Atmospheric Composition הרכב האטמוספירה
|
|
- Aubrey Sullivan
- 5 years ago
- Views:
Transcription
1 Atmospheric Composition הרכב האטמוספירה
2 N 2 O 2 Trace Gases Water Vapor (H 2 O) Argon (Ar) Carbon Dioxide (CO 2 ) Neon (Ne) Helium (He) Methane (CH 4 ) Nitrous Oxide (N 2 O) Ozone (O 3 )
3 Nitrogen and oxygen concentrations experience little change, but carbon dioxide, methane, nitrous oxides, and chlorofluorocarbons are gases experiencing great increases in concentration.
4 ppm % Real Air
5 Why so much Nitrogen? It is volatile in most forms Eg. Ammonia gas It is unreactive with most solid earth material It is stable in sunlight. Why so much Oxygen? Produced by photosynthesis. Why so much Argon? It slowly degasses from rocks It is unreactive so stays in the atmosphere Argon is a noble gas Why so little carbon dioxide? Original atmosphere was probably about 25% CO 2 It dissolves in water It is used by plants in photosynthesis
6
7 מחזור ההידרולוגי Water : The Hydrological Cycle
8
9 m Mixing Ratio w v = m d mass of water vapour mass of dry air [g/kg] Dry regions ~ 1 g/kg Tropics ~ 20g/kg Specific Humidity: q = w + m d 1 + w m v m v Since m v << m d q~w Specific humidity NOT dependent on volume
10
11 When evaporation = condensation w = w s w w s Saturation mixing ratio: PV = ρrt e s = water vapor pressure w s m vs m d ρ vs = ρ = e / s (p-e s ) d (R v T) (R d T) (mass of w.v. in saturated volume) w s = e s /(p-e s ) ~ e s /p e s depends only on T, and therefore w s depends only on T and p For a given T, w s is inversely proportional to the total pressure
12 Relative Humidity RH = 100 w = 100 e [%] w s e s RH is the ratio between the mixing ratio measured relative to the saturation value Dewpoint condensation of vapour to liquid
13 Dew Point Temperature: The temperature the air needs to be cooled in order to reach saturation (RH=100%) is called the dew point temp T d. Dry air T T d large Moist air T T d small Rule of thumb: T T d (100-RH) 5 If RH=85% T-Td ~3C Td T If T-Td = 15C RH ~ 25%
14
15 Clausius Clapeyron Equation The CC equation describes the phase transition between water vapour and water liquid (drops), and indicates the dependence of the saturation vapour pressure on temperature. L v de s dt = Td = L v T( 2-1 ) L v = latent heat of vaporization per unit mass (2.25x10 6 Jkg -1 ) 2, 1 = specific volume of vapour and water d = increase in volume as unit mass changes from liquid to gas >0 2 >> 1 d ~ 2 = 1/ρ = R v T/p de s = L e s dt R v T 2 P, T are values at the phase change
16 de s L e = s L~ const. dt R v T 2 e s = e o exp (- L ) R v T or for the relationship between vapour pressure and dew point: de dt = L e d R v T 2 d ( L ) e = e o exp - R v T d
17 RH=100%. הטל נקודת Dew point Temp.. D.. E.
18 Measurements of the Vapor Pressure in the Atmosphere
19 Warm air can absorb more vapor than cold air, so for a given parcel of air, specific humidity declines from its highest in the tropics to its lowest in the colder poles. Desert air, at 30, however, is not more saturated than polar air.
20 C How can we reach saturation in atmosphere? B A
21 CONTRAILS (Condensation Trails)
22
23 Evaporation Fog
24
25 Fog ערפל
26 Radiation Fog Occurs at the ground when dew point temperature is reached by radiational cooling.
27
28 Advection Fog Warm moist air that moves, or advects, above a cold surface may become cooled to its dew point temperature, creating an advection fog.
29
30 Dew טל frost קרה T>0C T<0C
31 Mixing of Air Parcels
32 טמפרטורה הגולה הלחה ) w Wet Bulb Temperature (T The measurement of the temperature air will cool by evaporation until it reaches saturation. Heat from the air evaporates water on the wet bulb, increasing the mixing ratio around the thermometer cooling air. At saturation T w there is no more evaporation, and therefore the air stops cooling RH=69% T d T w T In practice T w ~ T d +T 2
33 Psychrometer
34
Chapter 1: Earth with no Atmosphere (no rotation) - Introduction - Kepler Laws - Milankovich Theory - Seasons - Energy Balance Chapter 2: Earth with
Topics covered in Course: Chapter 1: Earth with no Atmosphere (no rotation) - Introduction - Kepler Laws - Milankovich Theory - Seasons - Energy Balance Chapter 2: Earth with Atmosphere (no rotation) -
More informationLecture Ch. 6. Condensed (Liquid) Water. Cloud in a Jar Demonstration. How does saturation occur? Saturation of Moist Air. Saturation of Moist Air
Lecture Ch. 6 Saturation of moist air Relationship between humidity and dewpoint Clausius-Clapeyron equation Dewpoint Temperature Depression Isobaric cooling Moist adiabatic ascent of air Equivalent temperature
More informationIntroduction. Lecture 6: Water in Atmosphere. How Much Heat Is Brought Upward By Water Vapor?
Lecture 6: Water in Atmosphere Introduction Over 70% of the planet is covered by water Water is unique in that it can simultaneously exist in all three states (solid, liquid, gas) at the same temperature
More informationThe Water Cycle. Water in the Atmosphere AOSC 200 Tim Canty. Class Web Site:
Water in the Atmosphere AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Latent Heat Evaporation & Saturation Relative Humidity Dew Point Lecture 11 Oct 2 2018
More informationCHAPTER 1. MEASURES OF ATMOSPHERIC COMPOSITION
1 CHAPTER 1. MEASURES OF ATMOSPHERIC COMPOSITION The objective of atmospheric chemistry is to understand the factors that control the concentrations of chemical species in the atmosphere. In this book
More informationScience Chapter 13,14,15
Science 1206 Chapter 13,14,15 1 Weather dynamics is the study of how the motion of water and air causes weather patterns. Energy from the Sun drives the motion of clouds, air, and water. Earth s tilt at
More informationWEATHER. Review Note Cards
WEATHER Review Note Cards Thermometer Weather instrument that measures air temperature Units include F, C, and K ESRT 13 Sling Psychrometer Weather instrument that measures relative humidity and dewpoint
More informationTemp 54 Dew Point 41 Relative Humidity 63%
Temp 54 Dew Point 41 Relative Humidity 63% Water in the Atmosphere Evaporation Water molecules change from the liquid to gas phase Molecules in liquids move slowly Heat energy makes them move faster When
More informationThe Atmosphere EVPP 110 Lecture Fall 2003 Dr. Largen
1 Physical Environment: EVPP 110 Lecture Fall 2003 Dr. Largen 2 Physical Environment: Atmosphere Composition Heat transfer Atmospheric moisture Atmospheric circulation Weather and climate 3 Physical Environment:
More information1. Water Vapor in Air
1. Water Vapor in Air Water appears in all three phases in the earth s atmosphere - solid, liquid and vapor - and it is one of the most important components, not only because it is essential to life, but
More informationChapter The transition from water vapor to liquid water is called. a. condensation b. evaporation c. sublimation d.
Chapter-6 Multiple Choice Questions 1. The transition from water vapor to liquid water is called. a. condensation b. evaporation c. sublimation d. deposition 2. The movement of water among the great global
More informationWater in the Atmosphere
Water in the Atmosphere Characteristics of Water solid state at 0 o C or below (appearing as ice, snow, hail and ice crystals) liquid state between 0 o C and 100 o C (appearing as rain and cloud droplets)
More informationName Class Date. 3. In what part of the water cycle do clouds form? a. precipitation b. evaporation c. condensation d. runoff
Skills Worksheet Directed Reading B Section: Water in the Air 1. What do we call the condition of the atmosphere at a certain time and place? a. the water cycle b. weather c. climate d. precipitation THE
More information7. The weather instrument below can be used to determine relative humidity.
1. What is the dewpoint temperature when the dry-bulb temperature is 12 C and the wet-bulb temperature is 7 C? A) 1 C B) -2 C C) -5 C D) 4 C 2. A parcel of air has a dry-bulb temperature reading of 16
More informationLecture 07 February 10, 2010 Water in the Atmosphere: Part 1
Lecture 07 February 10, 2010 Water in the Atmosphere: Part 1 About Water on the Earth: The Hydrological Cycle Review 3-states of water, phase change and Latent Heat Indices of Water Vapor Content in the
More informationChapter 5 - Atmospheric Moisture
Chapter 5 - Atmospheric Moisture Understanding Weather and Climate Aguado and Burt Water Water Vapor - water in a gaseous form, not droplets. Water can also achieve solid and liquid phases on Earth Temperature
More informationChapter 4 Water Vapor
Chapter 4 Water Vapor Chapter overview: Phases of water Vapor pressure at saturation Moisture variables o Mixing ratio, specific humidity, relative humidity, dew point temperature o Absolute vs. relative
More informationCh22&23 Test. Multiple Choice Identify the choice that best completes the statement or answers the question.
Ch22&23 Test Multiple Choice Identify the choice that best completes the statement or answers the question. 1. The two most abundant compounds in the atmosphere are carbon dioxide and a. particulates.
More informationDew Point and Cloud Formation
Name: Date: ES: 1 2 3 4 Dew Point and Cloud Formation Part A: Run some water over your hands. After shaking off the excess, wave them back and forth until they are dry. 1. Describe the change in temperature
More informationOutline. Aim. Gas law. Pressure. Scale height Mixing Column density. Temperature Lapse rate Stability. Condensation Humidity.
Institute of Applied Physics University of Bern Outline A planetary atmosphere consists of different gases hold to the planet by gravity The laws of thermodynamics hold structure as vertical coordinate
More informationLAB 3: Atmospheric Pressure & Moisture
Name School LAB 3: Atmospheric Pressure & Moisture Our atmosphere is a very dynamic area especially when we see what type of interactions it has with the surrounding environment. This lab will begin discussing
More informationWeather is the state or condition of the atmosphere at a given location for a brief time period.
Topic 8: WEATHER Workbook chapter 7 Weather is the state or condition of the atmosphere at a given location for a brief time period. Differences in how Earth s surfaces absorb and reradiate energy from
More information78% : component of atmosphere! 21% : 1% : Changes depending on origin of air: - originated over - originated over Ozone = O 3 Definition:
Unit 6 Part 1 Meteorology Name: Composition and Structure of the Atmosphere SWBAT: Describe the composition of the atmosphere. Diagram/describe the layers of the earth s atmosphere. Weather Climate Atmospheric
More informationThe Atmosphere. 1 Global Environments: 2 Global Environments:
1 Global Environments: 2 Global Environments: Composition Vertical structure Heat transfer Atmospheric moisture Atmospheric circulation Weather and climate 3 Global Environments: The earth s atmosphere
More informationaccording to and water. High atmospheric pressure - Cold dry air is other air so it remains close to the earth, giving weather.
EARTH'S ATMOSPHERE Composition of the atmosphere - Earth's atmosphere consists of nitrogen ( %), oxygen ( %), small amounts of carbon dioxide, methane, argon, krypton, ozone, neon and other gases such
More informationWeather, Atmosphere and Meteorology
S c i e n c e s Weather, Atmosphere and Meteorology Key words: Atmosphere, Ozone, Water vapor, solar radiation, Condensation, Evaporation, Humidity, Dew-Point Temperature, Cirrus Clouds, Stratus Clouds,
More informationThe Atmosphere. All weather occurs here 99% of water vapor found here ~75 % of total mass of the atmosphere
The Atmosphere Structure/Layers Contains 4 major layers See E.S.R.T pg 14 o Troposphere All weather occurs here 99% of water vapor found here ~75 % of total mass of the atmosphere o Stratosphere Contains
More informationAtmospheric Thermodynamics
Atmospheric Thermodynamics Atmospheric Composition What is the composition of the Earth s atmosphere? Gaseous Constituents of the Earth s atmosphere (dry air) Constituent Molecular Weight Fractional Concentration
More informationLecture 10: Climate Sensitivity and Feedback
Lecture 10: Climate Sensitivity and Feedback Human Activities Climate Sensitivity Climate Feedback 1 Climate Sensitivity and Feedback (from Earth s Climate: Past and Future) 2 Definition and Mathematic
More informationLecture 9: Climate Sensitivity and Feedback Mechanisms
Lecture 9: Climate Sensitivity and Feedback Mechanisms Basic radiative feedbacks (Plank, Water Vapor, Lapse-Rate Feedbacks) Ice albedo & Vegetation-Climate feedback Cloud feedback Biogeochemical feedbacks
More informationRadiation, Sensible Heat Flux and Evapotranspiration
Radiation, Sensible Heat Flux and Evapotranspiration Climatological and hydrological field work Figure 1: Estimate of the Earth s annual and global mean energy balance. Over the long term, the incoming
More informationP sat = A exp [B( 1/ /T)] B= 5308K. A=6.11 mbar=vapor press. 0C.
Lecture 5. Water and water vapor in the atmosphere 14 Feb 2008 Review of buoyancy, with an unusual demonstration of Archimedes principle. Water is a polar molecule that forms hydrogen bonds. Consequently
More informationClouds associated with cold and warm fronts. Whiteman (2000)
Clouds associated with cold and warm fronts Whiteman (2000) Dalton s law of partial pressures! The total pressure exerted by a mixture of gases equals the sum of the partial pressure of the gases! Partial
More informationAT 350 EXAM #1 February 21, 2008
This exam covers Ahrens Chapters 1 and 2, plus related lecture notes Write the letter of the choice that best completes the statement or answers the question. b_ 1. The Earth s atmosphere is currently
More informationWATER IN THE ATMOSPHERE
WATER IN THE ATMOSPHERE During a rainstorm, the air feels moist On a clear, cloudless day, the air may feel dry As the sun heats the land and oceans, the amount of water in the atmosphere changes Water
More informationRadiative equilibrium Some thermodynamics review Radiative-convective equilibrium. Goal: Develop a 1D description of the [tropical] atmosphere
Radiative equilibrium Some thermodynamics review Radiative-convective equilibrium Goal: Develop a 1D description of the [tropical] atmosphere Vertical temperature profile Total atmospheric mass: ~5.15x10
More informationAtmosphere Weather and Climate
Atmosphere Weather and Climate Weather and Climate Weather Atmospheric conditions at a particular time and place Climate Long-term average of weather conditions Often over decades or centuries Coastal
More informationPHYSICAL GEOGRAPHY. By Brett Lucas
PHYSICAL GEOGRAPHY By Brett Lucas INTRODUCTION TO ATMOSPHERIC MOISTURE Atmospheric Moisture The Nature of Water The Hydrologic Cycle Evaporation Measures of Humidity Condensation The Buoyancy of Air Precipitation
More informationATOC 3500/CHEM 3151 Air Pollution Chemistry Lecture 1
ATOC 3500/CHEM 3151 Air Pollution Chemistry Lecture 1 Note Page numbers refer to Daniel Jacob s online textbook: http://acmg.seas.harvard.edu/publications/ jacobbook/index.html Atmos = vapor + sphaira
More informationFunding provided by NOAA Sectoral Applications Research Project THE ATMOSPHERE. Basic Climatology Oklahoma Climatological Survey
Funding provided by NOAA Sectoral Applications Research Project THE ATMOSPHERE Basic Climatology Oklahoma Climatological Survey What we are going to cover 1. Composition of the Atmosphere 2. State Variables
More informationExam 1 (Chaps. 1-6 of the notes)
10/12/06 ATS 541 - Atmospheric Thermodynamics and Cloud Physics 1 Exam 1 (Chaps. 1-6 of the notes) ATS 541 students: Answer all questions ATS 441 students: You may delete problem 3 or problem 5 1. [10
More informationUnit 3 Review Guide: Atmosphere
Unit 3 Review Guide: Atmosphere Atmosphere: A thin layer of gases that forms a protective covering around the Earth. Photosynthesis: Process where plants take in carbon dioxide and release oxygen. Trace
More informationTemperature Scales
TEMPERATURE is a measure of the internal heat energy of a substance. The molecules that make up all matter are in constant motion. By internal heat energy, we really mean this random molecular motion.
More informationRadiative-Convective Models. The Hydrological Cycle Hadley Circulation. Manabe and Strickler (1964) Course Notes chapter 5.1
Climate Modeling Lecture 8 Radiative-Convective Models Manabe and Strickler (1964) Course Notes chapter 5.1 The Hydrological Cycle Hadley Circulation Prepare for Mid-Term (Friday 9 am) Review Course Notes
More informationAll objects emit radiation. Radiation Energy that travels in the form of waves Waves release energy when absorbed by an object. Earth s energy budget
Radiation Energy that travels in the form of waves Waves release energy when absorbed by an object Example: Sunlight warms your face without necessarily heating the air Shorter waves carry more energy
More informationWelcome. Vaisala Industrial Measure Webinar Series - Humidity Theory, Terms & Definitions. Yumi Alanoly Vaisala Application Engineer
Welcome Vaisala Industrial Measure Webinar Series - Humidity Theory, Terms & Definitions Yumi Alanoly Vaisala Application Engineer Agenda 1. Why do we measure humidity? 2. Dalton s Law 3. Relative humidity
More informationGeneral Chemistry. Contents. Chapter 8: The Atmospheric Gases and Hydrogen. Composition of Dry Air. 8-1 The Atmosophere. Chemicals from the Atmosphere
General Chemistry Principles and Modern Applications Petrucci Harwood Herring 8 th Edition Chapter 8: The Atmospheric Gases and Hydrogen Philip Dutton University of Windsor, Canada N9B 3P4 Contents 8-1
More informationWATER IN THE ATMOSPHERE
WATER IN THE ATMOSPHERE I. Humidity A. Defined as water vapor or moisture in the air (from evaporation and condensation). B. The atmosphere gains moisture from the evaporation of water from oceans, lakes,
More information1/2/2016 WEATHER DEFINITION
WEATHER DEFINITION Weather state or condition of the variables of the atmosphere at a given time Weather variables temperature, air pressure, wind, moisture, cloud cover, precipitation, storms Weather
More informationTemperature Pressure Wind Moisture
Chapter 1: Properties of Atmosphere Temperature Pressure Wind Moisture Thickness of the Atmosphere (from Meteorology Today) 90% 70% The thickness of the atmosphere is only about 2% of Earth s thickness
More informationGeneral Chemistry. Chapter 8: The Atmospheric Gases and Hydrogen. Principles and Modern Applications Petrucci Harwood Herring 8 th Edition
General Chemistry Principles and Modern Applications Petrucci Harwood Herring 8 th Edition Chapter 8: The Atmospheric Gases and Hydrogen Philip Dutton University of Windsor, Canada N9B 3P4 Prentice-Hall
More informationUnit 2: The atmosphere
Unit 2: The atmosphere 1. Composition and structure 2. Atmospheric pressure and humidity 3. Weather and climate 4. Atmospheric phenomena 5. Importance of the atmosphere Think and answer? a. What elements
More informationCAE 331/513 Building Science Fall 2015
CAE 331/513 Building Science Fall 2015 Week 5: September 24, 2015 Psychrometrics (equations) Advancing energy, environmental, and sustainability research within the built environment www.built-envi.com
More informationChapter 7. Water and Atmospheric Moisture. Water on Earth Unique Properties of Water Humidity Atmospheric Stability Clouds and Fog
Chapter 7 Water and Atmospheric Moisture Robert W. Christopherson Charlie Thomsen Water kept both the terrestrial and marine ecosystems closely linked with the atmosphere. (1) Air carries water vapor and
More informationSec Water vapour variables each has its own usefulness 2/11 The ideal gas law inter-relates vapour pressure (e) & absolute humidity ( ρv) 1 e
Ch7. Water vapour: the most variable gas & most important GHG Absolute humidity Specific humidity ρv ρv = q q= mass of water vapour volume of sample EAS270_Ch7_WaterVapour_A.odp JDW, EAS Ualberta, last
More informationThe Sun and Water Cycle
Have you ever jumped in a puddle or played in the rain? If so, you know you can get very wet. What you may not know is that a dinosaur could have walked through that same water millions of years ago. The
More informationGEF2200 atmospheric physics 2018
GEF2200 atmospheric physics 208 Solutions: thermodynamics 3 Oppgaver hentet fra boka Wallace and Hobbs (2006) er merket WH06 WH06 3.8r Unsaturated air is lifted (adiabatically): The first pair of quantities
More informationName Class Date STUDY GUIDE FOR CONTENT MASTERY
Atmosphere SECTION 11.1 Atmospheric Basics In your textbook, read about the composition of the atmosphere. Circle the letter of the choice that best completes the statement. 1. Most of Earth s atmosphere
More informationThe Atmosphere. Topic 3: Global Cycles and Physical Systems. Topic 3: Global Cycles and Physical Systems. Topic 3: Global Cycles and Physical Systems
The Atmosphere 1 How big is the atmosphere? Why is it cold in Geneva? Why do mountaineers need oxygen on Everest? 2 A relatively thin layer of gas over the Earths surface Earth s radius ~ 6400km Atmospheric
More informationUNIT 12: THE HYDROLOGIC CYCLE
UNIT 12: THE HYDROLOGIC CYCLE After Unit 12 you should be able to: o Effectively use the charts Average Chemical Composition of Earth s Crust, Hydrosphere and Troposphere, Selected Properties of Earth
More informationThermodynamics Review [?] Entropy & thermodynamic potentials Hydrostatic equilibrium & buoyancy Stability [dry & moist adiabatic]
Thermodynamics Review [?] Entropy & thermodynamic potentials Hydrostatic equilibrium & buoyancy Stability [dry & moist adiabatic] Entropy 1. (Thermodynamics) a thermodynamic quantity that changes in a
More informationAT 620 Notes. These notes were prepared by Prof. Steven A. Rutledge. (and adapted slightly for the Fall 2009 course, and again slightly for this year)
AT 620 Notes These notes were prepared by Prof. Steven A. Rutledge (and adapted slightly for the Fall 2009 course, and again slightly for this year) You may access Prof. Cotton s notes, password cloud9
More informationRelative Humidity and Dew Point Lab
Name: Relative Humidity and Dew Point Lab Weather is the present state of the atmosphere. Factors that determine the type of weather the world will have are: air pressure, wind, temperature and the air
More informationOn my honor, I have neither given nor received unauthorized aid on this examination.
Instructor(s): Prof. Whiting PHYSICS DEPARTMENT MET 1010 1st Midterm Exam Jan. 31, 2005 Name (print, last first): Signature: On my honor, I have neither given nor received unauthorized aid on this examination.
More informationClimate & Earth System Science. Introduction to Meteorology & Climate CHAPTER 1 LECTURE 1. Question: Introduction to the Atmosphere
Climate & Earth System Science Introduction to Meteorology & Climate MAPH 10050 Peter Lynch Peter Lynch Meteorology & Climate Centre School of Mathematical Sciences University College Dublin Meteorology
More informationCondensation: Dew, Fog and Clouds AT350
Condensation: Dew, Fog and Clouds AT350 T=30 C Water vapor pressure=12mb What is Td? What is the sat. water vapor T=30 C Water vapor pressure=12mb What is Td? What is the sat. water vapor ~12/42~29% POLAR
More informationChapter 4. Atmospheric Moisture, Condensation, and Clouds. 9/13/2012
Chapter 4 Atmospheric Moisture, Condensation, and Clouds. The sun s electromagnetic spectrum and some of the descriptive names of each region. The numbers underneath the curve approximate the percent of
More information9/13/2012. Chapter 4. Atmospheric Moisture, Condensation, and Clouds.
Chapter 2-3 review Chapter 2-3 review Chapter 4 Atmospheric Moisture, Condensation, and Clouds. The sun s electromagnetic spectrum and some of the descriptive names of each region. The numbers underneath
More informationFebruary 11, Weather and Water Investigation 6 Day 6
Weather and Water Investigation 6 Day 6 What is dew point? Bell Work Response Sheet: Water In The Air Answers When we put water on our hands and waved them in the air, our skin felt cooler. That's because
More informationEarth s Atmosphere. Describing Earth s Atmosphere
CHAPTER 4 Earth s Atmosphere LESSON 1 Describing Earth s Atmosphere What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column
More informationAtmospheric Basics Atmospheric Composition
Atmospheric Basics Atmospheric Composition Air is a combination of many gases, each with its own unique characteristics. About 99 percent of the atmosphere is composed of nitrogen and oxygen, with the
More informationAtmospheric and Oceanic Sciences 3/3L
Atmospheric and Oceanic Sciences 3/3L Introduction to the Atmospheric Environment 1 Instructor Dr. Jeffrey Lew Math Science 1961 310-825-3023 lew@atmos.ucla.edu AIM: jklew888 Twitter: atmosciproflew 2
More informationG109 Midterm Exam (Version A) October 10, 2006 Instructor: Dr C.M. Brown 1. Time allowed 50 mins. Total possible points: 40 number of pages: 5
G109 Midterm Exam (Version A) October 10, 2006 Instructor: Dr C.M. Brown 1 Time allowed 50 mins. Total possible points: 40 number of pages: 5 Part A: Short Answer & Problems (12), Fill in the Blanks (6).
More informationTemperature. Vertical Thermal Structure. Earth s Climate System. Lecture 1: Introduction to the Climate System
Lecture 1: Introduction to the Climate System T mass (& radiation) T & mass relation in vertical mass (& energy, weather..) Energy T vertical stability vertical motion thunderstorm What are included in
More informationChapter 15 The Atmosphere and Weather
Chapter 15 The Atmosphere and Weather Day Activity Homework 1 Notes I- II Layers of the atmosphere* 2 Notes III Air Pressure Labs* 3 Notes IV Global Winds Activity* 4 Complete Notes Concept Map Relative
More informationName 28-MAY-08. FA RP 1 Mr. Chase. 1. Which weather-station model shows an air pressure of millibars?
FA RP 1 Mr. Chase Name 28-MAY-08 1. Which weather-station model shows an air pressure of 993.4 millibars? 2. Which station model shows the correct form for indicating a northwest wind at 25 knots and an
More informationThe Atmosphere of Earth
The Atmosphere of Earth The probability of a storm can be predicted, but nothing can be done to stop or slow a storm. Understanding the atmosphere may help in predicting weather changes, but it is doubtful
More informationSection 4 Professor Donald McFarlane
Carbon cycle Present in atmosphere in low concentrations Autotrophs incorporate it into organic matter via photosynthesis Section 4 Professor Donald McFarlane Lecture 23 and Climate Carbon Cycle Respiration
More informationThickness of the Atmosphere
Lecture 1: A Brief Survey of the Atmosphere Origins of the atmosphere Vertical structure of composition Vertical structure of air pressure Vertical structure of temperature The ionosphere Thickness of
More information2. What are the four most common gasses in the atmosphere and their percentages?
Meteorology Review Directions: Answer the following open ended review questions. Utilize a diagram where appropriate and do make sure that you label and describe the drawing. Atmospheric Composition 1.
More information2/22/ Atmospheric Characteristics
17.1 Atmospheric Characteristics Atmosphere: the gaseous layer that surrounds the Earth I. In the past, gases came from volcanic eruptions A. Water vapor was a major component of outgassing B. Other gases
More information5) The amount of heat needed to raise the temperature of 1 gram of a substance by 1 C is called: Page Ref: 69
Homework #2 Due 9/19/14 1) If the maximum temperature for a particular day is 26 C and the minimum temperature is 14 C, what would the daily mean temperature be? (Page Ref: 66) 2) How is the annual mean
More informationNon-Reacting Gas Mixtures. Introduction. P-V-T Relationships for Ideal Gas Mixtures. Amagat Model (law of additive volumes)
Non-Reacting Gas Mixtures Reading Problems 13-1 13-3 13-52, 13-60 14-1 14-7 14-32, 14-35, 14-68, 14-71, 14-75 14-79, 14-103, 14-112 Introduction homogeneous gas mixtures are frequently treated as a single
More informationMultiple Choice (2 Points Each)
ATMO 336 -- Exam 1 Name Multiple Choice (2 Points Each) 1. The atmospheric greenhouse effect keeps the average surface temperature of the Earth about 60 F warmer than if there were no atmosphere. The two
More informationWeather & Atmospheric Variables Review
Weather & Atmospheric Variables Review Words that are bold, italicized and/or underlined are vocabulary you must KNOW! A) Atmospheric variables: a) Temperature as it relates to: 1) duration of insolation...longer
More informationINTRODUCTORY CHEMISTRY Concepts and Critical Thinking Seventh Edition by Charles H. Corwin
Lecture INTRODUCTORY CHEMISTRY Concepts and Critical Thinking Seventh Edition by Charles H. Corwin Gases by Christopher G. Hamaker Illinois State University Properties of Gases There are five important
More informationHumidity. Reid Pierce Fulbright Jr. High Bentonville, AR
Humidity Reid Pierce Fulbright Jr. High Bentonville, AR Humidity After water evaporates, where does it go? to the air Describe a humid day Humidity how much water vapor is in the air Warm air can hold
More informationDay 1 of Global Warming. Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Day 1 of Global Warming Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The Atmosphere Atmosphere = the thin layer (1/100 th of Earth s diameter) of gases that surrounds
More informationEvolution of the Atmosphere
Evolution of the Atmosphere Anticipation Guide Oxygen is the main gas found in the atmosphere The current atmosphere is the same atmosphere that the Earth had when it formed Water vapor is a gas found
More informationanemometer a weather instrument that measures wind speed with wind-catching cups (SRB, IG)
FOSS Weather on Earth Module Glossary 3 rd Edition 2012 absorb to soak in air the mixture of gases surrounding Earth air pressure the force exerted on a surface by the mass of the air above it anemometer
More informationTable of Contents. Chapter: Atmosphere. Section 1: Earth's Atmosphere. Section 2: Energy Transfer in the Atmosphere. Section 3: Air Movement
Table of Contents Chapter: Atmosphere Section 1: Earth's Atmosphere Section 2: Energy Transfer in the Atmosphere Section 3: Air Movement Table of Contents Chapter: Atmosphere Section 2: Energy Transfer
More informationThe Earth and Its Atmosphere: 1.Chemical composition and 2. Vertical structure
The Earth and Its Atmosphere: 1.Chemical composition and 2. Vertical structure RECAP Definition of an atmosphere: the gas surrounding a planet/satellite/comet/ Origin of the atmosphere. Three stages: I
More informationGEF2200 Atmosfærefysikk 2012
GEF2200 Atmosfærefysikk 2012 Løsningsforslag til oppgavesett 4 WH06 3.46 (WH 2.49) The air parcel has the properties p = 1000hPa, T = 15 C and T d = 4 C. b Lifting the air parcel to p 2 = 900hPa, T 2 we
More informationLecture 4: Global Energy Balance
Lecture : Global Energy Balance S/ * (1-A) T A T S T A Blackbody Radiation Layer Model Greenhouse Effect Global Energy Balance terrestrial radiation cooling Solar radiation warming Global Temperature atmosphere
More informationCAE 331/513 Building Science Fall 2017
CAE 331/513 Building Science Fall 2017 October 5, 2017 Psychrometrics (equations) Advancing energy, environmental, and sustainability research within the built environment www.built-envi.com Twitter: @built_envi
More informationASSESSMENT CHART FOR INVESTIGATIONS 1 AND 2 STUDENT NAME
ASSESSMENT CHART FOR INVESTIGATIONS 1 AND 2 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18. 19. 20. 21. 22. 23. 24. 25. 26. 27. 28. 29. 30. 31. 32. STUDENT NAME Weather Measurements (TO)
More informationLecture 4: Global Energy Balance. Global Energy Balance. Solar Flux and Flux Density. Blackbody Radiation Layer Model.
Lecture : Global Energy Balance Global Energy Balance S/ * (1-A) terrestrial radiation cooling Solar radiation warming T S Global Temperature Blackbody Radiation ocean land Layer Model energy, water, and
More information1. Base your answer to the following question on the weather map below, which shows a weather system that is affecting part of the United States.
1. Base your answer to the following question on the weather map below, which shows a weather system that is affecting part of the United States. Which sequence of events forms the clouds associated with
More informationCOMPOSITION OF THE ATMOSPHERE
Name Air COMPOSITION OF THE ATMOSPHERE 1. What are the two most abundant gases in the atmospherere? 2. Why do you think the percentage of water vapor in the air varies? 3. Would you classify carbon dioxide
More informationLecture Outlines PowerPoint. Chapter 17 Earth Science 11e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 17 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
More information