Parts of a Wave Defined:

Slides:



Advertisements
Similar presentations
Ocean Movements.
Advertisements

CHAPTER 8 Waves and Water Dynamics
Topic 16 Waves GEOL 2503 Introduction to Oceanography.
Chapter 9: Waves and Water Dynamics Fig Waves are moving energy Forces cause waves to move along air/water or within water Wind (most surface ocean.
Waves Anatomy of wave – Wave- transmission of energy through matter – Longitudinal wave- matter oscillates in same direction of energy transmission –
Wave Action Section 13.1.
How Waves Form When you watch the surfer's wave crash onto the beach, you are seeing the last step in the process of the wave's development. The process.
Question of the Day Question: How are topography and bathymetry different? Similar? Answer: ……… Turn In: -Article Summary -Worksheet 14-6.
WAVES.
Waves.
  waimea-bay-cam
Wave Action Chap 11, Sec 2. Essential Questions (Chap 11, Sec 2) 1. How does a wave form? 2. How do waves change near the shore? 3. How do waves affect.
Waves in the Ocean Words from these PPT slides are already on the course web site. Waves in the Ocean Words from these PPT slides are already on the course.
Ocean Waves Text Book Page #
How are waves formed and what are the characteristics of waves?
Chapter 8 Waves and Water Dynamics
Waves Caused by wind, tides, and earthquakes STORMSSWELL SURF (energy in) (energy out) Waves move away from the sea that generated them; this energy can.
Waves How Does Ocean Water Move?
Chapter 21 Section 2 Handout
Waves and Water Dynamics
Waves n Characteristics of All Wind-generated Waves n Deep Water Waves n Shallow Water Waves n Other Water Waves.
N Characteristics of All Wind-generated Waves n Deep Water Waves n Shallow Water Waves n Other Water Waves.
WAVE PROCESSES ON A COAST HOW WAVES ARE FORMED Ocean surface waves are occur on the free surface of the ocean. They usually result from wind, and are also.
WAVES By: Bridget Pettit & Victor Perez. Waves are a result of forces acting on the surface of the water. GENERATIONG FORCES : is a forces (ie rock or.
2005 Tropical Storms Storm tracks generally fall into three categories: 1) Atlantic U-turns 2) Gulf coast strikers 3) East coast skirters
Unit 3: Waves and tides.
Unit 3 – Oceanography Section 3: Currents, Waves, and Tides
Topic 5 Waves and Wave Depths If the wind blows hard enough (speed) and long enough (duration) over a long enough area (fetch), waves become fully developed.
Waves. Pre-Survey Draw your best wave. How do waves form? How can they be good? Bad?
WAVES. Wave – propagation of energy through a medium. Speed is determined by the properties of the medium. Gravity waves – sufficiently large waves where.
Waves Waves result from interplay between disturbing forces & restoring forces In the oceans, disturbances originate –At the surface, winds, ships, etc.
Waves Chapter 9.
Waves. What is a wave?  a transmission of energy through matter.
OCEAN MOTION Coulter. Most waves form when winds blowing across the water’s surface transmit their energy to the water. Wave-movement of energy through.
Waves Transmit energy (not mass) across the ocean’s surface
Unit 2 Lesson 2 Ocean Waves
Unit 7 Waves & Beaches.
WAVES.
Unit 7 Waves and Beaches Topic 1 Watching Waves.
Key Ideas Describe the formation of waves and the factors that affect wave size. Explain how waves interact with the coastline. Identify the cause of destructive.
Waves Transmit energy (not mass) across the ocean’s surface
Waves.
Chapter Four Prentice Hall
WAVES.
WAVES UNDULATIONS OF THE WATER CAUSED BY WINDS BLOWING ACROSS THE SURFACE OF THE SEA. They consist of orbital movements of water molecules which diminishes.
Section 13 – 1 Wave Action.
Lab 5 WAVES. What is waves ? how do waves form? Wave is a movement of upper surface of water due to transfer of energy from the wind into the water without.
Wave Parameters (Figure 7-1a)
Unit 2 Lesson 2 Ocean Waves
Water and the Atmosphere - Chapter 2 Lesson 2
Unit 7 Topic 5 Waves and Wave Depths
Wave Action Section 13.1.
Waves.
Chapter 14 Section 3 Waves Bellringer
Unit 7 Waves & Beaches.
Wave Parameters (Figure 7-1a)
Ocean Waves Text Book Page #
Waves in the Ocean.
Waves in the Sea An ocean wave is a rhythmic rise and fall of the water’s surface. Most commonly produced by wind. Also by undersea earthquakes and the.
Lesson 4.1: Waves *Refer to Chapter 12 in your Textbook.
Lets Review! Handout 10 Waves
Unit 7 Waves & Beaches.
Waves Transmit __________ (not __________) across the ocean’s surface
Waves!.
Unit 7 Waves & Beaches.
Unit 7 Waves & Beaches.
WAVES The motion of the ocean
Waves and Tides Earth Science 6th Grade.
Ocean Motions Chapter 13.
Presentation transcript:

Waves Sea is a term used to describe a confused mixture of waves that is often observed from ships.

Parts of a Wave Defined: Crest – highest point of a wave. Trough – lowest part of a wave; below the stillwater mark. Wave Height – vertical distance from crest to trough. Wave Length – horizontal distance from crest to crest. Wave Frequency – the # of wave crests that pass a fixed point per unit of time.

Labeling Parts of a Wave

Parts of a Wave Defined continued: Wave Period – the time in seconds that it takes for one complete wave to pass a fixed point. Wave Speed – the speed of a wave in a certain direction expressed as distance per unit of time.

Wave energy Many forms of energy are carried by waves: Heat, electricity, light, sound, and water All forms of energy can be transformed into work. Ocean waves break rock, carry sand away, and produce heat and sound when they slam into the shore. Energy in waves can be used to drive generators to produce electricity. We can measure the amount of energy in: Joules of work Kilocalories of heat Kilowatt hours of electricity If the energy is being transmitted or used at a constant rate (power) over a period of time, the total energy in kilowatt-hours is the product of the power in kilowatts and the time in hours. The kilowatt-hour is commonly used as a billing unit for energy delivered to consumers by electric utilities.

Wave energy The amount of energy in a wave depends on its height. The higher the wave, the more energy it releases. The energy per square meter is proportional to the square of its height.

Wind Waves Wind is the primary source of energy for waves. Most ocean waves are produced by the force of the wind. The force of the wind is influenced by: 1. Its duration, the length of time it’s been blowing 2. Its fetch (an old sailor’s term), the distance over which the wind is blowing. 3. Its average speed over the fetch

Understanding Movement of H2O Molecules: he waves on the surface of the water are neither longitudinal nor transverse. We can see in animation that red ball, which simulates the molecule of the water surface, moves in a circle path. So, the wave on the water surface is the superposition of transverse and longitudinal motions of the molecules. VIDEO

Calculating wave properties We can calculate the speed of a wave from its wavelength and period (time) using the formula: C = λ / t speed= wavelength/time Knowing that a wave has a wavelength of 20m and a period of 4 sec, we can calculate its speed. C= 20m/4sec C= 5 m/s

Wave frequency The frequency of a wave is the number of times it passes a given point in 1 second. The formula to calculate frequency is: ƒ=1/t

Where do waves break? Surf Zone – area near shore where waves break. Distance from shore where waves break depends on: Depth of water Length

How a wave breaks depends on: The steepness of the bottom slope Whether the slope is smooth or irregular Whether the bottom is composed of shifted sands or solid rock

Wave Properties Open ocean waves appear to change endlessly. Oceanographers and engineers who want to study waves must understand the basic properties of waves. Different waves have different speeds. Most waves travel at 20-40 mph.

Why do waves break? Steepness of bottom slope Composition of bottom: Shifting sands Solid rock

Force of Wind Duration – length of time it has been blowing. Fetch – the distance over which the wind is blowing.

Types of Breaking Waves: Spilling Breaker – Gently sloping coasts or flat coasts where the waves break slowly and over a long distance. Crest spills gently down the front of the wave. Wave energy is gradually released over time.

Types of Breaking Waves: Plunging Breaker – Formed when coast is moderately steep. Waves slow down more quickly, so crest curls way over the front of the wave and plunges down toward the base. As waves move towards the shore, they change from deep-water swells to shallow-water breaking waves. Constant pounding by waves erodes and changes coastal features.

Types of Breaking Waves: Surging Breaker – Very steep beach slope. Never really break; rush onto beach in a brief surge of water. Energy of wave is reflected.

Open Ocean Waves Ripple – small waves less than 1 foot in size Chop – Medium waves that come to a point at the crest. 1-3 feet in size Seas – Large waves associated with windy weather. 4 -10 feet in size Storm – Extremely large waves associated with tropical storm or greater winds. 6+ feet in size (winds exceeding 105 km/hr)

Interference patterns The wave patterns produced when two or more wave sets intersect are called interference patterns. Wave Reinforcement- exceptionally high waves when crests of two waves come together or very deep troughs when troughs combine. VIDEO