SAILING ROUTES GZV/ENDORSEMENT
|
|
|
- Laura Elfreda Tucker
- 5 years ago
- Views:
Transcription
1 SAILING ROUTES GZV/ENDORSEMENT
2 SETUP - Low & high pressure areas on earth - Prevailing winds - Ocean currents - Hurricane areas - Dangerous areas - Routeing per area - Use of Pilot charts and Ocean Passages
3 CONCEPTS - Doldrums - Horse latitudes - Trade winds - Monsoon - Continental shelf - Intertropical convergency zone
4
5 High pressure areas on earth
6 EZS 2013 C. Wassenaar
7 Ocean currents - Drawing pg 105/106 - Caused by prevailing wind - Course changed by Coriolis
8 Hurricane areas
9 Routes huricanes, cyclones, typhoons EZS 2013 C. Wassenaar
10 Piracy prone areas
11 Decrease in Piracy?
12 ROUTING General routes EZS 2013 C. Wassenaar
13 North Atlantic: Europe-Americas Westerlies! Directly: Seldom possible. MV s or fast ships when using professional routing bureaus! South: Pick up the tradewinds North: North of L pressure area (Short but cold!!)
14 Southern (tradewind) route Lizard Point course WSW to West Keep clear of Biscay! Ile d Ouessant should Not be sighted! Biskay, 100 fathom line, continental shelf
15 Bay of Biscay Make west! à veering wind after passing coldfront
16 EZS 2013 C. Wassenaar
17 Crossing doldrums and equator Not too far to the east: Doldrums area larger! Not too far to the west: S- hemisphere: SE tradewind Northern Summer: South-east tradewind more S! Northern Summer: pass between west Northern Winter: pass between west
18 Very little wind Horse lattitudes - Sir James Ross (descending of air: H ) Doldrums: Rising of air (L) Intertropical convergence zone
19 South-Atlantic: Cape Horn East to west: head South first! South side L But. NOT too far! West to east: prevailing winds, stay North of L! EZS 2013 C. Wassenaar
20 67 days 914 Edward Sewall EZS 2013 C. Wassenaar
21 South Atlantic: Cape of Good Hope - Roaring forties, screaming fifties - Agulhas current: freakwaves, southgoing stream 6 kt à Prevailing westerly wind
22 Indian ocean Monsoon! N winter: NE N summer: SW Difference in temperature
23 Indian ocean - In the winter head west, in the summer go east - NE monsoon 4-5 bf; SW monsoon 5-7 bf - Entrance Red sea 8 bf! - Suez channel: not sailable
24 Panama canal Pacific: area with no wind
25 Panama canal Leaving West side: first go south before heading West (Leaving East side: lee shore Caribian sea
26 Southern Pacific East to west: SE tradewind West to east: first go south (westerlies) Atolls: à Sun from behind and enter with daylight. Polaroid shades! àbe aware of strong currents! Differences in waterlevel inside-outside atol
27 Mediterranean Current goes counterclockwise! W-E stay south (in winter leeshore, N gales!) E-W stay north
28 Pilot Charts Averages of prevailing winds, currents, air and surface temperatures, wave heights, ice limits, visibility, pressure and weather conditions obtained from oceanographic and meteorologic observations over many decades Not to be used for navigation! Material: pilot charts containing the months Feb/April/May/ July/Sept copies of Ocean Passages of the World EZS 2013 C. Wassenaar
29 General questions: 1. Explain the meaning of the red lines 2. How far south have icebergs or growlers been spotted and in which year? Wind roses 1. What does the length of the shaft of the arrows mean? 2. What does the amount of feathers on the arrow indicate? 3. What does the figure in the centre of the wind rose indicate? EZS 2013 C. Wassenaar
30 Routeing question: Sailing from Brest (France) to Miami (USA). Plan a course on the map that offers the best chance on running winds. Also use recommendations from the Ocean Passages chapter 8. What are the disadvantages of a great circle route from Brest to Miami? Which ocean currents play a part here? EZS 2013 C. Wassenaar
CHAPTER 6 Air-Sea Interaction
CHAPTER 6 Air-Sea Interaction What causes Earth s seasons? Tilt (23.5 ) responsible for seasons 2011 Pearson Education, Inc. Distribution of Solar Energy Distribution of Solar Energy Atmosphere absorbs
Trade winds Prevailing westerlies east
Warm-up Page: 528, 1. What is the major wind belt that is nearest the equator? Trade winds Page: 528, 2. What is the major wind belt that the most of the USA belongs to: Prevailing westerlies Page: 528,
Atmospheric Circulation. Recall Vertical Circulation
Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and Sea Breezes Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation
3 Global Winds and Local Winds
CHAPTER 15 3 Global Winds and Local Winds SECTION The Atmosphere BEFORE YOU READ After you read this section, you should be able to answer these questions: What causes wind? What is the Coriolis effect?
3 Global Winds and Local Winds
CHAPTER 6 3 Global Winds and Local Winds SECTION The Atmosphere BEFORE YOU READ After you read this section, you should be able to answer these questions: What causes wind? What is the Coriolis effect?
Wind and Air Pressure
Wind and Air Pressure When air moves above the surface of the Earth, it is called wind. Wind is caused by differences in air pressure. When a difference in pressure exists, the air will move from areas
ATOMOSPERIC PRESSURE, WIND & CIRCULATION
ATOMOSPERIC PRESSURE, WIND & CIRCULATION A. INTRODUCTION Important because: pressure patterns drive wind patterns which in turn drive oceanic circulation patterns o atmospheric & oceanic circulation: major
Lesson: Atmospheric Dynamics
Lesson: Atmospheric Dynamics By Keith Meldahl Corresponding to Chapter 8: Atmospheric Circulation Our atmosphere moves (circulates) because of uneven solar heating of the earth s surface, combined with
Atmosphere Circulation
Atmosphere Circulation Winds What Causes Winds? Difference in air pressure due to unequal heating of the atmosphere. Temperatures vary according to the amount of sun it gets. Uneven heating of the Earth
Finish Characteristics of Climate
Bell Ringer Finish Characteristics of Climate Wind Coriolis Effect Newton s second law: a body in motion will continue in motion (unchanged) unless acted upon by an outside force. Liquid (water) and gas
What is Wind? Winds are caused by differences in air pressure. This is horizontal movement of air of high pressure to low pressure. Unequal heating of
What is Wind? Winds are caused by differences in air pressure. This is horizontal movement of air of high pressure to low pressure. Unequal heating of the atmosphere. Measuring Wind Wind direction is determined
Atmospheric Circulation. Density of Air. Density of Air: H 2 O and Pressure effects
Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and Sea Breezes Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation
Warm-up. color mass. albedo. mirage
Warm-up Page: 523, 1. The amount of solar energy reflected or absorbed depends on the, texture, composition, volume,, transparency and other properties. color mass Page: 523, 2. The fraction of solar radiation
Lecture 8: Pressure and Wind
Lecture 8: Pressure and Wind Pressure Distribution Forces Affect Wind Earth s Rotation Coriolis Force Geostrophic Balance Energy (Heat) The first law of thermodynamics Air Temperature Air Pressure Air
Think it Over. Now that we have completed the activity, make any necessary changes to your prediction.
Think it Over What do global wind patterns look like? Draw your prediction on your sheet. Now, let s try something. Does the wind turn? Let s find out! Now that we have completed the activity, make any
Global Winds and Local Winds
Global Winds and Local Winds National Science Education Standards ES 1j What is the Coriolis effect? What are the major global wind systems on Earth? What Causes Wind? Wind is moving air caused by differences
3 Global Winds and Local Winds
CHAPTER 1 3 Global Winds and Local Winds SECTION The Atmosphere BEFORE YOU READ After you read this section, you should be able to answer these questions: What causes wind? What is the Coriolis effect?
PHYSICAL GEOGRAPHY. By Brett Lucas
PHYSICAL GEOGRAPHY By Brett Lucas ATMOSPHERIC PRESSURE AND WIND Atmospheric Pressure and Wind Atmospheric Processes The Nature of Wind General Circulation of the Atmosphere Modifications of General Circulation
IN THE TABLE OF CONTENTS AND ON THE NEXT CLEAN PAGE, TITLE IT: WIND NOTES WIND!
IN THE TABLE OF CONTENTS AND ON THE NEXT CLEAN PAGE, TITLE IT: WIND NOTES WIND! Wind 8.10A recognize that the Sun provides the energy that drives convection within the atmosphere and oceans, producing
Meteorology. Circle the letter that corresponds to the correct answer
Chapter 7 Worksheet 2 Meteorology Name: Circle the letter that corresponds to the correct answer 1) Which of the following factors contributes to the general subsidence in the latitude zone 20 degrees
Write on your own paper.
Catalyst: 1. During the day, which one heats up faster, land or water? WHY?? 2. During the night which one cools down slower? 3. How does heat move? (hint: from what to what?) 4. What are the differences
Lecture The Oceans
Lecture 22 -- The Oceans ATMOSPHERE CIRCULATION AND WINDS Coriolis effect Prevailing winds and vertical circulation Zones of pressure, evap. & ppt. Factors modifying global winds -- Differential heating
Full Name: Class: Period: Date:
Topic/Objective: Essential Question: Full Name: Class: Period: Date: Tutor Use Only: Air Pressure and Wind (Chapter 19) Air Pressure the weight of the atmosphere pushing down on the Earth exerting a force
McKnight's Physical Geography 11e
Chapter 2 Lecture McKnight's Physical Geography 11e Lectures Chapter 5 Atmospheric Pressure and Wind Michael Commons Ohio Northern University Atmospheric Pressure and Wind The Nature of Atmospheric Pressure
9/25/2014. Scales of Atmospheric Motion. Scales of Atmospheric Motion. Chapter 7: Circulation of the Atmosphere
Chapter 7: Circulation of the Atmosphere The Atmosphere: An Introduction to Meteorology, 12 th Lutgens Tarbuck Lectures by: Heather Gallacher, Cleveland State University Scales of Atmospheric Motion Small-
SIO20 - Midterm Examination 2 v1 Winter Section A. Circle the letter corresponding to the best answer. (1 point each)
NAME: Section A. Circle the letter corresponding to the best answer. (1 point each) 1. Rainbows result from: a. refraction and reflection of sunlight by water droplets b. reflection of sunlight by oceans
3/22/11. General Circulation of the Atmosphere. General Circulation of the Atmosphere
Chapter 10 General refers to the average air flow, actual winds will vary considerably. Average conditions help identify driving forces. The basic cause of the general circulation is unequal heating of
Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa
Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa The Atmosphere in Motion Foundations, 6e - Chapter 13 Stan Hatfield Southwestern Illinois College Atmospheric pressure Force exerted by the weight
Global Winds AOSC 200 Tim Canty
Global Winds AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Global Wind Patterns Deserts Jet Stream Monsoons Ocean transport Ocean cycles Lecture 16 Oct 24
Section 3: Atmospheric Circulation
Section 3: Atmospheric Circulation Preview Key Ideas The Coriolis Effect Global Winds Local Winds Maps in Action Key Ideas Explain the Coriolis effect. Describe the global patterns of air circulation,
ATMOSPHERIC CIRCULATION. WIND = The horizontal movement of air. Results from the differences in air pressure. Always moves from HIGH to LOW.
ATMOSPHERIC CIRCULATION WIND = The horizontal movement of air. Results from the differences in air pressure. Always moves from HIGH to LOW. Pressure differences result from variations in temperature. AIR
AT350 EXAM #2 November 18, 2003
AT350 EXAM #2 November 18, 2003 Name and ID: Enter your name and student ID number on the answer sheet and on this exam. Record your answers to the 50 questions by using a No. 2 pencil to completely fill
SIO 210 Problem Set 3 November 4, 2011 Due Nov. 14, 2011
SIO 210 Problem Set 3 November 4, 2011 Due Nov. 14, 2011 1. At 20 N, both the ocean and the atmosphere carry approximately 2 PW of heat poleward, for a total of about 4 PW (see figure). If (at this latitude)
Ocean Currents Lecture Notes
Ocean Currents Lecture Notes (Topic 9A) page 1 Ocean Currents Lecture Notes Surface Currents Ocean Currents (What is an ocean current? How is a current different from a wave?) The water in an travels from
Climate & Earth System Science. Introduction to Meteorology & Climate. Chapter 07. Lecture 14. Global Scale Winds. Simple Introductory Examples:
Climate & Earth System Science Introduction to Meteorology & Climate MAPH 10050 Peter Lynch Peter Lynch Meteorology & Climate Centre School of Mathematical Sciences University College Dublin Meteorology
Chapter 6: Atmospheric Pressure, Wind, and Global Circulation
Discovering Physical Geography Third Edition by Alan Arbogast Chapter 6: Atmospheric Pressure, Wind, and Global Circulation Factors That Influence Air Pressure Air Pressure is the measured weight of air
Section 1. Global Wind Patterns and Weather. What Do You See? Think About It. Investigate. Learning Outcomes
Chapter 5 Winds, Oceans, Weather, and Climate Section 1 Global Wind Patterns and Weather What Do You See? Learning Outcomes In this section, you will Determine the effects of Earth s rotation and the uneven
Wind in the Atmosphere
Lesson 2 Wind in the Atmosphere ESSENTIAL QUESTION What is wind? By the end of this lesson, you should be able to explain how energy provided by the sun causes atmospheric movement, called wind. p 6.ESS2.2,
Ocean Currents Unit (4 pts)
Name: Section: Ocean Currents Unit (Topic 9A-1) page 1 Ocean Currents Unit (4 pts) Ocean Currents An ocean current is like a river in the ocean: water is flowing traveling from place to place. Historically,
OCEANOGRAPHY 101. Map, and temperature, salinity & density profiles of the water column at X, near mouth of the Columbia River.
OCEANOGRAPHY 101 EXAM 2 WINTER 00 NAME STUDENT NUMBER 1 Map, and temperature, salinity & density profiles of the water column at X, near mouth of the Columbia River. P a c i f i c O c e a n X WA Columbia
Weather & Atmosphere Study Guide
Weather & Atmosphere Study Guide 1. Draw a simple water cycle diagram using the following words: Precipitation, Evaporation, Condensation, Transpiration 2. In your own words, explain the difference between
The General Circulation and El Niño. Dr. Christopher M. Godfrey University of North Carolina at Asheville
The General Circulation and El Niño Dr. Christopher M. Godfrey University of North Carolina at Asheville Global Circulation Model Air flow broken up into 3 cells Easterlies in the tropics (trade winds)
Chapter. Air Pressure and Wind
Chapter Air Pressure and Wind 19.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. 19.1 Understanding Air Pressure Air Pressure Defined Air pressure
TOPICS YOU NEED TO KNOW
ATMO 101 Introduction to Meteorology Midterm Study Sheet Chapters 6, 7, 8 and 10 Exam Thursday 3/23/2017 Vocabulary Words for True and False, and Multiple Choice You are responsible for the following words:
6.1 Introduction to Weather Weather air mass Weather factors Temperature Pressure What is wind? Wind Convection in the atmosphere Thermals thermal
6.1 Introduction to Weather Weather is a term that describes the condition of the atmosphere in terms of temperature, atmospheric pressure, wind, and water. The major energy source for weather events is
Wind Patterns on Earth
Wind Patterns on Earth What causes air to move? Air pressure differences causes air to move. These differences in air pressure at the same altitude is caused by uneven heating of the Earth s surface. With
Chapter 10: Global Wind Systems
Chapter 10: Global Wind Systems Three-cell model of atmospheric circulation Intertropical Convergence Zone (ITCZ) Typical surface wind patterns Upper-level pressure and winds Climatological sea-level pressure
In Search of the Source of Wind.
In Search of the Source of Wind Role of Wind in the Voyage Atmospheric Pressure The Weight of Atmospheric Air on Earth Gravitational force helps Air to remain on Earth Variations in the Atmospheric Pressure
Exit Ticket: Coriolis Effect
Exit Ticket: Coriolis Effect 1. How does the Coriolis Effect influence the path of projectiles or wind traveling through the atmosphere? Causes them to curve 2. In which direction does the Coriolis Effect
Lornshill Academy. Geography Department Higher Revision Physical Environments - Atmosphere
Lornshill Academy Geography Department Higher Revision Physical Environments - Atmosphere Physical Environments Atmosphere Global heat budget The earth s energy comes from solar radiation, this incoming
Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are.
Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are. 1. A cool breeze is blowing toward the land from the ocean on a warm, cloudless summer day. This condition is
OCN 201 Surface Circulation
OCN 201 Surface Circulation Excess heat in equatorial regions requires redistribution toward the poles 1 In the Northern hemisphere, Coriolis force deflects movement to the right In the Southern hemisphere,
Air Pressure and Wind
Air Pressure and Wind 19.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. Air pressure is exerted in all directions down, up, and sideways. The
Length of day for a full year. Ocean Gyres. Wet. Adiabatic. lapse rate, starts at. dewpoint Dry Adiabatic lapse rate
Vernal Equinox March 20, 11:57 AM, CDT Sun will rise exactly in the east and set exactly in the west. All latitudes get 12 hours of day and 12 hours of dark. Length of day for a full year Wet Adiabatic
Circulation of the Atmosphere
Circulation of the Atmosphere World is made up of three regions: Atmosphere (air) Hydrosphere (water) Lithosphere (land) - Geosphere All regions interact to produce weather (day to day variations) and
REMINDERS: UPCOMING REVIEW SESSIONS: - Thursday, Feb 28, 6:30-8:00pm in CSB 002
REMINDERS: Midterm 2: Friday, March 1 - Lecture material covering chapters 6, 7, and 15 (since first midterm and through Wed lecture) - Multiple Choice, a few Short Answers, a few Definitions - Practice
ESCI 107 The Atmosphere Lesson 11 Global Circulation
Reading: Meteorology Today, Chapter 10 THE GLOBAL CIRCULATION ESCI 107 The Atmosphere Lesson 11 Global Circulation Latitudinal heat imbalance The tropics receive more radiation than they emit. The polar
Meteorology I Pre test for the Second Examination
Meteorology I Pre test for the Second Examination MULTIPLE CHOICE 1. A primary reason why land areas warm up more rapidly than water areas is that a) on land, all solar energy is absorbed in a shallow
Local and Global Winds
PART 2 Wind Local and Global Winds Wind is the horizontal movement of air. All wind is caused by air pressure differences due to the uneven heating of Earth's surface, which sets convection currents in
THE ATMOSPHERE. WEATHER and CLIMATE. The Atmosphere 10/12/2018 R E M I N D E R S. PART II: People and their. weather. climate?
R E M I N D E R S Two required essays are due by Oct. 30, 2018. (A third may be used for extra credit in place of a Think Geographically essay.) ESSAY TOPICS (choose any two): Contributions of a noted
Earth s Atmosphere. Air Currents
CHAPTER 12 Earth s Atmosphere LESSON 3 Air Currents What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with
Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all. interconnected as part of a single large global ocean.
Ocean Motion Met 101: Introduction to the World's Oceans Produced by The COMET Program Geography: Name Pd. Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all
Atmospheric Circulation
Atmospheric Circulation Why do we say Earth's temperature is moderate? It may not look like it, but various processes work to moderate Earth's temperature across the latitudes. Atmospheric circulation
Lesson: Ocean Circulation
Lesson: Ocean Circulation By Keith Meldahl Corresponding to Chapter 9: Ocean Circulation As this figure shows, there is a connection between the prevailing easterly and westerly winds (discussed in Chapter
Envs, Geol, Phys 112: Global Climate. Energy-Atmosphere System Review Aguado & Bert, Ch. 1, 2, 3, 4, 5, 6, 9, 10
Exam 1 Review Energy-Atmosphere System Review Aguado & Bert, Ch. 1, 2, 3, 4, 5, 6, 9, 10 Location on Earth (L04) Latitude & Longitude great circles, prime meridian, time zones, cardinal points, azimuth
Atmospheric and Ocean Circulation Lab
Atmospheric and Ocean Circulation Lab name Key Objectives: The main goal of this lab is to learn about atmospheric and oceanic circulation and how these two processes are strongly inter-dependent and strongly
Chapter 13 Lecture Outline. The Atmosphere in Motion
Chapter 13 Lecture Outline The Atmosphere in Motion Understanding Air Pressure Air pressure is the force exerted by weight of air above Weight of the air at sea level 14.7 psi or 1 kg/cm 2 Decreases with
For Class Today How does ocean water circulate? Ocean currents, surface currents, gyres, currents & climate, upwelling, deep ocean circulation
For Class Today Modified Cornell Notes on section 16.1 (pg. 448-453) **Follow the guide in your ISN and previous notes for help** Heading: How does ocean water circulate? Left hand side categories: Ocean
EARTH, PLANETARY, & SPACE SCIENCES 15 INTRODUCTION TO OCEANOGRAPHY. LABORATORY SESSION #6 Fall Ocean Circulation
EARTH, PLANETARY, & SPACE SCIENCES 15 INTRODUCTION TO OCEANOGRAPHY LABORATORY SESSION #6 Fall 2017 Ocean Circulation The focus of the Lab this week is circulation of the ocean and atmosphere. Here, you
Duckies have been found in Hawaii, Alaska, S. America, Scotland, Washington state and Australia as of 2012.
Duckies have been found in Hawaii, Alaska, S. America, Scotland, Washington state and Australia as of 2012. We learned that it takes 3 years to complete one circuit of the North Pacific Gyre flow in the
Wind in the Atmosphere
Lesson 1 Wind in the Atmosphere Essential Question What is wind? By the end of this lesson, you should be able to explain how energy provided by the sun causes atmospheric movement, called wind. 8.10A
6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of
6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of elements comprise the largest portion of oceans and atmosphere
8 th Grade Science Meteorology Review
8 th Grade Science Meteorology Review #1 Where does Earth get the energy that produces global weather patterns? A: The sun B: Humidity C: Air masses D: Cyclones A. The Sun #2 Do all of the areas on Earth
Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction. Idealized 3-Cell Model of Wind Patterns on a Rotating Earth. Previous Lecture!
Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction Previous Lecture! Global Winds General Circulation of winds at the surface and aloft Polar Jet Stream Subtropical Jet Stream Monsoons 1 2 Radiation
Physics 107 Ideas of Modern Physics
Physics 107 Ideas of Modern Physics Course home page: http://uw.physics.wisc.edu/~himpsel/107/lectures/lectures.htm Syllabus: http://uw.physics.wisc.edu/~himpsel/107/lectures/syllabus.pdf Course info:
Exploring Wind Energy
2013-2014 Exploring Wind Energy Student Guide SECONDARY Introduction to Wind What is Wind? Wind is simply air in motion. It is produced by the uneven heating of the Earth s surface by energy from the sun.
Chapter 9: Circulation of the Ocean
Chapter 9: Circulation of the Ocean Tropical gardens on Britain s Scilly Isles. Only 48 kilometers (30 miles) off the coast of Cornwall at 50 N, these scenic islands lie in the path of the warm waters
Atmospheric Circulation. Recall Vertical Circulation
Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and El Niño Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation
Applied Earth Science Climate Exam Practice Questions Page 1
Name: 1. Which combination of climate factors generally results in the coldest temperatures? A) low elevation and low latitude B) low elevation and high latitude C) high elevation and low latitude D) high
OCEANOGRAPHY STUDY GUIDE
OCEANOGRAPHY STUDY GUIDE Chapter 2 Section 1 1. Most abundant salt in ocean. Sodium chloride; NaCl 2. Amount of Earth covered by Water 71% 3. Four oceans: What are they? Atlantic, Pacific, Arctic, Indian
SURFACE CURRENTS AND TIDES
NAME SURFACE CURRENTS AND TIDES I. Origin of surface currents Surface currents arise due to the interaction of the prevailing wis a the ocean surface. Hence the surface wi pattern (Figure 1) plays a key
Small- and large-scale circulation
The Earth System - Atmosphere II Small- and large-scale circulation Atmospheric Circulation 1. Global atmospheric circulation can be thought of as a series of deep rivers that encircle the planet. 2. Imbedded
Lecture Outlines PowerPoint. Chapter 18 Earth Science 11e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 18 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
Prevailing Winds. The Coriolis Effect
Prevailing Winds 1. Wind: a movement of air in the atmosphere. Bill Nye wind (2 minutes) 2. Local or regional wind: occur in fairly small areas. 3. Prevailing winds: Major wind pattern that affect large
Lecture 15 General Circulation of the Atmosphere and Ocean
Lecture 15 General Circulation of the Atmosphere and Ocean Non-rotating model of atmospheric general circulation Hadley (1735) Cell is induced by uneven distribution of solar heating. Conceptual models
Enviro Sci 1A03 Quiz 3
Enviro Sci 1A03 Quiz 3 Question 1 (1 point) Which of the following measure wind direction and speed? Question 1 options: a) aerovane b) anemometer c) wind vane d) all of the above Question 2 (1 point)
The student will be expected to demonstrate an understanding of the cause of winds and how winds affect climate.
The student will be expected to demonstrate an understanding of the cause of winds and how winds affect climate. In this lesson you will: 2.3.1 Define the term prevailing winds. (k) 2.3.3 State the impact
El Nino/La Nina. What is El Nino? From NOAA website
El Nino/La Nina What is El Nino? From NOAA website El Nino was originally recognized by fishermen off the coast of South America as the appearance of unusually warm water in the Pacific Ocean, occurring
Wind and Wind Patterns
Wind and Wind Patterns What is Weather? Weather is the condition of Earth s atmosphere at a particular time and place. What is Wind? Wind is air moving across the surface of the Earth. It can move horizontally
9.3. Storing Thermal Energy. Transferring Thermal Energy
9.3 If you have been to a beach on a hot summer day, you have likely cooled off by going for a dip in the water. The water, which is cooler than you are, removes thermal energy from your body, making you
Global Wind Paerns. specific. higher. convection. rises. rotates. equator Equatorial. Subtropical High. long. lower. troposphere. sinks.
Global Wind Paerns Global Winds Winds that b steadily from direcons long over distances. specific Created by the of Earth s surface. Result of Sun striking the surface at angles near the equator and at
Private Bag X097, Pretoria, 0001 Tel: + 27 (0) USSD: *120*7297#
Private Bag X097, Pretoria, 0001 Tel: + 27 (0) 12 367 6000 www.weathersa.co.za USSD: *120*7297# FQZA31 FAPR 241330 SECURITE: ========= WEATHER BULLETIN FOR THE HIGH SEAS FOR METAREA VII. ISSUED BY THE
Equatorial upwelling. Example of regional winds of small scale
Example of regional winds of small scale Sea and land breezes Note on Fig. 8.11. Shows the case for southern hemisphere! Coastal upwelling and downwelling. Upwelling is caused by along shore winds, that
GEOGRAPHY UNIT 2 REVIEW. 1. The daily atmospheric conditions, such as heat, moisture and air movement for a particular area are known as
UNIT 2 REVIEW GEOGRAPHY Name: 1. The daily atmospheric conditions, such as heat, moisture and air movement for a particular area are known as 2. The average conditions of the weather for a long period
The atmospheric circulation system
The atmospheric circulation system Key questions Why does the air move? Are the movements of the winds random across the surface of the Earth, or do they follow regular patterns? What implications do these
6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of
6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of elements comprise the largest portion of oceans and atmosphere
Air Pressure and Wind. Goal: Explain the formation of wind based on differences in air pressure
Air Pressure and Wind Goal: Explain the formation of wind based on differences in air pressure What is Air Pressure? Reminder: Air pressure is thickest near Earth s surface and becomes thinner as we move
10% water in the world is tied up in the surface ocean currents. (above the pycnocline) Primary source is wind: Westerlies, Trades, Polar Easterlies
Oceanography Chapter 9 10% water in the world is tied up in the surface ocean currents. (above the pycnocline) Primary source is wind: Westerlies, Trades, Polar Easterlies Coriolis deflects winds (and
Ocean Currents Shortcut method by to learn faster
Ocean Currents Shortcut method by to learn faster In our geography notes on the hydrosphere, we have seen the major movements of the ocean water. They are waves, tides and ocean currents. Having covered
Ocean Currents Shortcut method by to learn faster
Ocean Currents Shortcut method by to learn faster In our geography notes on the hydrosphere, we have seen the major movements of the ocean water. They are waves, tides and ocean currents. Having covered