The Earth and Its Atmosphere. Chapter 1
|
|
- Colleen Young
- 7 years ago
- Views:
Transcription
1 The Earth and Its Atmosphere Chapter 1
2 Overview of the Earth s Atmosphere The atmosphere is a delicate life giving blanket of air surrounding the Earth. Without the atmosphere the Earth would not have lakes or oceans. Radiant energy from the sun energizes the atmosphere driving day to day weather.
3 Composition Overview of the Earth s Atmosphere 99% of the atmosphere is within 30km of the Earth s surface N 2 78% and O 2 21% The percentages represent a constant amount of gas but cycles of destruction and production are constantly maintaining this amount.
4
5 Overview of the Earth s Composition Atmosphere Water a variable gas following the hydrologic cycle. Carbon dioxide has risen in recent years and is an important greenhouse gas. Other greenhouse gases exist beyond carbon dioxide.
6 The main components of the atmospheric carbon dioxide cycle. The gray lines show processes that put carbon dioxide into the atmosphere, whereas the red lines show processes that remove carbon dioxide from the atmosphere.
7 Stepped Art
8 (a) The solid blue line shows the average yearly measurements of CO2 in parts per million (ppm) at Mauna Loa Observatory, Hawaii, from 1958 to The jagged dark line illustrates how higher readings occur in winter where plants die and release CO2 to the atmosphere, and how lower readings occur in summer when more abundant vegetation absorbs CO2 from the atmosphere. (b) The insert shows CO2 values in ppm during the past 1000 years from ice cores in Antarctica (orange line) and from Mauna Loa Observatory (blue line). (Mauna Loa data NOAA-Ice Core data courtesy of Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory
9 The darkest color represents the area of lowest ozone concentration, or ozone hole, over the Southern Hemisphere on September 25, Notice that the hole is larger than the continent of Antarctica. A Dobson unit (DU) is the physical thickness of the ozone layer if it were brought to the earth s surface, where 500 DU equals 5 millimeters.
10 Variable components of air Ozone Three atoms of oxygen (O 3 ) Distribution not uniform Concentrated between 10 and 50 km above the surface Absorbs harmful UV radiation Human activity is depleting ozone by adding Chlorofluorocarbons (CFCs)
11 Ozone Depletion
12 Variable components of air Water vapor Up to 4% of air s volume Forms clouds and precipitation It is also a greenhouse gas Important role in absorbing and releasing latent heat during phase change Aerosols Tiny solid and liquid particles Water vapor can condense on solids Reflect sunlight Color sunrise and sunset
13 Overview of the Earth s Atmosphere The Early Atmosphere The Earth s first atmosphere was composed mostly of hydrogen and helium. The atmosphere evolved due to outgassing of CO 2 and H 2 O from the cooling center of the Earth causing rain and eventually lakes and oceans. Lakes and oceans acted as a sink, absorbing CO 2 from atmosphere. Plants evolved producing oxygen to form our current atmosphere several 100 million ybp.
14 Vertical Structure of the Atmosphere Air Pressure and Air Density Weight = mass x gravity Density = mass/volume Pressure = force/area At the Earth s surface the pressure of the atmosphere is 14.7 lbs/in 2. Standard sea level pressure is mb = hpa = in Hg Atmospheric pressure decreases with an increase in height.
15 Both air pressure and air density decrease with increasing altitude. The weight of all the air molecules above the earth s surface produces an average pressure near 14.7 lbs/in.2
16 Atmospheric pressure decreases rapidly with height. Climbing to an altitude of only 5.5 km, where the pressure is 500 mb, would put you above one-half of the atmosphere s molecules.
17 Vertical Structure of the Atmosphere Lapse rate = change in temperature with a change in height Isothermal environment = no change in temperature with height Inversion layer = change in the sign of the lapse rate
18 Near the earth s surface the air temperature lapse rate is often close to 3.5F per 1000 ft. If this temperature lapse rate is present and the air temperature at the surface (0 ft) is 46F, the air temperature about 4000 ft above the surface would be at freezing, and snow and ice might be on the ground.
19 Vertical Structure of the Atmosphere Layers of the Atmosphere Troposphere: decrease in temperature, day to day weather, tropopause Stratosphere: increase in temperature, ozone, stratopause Mesosphere: decrease in temperature, mesopause Thermosphere: increase in temperature, suns strongest radiation
20 Troposphere Bottom layer Temperature decreases with altitude Environmental lapse rate Average 6.5 C per km or 3.5 F per 1000 feet Thickness varies Average height is about 12 km Outer boundary is the tropopause Where weather happens!
21 Stratosphere 12 to 50 km Temperature increases at top Outer boundary is the stratopause Mesosphere 50 to 80 km Temperature decreases Outer boundary is the mesopause Thermosphere No well-defined upper limit Fraction of atmosphere s mass Gases moving at high speeds
22 Layers of the atmosphere as related to the average profile of air temperature above the earth s surface. The red line illustrates how the average temperature varies in each layer. Stepped Art
23 Special Topic: The Atmospheres of Other Planets Each planet s atmosphere is unique in terms of temperature and composition. Earth: N 2, O 2 Venus: 95% CO 2, thick Mars: 95% CO 2, thin Jupiter: H 2, He, Red Spot
24 Vertical Structure of the Atmosphere Observation: Radiosonde Weather balloon Instrument and transmitter Air temperature, humidity, pressure
25 Vertical Structure of the The Ionosphere Atmosphere Not a true layer but an electrified region Ions = molecule with an additional or minus an electron Exists at the top of the atmosphere in the thermosphere F,E,D layer Sun light creates layers, D disappears at night and less interference with AM radio transmissions.
26 At night, the higher region of the ionosphere (F region) strongly reflects AM radio waves, allowing them to be sent over great distances. During the day, the lower D region strongly absorbs and weakens AM radio waves, preventing them from being picked up by distant receivers.
27 (left) Layers of the atmosphere based on temperature (red line), composition (green line), and electrical properties (dark blue line). (An active sun is associated with large numbers of solar eruptions.)
28 Weather and Climate Weather: short term Air temperature Air pressure Humidity Clouds Precipitation Visibility Wind Climate: long term patterns and average weather; not just magnitude but also frequency
29 Weather & Climate Meteorology brief history Study of the atmosphere and its phenomena Aristotle 340 B.C. Meterologica, meteoros: high in air 1843 telegraph 1920s air masses 1940s upper air 1950s radar and computers 1960s satellite
30 Doppler radar has the capacity of estimating rainfall intensity. In this composite image, the areas shaded green and blue indicate where light-tomoderate rain is falling. Yellow indicates heavier rainfall. The red-shaded area represents the heaviest rainfall and the possibility of intense thunderstorms. (Notice that a thunderstorm is approaching Chicago from the west.)
31 Weather & Climate Satellite s View Geostationary satellite 22,300 mi above equator Meridians measure longitude (W-E) Parallels measure latitude (N-S) Weather maps: pressure cells, fronts, surface stations
32 This satellite image (taken in visible reflected light) shows a variety of cloud patterns and storms in the earth s atmosphere.
33 Simplified surface weather map that correlates with the satellite image shown in Fig The shaded green area represents precipitation. The numbers on the map represent air temperatures in o F.
34 Weather & Climate Weather and Climate in Our Lives Two general reasons for studying how weather and climate impacts our lives: economic efficiency and public safety. Clothing Crops Utilities Extreme cold and heat Tornados and hurricanes
35 Ice storm near Oswego, New York, caused utility poles and power lines to be weighed down, forcing road closur
36 A tornado and a rainbow form over south-central Kansas during June, White streaks in the sky are descending hailstones. Flooding during April, 1997, inundates Grand Forks, North Dakota, as flood waters of the Red River extend over much of the city. Estimates are that lightning strikes the earth about 100 times every second. About 25 million lightning strikes hit the United States each year. Consequently, lightning is a very common, and sometimes deadly, weather phenomenon.
ATMOSPHERIC STRUCTURE. The vertical distribution of temperature, pressure,
ATMOSPHERIC STRUCTURE. The vertical distribution of temperature, pressure, density, and composition of the atmosphere constitutes atmospheric structure. These quantities also vary with season and location
More informationCHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles
CHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles I. Air Temperature: Five important factors influence air temperature: A. Insolation B. Latitude C. Surface types D. Coastal vs. interior
More informationThe Earth's Atmosphere. Layers of the Earth's Atmosphere
The Earth's Atmosphere The atmosphere surrounds Earth and protects us by blocking out dangerous rays from the sun. The atmosphere is a mixture of gases that becomes thinner until it gradually reaches space.
More informationLecture 1: A Brief Survey of the Atmosphere
Lecture 1: A Brief Survey of the Atmosphere Origins of the atmosphere Vertical structures of the atmosphere Weather maps Thickness of the Atmosphere (from Meteorology Today) 70% The thickness of the atmosphere
More informationReview 1. Multiple Choice Identify the choice that best completes the statement or answers the question.
Review 1 Multiple Choice Identify the choice that best completes the statement or answers the question. 1. When hydrogen nuclei fuse into helium nuclei a. the nuclei die. c. particles collide. b. energy
More informationThe Earth s Atmosphere
THE SUN-EARTH SYSTEM III The Earth s Atmosphere Composition and Distribution of the Atmosphere The composition of the atmosphere and the way its gases interact with electromagnetic radiation determine
More informationAtmospheric Layers. Ionosphere. Exosphere. Thermosphere. Mesosphere. Stratosphere. Troposphere. mi (km) above sea level 250 (400) 50 (80) 30 (50)
mi (km) above sea level Atmospheric Layers Exosphere 250 (400) Thermosphere Ionosphere 50 (80) Mesosphere Ozone Layer 30 (50) 7 (12) Stratosphere Troposphere Atmospheric Layers Earth s atmosphere is held
More information6 th Grade Science Assessment: Weather & Water Select the best answer on the answer sheet. Please do not make any marks on this test.
Select the be answer on the answer sheet. Please do not make any marks on this te. 1. Weather is be defined as the A. changes that occur in cloud formations from day to day. B. amount of rain or snow that
More informationCharacteristics of the. thermosphere
Characteristics of the Atmosphere. If you were lost in the desert, you could survive for a few days without food and water. But you wouldn't last more than five minutes without the ' Objectives Describe
More informationSection 1 The Earth System
Section 1 The Earth System Key Concept Earth is a complex system made up of many smaller systems through which matter and energy are continuously cycled. What You Will Learn Energy and matter flow through
More informationCalifornia Standards Grades 9 12 Boardworks 2009 Science Contents Standards Mapping
California Standards Grades 912 Boardworks 2009 Science Contents Standards Mapping Earth Sciences Earth s Place in the Universe 1. Astronomy and planetary exploration reveal the solar system s structure,
More informationThe atmospheres of different planets
The atmospheres of different planets Thomas Baron October 13, 2006 1 Contents 1 Introduction 3 2 The atmosphere of the Earth 3 2.1 Description and Composition.................... 3 2.2 Discussion...............................
More informationESCI 107/109 The Atmosphere Lesson 2 Solar and Terrestrial Radiation
ESCI 107/109 The Atmosphere Lesson 2 Solar and Terrestrial Radiation Reading: Meteorology Today, Chapters 2 and 3 EARTH-SUN GEOMETRY The Earth has an elliptical orbit around the sun The average Earth-Sun
More informationThe Earth System. The geosphere is the solid Earth that includes the continental and oceanic crust as well as the various layers of Earth s interior.
The Earth System The atmosphere is the gaseous envelope that surrounds Earth. It consists of a mixture of gases composed primarily of nitrogen, oxygen, carbon dioxide, and water vapor. The atmosphere and
More informationSolar Flux and Flux Density. Lecture 3: Global Energy Cycle. Solar Energy Incident On the Earth. Solar Flux Density Reaching Earth
Lecture 3: Global Energy Cycle Solar Flux and Flux Density Planetary energy balance Greenhouse Effect Vertical energy balance Latitudinal energy balance Seasonal and diurnal cycles Solar Luminosity (L)
More informationChapter 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.
More informationComposition of the Atmosphere. Outline Atmospheric Composition Nitrogen and Oxygen Lightning Homework
Molecules of the Atmosphere The present atmosphere consists mainly of molecular nitrogen (N2) and molecular oxygen (O2) but it has dramatically changed in composition from the beginning of the solar system.
More information7613-1 - Page 1. Weather Unit Exam Pre-Test Questions
Weather Unit Exam Pre-Test Questions 7613-1 - Page 1 Name: 1) Equal quantities of water are placed in four uncovered containers with different shapes and left on a table at room temperature. From which
More informationTemperature. PJ Brucat
PJ Brucat Temperature - the measure of average kinetic energy (KE) of a gas, liquid, or solid. KE is energy of motion. KE = ½ mv 2 where m=mass and v=velocity (speed) 1 All molecules have KE whether solid,
More informationName 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
More informationChapter 6: Cloud Development and Forms
Chapter 6: Cloud Development and Forms (from The Blue Planet ) Why Clouds Form Static Stability Cloud Types Why Clouds Form? Clouds form when air rises and becomes saturated in response to adiabatic cooling.
More informationFACTS ABOUT CLIMATE CHANGE
FACTS ABOUT CLIMATE CHANGE 1. What is climate change? Climate change is a long-term shift in the climate of a specific location, region or planet. The shift is measured by changes in features associated
More informationWater, Phase Changes, Clouds
TUESDAY: air & water & clouds Water, Phase Changes, Clouds How can freezing make something warmer? 'warm air can hold more water' why? How do clouds form? The (extraordinary) properties of Water Physical
More informationThe Ideal Gas Law. Gas Constant. Applications of the Gas law. P = ρ R T. Lecture 2: Atmospheric Thermodynamics
Lecture 2: Atmospheric Thermodynamics Ideal Gas Law (Equation of State) Hydrostatic Balance Heat and Temperature Conduction, Convection, Radiation Latent Heating Adiabatic Process Lapse Rate and Stability
More informationJessica Blunden, Ph.D., Scientist, ERT Inc., Climate Monitoring Branch, NOAA s National Climatic Data Center
Kathryn Sullivan, Ph.D, Acting Under Secretary of Commerce for Oceans and Atmosphere and NOAA Administrator Thomas R. Karl, L.H.D., Director,, and Chair of the Subcommittee on Global Change Research Jessica
More informationClouds and the Energy Cycle
August 1999 NF-207 The Earth Science Enterprise Series These articles discuss Earth's many dynamic processes and their interactions Clouds and the Energy Cycle he study of clouds, where they occur, and
More informationEarth Sciences -- Grades 9, 10, 11, and 12. California State Science Content Standards. Mobile Climate Science Labs
Earth Sciences -- Grades 9, 10, 11, and 12 California State Science Content Standards Covered in: Hands-on science labs, demonstrations, & activities. Investigation and Experimentation. Lesson Plans. Presented
More informationCHAPTER 6 THE TERRESTRIAL PLANETS
CHAPTER 6 THE TERRESTRIAL PLANETS MULTIPLE CHOICE 1. Which of the following is NOT one of the four stages in the development of a terrestrial planet? 2. That Earth, evidence that Earth differentiated.
More informationSTUDY GUIDE: Earth Sun Moon
The Universe is thought to consist of trillions of galaxies. Our galaxy, the Milky Way, has billions of stars. One of those stars is our Sun. Our solar system consists of the Sun at the center, and all
More informationThe Earth, Sun, and Moon
reflect The Sun and Moon are Earth s constant companions. We bask in the Sun s heat and light. It provides Earth s energy, and life could not exist without it. We rely on the Moon to light dark nights.
More informationWELCOME to Aurorae In the Solar System. J.E. Klemaszewski
WELCOME to Aurorae In the Solar System Aurorae in the Solar System Sponsoring Projects Galileo Europa Mission Jupiter System Data Analysis Program ACRIMSAT Supporting Projects Ulysses Project Outer Planets
More informationWEATHER AND CLIMATE practice test
WEATHER AND CLIMATE practice test Multiple Choice Identify the choice that best completes the statement or answers the question. 1. What role does runoff play in the water cycle? a. It is the process in
More informationFull name:.. Date:. School: Teacher: Contents:
Contents: 1.- The atmosphere. 2.- Weather and climate. 3.- The elements of climate 3.1 Temperatures 3.2 Rainfalls 3.3 Atmospheric pressure 3.4 Wind 4.-The Natural Environment. Full name:.. Date:. Class:
More informationThis chapter discusses: 1. Definitions and causes of stable and unstable atmospheric air. 2. Processes that cause instability and cloud development
Stability & Cloud Development This chapter discusses: 1. Definitions and causes of stable and unstable atmospheric air 2. Processes that cause instability and cloud development Stability & Movement A rock,
More informationFundamentals of Climate Change (PCC 587): Water Vapor
Fundamentals of Climate Change (PCC 587): Water Vapor DARGAN M. W. FRIERSON UNIVERSITY OF WASHINGTON, DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 2: 9/30/13 Water Water is a remarkable molecule Water vapor
More informationTemperature affects water in the air.
KEY CONCEPT Most clouds form as air rises and cools. BEFORE, you learned Water vapor circulates from Earth to the atmosphere Warm air is less dense than cool air and tends to rise NOW, you will learn How
More informationMultiple Choice Identify the choice that best completes the statement or answers the question.
Test 2 f14 Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Carbon cycles through the Earth system. During photosynthesis, carbon is a. released from wood
More informationRead and study the following information. After reading complete the review questions. Clouds
Name: Pd: Read and study the following information. After reading complete the review questions. Clouds What are clouds? A cloud is a large collection of very tiny droplets of water or ice crystals. The
More information6. The greatest atmospheric pressure occurs in the 1) troposphere 3) mesosphere 2) stratosphere 4) thermosphere
1. The best evidence of the Earth's nearly spherical shape is obtained through telescopic observations of other planets photographs of the Earth from an orbiting satellite observations of the Sun's altitude
More informationORANGE PUBLIC SCHOOLS OFFICE OF CURRICULUM AND INSTRUCTION OFFICE OF SCIENCE. GRADE 6 SCIENCE Post - Assessment
ORANGE PUBLIC SCHOOLS OFFICE OF CURRICULUM AND INSTRUCTION OFFICE OF SCIENCE GRADE 6 SCIENCE Post - Assessment School Year 2013-2014 Directions for Grade 6 Post-Assessment The Grade 6 Post-Assessment is
More informationEducation and Outreach Lesson Plan
Education and Outreach Lesson Plan Visit our online activities collection http://education.arm.gov/ Grade levels K 2 Common Covering Clouds Common Covering Clouds Approximate Time 1 1/2 hours, or two 45-minute
More informationClouds. A simple scientific explanation for the weather-curious. By Kira R. Erickson
Clouds A simple scientific explanation for the weather-curious By Kira R. Erickson Table of Contents 1 3 4 INTRO 2 Page 3 How Clouds Are Formed Types of Clouds Clouds and Weather More Information Page
More informationStorms Short Study Guide
Name: Class: Date: Storms Short Study Guide Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. A(n) thunderstorm forms because of unequal heating
More information2007 Pearson Education Inc., publishing as Pearson Addison-Wesley. The Jovian Planets
The Jovian Planets The Jovian planets are gas giants - much larger than Earth Sizes of Jovian Planets Planets get larger as they get more massive up to a point... Planets more massive than Jupiter are
More informationclimate science A SHORT GUIDE TO This is a short summary of a detailed discussion of climate change science.
A SHORT GUIDE TO climate science This is a short summary of a detailed discussion of climate change science. For more information and to view the full report, visit royalsociety.org/policy/climate-change
More informationSouthern AER Atmospheric Education Resource
Southern AER Atmospheric Education Resource Vol. 9 No. 5 Spring 2003 Editor: Lauren Bell In this issue: g Climate Creations exploring mother nature s remote control for weather and Climate. g Crazy Climate
More informationSIXTH GRADE WEATHER 1 WEEK LESSON PLANS AND ACTIVITIES
SIXTH GRADE WEATHER 1 WEEK LESSON PLANS AND ACTIVITIES WATER CYCLE OVERVIEW OF SIXTH GRADE WATER WEEK 1. PRE: Evaluating components of the water cycle. LAB: Experimenting with porosity and permeability.
More informationThe Balance of Power in the Earth-Sun System
NASA Facts National Aeronautics and Space Administration www.nasa.gov The Balance of Power in the Earth-Sun System The Sun is the major source of energy for Earth s oceans, atmosphere, land, and biosphere.
More informationTHIRD GRADE WEATHER 1 WEEK LESSON PLANS AND ACTIVITIES
THIRD GRADE WEATHER 1 WEEK LESSON PLANS AND ACTIVITIES WATER CYCLE OVERVIEW OF THIRD GRADE WATER WEEK 1. PRE: Comparing the different components of the water cycle. LAB: Contrasting water with hydrogen
More information8.5 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
More informationUNIT 6a TEST REVIEW. 1. A weather instrument is shown below.
UNIT 6a TEST REVIEW 1. A weather instrument is shown below. Which weather variable is measured by this instrument? 1) wind speed 3) cloud cover 2) precipitation 4) air pressure 2. Which weather station
More informationGeorgia Performance Standards Framework for Natural Disasters 6 th Grade
The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are
More informationSeasonal Temperature Variations
Seasonal and Daily Temperatures Fig. 3-CO, p. 54 Seasonal Temperature Variations What causes the seasons What governs the seasons is the amount of solar radiation reaching the ground What two primary factors
More informationFOR SUBSCRIBERS ONLY! - TRIAL PASSWORD USERS MAY NOT REPRODUCE AND DISTRIBUTE PRINTABLE MATERIALS OFF THE SOLPASS WEBSITE!
FOR SUBSCRIBERS ONLY! - TRIAL PASSWORD USERS MAY NOT REPRODUCE AND DISTRIBUTE PRINTABLE MATERIALS OFF THE SOLPASS WEBSITE! 1 NAME DATE GRADE 5 SCIENCE SOL REVIEW WEATHER LABEL the 3 stages of the water
More informationGETTING TO THE CORE: THE LINK BETWEEN TEMPERATURE AND CARBON DIOXIDE
DESCRIPTION This lesson plan gives students first-hand experience in analyzing the link between atmospheric temperatures and carbon dioxide ( ) s by looking at ice core data spanning hundreds of thousands
More information- 1 - Jennifer McClure. To: env.essay@physics.org. From: Jennifer McClure (j.m.mcclure@student.liverpool.ac.uk)
To: env.essay@physics.org Jennifer McClure From: Jennifer McClure (j.m.mcclure@student.liverpool.ac.uk) 1 st year Physics (F300), Department of Physics, University of Liverpool. - 1 - The Northern Lights;
More informationThe Clouds Outside My Window. National Weather Service NOAA
The Clouds Outside My Window National Weather Service NOAA The Clouds Out My Window Written and illustrated by John Jensenius My window With help from Owlie Skywarn 1 The Clouds Outside My Window Whether
More informationCHARACTERISTICS OF THE SOLAR SYSTEM
reflect Our solar system is made up of thousands of objects, at the center of which is a star, the Sun. The objects beyond the Sun include 8 planets, at least 5 dwarf planets, and more than 170 moons.
More informationMultiple Choice Exam Questions
Chapter 1 Multiple Choice Exam Questions 1. The primary source of energy for the earth's atmosphere is: a. energy from within the earth b. the sun c. erupting volcanoes d. lightning discharges associated
More informationGEOLOGY 10 Extended Notes #6 The Atmosphere (LT Chapter 11)
GEOLOGY 10 Extended Notes #6 The Atmosphere (LT Chapter 11) Weather vs. climate? Composition of Air Major Gases Mostly N and O (Fig. 11.2 on p. 283). Additives Water vapor the source of clouds and precipitation
More informationSeasonal & Daily Temperatures. Seasons & Sun's Distance. Solstice & Equinox. Seasons & Solar Intensity
Seasonal & Daily Temperatures Seasons & Sun's Distance The role of Earth's tilt, revolution, & rotation in causing spatial, seasonal, & daily temperature variations Please read Chapter 3 in Ahrens Figure
More informationDescription: This competition will test the student's knowledge of meteorological terms, techniques, and events.
Weather or Not Description: This competition will test the student's knowledge of meteorological terms, techniques, and events. Number of Participants: 2 Approximate Time: 45 minutes The Competition: 1.
More informationClouds: What They Are and What They Mean. Susannah Lopez. Introduction to Meteorology. 2 December 2008
Clouds: What They 1 Clouds: What They Are and What They Mean Susannah Lopez Introduction to Meteorology 2 December 2008 Clouds: What They 2 Clouds: What They Are and What They Mean Clouds are composed
More informationEmpirical study of the temporal variation of a tropical surface temperature on hourly time integration
Global Advanced Research Journal of Physical and Applied Sciences Vol. 4 (1) pp. 051-056, September, 2015 Available online http://www.garj.org/garjpas/index.htm Copyright 2015 Global Advanced Research
More informationCorso di Fisica Te T cnica Ambientale Solar Radiation
Solar Radiation Solar radiation i The Sun The Sun is the primary natural energy source for our planet. It has a diameter D = 1.39x10 6 km and a mass M = 1.989x10 30 kg and it is constituted by 1/3 of He
More informationUNIVERSITY OF VICTORIA CHEMISTRY 102 Midterm Test 1 January 31, 2014 5-6 pm (60 minutes) DISPLAY YOUR STUDENT ID CARD ON THE TOP OF YOUR DESK NOW
Version B UNIVERSITY OF VICTORIA CHEMISTRY 102 Midterm Test 1 January 31, 2014 5-6 pm (60 minutes) Version B DISPLAY YOUR STUDENT ID CARD ON THE TOP OF YOUR DESK NOW Answer all multiple choice questions
More informationStability and Cloud Development. Stability in the atmosphere AT350. Why did this cloud form, whereas the sky was clear 4 hours ago?
Stability and Cloud Development AT350 Why did this cloud form, whereas the sky was clear 4 hours ago? Stability in the atmosphere An Initial Perturbation Stable Unstable Neutral If an air parcel is displaced
More informationWeather Help - NEXRAD Radar Maps. Base Reflectivity
Weather Help - NEXRAD Radar Maps Base Reflectivity Base Reflectivity Severe Thunderstorm/Torna do Watch Areas 16 levels depicted with colors from dark green (very light) to red (extreme) that indicate
More informationLESSON PLAN UNIT: THE EARTH S CLIMATES SESSIONS: 6. Ana Fructuoso Sánchez. Social Sciences teacher. Bilingual group. 1º ESO. IES El Palmar. Murcia.
LESSON PLAN UNIT: THE EARTH S CLIMATES SESSIONS: 6 Ana Fructuoso Sánchez teacher. Bilingual group. 1º ESO IES El Palmar. Murcia. INTRODUCTION: In this unit we are going to analyze the layers of the atmosphere
More informationCHAPTER 2 Energy and Earth
CHAPTER 2 Energy and Earth This chapter is concerned with the nature of energy and how it interacts with Earth. At this stage we are looking at energy in an abstract form though relate it to how it affect
More informationFormation & Classification
CLOUDS Formation & Classification DR. K. K. CHANDRA Department of forestry, Wildlife & Environmental Sciences, GGV, Bilaspur What is Cloud It is mass of tiny water droplets or ice crystals or both of size
More informationLecture 23: Terrestrial Worlds in Comparison. This lecture compares and contrasts the properties and evolution of the 5 main terrestrial bodies.
Lecture 23: Terrestrial Worlds in Comparison Astronomy 141 Winter 2012 This lecture compares and contrasts the properties and evolution of the 5 main terrestrial bodies. The small terrestrial planets have
More information2. 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
More informationFor further information, and additional background on the American Meteorological Society s Education Program, please contact:
Project ATMOSPHERE This guide is one of a series produced by Project ATMOSPHERE, an initiative of the American Meteorological Society. Project ATMOSPHERE has created and trained a network of resource agents
More informationMeteorology Practice Exam
Class: Date: Meteorology Practice Exam Multiple Choice Identify the choice that best completes the statement or answers the question. 1. In a volume of air near the earth's surface, occupies 78 percent
More informationHow 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.
More informationSevere Weather A Reading A Z Level T Leveled Book Word Count: 1,775
Severe Weather A Reading A Z Level T Leveled Book Word Count: 1,775 LEVELED BOOK T SEVERE WEATHER Written by Bruce D. Cooper Illustrated by Cende Hill Visit www.readinga-z.com for thousands of books and
More informationThe Atmosphere and Winds
Oceanography 10, T. James Noyes, El Camino College 8A-1 The Atmosphere and Winds We need to learn about the atmosphere, because the ocean and atmosphere are tightly interconnected with one another: you
More informationTOPIC: CLOUD CLASSIFICATION
INDIAN INSTITUTE OF TECHNOLOGY, DELHI DEPARTMENT OF ATMOSPHERIC SCIENCE ASL720: Satellite Meteorology and Remote Sensing TERM PAPER TOPIC: CLOUD CLASSIFICATION Group Members: Anil Kumar (2010ME10649) Mayank
More informationPartnerships Implementing Engineering Education Worcester Polytechnic Institute Worcester Public Schools
Partnerships Implementing Engineering Education Worcester Polytechnic Institute Worcester Public Schools Supported by: National Science Foundation Weather: 4.H.3 Weather and Classical Instruments Grade
More informationCh. 15 - Air, Weather, and Climate. Outline
Ch. 15 - Air, Weather, and Climate 1 Outline The Atmosphere and Climate Convection Currents Greenhouse Effect Weather Winds Frontal Systems Cyclonic Storms Climate El Nino Climate Change Kyoto Protocol
More informationSECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES
SECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES WATER CYCLE OVERVIEW OF SECOND GRADE WATER WEEK 1. PRE: Exploring the properties of water. LAB: Experimenting with different soap mixtures. POST: Analyzing
More informationSolar System Fact Sheet
Solar System Fact Sheet (Source: http://solarsystem.nasa.gov; http://solarviews.com) The Solar System Categories Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune Rocky or Gas Rocky Rocky Rocky Rocky
More informationBasics 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,
More informationThe Greenhouse Effect. Lan Ma Global Warming: Problems & Solutions 17 September, 2007
The Greenhouse Effect Lan Ma Global Warming: Problems & Solutions 17 September, 2007 What to cover today: How do we calculate the Earth s surface temperature? What makes a gas a greenhouse gas and how
More informationTHE SOLAR SYSTEM - EXERCISES 1
THE SOLAR SYSTEM - EXERCISES 1 THE SUN AND THE SOLAR SYSTEM Name the planets in their order from the sun. 1 2 3 4 5 6 7 8 The asteroid belt is between and Which planet has the most moons? About how many?
More informationATM S 111, Global Warming: Understanding the Forecast
ATM S 111, Global Warming: Understanding the Forecast DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 1: OCTOBER 1, 2015 Outline How exactly the Sun heats the Earth How strong? Important concept
More informationClimate Control and Ozone Depletion. Chapter 19
Climate Control and Ozone Depletion Chapter 19 Global Warming and Global Cooling Are Not New Over the past 4.5 billion years the climate has been altered by Volcanic emissions Changes in solar input Movement
More informationActivity 8 Drawing Isobars Level 2 http://www.uni.edu/storm/activities/level2/index.shtml
Activity 8 Drawing Isobars Level 2 http://www.uni.edu/storm/activities/level2/index.shtml Objectives: 1. Students will be able to define and draw isobars to analyze air pressure variations. 2. Students
More informationElectromagnetic Radiation Energy that comes to us from the sun is transported in the form of waves known as electromagnetic energy.
Electromagnetic Radiation Energy that comes to us from the sun is transported in the form of waves known as electromagnetic energy. This combines electricity and magnetism such that setting up an electric
More informationSunlight and its Properties. EE 495/695 Y. Baghzouz
Sunlight and its Properties EE 495/695 Y. Baghzouz The sun is a hot sphere of gas whose internal temperatures reach over 20 million deg. K. Nuclear fusion reaction at the sun's core converts hydrogen to
More informationCloud Development and Forms. LIFTING MECHANISMS 1. Orographic 2. Frontal 3. Convergence 4. Convection. Orographic Cloud. The Orographic Cloud
Introduction to Climatology GEOGRAPHY 300 Cloud Development and Forms Tom Giambelluca University of Hawai i at Mānoa LIFTING MECHANISMS 1. Orographic 2. Frontal 3. Convergence 4. Convection Cloud Development
More informationThe Water Cycle. 4 th Grade Pre-Visit Activity #1
th Grade Pre-Visit Activity # The Water Cycle Overview Objectives Subjects Earth s water molecules circulate among air, plants, animals, and soil by way of the water cycle. This activity uses a game to
More informationAtmospheric Dynamics of Venus and Earth. Institute of Geophysics and Planetary Physics UCLA 2 Lawrence Livermore National Laboratory
Atmospheric Dynamics of Venus and Earth G. Schubert 1 and C. Covey 2 1 Department of Earth and Space Sciences Institute of Geophysics and Planetary Physics UCLA 2 Lawrence Livermore National Laboratory
More informationUnderstanding Basic Concepts demonstrate an awareness of air as a substance that surrounds us and takes up space, and whose movement we feel as wind
Designation: Ontario Curriculum: Science and Technology Earth and Space Systems: Grade 2 Air and Water in the Environment Written by: Andrea Schultz-Allison, Department of Earth Sciences, The University
More informationWater & Climate Review
Water & Climate Review 1. The cross section below shows the direction of air flowing over a mountain. Points A and B are at the same elevation on opposite sides of the mountain. 4. The graph below shows
More informationEXPLANATION OF WEATHER ELEMENTS AND VARIABLES FOR THE DAVIS VANTAGE PRO 2 MIDSTREAM WEATHER STATION
EXPLANATION OF WEATHER ELEMENTS AND VARIABLES FOR THE DAVIS VANTAGE PRO 2 MIDSTREAM WEATHER STATION The Weather Envoy consists of two parts: the Davis Vantage Pro 2 Integrated Sensor Suite (ISS) and the
More informationESCI-61 Introduction to Photovoltaic Technology. Solar Radiation. Ridha Hamidi, Ph.D.
1 ESCI-61 Introduction to Photovoltaic Technology Solar Radiation Ridha Hamidi, Ph.D. 2 The Sun The Sun is a perpetual source of energy It has produced energy for about 4.6 billions of years, and it is
More informationOverview. What is EMR? Electromagnetic Radiation (EMR) LA502 Special Studies Remote Sensing
LA502 Special Studies Remote Sensing Electromagnetic Radiation (EMR) Dr. Ragab Khalil Department of Landscape Architecture Faculty of Environmental Design King AbdulAziz University Room 103 Overview What
More informationThe Sun and the Stars
www.k5learning.com Objective Concepts (gravity, climate, solar system, hydrogen, helium, elements, core, ultraviolet rays, cluster, galaxy, Milky Way Galaxy); Sight words (surface, middle, dangerous, causes,
More information