Tides are generated by:
Clima en España: Pasado, presente y futuro Madrid, Spain, 11 – 13 February 1 IMEDEA (UIB - CSIC), Mallorca, SPAIN. 2 National Oceanography Centre, Southampton,
Estimates of Global Sea Level Change from Tide Gauges Sampling Issues 20th Century Global Sea Level (GSL) Rise Estimates Average of Trends (Douglas et.
Both NOAA’s calculated absolute sea level trend estimates and the more precise difference between the two sites suggest that North Spit subsides relative.
“Eternity begins and ends with the ocean's tides.”
Ivan Haigh, Matt Eliot and Chari Pattiaratchi
Coastal Zone 2011 Conference “Cool Geodetic Resources For Your Project” A National Ocean Service, NOAA, Presentation 1)TOOLS TO OBTAIN GEODETIC CONTROL.

3 feet 6 feet Sun (flashlight) Moon Earth Moon walks around Earth and stops at each quarter turn. Earth records what it sees. Each student should take.
& : Maryland Weather Service Report, Vol. 2, pp & : US Historical Climatology Network. Baltimore WSO.
Ostende GLOSS Course 2006 Characteristics of Sea Level Records Philip L. Woodworth Permanent Service for Mean Sea Level With thanks to Simon Williams.
Sea Level Change in Hong Kong and ENSO DW Zheng 1,2, XL Ding 1, YQ Chen 1, C Huang 2 1 Department of Land Surveying and Geo-Informatics Hong Kong Polytechnic.
Estimates of Global Sea Level Rise from Tide Gauges Sea level trend,
A Flexible Sea Level Generator for Small Island States Xianfu Lu (SIS09) By At AIACC Asia Regional Workshop March 25~27, 2003 Bangkok, Thailand.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Observed Oceans & Sea Level (from IPCC WG-I, Chapter 5) Observed Changes in Oceanic Climate and Sea Level Primary.
Environmental Effects of Increased Atmospheric Carbon Dioxide What is the Truth?
Tide gauge stations: requirements, status, and issues Mark Merrifield University of Hawaii Sea Level Center.
Eda Tide Gauge & AVISO. background John et al. (2001) Tide gauge ∆SSHA Observed Kuroshio transport fv=g(d ƞ /dx ) Goal: Kuroshio variation east.
Ocean Currents Chapter 16.1.
Global Climate Change. 150 Authors 1,000 Contributing Authors 5 Years Work 130 Countries 1,000 Expert Reviewers The Famous “IPCC Report”
NOAA’s CENTER for OPERATIONAL OCEANOGRAPHIC PRODUCTS and SERVICES TIDAL DATUM COMPUTATION OVERVIEW.
In-Situ Sea Level Measurements Mark A. Merrifield University of Hawaii 1.The GCOS Network - Progress Report 2.Global Sea Level Rise 3.Relative Sea Level.
Tides Cause Tides- daily variations in sea level
4 to 6-May-2011 Waikiki Beach Mariott Resort and Spa Honolulu, Hawaii Hydrographic Products and Services in support of Climate Services in the Pacific.
Finish Examples for 2 nd Block. Warm UpMay 13 th Sketch a graph of the following:
Tides Gravity- pull or attraction between objects; varies with mass of object Centrifugal force- because the earth and moon are rotating simultaneously.
Tides.
Hazards Profile. Objective: To identify key hazards issues and priorities Identify information gaps to address these concerns.
GLOSS Training Workshop Course Japan Meteorological Agency May 15-26, 2006 Sea Level Data Processing with SLPR2 3. Tidal Analysis and Prediction.
Tides and Tsunamis. Causes of Tides Interaction of earth and moon Interaction of earth and moon Two bulges on either side of the planet Two bulges on.
Tides. What are they? The rhythmic rising and falling of ocean surface levels.
Tides Oceans 11. What causes tides? Winds and currents move the surface water causing waves. Winds and currents move the surface water causing waves.
Jorge Vazquez Universidad Del Norte Barranquilla, Columbia 11/16/2012 Jet Propulsion Laboratory/Caltech How the Oceans Ended.
– Jani Hitesh – Prajapati Dharmesh Prajapati Shivam TIDES.
NAME SINDHU.M.P SUBJECT SOCIAL STUDIES. HYDROSPHERE The hydrosphere ] in physical geography describes the combined mass of water found on, under, and.
Tides Physical Oceanography
Tides The rising of Earth's ocean surface caused by the tidal forces of the Moon and the Sun acting on the oceans. Bay of Fundy at high tide Bay of Fundy.
Tides.
Παλίρροιες.
Focus on Tides Objectives: Students will learn what causes tides.
Applied Power Spectrum
Tides Gravity- pull or attraction between objects; varies with mass of object Centrifugal force- because the earth and moon are rotating simultaneously.
Climate Change.
Warm-up Week 4 The vertical distance between trough and crest is called the ____. a. wave height c. fetch b. wavelength d. wave period A fetch is _________.
The Hydrosphere.
Tides Tides are the daily change in sea level of the ocean.
Measures of Model Performance
Waves and Tides Notes.
Tides Gravity- pull or attraction between objects; varies with mass of object Centrifugal force- because the earth and moon are rotating simultaneously.
Tides Page 46 in Your Notebook.
Tides Tides are daily changes in the elevation of the ocean surface (sea level) Ocean tides result from the gravitational attraction exerted upon Earth.
Understanding Tidal Datums
Warm-up Week 4 The energy that drives surface ocean currents comes from ____. a. wave action c. temperature differences b. wind d. salinity variations.
Warm-up Week 4 The vertical distance between trough and crest is called the ____. a. wave height c. fetch b. wavelength d. wave period A fetch is _________.
Tides Tide- the rise and fall in sea level is called.
(Discussion – The Ocean in Motion: Tides)
Tides Gravity- pull or attraction between objects; varies with mass of object Centrifugal force- because the earth and moon are rotating simultaneously.
Tides.
Bellwork Week 8, Day 1 Why do you think it is easier to predict where an earthquake will occur than when it will occur?
Lesson 10: Tides Physical Oceanography
Both NOAA’s calculated absolute sea level trend estimates and the more precise difference between the two sites suggest that North Spit subsides relative.
Ocean Waves and Tides.
Lesson 10: Tides Physical Oceanography
Goal Setting Life skills continued.
Tides Tides are daily changes in the elevation of the ocean surface (sea level) Ocean tides result from the gravitational attraction exerted upon Earth.
Wave Characteristics Most ocean waves derive their energy from the wind Wave height: the vertical distance between trough and peak Wavelength: horizontal.
Presentation transcript:

 Nawiliwili  Honolulu  Hilo Tide and Sea Level Trends for the State of Hawaii Source: www.tidesandcurrents.noaa.gov Tides: under “Products”  “Tides”  “Observed Data-Active Stations” Sea Level: under “Products”  “Sea Level Trends” “CO-OPS Stations” Hawaii Stations Considered: Hilo Honolulu Nawiliwili  Nawiliwili  Honolulu Group 1 Clint Conrad  Hilo

Hilo 1 Week of Data: Very similar trends for each station: Mostly Diurnal (1/day), Some semidiurnal (2/day) Amplitude of tidal variation: About 2-3 feet Amplitude of sea level anomaly: About 0.25 feet (a few inches) Honolulu Nawiliwili

Long-Term Sea Level Trends: State of Hawaii Nawiliwili: Sea Level Rise = 1.5 mm/yr (45 years)

Long-Term Sea Level Trends: State of Hawaii Honolulu: Sea Level Rise = 1.5 mm/yr (94 years)

Long-Term Sea Level Trends: State of Hawaii Hilo: Sea Level Rise = 3.4 mm/yr (72 years)

Summary: State of Hawaii Short-Term Tidal Variations:  Mostly diurnal, a few feet in amplitude  Tidal fluctuations are similar across Hawaii  Water level anomalies are small: only a few inches Long-Term Sea Level Change:  Honolulu and Nawiliwili show 1.5 mm/yr of sea level rise during the last century  Hilo is anomalous: 3.4 mm/yr of sea level rise  Hilo’s larger rise might be due to: Gap in tide gauge data? Something to do with big island volcanism?