Garantie de satisfaction à 100% Disponible immédiatement après paiement En ligne et en PDF Tu n'es attaché à rien 4.2 TrustPilot
logo-home
Examen

Test Bank Solution Manual for Eosc 114 - Waves Already Passed

Note
-
Vendu
-
Pages
19
Grade
A+
Publié le
17-10-2024
Écrit en
2024/2025

Test Bank Solution Manual for Eosc 114 - Waves Already Passed How many oceans and ocean basins does earth's surface have? - Answers one ocean 5 basins - artic, atlantic, indian, pacific, southern what is the difference between the surface current and waves - Answers surface current - large permanent winds that blow over the ocean create surface currents that transport matter and energy waves - occasional winds that blow over smaller areas ---> transport energy only Crest Trough Wavelength Waveheight amplitude Period Frequency celerity steepenss - Answers -top of wave -bottom of wave - top - top/ crest=crest -crest to trough - sea level to trough or crest - time/cycle - cycles /sec -speed m/s - peakedness of wave, ratio of height to wavelength H/L Wave height of waves is related to - Answers energy transported by waves - applies only to deep-water waves Does the energy generated by wind waves equal to more than the waves generated by earthquakes/storms/gravitational attraction etc - Answers - wind waves can carry more energy at one instance - but the total amount of energy over time is greater in earrthquakes etc. What are the two ways of classifying waves - Answers 1. generating/disturbing force - waves are classified according to the force that generates the waves - wind - wind wave - changes in atmospheric pressure, storm surge, tsunami - seiche - seismic activity, landslide - tsunami - gravitational attraction - tide 2. Restoring Force - classified according to their restoring force --> force that causes water to return to undisturbed state - surface tension --> capillary wave - gravity - surface gravity waves (wind wave, seiche, tsunami, tide) Capillary waves - Answers - tiny waves with tiny wavelengths - waves restored by surface tension - generated when wind blows sea state - depends on what 3 factors - types of waves - Answers an assessment of the ocean's conditions of the ocean surface - depends on 3 factors: 1. wind strength/speed 2. fetch 3. wind duration ( length of time wind blowing over fetch) - when wind blows over a fetch waves are transformed in this order: - cappilary waves --> ripples --> chop --> swells When is a fetch fully developed - Answers - once it has absorbed the max amount of energy it can contain - includes chaotic waves of varying heights/lengths/speed/direction where MAXIMUM HEIGHT is achieved for a given wind What happens to waves as they move away from the fetch? - Answers - they become well sorted with long waves leading the wave train - swells - sorted by speed and wavelengths - fastest/ longest wavelengths leave first - slowest/shortest wavelengths leave last - swells propagate away from fetch in groups called wave trains What parameters do you need to determine when a fetch is fully developed - Answers - x axis = duration - y axis - fetch (km) - slope = wind speed - can determine distance of fetch, wind speed, and duration needed to create fully developed sea where max height is achieved Significant wave height - what - how to estimate - Answers the average height of the highest one-third of the waves present - avg number so we can encounter waves whose max wave height is 2x the significant wave height**

Montrer plus Lire moins
Établissement
Eosc 114 - Waves
Cours
Eosc 114 - Waves










Oups ! Impossible de charger votre document. Réessayez ou contactez le support.

École, étude et sujet

Établissement
Eosc 114 - Waves
Cours
Eosc 114 - Waves

Infos sur le Document

Publié le
17 octobre 2024
Nombre de pages
19
Écrit en
2024/2025
Type
Examen
Contient
Questions et réponses

Sujets

Aperçu du contenu

Test Bank Solution Manual for Eosc 114 - Waves Already Passed

How many oceans and ocean basins does earth's surface have? - Answers one ocean

5 basins - artic, atlantic, indian, pacific, southern

what is the difference between the surface current and waves - Answers surface current - large
permanent winds that blow over the ocean create surface currents that transport matter and energy



waves - occasional winds that blow over smaller areas ---> transport energy only

Crest

Trough

Wavelength

Waveheight

amplitude

Period

Frequency

celerity

steepenss - Answers -top of wave

-bottom of wave

- top - top/ crest=crest

-crest to trough

- sea level to trough or crest

- time/cycle

- cycles /sec

-speed m/s

- peakedness of wave, ratio of height to wavelength H/L

Wave height of waves is related to - Answers energy transported by waves

- applies only to deep-water waves

,Does the energy generated by wind waves equal to more than the waves generated by
earthquakes/storms/gravitational attraction etc - Answers - wind waves can carry more energy at one
instance

- but the total amount of energy over time is greater in earrthquakes etc.

What are the two ways of classifying waves - Answers 1. generating/disturbing force

- waves are classified according to the force that generates the waves

- wind - wind wave

- changes in atmospheric pressure, storm surge, tsunami - seiche

- seismic activity, landslide - tsunami

- gravitational attraction - tide



2. Restoring Force

- classified according to their restoring force --> force that causes water to return to undisturbed state

- surface tension --> capillary wave

- gravity - surface gravity waves (wind wave, seiche, tsunami, tide)

Capillary waves - Answers - tiny waves with tiny wavelengths

- waves restored by surface tension

- generated when wind blows

sea state

- depends on what 3 factors

- types of waves - Answers an assessment of the ocean's conditions of the ocean surface



- depends on 3 factors:

1. wind strength/speed

2. fetch

3. wind duration ( length of time wind blowing over fetch)

, - when wind blows over a fetch waves are transformed in this order:

- cappilary waves --> ripples --> chop --> swells

When is a fetch fully developed - Answers - once it has absorbed the max amount of energy it can
contain

- includes chaotic waves of varying heights/lengths/speed/direction where MAXIMUM HEIGHT is
achieved for a given wind

What happens to waves as they move away from the fetch? - Answers - they become well sorted with
long waves leading the wave train

- swells

- sorted by speed and wavelengths

- fastest/ longest wavelengths leave first

- slowest/shortest wavelengths leave last

- swells propagate away from fetch in groups called wave trains

What parameters do you need to determine when a fetch is fully developed - Answers - x axis = duration

- y axis - fetch (km)

- slope = wind speed



- can determine distance of fetch, wind speed, and duration needed to create fully developed sea where
max height is achieved

Significant wave height

- what

- how to estimate - Answers the average height of the highest one-third of the waves present

- avg number so we can encounter waves whose max wave height is 2x the significant wave height**



- estimating:

1. list all wave heights observed from tall to short

Faites connaissance avec le vendeur

Seller avatar
Les scores de réputation sont basés sur le nombre de documents qu'un vendeur a vendus contre paiement ainsi que sur les avis qu'il a reçu pour ces documents. Il y a trois niveaux: Bronze, Argent et Or. Plus la réputation est bonne, plus vous pouvez faire confiance sur la qualité du travail des vendeurs.
TutorJosh Chamberlain College Of Nursing
Voir profil
S'abonner Vous devez être connecté afin de suivre les étudiants ou les cours
Vendu
350
Membre depuis
1 année
Nombre de followers
16
Documents
29214
Dernière vente
4 heures de cela
Tutor Joshua

Here You will find all Documents and Package Deals Offered By Tutor Joshua.

3.6

55 revues

5
19
4
14
3
12
2
0
1
10

Récemment consulté par vous

Pourquoi les étudiants choisissent Stuvia

Créé par d'autres étudiants, vérifié par les avis

Une qualité sur laquelle compter : rédigé par des étudiants qui ont réussi et évalué par d'autres qui ont utilisé ce document.

Le document ne convient pas ? Choisis un autre document

Aucun souci ! Tu peux sélectionner directement un autre document qui correspond mieux à ce que tu cherches.

Paye comme tu veux, apprends aussitôt

Aucun abonnement, aucun engagement. Paye selon tes habitudes par carte de crédit et télécharge ton document PDF instantanément.

Student with book image

“Acheté, téléchargé et réussi. C'est aussi simple que ça.”

Alisha Student

Foire aux questions