MAR 110 LECTURE #10 The Oceanic Conveyor Belt Oceanic Thermohaline Circulation
|
|
- Arline Page
- 6 years ago
- Views:
Transcription
1 1 MAR 110 LECTURE #10 The Oceanic Conveyor Belt Oceanic Thermohaline Circulation Ocean Climate Temperature Zones The pattern of approximately parallel oceanic surface isotherms (lines of constant temperature) reflects the equator to pole solar heating contrasts. (?)
2 2 Surface Ocean Heat Transport The latitudinal deviations in the isotherms reflect the effects of ocean surface currents, which consist of clockwise gyres with particularly intense currents along the western boundaries in northern hemisphere ocean basins (counterclockwise in the southern hemisphere ocean basins). The arrows show the effect on the surface temperature field by both the Gulf Stream and the Brazil Currents, which transport warm water from the equatorial region towards the poles. (??) Wind-Driven Surface Ocean Currents The juxtaposition of the zonal winds trades, westerlies and easteries produces gyre circulations with intensified western boundary currents in the major ocean basins the North & South Atlantic, North Pacific, and Indian Ocean basins. (LEiO)
3 3 The World s Oceans A Bartholomew projection of the geography of the oceans. Nearly three-fourths (72%) of the Earth s surface is covered by oceans
4 4 The Oceanic Conveyor Belt Moves Heat Poleward The oceanic conveyor belt consists of (1) sinking in the North Atlantic polar region - as the ocean gives up its heat to the atmosphere- (2) deep southward transport of the colder water to the Southern Ocean around Antarctica, (3) distribution to the Indian and Pacific Ocean basins (4) upwelling primarily along the equator, and (5) surface flow returning to the North Atlantic via a series of intensified western boundary currents caused by the surface winds (CCaMA) The Oceanic Conveyor Belt - ON The oceanic conveyor belt consists of (1) sinking in the North Atlantic polar region - as the ocean gives up its heat to the atmosphere- (2) deep southward transport of the colder water to the Southern Ocean around Antarctica, (3) distribution to the Indian and Pacific Ocean basins (4) upwelling primarily along the equator, and (5) surface flow returning to the North Atlantic via a series of intensified western boundary currents caused by the surface winds. (CCaMA)
5 5 The Oceanic Conveyor Belt - OFF In this configuration the oceanic conveyor belt the sinking component disappears because fresh water and ice inhibit sinking in the polar North Atlantic. Only the wind-driven warm surface flow remains. (CCaMA) Ocean Surface Temperature Distribution - NH Winter (??)
6 6 Salinity Salinity is the term used to reflect the saltiness of the water. Salts (and other constituents of ocean water) are derived from erosion of continental land masses slowly being carried into the ocean with river water. Eventually these salts became concentrated in the ocean and are now in a steady state (loss of salts to sedimentation and other processes equals the input of salt from river discharges). Many factors may affect the local salinity value in the ocean, including evaporation, precipitation, river input, and mixing between two water masses. Salinity is measured in units of parts per thousand (ppt).
7 7 Ocean Density Sensitivity to Temperature (T) & Salinity (S) The density of the ocean varies with respect to both temperature (negative relationship) and salinity (positive relationship).
8 8 Ocean Surface Salinity Distribution Graph of evaporation and surface salinity as a function of latitude (top). Map of surface salinity distribution over the globe (bottom). Note that regions with increased evaporation also have higher levels of salinity. (??,??) Ocean Temperature & Salinity & Density Profiles The changes of temperature, salinity, and density with increasing depth. The clines are regions where the particular property in question (temperature, salinity, or density) changes rapidly with depth. (ItO)
9 An Atlantic Ocean Density section (??) MAR 110: Lecture 10 Outline Oceanic Conveyor Belt 9
10 10 Global Ocean Thermohaline Circulation A rough schematic cross section of circulation between the poles. Cold water at the poles becomes dense as it cools and sinks to a depth dependant on the density with the coldest and densest water sinking the deepest. As the water warms it becomes less dense and rises. (??)
11 11 A Two Layered Atlantic Ocean Cold water at the poles becomes dense as it cools and sinks to a depth dependant on the density with the coldest and densest water sinking the deepest. A surface layer of warm, less dense water exists nearer the equator, separated from the deeper and colder water by the pycnocline, an area where the density changes rapidly with depth. (ItO)
12 12 Atlantic Ocean-Deep Western Boundary Current (DWBC) The DWBC is a current that originates in the Norwegian Sea as very cold and dense water that travels along the deep sea bed towards the south. (??) Gulf Stream & the Deep Western Boundary Current off of Cape Hatteras (BG)
13 13 The Oceanic Conveyor Belt Moves Heat Poleward The oceanic conveyor belt consists of (1) sinking in the North Atlantic polar region - as the ocean gives up its heat to the atmosphere- (2) deep southward transport of the colder water to the Southern Ocean around Antarctica, (3) distribution to the Indian and Pacific Ocean basins (4) upwelling primarily along the equator, and (5) surface flow returning to the North Atlantic via a series of intensified western boundary currents caused by the surface winds. (CCaMA)
Surface Circulation Ocean current Surface Currents:
All Write Round Robin G1. What makes up the ocean water? G2. What is the source of the salt found in ocean water? G3. How does the water temperature affect the density of ocean water? G4. How does the
More informationDirected Reading. Section: Ocean Currents. a(n). FACTORS THAT AFFECT SURFACE CURRENTS
Skills Worksheet Directed Reading Section: Ocean Currents 1 A horizontal movement of water in a well-defined pattern is called a(n) 2 What are two ways that oceanographers identify ocean currents? 3 What
More informationUpper Ocean Circulation
Upper Ocean Circulation C. Chen General Physical Oceanography MAR 555 School for Marine Sciences and Technology Umass-Dartmouth 1 MAR555 Lecture 4: The Upper Oceanic Circulation The Oceanic Circulation
More informationWeather & Ocean Currents
Weather & Ocean Currents Earth is heated unevenly Causes: Earth is round Earth is tilted on an axis Earth s orbit is eliptical Effects: Convection = vertical circular currents caused by temperature differences
More informationOceans I Notes. Oceanography
Oceans I Notes Outlines on the front table Oceanography the science of our oceans that mixes biology, geology, chemistry, and physics (among other sciences) to unravel the mysteries of our seas. Divisions
More informationHYDROSPHERE NOTES. Water cycle: The continuous movement of water into the air, onto land, and then back to water sources.
Hon Environmental Science HYDROSPHERE NOTES The Hydrosphere and the Water Cycle: Water cycle: The continuous movement of water into the air, onto land, and then back to water sources. Evaporation: the
More informationOcean Mixing and Climate Change
Ocean Mixing and Climate Change Factors inducing seawater mixing Different densities Wind stirring Internal waves breaking Tidal Bottom topography Biogenic Mixing (??) In general, any motion favoring turbulent
More information1. Introduction 2. Ocean circulation a) Temperature, salinity, density b) Thermohaline circulation c) Wind-driven surface currents d) Circulation and
1. Introduction 2. Ocean circulation a) Temperature, salinity, density b) Thermohaline circulation c) Wind-driven surface currents d) Circulation and climate change e) Oceanic water residence times 3.
More informationCurrents & Gyres Notes
Currents & Gyres Notes Current A river of water flowing in the ocean. 2 Types of Currents Surface Currents wind-driven currents that occur in the top 100m or less Deep Currents density-driven currents
More informationWinds and Currents in the Oceans
Winds and Currents in the Oceans Atmospheric Processes Density of air is controlled by temperature, pressure, and moisture content. 1. Warm air is less dense than cold air and moist air is less dense than
More informationAlmost of Earth is covered by water. On a map, the continents appear as huge islands surrounded by a vast global ocean.
Earth s Oceans & Ocean Floor Date: Feelin Blue What are Earth s five main oceans? Almost of Earth is covered by water. On a map, the continents appear as huge islands surrounded by a vast global ocean.
More informationThe Dynamic Earth Section 3. Chapter 3 The Dynamic Earth Section 3: The Hydrosphere and Biosphere DAY 1
Chapter 3 The Dynamic Earth Section 3: The Hydrosphere and Biosphere DAY 1 The Hydrosphere The hydrosphere includes all of the water on or near the Earth s surface. This includes water in the oceans, lakes,
More informationSurface Circulation. Key Ideas
Surface Circulation The westerlies and the trade winds are two of the winds that drive the ocean s surface currents. 1 Key Ideas Ocean water circulates in currents. Surface currents are caused mainly by
More informationActual bathymetry (with vertical exaggeration) Geometry of the ocean 1/17/2018. Patterns and observations? Patterns and observations?
Patterns and observations? Patterns and observations? Observations? Patterns? Observations? Patterns? Geometry of the ocean Actual bathymetry (with vertical exaggeration) Continental Continental Basin
More informationEarth/Environmental Science Oceanography
Earth/Environmental Science Oceanography Name Part I. Modeling Deep Ocean Currents LAB: Ocean Circulation and Climate DIRECTIONS DO NOT RINSE the container between solutions! A. Effect of Temperature 1.
More informationDensity, Salinity & Temperature
Density, Salinity & Temperature Density and Oceans l Density = how much mass is contained in a given unit volume (density = mass/volume). l Temperature, salinity and pressure work together to determine
More informationCHAPTER 7 Ocean Circulation Pearson Education, Inc.
CHAPTER 7 Ocean Circulation 2011 Pearson Education, Inc. Types of Ocean Currents Surface currents Deep currents 2011 Pearson Education, Inc. Measuring Surface Currents Direct methods Floating device tracked
More informationisopycnal outcrop w < 0 (downwelling), v < 0 L.I. V. P.
Ocean 423 Vertical circulation 1 When we are thinking about how the density, temperature and salinity structure is set in the ocean, there are different processes at work depending on where in the water
More informationThe Planetary Circulation System
12 The Planetary Circulation System Learning Goals After studying this chapter, students should be able to: 1. describe and account for the global patterns of pressure, wind patterns and ocean currents
More informationOcean Currents and Climate
Ocean Currents and Climate Ocean water contains streamlike movements of water called ocean currents. Currents are influenced by a number of factors, including weather, the Earth's rotation, and the position
More informationDeep Ocean Circulation & implications for Earth s climate
Deep Ocean Circulation & implications for Earth s climate I. Ocean Layers and circulation types 1) Ocean Layers Ocean is strongly Stratified Consists of distinct LAYERS controlled by density takes huge
More informationBiome type of plant and animal community that covers large geographic areas
1 Physical Environment: Atmosphere and Oceans - Circulation EVPP 110 Lecture Fall 2003 Dr. Largen 2 Global Environments 3 Biome type of plant and animal community that covers large geographic areas Global
More informationOceanography Quiz 2. Multiple Choice Identify the choice that best completes the statement or answers the question.
Oceanography Quiz 2 Multiple Choice Identify the choice that best completes the statement or answers the question. 1. The highest and lowest tides are known as the spring tides. When do these occur? a.
More information2/15/2012. Earth System Science II EES 717 Spring 2012
Earth System Science II EES 717 Spring 2012 1. The Earth Interior Mantle Convection & Plate Tectonics 2. The Atmosphere - Climate Models, Climate Change and Feedback Processes 3. The Oceans Circulation;
More informationBasic Ocean Current Systems. Basic Ocean Structures. The State of Oceans. Lecture 6: The Ocean General Circulation and Climate. Temperature.
Lecture 6: The Ocean General Circulation and Climate Basic Ocean Current Systems Upper Ocean surface circulation Basic Structures Mixed Layer Wind-Driven Circulation Theories Thermohaline Circulation Ocean
More information4.3 Climate (6.3.3) Explore this Phenomena. The same sun shines on the entire Earth. Explain why these two areas have such different climates.
Explore this Phenomena The same sun shines on the entire Earth. 4.3 Climate (6.3.3) Explain why these two areas have such different climates. 89 6.3.3 Climate Develop and use a model to show how unequal
More informationTEMPERATURE AND DEEP OCEAN CIRCULATION
TEMPERATURE AND DEEP OCEAN CIRCULATION OVERVIEW Ocean currents arise in several ways. For example, wind pushes the water along the surface to form wind-driven currents. Over larger areas, circular wind
More information1 Earth s Oceans. TAKE A LOOK 2. Identify What are the five main oceans?
CHAPTER 13 1 Earth s Oceans SECTION Exploring the Oceans BEFORE YOU READ After you read this section, you should be able to answer these questions: What affects the salinity of ocean water? What affects
More informationActivity #2 - Major Ocean Surface Currents
Activity #2 - Major Ocean Surface Currents Concepts # 3 & 6 # 3 Atmospheric cells and ocean gyres redistribute heat from low to high latitudes, which influences climate, weather, and ocean temperature.
More informationEarth s Oceans. Divisions of the Global Ocean
Earth s Oceans 1 Key Concept The characteristics of ocean water, such as temperature and salinity, affect the circulation of the ocean. What You Will Learn Earth is unique in our solar system because 71%
More informationSun, Moon, Hydrosphere Worksheet - Answers
Sun, Moon, Hydrosphere Worksheet - Answers Question 1 WHAT TERM CORRESPONDS TO EACH OF THE FOLLOWING DEFINITIONS? a) a landform, slope or terrain that can affect water circulation b) the Earth s blue envelope
More informationWhat is a system? What do the arrows in this diagram represent? What do the boxes represent? Why is it useful to study and understand systems?
Systems What is a system? What do the arrows in this diagram represent? What do the boxes represent? Why is it useful to study and understand systems? evaporation River & Lake water rain Atmosphere Water
More informationPhysical Oceanography
Physical Oceanography SECTION 15.1 The Oceans In your textbook, read about modern oceanography. For each item in Column A, write the letter of the matching item in Column B. Column A 1. German research
More informationPhysical Oceanography
Physical Oceanography SECTION 15.1 The Oceans In your textbook, read about modern oceanography. For each item in Column A, write the letter of the matching item in Column B. e b c d a Column A 1. German
More informationHomework 5: Background Ocean Water Properties & Stratification
14 August 2008 MAR 110 HW5: Ocean Properties 1 Homework 5: Background Ocean Water Properties & Stratification The ocean is a heterogeneous mixture of water types - each with its own temperature, salinity,
More informationMAR110 LECTURE #22 Climate Change
MAR 110: Lecture 22 Outline Climate Change 1 MAR110 LECTURE #22 Climate Change Climate Change Diagnostics Drought and flooding represent just a couple of hazards related to climate variability (O) The
More informationOcean Circulation. In partnership with Dr. Zafer Top
Ocean Circulation In partnership with Dr. Zafer Top Samantha Hampton Honors Science December 15, 2014 Ocean Circulation is the large scale movement of waters in the ocean basins. Dr. Zafer Top studies
More informationScience 1206 Chapter 1 - Inquiring about Weather
Science 1206 Chapter 1 - Inquiring about Weather 1.1 - The Atmosphere: Energy Transfer and Properties (pp. 10-25) Weather and the Atmosphere weather the physical conditions of the atmosphere at a specific
More informationGlobal Weather Trade Winds etc.notebook February 17, 2017
Global Weather 1 north pole northern hemisphere equator southern hemisphere south pole 2 We have seasons because of the Earth's tilt The seasons are opposite in the northern and southern hemispheres winter
More informationThe surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are
11.1 Ocean Basins The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are w the Pacific w the Atlantic w the Indian w the Southern w the Arctic The
More informationHomework. Oceanography and Climate Review due Friday Feb 12 th (test day!!)
Homework Oceanography and Climate Review due Friday Feb 12 th (test day!!) Learning Targets I can define the term climate and explain the factors that influence the climate of an area. I can identify the
More informationThe Deep Circulation of the Ocean
Activity 2 The Deep Circulation of the Ocean Activity 2 The Deep Circulation of the Ocean Goals In this activity you will: Understand how water temperature affects circulation within a body of water. Understand
More informationPlease be ready for today by:
Please be ready for today by: 1. HW out for a stamp 2. Paper and pencil/pen for notes 3. Be ready to discuss what you know about El Nino after you view the video clip What is El Nino? El Nino Basics El
More informationOcean surface circulation
Ocean surface circulation Recall from Last Time The three drivers of atmospheric circulation we discussed: Differential heating Pressure gradients Earth s rotation (Coriolis) Last two show up as direct
More informationPart 1. Ocean Composition & Circulation
OCN 401 Biogeochemical Systems (10.19.17) (Schlesinger: Chapter 9) Part 1. Ocean Composition & Circulation 1. Introduction Lecture Outline 2. Ocean Circulation a) Global Patterns in T, S, ρ b) Thermohaline
More informationCHAPTER 2 - ATMOSPHERIC CIRCULATION & AIR/SEA INTERACTION
Chapter 2 - pg. 1 CHAPTER 2 - ATMOSPHERIC CIRCULATION & AIR/SEA INTERACTION The atmosphere is driven by the variations of solar heating with latitude. The heat is transferred to the air by direct absorption
More informationLecture 3 questions Temperature, Salinity, Density and Circulation
Lecture 3 questions Temperature, Salinity, Density and Circulation (1) These are profiles of mean ocean temperature with depth at various locations in the ocean which in the following (a, b, c) figures
More informationThe Ocean Conveyor Belt
6E3 Earth s Water The Ocean onveyor elt Lexile 700L 1 Water in the ocean is always moving. Waves break the surface. urrents move in the shallows and in the depths. urrents near the surface are mainly caused
More informationWhere is all the water?
Where is all the water? The distribution of water at the Earth's surface % of total Oceans 97.25 Ice caps and glaciers 2.05 Groundwater 0.68 Lakes 0.01 Soils 0.005 Atmosphere (as vapour) 0.001 Rivers 0.0001
More informationMidterm 2: Nov. 20 (Monday)
Introduction to Oceanography Lecture 18, Current 2 Surface Ocean Currents. Video by Chris Henze, NASA Ames, Public Domain Midterm 2: Nov. 20 (Monday) Review Session & Video Screenings TBA Image from Sverdrup,
More information5.1. Weather, climate, and components of the climate system
5. The climate system 5.1. Weather, climate, and components of the climate system The weather is characterized by the atmospheric conditions (e.g. temperature, precipitations, cloud cover, wind speed)
More informationChapter 4. Understanding the Weather. Weather is short-term and caused by various air and ocean circulations
Video: Meteorologist Paul Douglas April 2013 Understanding the Weather Weather is short-term and caused by various air and ocean circulations There are natural climate cycle that cause large climate changes
More informationWebsite Lecture 3 The Physical Environment Part 1
Website http://websites.rcc.edu/halama Lecture 3 The Physical Environment Part 1 1 Lectures 3 & 4 1. Biogeochemical Cycling 2. Solar Radiation 3. The Atmosphere 4. The Global Ocean 5. Weather and Climate
More informationWinds and Global Circulation
Winds and Global Circulation Atmospheric Pressure Winds Global Wind and Pressure Patterns Oceans and Ocean Currents El Nino How is Energy Transported to its escape zones? Both atmospheric and ocean transport
More informationMAR 110 LECTURE #9 Earth s Heat Budget / Atmosphere Dynamics
MAR 110: Lecture 9 Outline Heat Budget / Atmosphere Dynamics 1 MAR 110 LECTURE #9 Earth s Heat Budget / Atmosphere Dynamics External Energy Source-the Sun The portion of the sun s energy that is intercepted
More informationMarine Ecoregions. Marine Ecoregions. Slide 1. Robert G. Bailey. USDA Forest Service Rocky Mountain Research Station
Slide 1 Marine Ecoregions Robert G. Bailey Marine Ecoregions Robert G. Bailey USDA Forest Service Rocky Mountain Research Station rgbailey@fs.fed.us Draft of 7/20/2006 8:44 PM Abstract: Oceans occupy some
More informationThe Ocean Floor THE VAST WORLD OCEAN
OCEANOGRAPHY Name Color all water LIGHT BLUE. Color all land LIGHT GREEN. Label the 5 Oceans: Pacific, Atlantic, Indian, Arctic, Antarctic. Label the 7 Continents: N.America, S.America, Europe, Asia, Africa,
More informationOcean Sciences 101 The Marine Environment OCEA 101 THE MARINE ENVIRONMENT MID-TERM EXAM
OCEA 101 THE MARINE ENVIRONMENT MID-TERM EXAM Part I. Multiple Choice Questions. Choose the one best answer from the list, and write the letter legibly in the blank to the left of the question. 2 points
More informationGlobal Wind Patterns
Name: Earth Science: Date: Period: Global Wind Patterns 1. Which factor causes global wind patterns? a. changes in the distance between Earth and the Moon b. unequal heating of Earth s surface by the Sun
More informationRISING SEA. Reading Practice. Paragraph 1. INCREASED TEMPERATURES
Reading Practice RISING SEA Paragraph 1. INCREASED TEMPERATURES The average air temperature at the surface of the earth has risen this century, as has the temperature of ocean surface waters. Because water
More informationWater percolating through hot lava dissolves soluble minerals containing chlorine, bromine and sulphur compounds
Figure 5 The sources of dissolved ions in sea water. Water falls as rain Compounds containing mainly calcium, magnesium, carbonate and silicate ions are leached from the soil Rivers carry ions in solution
More informationChapter 9 External Energy Fuels Weather and Climate
Natural Disasters Tenth Edition Chapter 9 External Energy Fuels Weather and Climate Copyright The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 9-1 Weather Versus Climate
More informationOceanography. Oceanography is the study of the deep sea and shallow coastal oceans.
Oceanography Oceanography is the study of the deep sea and shallow coastal oceans. Studying the Ocean Floor To determine the shape and composition of the ocean floor, scientists use techniques such as
More informationclimate system and its subcomponents: the atmosphere, ocean, land surface, Prof. Jin-Yi Yu ESS200A A general description of the Earth
Earth System Climate () Course Time Lectures: Tu, Th 9:30-10:20 Discussion: 3315 Croul Hall Text Book The Earth System, Kump, Kasting, and Crane, Prentice-Hall Global Physical Climatology, Hartmann; Academic
More informationI. Ocean Layers and circulation types
OCEAN Title CIRCULATION slide I. Ocean Layers and circulation types 1) Ocean Layers Ocean is strongly Stratified Consists of distinct LAYERS controlled by density takes huge amounts of energy to mix up
More information2. Can you describe how temperature and dissolved solids changes the density of water?
Unit 4: Oceanography LT 4.1 Density: I can explain the role density plays to help form some currents. #1 Yes I can: 1. Can you explain what density is and how you calculate it? 2. Can you describe how
More informationI. Ocean Layers and circulation types
OCEAN CIRCULATION I. Ocean Layers and circulation types 1) Ocean Layers Ocean is strongly Stratified Consists of distinct LAYERS controlled by density takes huge amounts of energy to mix up the stable
More informationIELTS Academic Reading Sample 1 - Rising Sea RISING SEA
IELTS Academic Reading Sample 1 - Rising Sea You should spend about 20 minutes on Questions 15-28 which are based on Reading Passage 1 below. RISING SEA Paragraph 1 - INCREASED TEMPERATURES The average
More informationMAR110 LECTURE #28 Climate Change I
25 November 2007 MAR 110 Lec28 Climate Change I 1 MAR110 LECTURE #28 Climate Change I Figure 28.1 Climate Change Diagnostics Drought and flooding represent just a couple of hazards related to climate variability
More informationSIO 210 Final examination Answer Key for all questions except Daisyworld. Wednesday, December 10, PM Name:
SIO 210 Final examination Answer Key for all questions except Daisyworld. Wednesday, December 10, 2008 3-6 PM Name: This is a closed book exam. You may use a calculator. There are two parts: Talley (weighted
More informationWind: Global Systems Chapter 10
Wind: Global Systems Chapter 10 General Circulation of the Atmosphere General circulation of the atmosphere describes average wind patterns and is useful for understanding climate Over the earth, incoming
More informationLecture 1. Amplitude of the seasonal cycle in temperature
Lecture 6 Lecture 1 Ocean circulation Forcing and large-scale features Amplitude of the seasonal cycle in temperature 1 Atmosphere and ocean heat transport Trenberth and Caron (2001) False-colour satellite
More information1. Oceans. Example 2. oxygen.
1. Oceans a) Basic facts: There are five oceans on earth, making up about 72% of the planet s surface and holding 97% of the hydrosphere. Oceans supply the planet with most of its oxygen, play a vital
More informationLecture 4:the observed mean circulation. Atmosphere, Ocean, Climate Dynamics EESS 146B/246B
Lecture 4:the observed mean circulation Atmosphere, Ocean, Climate Dynamics EESS 146B/246B The observed mean circulation Lateral structure of the surface circulation Vertical structure of the circulation
More informationRapid Climate Change: Heinrich/Bolling- Allerod Events and the Thermohaline Circulation. By: Andy Lesage April 13, 2010 Atmos.
Rapid Climate Change: Heinrich/Bolling- Allerod Events and the Thermohaline Circulation By: Andy Lesage April 13, 2010 Atmos. 6030 Outline Background Heinrich Event I/Bolling-Allerod Transition (Liu et
More informationLevel 3 Earth and Space Science, 2016
91413 914130 3SUPERVISOR S Level 3 Earth and Space Science, 2016 91413 Demonstrate understanding of processes in the ocean system 2.00 p.m. Wednesday 30 November 2016 Credits: Four Achievement Achievement
More informationPathways in the ocean
Pathways Pathways in the in the ocean by Sybren Drijfhout Introduction The properties of water masses in the ocean are set by air-sea interactions at the surface and convective overturning. As direct transfer
More informationVersion2 Fall True/False Indicate whether the sentence or statement is true or false.
Version2 Fall 2004 True/False Indicate whether the sentence or statement is true or false. 1. Short residence time elements are found in the greatest concentration near their point of removal from the
More informationThe Hydrosphere ART9.1. Name: Period: 1. How much of the Earth s mass is in the hydrosphere? 2. How much of the Earth s surface is covered in oceans?
ART9.1 Question 1. How much of the Earth s mass is in the hydrosphere? Name: Period: Answer 2. How much of the Earth s surface is covered in oceans? 3. How much of the Earth s water is found in oceans,
More informationOcean and Climate I.
Ocean and Climate I http://www.gerhardriessbeck.de/ Physical Characteristics of the Ocean Surface area: 3.61 10 14 m 2 Mean depth: 3.7 km Ocean volume: 3.2 10 17 m 3 Mean density: 1.035 10 3 kg/m 3 Ocean
More informationThe Transfer of Heat
The Transfer of Heat Outcomes: S2-4-03 Explain effects of heat transfer within the atmosphere and hydrosphere on the development and movement of wind and ocean currents. Coriolis Effect In our ecology
More informationReal World Globes Investigating Surface Currents around the Globe Authored by Ryan Glaubke, Graduate Student at Old Dominion University, Norfolk, VA
Real World Globes Investigating Surface Currents around the Globe Authored by Ryan Glaubke, Graduate Student at Old Dominion University, Norfolk, VA Purpose: - To practice basic plotting techniques using
More informationOcean Boundary Currents Guiding Question: How do western boundary currents influence climate and ocean productivity?
Name: Date: TEACHER VERSION: Suggested Student Responses Included Ocean Boundary Currents Guiding Question: How do western boundary currents influence climate and ocean productivity? Introduction The circulation
More informationLand Surface Sea Ice Land Ice. (from Our Changing Planet)
Lecture 5: Land Surface and Cryosphere (Outline) Land Surface Sea Ice Land Ice (from Our Changing Planet) Earth s s Climate System Solar forcing Atmosphere Ocean Land Solid Earth Energy, Water, and Biochemistry
More informationCHAPTER 9 ATMOSPHERE S PLANETARY CIRCULATION MULTIPLE CHOICE QUESTIONS
CHAPTER 9 ATMOSPHERE S PLANETARY CIRCULATION MULTIPLE CHOICE QUESTIONS 1. Viewed from above in the Northern Hemisphere, surface winds about a subtropical high blow a. clockwise and inward. b. counterclockwise.
More informationLecture 9: General Circulation Explains Why There are Tropical Easterlies
Lecture 9: General Circulation Single-Cell Model: Explains Why There are Tropical Easterlies JS JP Hadley Cell Ferrel Cell (driven by eddies) Polar Cell Without Earth Rotation With Earth Rotation L H L
More informationLecture 9: General Circulation
Lecture 9: General Circulation JS JP Hadley Cell Ferrel Cell (driven by eddies) Polar Cell L H L H Three-Cell Circulation in the Atmosphere Gyres in the Oceans Single-Cell Model: Explains Why There are
More informationEarth s Climate System. Surface Albedo. Climate Roles of Land Surface. Lecture 5: Land Surface and Cryosphere (Outline) Land Surface Sea Ice Land Ice
Lecture 5: Land Surface and Cryosphere (Outline) Earth s Climate System Solar forcing Land Surface Sea Ice Land Ice Atmosphere Ocean Land Solid Earth Energy, Water, and Biochemistry Cycles (from Our Changing
More informationEarth s Climate Patterns
Earth s Climate Patterns Reading: Chapter 17, GSF 10/2/09 Also Jackson (linked on course web site) 1 What aspects of climate affect plant distributions? Climate: long-term distribution of weather in an
More informationSeawater Chemistry and Chemical Oceanography. The Universal Solvent. Sphere of Hydration
Seawater Chemistry and Chemical Oceanography The Universal Solvent Polarity of molecule makes water very effective at hydrating even weakly charged ions Sphere of Hydration Polarity of water molecules
More informationBell Work. REVIEW: Our Planet Earth Page 29 Document A & B Questions
9.12.16 Bell Work REVIEW: Our Planet Earth Page 29 Document A & B Questions Intro to Climate & Weather https://www.youtube.com/watch?v=vhgyoa70q7y Weather vs. Climate Video Climate & Weather 3.1 Weather
More informationHow Will Melting Ice Sheets Affect Us?
PASSAGE 4 How Will Melting Ice Sheets Affect Us? Variation is normal. During the last ice age, for example, ice sheets also covered much of North America and Scandinavia. Why is what s happening now different
More information1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures?
CHAPTER 17 1 What Is Climate? SECTION Climate BEFORE YOU READ After you read this section, you should be able to answer these questions: What is climate? What factors affect climate? How do climates differ
More informationProject Retrograde imagine Earth rotated in the opposite direction
Project Retrograde imagine Earth rotated in the opposite direction The rotation of Earth shapes our climate system in various ways: It controls the major wind directions, lets the weather systems swirl,
More informationATOC OUR CHANGING ENVIRONMENT Class 19 (Chp 6) Objectives of Today s Class: The Cryosphere [1] Components, time scales; [2] Seasonal snow
ATOC 1060-002 OUR CHANGING ENVIRONMENT Class 19 (Chp 6) Objectives of Today s Class: The Cryosphere [1] Components, time scales; [2] Seasonal snow cover, permafrost, river and lake ice, ; [3]Glaciers and
More informationJacob Schewe Potsdam Institute for Climate Impact Research. Ocean circulation under climate change: Examples of qualitative changes
Jacob Schewe Potsdam Institute for Climate Impact Research Ocean circulation under climate change: Examples of qualitative changes Acknowledgments Anders Levermann Potsdam Institute for Climate Impact
More informationThermohaline Circulation
OCEAN CIRCULATION / Thermohaline Circulation 1549 distinctly nonsteady character of the ocean circulation. Ocean currents are remarkably variable. Variability on much shorter time scales of weeks and months,
More informationThe North Atlantic Oscillation: Climatic Significance and Environmental Impact
1 The North Atlantic Oscillation: Climatic Significance and Environmental Impact James W. Hurrell National Center for Atmospheric Research Climate and Global Dynamics Division, Climate Analysis Section
More informationWhat makes the Arctic hot?
1/3 total USA UN Environ Prog What makes the Arctic hot? Local communities subsistence Arctic Shipping Routes? Decreasing Ice cover Sept 2007 -ice extent (Pink=1979-2000 mean min) Source: NSIDC Oil/Gas
More informationESS15 Lecture 13. End of the oceans (tropical / El Nino, thermohaline circulation) Weather vs. climate.
ESS15 Lecture 13 End of the oceans (tropical / El Nino, thermohaline circulation) Weather vs. climate. Please give me feedback through the EEE midterm evaluation survey. I promise to adapt to it. Review
More information