Test 1: Ocean 116 (Oceanography Lab.)

Similar documents
g) Use the map compass to provide the general locality of the knoll on the chart.

Ocean Waves. Capillary. Gravity. Wind generated. Tides Tsunamis Seiches

Homework 2 Bathymetric Charts [based on the Chauffe & Jefferies (2007)]

Geology 10 Activity 8 A Tsunami

Navigation & Orienteering: Pre- Test

Lesson 2: Sailing. A league is three nautical miles. (A nautical mile is about 800 feet longer than a mile on land.)

Homework 2a Bathymetric Charts [based on the Chauffe & Jefferies (2007)]

HYDROSPHERE, OCEANS AND TIDES

Nautical Navigation: Final Quiz

Basic Chartwork. Necessary Tools. Navigation is the one science in which no margin whatever is left for the faker. - Felix Riesenberg

Homework 2b: Bathymetric Profiles [based on the Chauffe & Jefferies (2007)]

OCEAN WAVES NAME. I. Introduction

SIO 210 Problem Set 3 November 4, 2011 Due Nov. 14, 2011

Chartwork Learn the basics for position fixing using a number of techniques and a simple equation for speed, distance and time.

General Oceanography Geology 105 Expedition #19 The Ocean and Climate

/50. Physical Geology Shorelines

3.6 Magnetic surveys. Sampling Time variations Gradiometers Processing. Sampling

In this lesson, students determine the speed of a tsunami using tsunami time travel maps and Google Earth.

Section 6. The Surface Circulation of the Ocean. What Do You See? Think About It. Investigate. Learning Outcomes

SOCCOM.Act.PDS.1.1: Tracking Ocean Currents

SURFACE CURRENTS AND TIDES

Utilizing Vessel Based Mobile LiDAR & Bathymetry Survey Techniques for Survey of Four Southern California Breakwaters

SIO 210 MIDTERM, 26 October 2009.

Imagine that you can see a side view of a wave as it approaches a beach. Describe how the wave changes as the wave approaches the beach.

Eilat 's artificial lagoons project on the Red Sea - Israel R. Raviv Ir. R. Raviv, Coastal Engineering Ltd., P.O. Box 7322, z/b 37072,

Lesson one. Linear Motion. Terminal Objective. Lesson 1. Linear Motion

Lat. & Long. Review. Angular distance N or S of equator Equator = 0º Must indicate N or S North pole = 90º N

Name: Unit 5-6 Pretest. 28. Circle the picture(s) that show erosion.

Motion. 1 Describing Motion CHAPTER 2

Chapter 22, Section 1 - Ocean Currents. Section Objectives

United Nations Convention on the Law of the Sea

Chart Features Maritime maps and Admiralty charts have these features:

N. Robinson and A. Pyne

Oceans - Laboratory 12

Marine Survey & Cable Routing

Southern Region, B.S.A. Yachting Initiative Program Elements PILOTING ESSENTIALS. Learning Objectives:

The speed of an inline skater is usually described in meters per second. The speed of a car is usually described in kilometers per hour.

EXECUTIVE SUMMARY (Revised)

The ocean water is dynamic. Its physical

COXSWAIN NAVIGATION EXERCISES AUS197 NAME:

Swell and Wave Forecasting

Swell and Wave Forecasting

Ocean Waves and Surf Forecasting: Wave Climate and Forecasting

SCI-5 MES_Lamb_Oceans Exam not valid for Paper Pencil Test Sessions

Available online at ScienceDirect. Procedia Engineering 116 (2015 )

Terrestrial Observations Chart Plot - Chesapeake Bay Entrance - Operational Level

Centre for Marine Science and Technology

Position and displacement

and the Link between Oceans, Atmosphere, and Weather

COASTAL ENVIRONMENTS. 454 lecture 12

Pathways and Effects of Indonesian Throughflow water in the Indian Ocean using Trajectory and Tracer experiments in an OGCM

Yellow Sea with contributions by John R. Apel

Currents measurements in the coast of Montevideo, Uruguay

Name: Date: Day/Period: CGC1P1: Interactions in the Physical Environment. Factors that Affect Climate

Current: large mass of continuously moving ocean water

The events associated with the Great Tsunami of 26 December 2004 Sea Level Variation and Impact on Coastal Region of India

17. High Resolution Application of the Technology Development Index (TDI) in State Waters. South of Block Island

Understanding the Tsunami Wave

An Atlas of Oceanic Internal Solitary Waves (February 2004) by Global Ocean Associates Prepared for Office of Naval Research Code 322 PO

OCEANOGRAPHY STUDY GUIDE

SEASONDE DETECTION OF TSUNAMI WAVES

An IOOS Operational Wave Observation Plan Supported by NOAA IOOS Program & USACE

4/20/17. #31 - Coastal Erosion. Coastal Erosion - Overview

page - Laboratory Exercise #5 Shoreline Processes

GEOS 201 Lab 13 Climate of Change InTeGrate Module Case studies 2.2 & 3.1

Canada s vast size creates a diverse range of weather conditions and climatic conditions. Warming trend for last 10 years Wet Spring Dry five summers

Figure 4, Photo mosaic taken on February 14 about an hour before sunset near low tide.

National Maritime Center

An Atlas of Oceanic Internal Solitary Waves (February 2004) by Global Ocean Associates Prepared for Office of Naval Research Code 322 PO

Geology 15 Activity 5 A Tsunami

THE POLARIMETRIC CHARACTERISTICS OF BOTTOM TOPOGRAPHY RELATED FEATURES ON SAR IMAGES


} to. Identifying or categorizing characteristics (shape, dimensions, total relief, least depth, steepness, etc.): Shown with name on chart No.

Station 1: Ocean Currents Use the ocean currents map copied from page 4 of the ESRT and the passage to answer the questions that follow.

"Real-Time Vertical Temperature, and Velocity Profiles from a Wave Glider"

Waves. Types of Waves. Parts of a wave. Insert wind_wave.wmv. Shark attack

Design and Planning Considerations For a Seabed Survey

Force, Motion and Energy Review

New Bedford Fishing Heritage Center

Lecture Outlines PowerPoint. Chapter 15 Earth Science, 12e Tarbuck/Lutgens

BUREAU OF MINERAL RESOURCES, GEOLOGY AND GEO HYSICS

46 Chapter 8 Statistics: An Introduction

Chapter - Oceans and Coasts

Heating of Land and Water. Evaluation copy. lamp with a 100 W (or greater) bulb. 2 Temperature Probes 2 one-hole stoppers 2 pans beaker.


Chapter 10 Lecture Outline. The Restless Oceans

Tsunami STUDENT ACTIVITIES

SAILING ROUTES GZV/ENDORSEMENT

Australian Northwest Shelf

BEACH NOURISHMENT BY RAINBOWING FOR THE VISAKHAPATNAM PORT TRUST BY DCI. Capt. MVR MURTHY ABSTRACT

LAKKOPETRA (GREECE) EUROSION Case Study. Contact: Kyriakos SPYROPOULOS. TRITON Consulting Engineers. 90 Pratinou Str Athens (GREECE)

MULTIDECADAL SHORELINE EVOLUTION DUE TO LARGE-SCALE BEACH NOURISHMENT JAPANESE SAND ENGINE? Abstract

South Bay Coastal Ocean Observing System California Clean Beaches Initiative

Advanced Hydraulics Prof. Dr. Suresh A. Kartha Department of Civil Engineering Indian Institute of Technology, Guwahati

David Monahan, Canadian Hydrographic Service and Dave Wells, Ocean Mapping Group, Canada

Draw a picture of a water source. Don t forget to include yourself in the picture!

EFFECTS OF WAVE, TIDAL CURRENT AND OCEAN CURRENT COEXISTENCE ON THE WAVE AND CURRENT PREDICTIONS IN THE TSUGARU STRAIT

Where the Swell Begins

MESSOLOGI LAGOON AREA (GREECE)

Figure 1, Chart showing the location of the Breach at Old Inlet and sensors deployed in Great South Bay.

Transcription:

GLENDALE COMMUNITY COLLEGE Name Marks secured /25 Test 1: Ocean 116 (Oceanography Lab.) Dr. Poorna Pal Note: Answer all questions/solve all problems, giving detailed answers, as may be needed. Show all your work. 1. Tabulated alongside are the latitudes and longitudes of selected locations on the Pacific Ocean region while the coordinates of Glendale, CA, are given below: Glendale latitude: Glendale longitude: 34 12 N 118 15 W (a) Relative to Glendale, CA, which of the locations tabulated above is the farthest Latitude Longitude Sand Point, AK 55 2 N 16 3 W Honolulu, HI 21 18 N 157 5 W Tahiti, S. Pacific 17 37 S 149 27 W Shimazu, Japan 32 46 N 132 57 E (2 points) North? East? South? West? (b) Use the longitude data tabulated above to compute the differences in local time between Glendale, CA, and the other locations and enter the results, to the nearest minutes (time), in the blank spaces below. (3 points) Show work. Note that 15 longitude = 1 hour (time) 1 longitude = 4 minutes (time) 15 longitude = 1 minute (time) (i) Longitude difference between Glendale, CA, and Sand Point, AK = Time difference between Glendale, CA, and Sand Point, AK = (ii) Longitude difference between Glendale, CA, and Honolulu, HI = Time difference between Glendale, CA, and Honolulu, HI = (iii) Longitude difference between Glendale, CA, and Tahiti, S. Pacific = Time difference between Glendale, CA, and Tahiti, S. Pacific =

(c) Use the coordinates tabulated above and plot all these locations (i.e., Sand Point, AK; Honolulu, HI; Tahiti, South Pacific; Shimazu, Japan; and Glendale, CA) on the map of the Pacific Ocean region below. (2½ points) 2. Tabulated below are the depth soundings data obtained across the North Atlantic along an East- West profile on 45 N latitude from the coast off Halifax, Nova Scotia, Canada, to that of Soulac, France. (a) Covert the one-way travel time data to depth values, using 148 m/sec for the velocity of sound in water. (2½ points) (b) Plot these data on the graph below, and construct the depth profile. (2½ points) 2

Distance from Nova Scotia coast (km) 39 696 183 1238 147 186 2243 2398 263 2785 2862 317 343 379 4177 4564 4642 4874 One-way travel time for the depth soundings (seconds).61.89.49 2.373 2.719 2.571 2.82 2.324 2.76 1.186 1.483 2.126 2.868 3.115 3.362 2.917.99 Depth below the sea level surface (meters) Depth below the MSL (mean sea level), in meters 5 4 3 2 1 1 2 3 4 5 Distance from the Nova Scotia coast, in kilometers (c) Is the continental shelf wider off Canada or off France? (d) At what distance from Nova Scotia coast does this profile cross the Mid-Atlantic Ridge? Also show it on your profile..... (½ point) (½ point) (e) Identify the abyssal sea floor on the profile that you have drawn above. (½ point) 3. The map of part of San Pedro channel shows depth soundings in fathoms. (a) Contour these depth values with 5, 1, 15, 2, 25, 3, 35, 4 and 45 fathom bathymetric contours. (4 points) 3

(b) Use this contour map to draw an ocean-depth profile from Avalon to San Pedro. (Note: Measure depth from the surface down on the graph). (2 points) 4

Avalon San Pedro Depth below sea level (fathoms) 4. The model interpretation of an observed magnetic anomaly over the Carlsberg Ridge, NW Indian Ocean, is shown below. Find the rate of seafloor spread here. (1½ points) 4 2 2 4 Ma 4 2 2 4 Km Source: Chaubey, Bhattacharya, Murty and Desa, 1993, Spreading history of the Arabian Sea: some new constraints, Marine Geology, v.112, p.343-352. Find the spread rate. Show work. Give the answer in mm/yr (1½ points) 5

5. The chart below is part of a seismic reflection profile across the outer continental shelf and slope off Mexico s west coast. (a) What is the depth to the ocean bottom below point X (assume velocity of sound in water as 15 meters per second). (1 points) Show work. Give answer in meters... (b) What is the thickness of the sediments below point X (assume velocity of sound in the sediments as 18 meters per second). (1 points) Show work. Give answer in meters.. X Ocean bottom.75 One-way travel time (seconds).5.25 Mio-Pliocene sediments 6

6. A speedboat is running at 15 knots in the straight stretch of a canal and, along the parallel coastal road, a tractor is racing it at 25 km/hour. Which one is faster, the speedboat or the tractor? Find boat s speed in km/hr and tractor s speed in knots. Notes: 1 knot = 1 nautical mile per hour (1½ points) 1 nautical mile = 1.15 statute miles = 1.85 km (a) Which one is faster, speedboat or the tractor?. (b) Find the speedboat s speed in kilometers per hour and the tractor s speed in knots. Speedboat km/hr (Show work) Tractor Knots (Show work) 7