# Dynamics IV: Geostrophy SIO 210 Fall, 2014

Save this PDF as:

Size: px
Start display at page:

Download "Dynamics IV: Geostrophy SIO 210 Fall, 2014"

## Transcription

1 Dynamics IV: Geostrophy SIO 210 Fall, 2014 Geostrophic balance Thermal wind Dynamic height READING: DPO: Chapter (S)7.6.1 to (S)7.6.3 Stewart chapter 10.3, 10.5, 10.6 (other sections are useful for those of you wishing more dynamics

2 Example from atmosphere of nearly geostrophic flow NWS daily weather map High and low pressure centers Winds blow around the highs and lows Clockwise around the highs (northern hemisphere) due to Coriolis

3 Coriolis effect at very short time scales? NO What about your bathroom sink? Can you see the Coriolis effect on the spiral of water? NO, unless you have an extremely good laboratory! WHY? Because time scale is much shorter than 1 day (Pressure gradient force or sloshing force is balanced by acceleration, not Coriolis)

4 Geostrophy: PGF balanced by Coriolis force Northern hemisphere: flow to the right of the PGF

5 Other views Looking down onto the ocean (Northern hemisphere examples for velocity directions) Looking at a crosssection Think of ball rolling down hill from high to low pressure, turning to the right due to Coriolis DPO Fig. 7.9

6 Complete force balance with rotation Three equations: Horizontal (x) (west-east) acceleration + advection + Coriolis = Inertial motion Geostrophic flow pressure gradient force + viscous term Horizontal (y) (south-north) acceleration + advection + Coriolis = pressure gradient force + viscous term Vertical (z) (down-up) acceleration +advection (+ neglected very small Coriolis) = pressure gradient force + effective gravity (including centrifugal force) + viscous term

7 Geostrophic (and hydrostatic) force balance Three (approximate) equations: Horizontal (x) (west-east) Coriolis = pressure gradient force - fv = - (1/ρ) p/ x Horizontal (y) (south-north) Coriolis = pressure gradient force fu = - (1/ρ) p/ y Vertical (z) (down-up) 0 = pressure gradient force + effective gravity 0 = - (1/ρ) p/ z - g

8 Definitions: Cyclonic and Anticyclonic NWS daily weather map Cyclonic: around a low pressure center Anticyclonic: around a high pressure center Cyclonic is counterclockwise in the northern hemisphere, clockwise in the southern hemisphere

9 Example from ocean of geostrophic flow Surface height/pressure and surface geostrophic circulation Circulation is counterclockwise around the Low LOW HIGH LOW LOW (cyclonic) and clockwise around the High (anticyclonic)." (northern hemisphere)" LOW HIGH LOW Southern Hem:" LOW Cyclonic is clockwise, etc.." Reid, 1997

10 Sea surface height Compare with surface circulation (next slide)

11 Gulf Stream Surface (geostrophic) circulation schematic Antarctic Circumpolar Current DPO Fig after Schmitz (1995)

12 Low Vertical structure of the circulation (Atlantic section of potential density) High pressure Antarctic Circumpolar Current DPO Fig. 4.10

13 To observe geostrophic circulation Density (temperature, salinity) is what we measure for the most part Current speed and direction is what we want We can t measure the sea surface height accurately enough (this will change with improved observing systems, but is historically the case) Steady-state isopycnal slopes tell us that the geostrophic current is varying with depth ( vertically sheared ) Most currents we see are wind-driven and therefore strongest at the sea surface, decaying with depth We therefore make a very educated (or very uneducated guess) at the current speed and direction at some depth, and use the density field to figure out how the current changes with depth AT THAT LOCATION in latitude and longitude Another example - Gulf Stream ----->>

14 Gulf Stream vertical sections in Florida Strait (west on left) (ignore blobbiness of contouring) 160 cm/sec Roemmich, 1983

15 Thermal wind ( geostrophic method ): How does the geostrophic flow change with depth (below the sea surface)? Look at mass (density) distribution Near the sea surface (at h 1 ), there is more mass at B than at A, so there is higher pressure at B than at A, so there is a westward PGF and northward flow (northern hemisphere). Farther down (at h 2 ), the difference in mass above h 2 at B and A is smaller since the density at B is lower than an A. So the pgf is smaller and the current is weaker. Density at A is higher than density at B ρ A > ρ B Even farther down (at h 3 ), we can have equal mass (equal pressure, hence NO pgf) since total mass at B and A is the SAME. DPO Fig. S7.20

16 Thermal wind ( geostrophic method ): slide 2 Now assume that density varies continuously. We measure density (RED lines). The slope down to the right means that flow increases into the page with height (decreases with depth) We assume (or measure) that velocity is, say, 0 at depth 3. Therefore the pressure contour p 3 must be flat there. (And below level 3, the flow would start going back the other way, out of the page) DPO Fig. 7.10

17 Dynamic height and geopotential anomaly: proxies for pressure The pgf is calculated as the difference of pressure between two stations at a given depth (flat surface relative to the geoid). a) If the velocity is known at a given depth, then the pgf at that depth is also known (from geostrophy) b) From the measured density profiles at the two stations, we can calculate how the pgf changes with depth, which tells us the velocity change with depth. c) Using the known velocity from (a), which we call the reference velocity, and knowing how velocity changes with depth from (b), we can compute velocity at every depth.

18 Thermal wind (formal expressions) Thermal wind relation formally: - f v/ z = (g/ρ o ) ρ/ x f u/ z = (g/ρ o ) ρ/ y Relates vertical shear to horizontal density variations

19 Geopotential anomaly and dynamic height To get the change in pgf from depth 1 to 2, get the mass of water on both profiles between depths 1 and 2. Historically use the specific volume anomaly δ, which is δ = α - α(35, 0, p) where α = 1/ρ is specific volume. Then choose/measure/guess the reference velocity at, say, depth 1 and compute velocity at depth 2 ΔΦ = - δ dp geopotential anomaly f (v 2 - v 1 ) = - ΔΦ/ x (8.26a) f (u 2 - u 1 ) = ΔΦ/ y (8.26b) OR ΔD = -ΔΦ / 10= - δ dp /10 dynamic height 1 dyn m = 10 m 2 /sec 2 f (v 2 - v 1 ) = 10 ΔD/ x (8.26a) f (u 2 - u 1 ) = - 10 ΔD/ y (8.26b)

20 Geopotential anomaly and dynamic height Reference velocities: Level of no motion: Old-fashioned - assume 0 velocity at some great depth, and compute velocities at all shallower depths. This is useful if you are focused on very energetic upper ocean flows, but not useful if you want to look at small deep flows. Level of known motion: Much better - observe or determine through external means (use of tracers, mass balance, etc) a good guess at the velocity at some depth. This is essential if you want to study deep circulation.

21 Gulf Stream density, dynamic height and geostrophic velocity In this example, compute geostrophic velocities relative to 0 cm/sec at 3000 dbar. If we KNOW v at 3000 dbar, then just add it to the whole profile DPO Fig. 7.11

22 Steric height at the sea surface in the N. Atlantic. Values are similar to sea surface height in meters. (Reid, 1994) DPO Fig. 9.2a

23 Sea surface height in the Atlantic. (Using Niiler et al., 2003, surface heights based on drifters) DPO Fig. S9.1

24 Steric height at the sea surface in the Pacific. Values are similar to sea surface height in meters. (Reid, 1997) DPO Fig. 10.2a

25 Sea surface height in the Pacific. (Using Niiler et al., 2003, surface heights based on drifters) DPO Fig. S10.1

26 Sea surface height in the Indian. (Using Niiler et al., 2003, surface heights based on drifters) DPO Fig. S11.1

27 Steric height at 1000 dbar in the N. Atlantic. Values are similar to sea surface height in meters. (Reid, 1994) DPO Fig. S9.2b

28 Steric height at 1000 dbar in the Pacific. Values are similar to sea surface height in meters. (Reid, 1997) DPO Fig

### Pressure, Forces and Motion

Pressure, Forces and Motion Readings A&B: Ch. 4 (p. 93-114) CD Tutorials: Pressure Gradients, Coriolis, Forces & Winds Topics 1. Review: What is Pressure? 2. Horizontal Pressure Gradients 3. Depicting

### Ocean Circulation: review

Joe LaCasce Section for Meteorology and Oceanography December 2, 2014 Outline Physical characteristics Observed circulation Geostrophic, hydrostatic and thermal wind balances Wind-driven circulation Buoyancy-driven

### Ocean Processes I Oceanography Department University of Cape Town South Africa

Ocean Processes I Isabelle.Ansorge@uct.ac.za Oceanography Department University of Cape Town South Africa 1 9/17/2009 Lecturer in Oceanography at UCT About me! BSc in England University of Plymouth MSc

### ATM 316: Dynamic Meteorology I Final Review, December 2014

ATM 316: Dynamic Meteorology I Final Review, December 2014 Scalars and Vectors Scalar: magnitude, without reference to coordinate system Vector: magnitude + direction, with reference to coordinate system

### Lecture 4: Pressure and Wind

Lecture 4: Pressure and Wind Pressure, Measurement, Distribution Forces Affect Wind Geostrophic Balance Winds in Upper Atmosphere Near-Surface Winds Hydrostatic Balance (why the sky isn t falling!) Thermal

### Ocean Circulation and Climate. The Thermohaline Circulation

Ocean Circulation and Climate In addition to the atmospheric circulation heat is also transported to the poles by the ocean circulation. The ocean circulation is therefore an important part of the climate

### List the Oceans that hurricanes can form in. (There should be 4) Describe the shape of the winds and the direction that they spin.

Heat Transfer Tab: (Use the textbook or the ScienceSaurus book) Box 1: Radiation: (on the colored tab) Draw a picture (on the white tab directly below it) Box 2: Convection: (on the colored tab) Draw a

### One Atmospheric Pressure. Measurement of Atmos. Pressure. Units of Atmospheric Pressure. Chapter 4: Pressure and Wind

Chapter 4: Pressure and Wind Pressure, Measurement, Distribution Hydrostatic Balance Pressure Gradient and Coriolis Force Geostrophic Balance Upper and Near-Surface Winds One Atmospheric Pressure (from

### How Do Oceans Affect Weather and Climate?

How Do Oceans Affect Weather and Climate? In Learning Set 2, you explored how water heats up more slowly than land and also cools off more slowly than land. Weather is caused by events in the atmosphere.

### Air Pressure and Winds-I. GEOL 1350: Introduction To Meteorology

Air Pressure and Winds-I GEOL 1350: Introduction To Meteorology 1 2 Pressure gradient force is in balance with gravity Hydrostatic relations Means no vertical motion initially 3 How does atmospheric pressure

### Outline. Jet Streams I (without the math) Definitions. Polar Jet Stream. Polar Jet Stream

Jet Streams I (without the math) Outline A few definitions, types, etc Thermal wind and the polar jet Ageostrophic circulations, entrance and exit regions Coupled Jets Definitions Jet Stream An intense,

### Chapter 4 Atmospheric Pressure and Wind

Chapter 4 Atmospheric Pressure and Wind Understanding Weather and Climate Aguado and Burt Pressure Pressure amount of force exerted per unit of surface area. Pressure always decreases vertically with height

### CHAPTER 6 THE DYNAMICS OF OCEAN CIRCULATION

Chapter 6 - pg. 1 CHAPTER 6 THE DYNAMICS OF OCEAN CIRCULATION The upper ocean circulation in the subtropical regions of the Atlantic and Pacific oceans is dominated by the concentrated currents along the

### MOVEMENTS OF OCEAN WATER

CHAPTER T he ocean water is dynamic. Its physical characteristics like temperature, salinity, density and the external forces like of the sun, moon and the winds influence the movement of ocean water.

### Module 2 Elements of Basic Meteorology and Oceanography

Module 2 Elements of Basic Meteorology and Oceanography 2.1 Understanding weather The atmospheric general circulation and its variance produced by the embedded movements of moisture laden air masses, constant

### Ocean Currents Paper. Lauren Murray SME 301, Section 3

Ocean Currents Paper Lauren Murray SME 301, Section 3 Background The topic of ocean currents is part of the earth science content area. Earth science is the study of forces on and inside the Earth and

### Circulation Bjerknes Circulation Theorem Vorticity Potential Vorticity Conservation of Potential Vorticity. ESS227 Prof. Jin-Yi Yu

Lecture 4: Circulation and Vorticity Circulation Bjerknes Circulation Theorem Vorticity Potential Vorticity Conservation of Potential Vorticity Measurement of Rotation Circulation and vorticity are the

### The Ocean-Atmosphere Connection, Winds & Surface Currents

The Ocean-Atmosphere Connection, Winds & Surface Currents Geosc040, Lecture 8 Feb 4, 2016 BORN RUFFIANS - Oceans Deep Somewhere Beyond The Sea, Sinatra Ocean Avenue Yellowcard Zedd - Lost At Sea Thanks

### Lecture 4: OCEANS (Outline) Basic Ocean Structures. Basic Ocean Current Systems. The State of Oceans. Temperature. Salinity.

Lecture 4: OCEANS (Outline) Basic Structures and Dynamics Ekman transport Geostrophic currents Surface Ocean Circulation Subtropicl gyre Boundary current Deep Ocean Circulation Thermohaline conveyor belt

### Chapter 8 Circulation of the Atmosphere

Chapter 8 Circulation of the Atmosphere The Atmosphere Is Composed Mainly of Nitrogen, Oxygen, and Water Vapor What are some properties of the atmosphere? Solar Radiation - initial source of energy to

### Weather. Weather is the set of environmental conditions encountered from day to day in a particular location.

WEATHER 1 Weather Weather is the set of environmental conditions encountered from day to day in a particular location. Climate is the set of environmental conditions averaged over many years for a geographic

### Hurricanes. Characteristics of a Hurricane

Hurricanes Readings: A&B Ch. 12 Topics 1. Characteristics 2. Location 3. Structure 4. Development a. Tropical Disturbance b. Tropical Depression c. Tropical Storm d. Hurricane e. Influences f. Path g.

### Introduction Ocean Sciences

CHAPTER 8 Ocean Circulation Introduction to Ocean Sciences Third Edition First electronic edition ver. DOUGLAS A. SEGAR Contributing author Elaine Stamman Segar 0 by Douglas A. Segar This work is licensed

### ATMS 310 Jet Streams

ATMS 310 Jet Streams Jet Streams A jet stream is an intense (30+ m/s in upper troposphere, 15+ m/s lower troposphere), narrow (width at least ½ order magnitude less than the length) horizontal current

### Atmospheric and Oceanic Circulation

Atmospheric and Oceanic Circulation Atmospheric circulation transfers energy and mass over the Earth Redistributes surplus energy along the tropics to deficit areas Generates weather patterns Produces

### Weather Systems, Hurricanes, Nili Harnik DEES, Lamont-Doherty Earth Observatory

Weather Systems, Hurricanes, etc Nili Harnik DEES, Lamont-Doherty Earth Observatory nili@ldeo.columbia.edu Coriolis Force Coriolis force The Coriolis Force On Earth Cloud types, as a function of height

### Thought Questions on the Geostrophic Wind and Real Winds Aloft at Midlatitudes

Thought Questions on the Geostrophic Wind and Real Winds Aloft at Midlatitudes (1) The geostrophic wind is an idealized, imaginary wind that we define at each point in the atmosphere as the wind that blows

### Hurricane Naming, Track, Structure Tropical Cyclone Development

Chapter 24: Tropical Cyclones Hurricane Naming, Track, Structure Tropical Cyclone Development Hurricane Characteristics Definition: Hurricanes have sustained winds of 120 km/hr (74 mph) or greater. Size:

### Chapter 6 Air Pressure and Winds

6.1 Pressure The difference in pressure between two points on the surface of the earth is responsible for the winds that blow from the higher pressure area to the lower pressure area. These winds in turn

### WIND. Chapter 4 CONVECTION

Chapter 4 WIND Differences in temperature create differences in pressure. These pressure differences drive a complex system of winds in a never ending attempt to reach equilibrium. Wind also transports

### Chapter 3: Weather Map. Weather Maps. The Station Model. Weather Map on 7/7/2005 4/29/2011

Chapter 3: Weather Map Weather Maps Many variables are needed to described weather conditions. Local weathers are affected by weather pattern. We need to see all the numbers describing weathers at many

### The Hydrostatic Equation

The Hydrostatic Equation Air pressure at any height in the atmosphere is due to the force per unit area exerted by the weight of all of the air lying above that height. Consequently, atmospheric pressure

### Thompson/Ocean 420/Winter 2005 Tide Dynamics 1

Thompson/Ocean 420/Winter 2005 Tide Dynamics 1 Tide Dynamics Dynamic Theory of Tides. In the equilibrium theory of tides, we assumed that the shape of the sea surface was always in equilibrium with the

### Exploring Florida: Teaching Resources for Science 1 of 6

Exploring Florida: Teaching Resources for Science 1 of 6 Tropical Cyclones This document describes tropical cyclones and the dangers they pose to coastal populations. It is intended to help teachers improve

### 3 Vorticity, Circulation and Potential Vorticity.

3 Vorticity, Circulation and Potential Vorticity. 3.1 Definitions Vorticity is a measure of the local spin of a fluid element given by ω = v (1) So, if the flow is two dimensional the vorticity will be

### 4.1 Momentum equation of the neutral atmosphere

Chapter 4 Dynamics of the neutral atmosphere 4.1 Momentum equation of the neutral atmosphere Since we are going to discuss the motion of the atmosphere of a rotating planet, it is convenient to express

### Meteorology Study Guide

Name: Class: Date: Meteorology Study Guide Modified True/False Indicate whether the sentence or statement is true or false. If false, change the identified word or phrase to make the sentence or statement

### Physics of the Atmosphere I

Physics of the Atmosphere I WS 2008/09 Ulrich Platt Institut f. Umweltphysik R. 424 Ulrich.Platt@iup.uni-heidelberg.de heidelberg.de Last week The conservation of mass implies the continuity equation:

### William Kessler NOAA / Pacific Marine Environmental Laboratory Seattle, USA

El Niño: How it works, how it affects the South Pacific William Kessler NOAA / Pacific Marine Environmental Laboratory Seattle, USA Outline of talk The normal situation in the tropical Pacific: a coupled

### Chapter Overview. Seasons. Earth s Seasons. Distribution of Solar Energy. Solar Energy on Earth. CHAPTER 6 Air-Sea Interaction

Chapter Overview CHAPTER 6 Air-Sea Interaction The atmosphere and the ocean are one independent system. Earth has seasons because of the tilt on its axis. There are three major wind belts in each hemisphere.

### SEVERE AND UNUSUAL WEATHER

SEVERE AND UNUSUAL WEATHER Basic Meteorological Terminology Adiabatic - Referring to a process without the addition or removal of heat. A temperature change may come about as a result of a change in the

### Weather and Climate Review

Weather and Climate Review STUFF YOU NEED TO KNOW and to UNDERSTAND! 1) Because water has a higher specific heat than land, water will warm and cool more slowly than the land will. Because of this: a)

### 2. The map below shows high-pressure and low-pressure weather systems in the United States.

1. Which weather instrument has most improved the accuracy of weather forecasts over the past 40 years? 1) thermometer 3) weather satellite 2) sling psychrometer 4) weather balloon 6. Wind velocity is

### Chapter 3: Weather Map. Station Model and Weather Maps Pressure as a Vertical Coordinate Constant Pressure Maps Cross Sections

Chapter 3: Weather Map Station Model and Weather Maps Pressure as a Vertical Coordinate Constant Pressure Maps Cross Sections Weather Maps Many variables are needed to described dweather conditions. Local

### 1. Isobars (i-so-bar from the Greek word isobares meaning of equal weight)

1. Isobars (i-so-bar from the Greek word isobares meaning of equal weight) Isobars are lines on a weather map that join places of equal pressure. Meteorologists collect information from weather stations,

### INTERNATIONAL INDIAN SCHOOL, RIYADH SA I 2016-17

INTERNATIONAL INDIAN SCHOOL, RIYADH SA I 2016-17 STD V WORKSHEET Page 1 of 7 SOCIAL STUDIES LESSON - 1. KNOW YOUR PLANET Fill in the blanks: 1. A book containing maps is called an. 2. A Flemish map maker,

### When the fluid velocity is zero, called the hydrostatic condition, the pressure variation is due only to the weight of the fluid.

Fluid Statics When the fluid velocity is zero, called the hydrostatic condition, the pressure variation is due only to the weight of the fluid. Consider a small wedge of fluid at rest of size Δx, Δz, Δs

### Our Coasts and Climate

GRADE: adaptable for all levels BY: Jill Rivero, MA Science Educator for the Wyland Foundation OBJECTIVE: Students will understand the difference between warm salty water near the ocean s surface and cold,

### 8.5 Comparing Canadian Climates (Lab)

These 3 climate graphs and tables of data show average temperatures and precipitation for each month in Victoria, Winnipeg and Whitehorse: Figure 1.1 Month J F M A M J J A S O N D Year Precipitation 139

### 2 Atmospheric Pressure

2 Atmospheric Pressure meteorology 2.1 Definition and Pressure Measurement 2.1.1 Definition Pressure acts in all directions, up and sideways as well as down, but it is convenient in meteorology to regard

### LESSON 1: THE EARTH S ENERGY BALANCE. Key Concepts X-PLANATION. Energy Balance and Heating of the Atmosphere

LESSON 1: THE EARTH S ENERGY BALANCE Key Concepts In this lesson we will focus on summarising what you need to know about: Define the term Energy Balance Clearly understand the concept of the heating of

### Weather Notes with Poole Sailing It is a requirement of the SOLAS rules that we have a passage plan whenever we take a boat to sea, and an essential

Weather Notes with Poole Sailing It is a requirement of the SOLAS rules that we have a passage plan whenever we take a boat to sea, and an essential part of that plan is an understanding of the weather

### Ocean in Motion 2: What Causes Ocean Currents and How Do We Measure Them?

Ocean in Motion 2: What Causes Ocean Currents and How Do We Measure Them? A. Overview 1. The Ocean in Motion -- Circulation In this program, students will learn about the driving forces responsible for

### OPERATIONS SEAFARER CERTIFICATION GUIDANCE NOTE SA MARITIME QUALIFICATIONS CODE. Deck: Marine Environmental Studies

Page 1 of 12 Compiled by Approved by Chief Examiner Syllabus Committee: 26 February 2013 OPERATIONS SEAFARER CERTIFICATION GUIDANCE NOTE SA MARITIME QUALIFICATIONS CODE Deck: Page 2 of 12 KNOWLEDGE, UNDERSTANDING

### 4/14/2012. The Oceans. Ocean Floor Geologic Provinces. Continental Margin. Turbidity Currents. Major Ocean Basins:

The Oceans Major Ocean Basins: Pacific Ocean largest and deepest Atlantic Ocean Indian Ocean S. Hemisphere Arctic smallest and most shallow Ocean Floor Geologic Provinces Continental Margin Continental

### Geog 531 Exercise #2 UNDERSTANDING SYNOPTIC CHARTS

Geog 531 Exercise #2 UNDERSTANDING SYNOPTIC CHARTS (Please answer right on this handout where sketches are requested in Question # 1, # 4, and # 6b. For the other questions, type out your answers and staple

### MET 200 Lecture 19 Midlatitude Cyclones. Hallow s Eve Mask. Midlatitude Cyclones or Winter Storms

MET 200 Lecture 19 Midlatitude Cyclones Hallow s Eve Mask 1 2 Lecture 19 Midlatitude Cyclones Midlatitude Cyclones or Winter Storms Cyclogenesis Energy Source Life Cycle Air Streams Vertical Structure

### TIDES. 1. Tides are the regular rise and fall of sea level that occurs either once a day (every 24.8 hours) or twice a day (every 12.4 hours).

TIDES What causes tides? How are tides predicted? 1. Tides are the regular rise and fall of sea level that occurs either once a day (every 24.8 hours) or twice a day (every 12.4 hours). Tides are waves

### Unit 2: Weather Dynamics Investigating Weather Maps

UNIT 2 Chapter 2: Weather Forecasting Section 2.2 Unit 2: Weather Dynamics Investigating Weather Maps Science 10 Mrs. Purba UNIT 2 Investigating Weather Maps Section 2.2 What can a weather map tell you?

### The Oceans Role in Climate

The Oceans Role in Climate Martin H. Visbeck A Numerical Portrait of the Oceans The oceans of the world cover nearly seventy percent of its surface. The largest is the Pacific, which contains fifty percent

### SUBTROPICAL ANTICYCLONES & ASSOCIATED WEATHER CONDITIONS 20 FEBRUARY 2014

SUBTROPICAL ANTICYCLONES & ASSOCIATED WEATHER CONDITIONS 20 FEBRUARY 2014 In this lesson we: Lesson Description Discuss the THREE high pressure cells that affect South Africa: Location, identification,

### An Analysis of the Rossby Wave Theory

An Analysis of the Rossby Wave Theory Morgan E. Brown, Elise V. Johnson, Stephen A. Kearney ABSTRACT Large-scale planetary waves are known as Rossby waves. The Rossby wave theory gives us an idealized

### OCEANIC CIRCULATION 434 OCEAN CURRENTS

CHAPTER 31 OCEAN CURRENTS TYPES AND CAUSES OF CURRENTS 3100. Definitions The movement of ocean water is one of the two principal sources of discrepancy between dead reckoned and actual positions of vessels.

### DO NOT WRITE ON THIS PAPER WEATHER NOTES WARM/COLD FRONTS

WEATHER NOTES WARM/COLD FRONTS What is a Front? Definition: A narrow transition zone, or boundary, between disparate synoptic scale air masses whose primary discontinuity is density. It is synoptic scale

### Follow That Hurricane!

Discover Your World With NOAA Follow That Hurricane! What You Will Do Devastating damage expected A most Track a hurricane on the same powerful hurricane with unprecedented type of chart used at the strength

### INDIAN SCHOOL MUSCAT MIDDLE SECTION DEPARTMENT OF SOCIAL SCIENCE

INDIAN SCHOOL MUSCAT MIDDLE SECTION DEPARTMENT OF SOCIAL SCIENCE THE FOUR REALMS OF THE EARTH Name: Class VI Sec. Roll No: Date: 22.10. 2014 I NAME THE FOLLOWING: 1. The solid surface layer of the Earth:

### M.Sc and Ph.D in Environment Engineering/Air Pollution: Curricula 1-Processing & Recycling of Solid Waste 2-Composting 3- Hazardous Solid Waste 4-

M.Sc and Ph.D in Environment Engineering/Air Pollution: Curricula 1-Processing & Recycling of Solid Waste 2-Composting 3- Hazardous Solid Waste 4- Meteorology 5- Air Pollutant Emission Control 6- Atmospheric

### GlobCurrent User Consultation Modelling & Prediction needs Mike Bell November Crown copyright Met Office

GlobCurrent User Consultation Modelling & Prediction needs Mike Bell November 2014 Crown copyright Met Office Contents Different types of - motion - use - modelling and prediction - data Some examples

### Practice: Developing and Using Models Crosscutting Concept: Systems and System Models

MS-ESS2-6 Develop and use a model to describe how unequal heating and rotation of the Earth cause patterns of atmospheric and oceanic circulation that determine regional climates. [Clarification statement:

### The water circulation in Kavala Bay (North Aegean)

Mediterranean Marine Science Volume 6/2, 2005, 05-16 The water circulation in Kavala Bay (North Aegean) TH. KARDARAS Hellenic Navy Hydrographic Service, T.G.N. 10 40 Holargos, Athens, Greece e-mail: ocean@hnhs.gr

### ES 106 Laboratory # 3 INTRODUCTION TO OCEANOGRAPHY. Introduction The global ocean covers nearly 75% of Earth s surface and plays a vital role in

ES 106 Laboratory # 3 INTRODUCTION TO OCEANOGRAPHY 3-1 Introduction The global ocean covers nearly 75% of Earth s surface and plays a vital role in the physical environment of Earth. For these reasons,

### 3 1.11 10 5 mdeg 1 = 4.00 4.33 3.33 10 5. 2.5 10 5 s 1 2

Chapter 7 7.7 At a certain location along the ITCZ, the surface wind at 10 Nisblowing from the east northeast (ENE) from a compass angle of 60 at a speed of 8ms 1 and the wind at 7 N is blowing from the

### ESCI 344 Tropical Meteorology Lesson 1 Introduction to the Tropics

ESCI 344 Tropical Meteorology Lesson 1 Introduction to the Tropics References: Forecaster s Guide to Tropical Meteorology (updated), Ramage Tropical Climatology (2 nd ed), McGregor and Nieuwolt Tropical

### LESSON 3 PREDICTING WEATHER. Chapter 7, Weather and Climate

LESSON 3 PREDICTING WEATHER Chapter 7, Weather and Climate OBJECTIVES Describe high- and low- pressure systems and the weather associated with each. Explain how technology is used to study weather. MAIN

### Ocean Modelling 32 (2010) 72 85. Contents lists available at ScienceDirect. Ocean Modelling. journal homepage:

Ocean Modelling 32 (21) 72 5 Contents lists available at ScienceDirect Ocean Modelling journal homepage: www.elsevier.com/locate/ocemod Non-local topographic influences on deep convection: An idealized

### Basics of weather interpretation

Basics of weather interpretation Safety at Sea Seminar, April 2 nd 2016 Dr. Gina Henderson Oceanography Dept., USNA ghenders@usna.edu Image source: http://earthobservatory.nasa.gov/naturalhazards/view.php?id=80399,

### Latitude and Longitude Vocabulary. Equator imaginary line separating the northern and southern hemispheres.

Latitude and Longitude Vocabulary Degrees the unit for measuring distance on a map Equator imaginary line separating the northern and southern hemispheres. Globe a miniature model of the Earth Hemisphere

### GEF 1100 Klimasystemet. Chapter 8: The general circulation of the atmosphere

GEF1100 Autumn 2015 29.09.2015 GEF 1100 Klimasystemet Chapter 8: The general circulation of the atmosphere Prof. Dr. Kirstin Krüger (MetOs, UiO) 1 Lecture Outline Ch. 8 Ch. 8 The general circulation of

### How to analyze synoptic-scale weather patterns Table of Contents

How to analyze synoptic-scale weather patterns Table of Contents Before You Begin... 2 1. Identify H and L pressure systems... 3 2. Locate fronts and determine frontal activity... 5 3. Determine surface

### CHAPTER 6 Air-Sea Interaction. Overview. Seasons

CHAPTER 6 Air-Sea Interaction Fig. 6.11 Overview Atmosphere and ocean one interdependent system Solar energy creates winds Winds drive surface ocean currents and waves Examples of interactions: El Niño-Southern

### Gravitational potential

Gravitational potential Let s assume: A particle of unit mass moving freely A body of mass M The particle is attracted by M and moves toward it by a small quantity dr. This displacement is the result of

### Weather Basics. Temperature Pressure Wind Humidity. Climate vs. Weather. Atmosphere and Weather

Climate vs. Weather Atmosphere and Weather Weather The physical condition of the atmosphere (moisture, temperature, pressure, wind) Climate Long term pattern of the weather in a particular area Weather

### Wind and Weather Notes. 8 th Grade Science Mrs. Melka

Wind and Weather Notes 8 th Grade Science Mrs. Melka 2015-16 Why is Wind Important? Part 1 Because wind systems determine major weather patterns on Earth. Wind also helps determine where planes and ships

### Fig. 1. Sketch of the wind-driven circulation. Under the Ekman pumping (upwelling) water moves equatorward (poleward) in order to conserve f/h.

Lecture 8. The physics of wind-driven circulation 3/7/006 11:50 AM 1. Interior solution Our discussion about wind-driven circulation in the previous lecture is based on detailed dynamic analysis; however,

### Chapter 4 Rotating Coordinate Systems and the Equations of Motion

Chapter 4 Rotating Coordinate Systems and the Equations of Motion 1. Rates of change of vectors We have derived the Navier Stokes equations in an inertial (non accelerating frame of reference) for which

### Page 1. Earth's Shape/Mapping Practice Questions. Name:

Earth's Shape/Mapping Practice Questions 1002-1 - Page 1 Name: 1) How are latitude and longitude lines drawn on a globe of the Earth? A) Longitude lines are parallel and latitude lines meet at the Equator.

### Name Period 4 th Six Weeks Notes 2015 Weather

Name Period 4 th Six Weeks Notes 2015 Weather Radiation Convection Currents Winds Jet Streams Energy from the Sun reaches Earth as electromagnetic waves This energy fuels all life on Earth including the

### Coriolis Effects on Wind-Driven Ocean Currents

hands-on Oceanography A Laboratory Demonstration of Coriolis Effects on Wind-Driven Ocean Currents Purpose of Activity Here we study the mechanism by which the wind drives ocean circulation. We induce

### Activity Title: Causes and Effects of Melting Ice

BEST OF COSEE HANDS-ON ACTIVITIES Activity Title: Causes and Effects of Melting Ice Learning Objectives Ocean Literacy Principles #1 -- The Earth has one big ocean with many features c. Throughout the

### ESCI 344 Tropical Meteorology Lesson 5 Tropical Cyclones: Climatology

ESCI 344 Tropical Meteorology Lesson 5 Tropical Cyclones: Climatology References: A Global View of Tropical Cyclones, Elsberry (ed.) The Hurricane, Pielke Tropical Cyclones: Their evolution, structure,

### Chapter 15. Hydrology of the Atlantic Ocean

Chapter 15 Hydrology of the Atlantic Ocean The hydrology of the Atlantic Ocean basins is deeply affected by the formation and recirculation of North Atlantic Deep Water, which was discussed in Chapter

### Anticyclones, depressions, hot & drought, cold & snow

AS/A2-Level Geography Anticyclones, depressions, hot & drought, cold & snow Learning Objectives: To describe and explain the weather associated with high and low pressure systems and their links to extreme

### Module 11: The Cruise Ship Sector. Destination #3

Module 11: The Cruise Ship Sector Destination #3 Cruise Destinations Welcome to your third destination. Use the following resource article to learn about the different oceans and time zones. Seen from

### How Can You Predict When Severe Weather Will Occur?

4.7 Explain How Can You Predict When Severe Weather Will Occur? In this Learning Set, you have been exploring how winds and oceans affect weather and climate. You then used what you know to explain how

### The Climatological Distribution of Potential Vorticity over the Abyssal Ocean

2488 JOURNAL OF PHYSICAL OCEANOGRAPHY The Climatological Distribution of Potential Vorticity over the Abyssal Ocean JANE O DWYER AND RICHARD G. WILLIAMS Oceanography Laboratories, Department of Earth Sciences,

### not to be republished NCERT Do you feel air around you? Do you SOLAR RADIATION, HEAT BALANCE AND TEMPERATURE SOLAR RADIATION

SOLAR RADIATION, HEAT BALANCE AND TEMPERATURE Do you feel air around you? Do you know that we live at the bottom of a huge pile of air? We inhale and exhale but we feel the air when it is in motion. It

### Satellite Derived Dynamic Ocean Currents in the Arctic. Jens Olaf Pepke Pedersen Polar DTU / DTU Space www.polar.dtu.dk www.space.dtu.

Satellite Derived Dynamic Ocean Currents in the Arctic Jens Olaf Pepke Pedersen Polar DTU / DTU Space www.polar.dtu.dk www.space.dtu.dk Benefits of exploiting ocean currents Benjamin Franklins map of the

### ebb current, the velocity alternately increasing and decreasing without coming to

Slack water (slack tide): The state of a tidal current when its velocity is near zero, especially the moment when a reversing current changes its direction and its velocity is zero. The term is also applied