Introduction Outline Big picture Cloud types according to WMO Appendix. Atmospheric Physics. An Introduction to Clouds: From the Microscale to Climate
|
|
|
- Ashley Ball
- 5 years ago
- Views:
Transcription
1 Atmospheric Physics An Introduction to Clouds: From the Microscale to Climate Ulrike Lohmann and Alexander Beck ETH Zurich Institute for Atmospheric and Climate Science Ulrike Lohmann (IACETH) Atmospheric Physics / 22
2 Introduction Outline Big picture Cloud types according to WMO Appendix Lecturers and tutors Alex Beck Lea Beusch Ulrike Lohmann Annika Lauber Ulrike Lohmann (IACETH) Atmospheric Physics Bernhard Enz / 22
3 Introduction Outline Big picture Cloud types according to WMO Appendix My research interests (modelling) Sources: Remo Dietlicher (IAC), Gilgen et al., ACP (2018), TC Florence (NASA) Ulrike Lohmann (IACETH) Atmospheric Physics / 22
4 Introduction Outline Big picture Cloud types according to WMO Appendix Experimental interests µm particle size [µm] Ulrike Lohmann (IACETH) Atmospheric Physics / 22
5 Learning objectives: You will be able to explain the mechanisms of cloud and precipitation formation using knowledge of humidity processes and thermodynamics. to evaluate the significance of clouds and aerosol particles for climate and artificial weather modification. Ulrike Lohmann (IACETH) Atmospheric Physics / 22
6 Organizational details: Prerequisite: Any introduction to Atmospheric Science Mixture of traditional lectures and flipped classroom Tutorials and question time: Wednesdays 12-12:45h Website and moodle platform for the course: iac.ethz.ch/edu/courses/bachelor/vertiefung/atmospheric_physics moodle-app2.let.ethz.ch/course/view.php?id=4729 How to reach us: Ulrike Lohmann (IACETH) Atmospheric Physics / 22
7 Flipped classroom - Pedagogical motivation Ulrike Lohmann (IACETH) Atmospheric Physics / 22
8 Flipped classroom - How do we achieve this? Book Video Questionnaire Exercises EduApp Presentations Exercises Ulrike Lohmann (IACETH) Atmospheric Physics / 22
9 Introduction Outline Big picture Cloud types according to WMO Appendix Flipped classroom - How do we achieve this? Ulrike Lohmann (IACETH) Atmospheric Physics / 22
10 Flipped classroom at ETH Im Duell: Vorlesung vs. Flipped Classroom - Die erste Runde blogs.ethz.ch/deliscope/2017_07_17/im-duell-vorlesung-vs-flipped-classroom-die-erste-runde/ Ulrike Lohmann (IACETH) Atmospheric Physics / 22
11 Organizational Details Flipped classroom: Prior to class: reading of book chapter 10 online multiple choice questions about the book chapter will be provided on moodle by Wednesday 8 pm here: The online questions need to be answered by Monday at 2 pm In class: we will discuss your open questions from the textbook and online questions and apply your new knowledge to problem sets. These problem sets can be finished at home and be discussed in the tutorial in the following week Question time (if wanted): Wednesdays 12-12:45h Ulrike Lohmann (IACETH) Atmospheric Physics / 22
12 Organizational Details Traditional lectures and assignments: The lecture notes will be put on moodle latest by Tuesday noon Handing assignments in for correction is voluntary but it is highly recommended and will be important for a successful exam Assignments are discussed in the tutorials on Wednesdays 12-12:45h in the same room Ulrike Lohmann (IACETH) Atmospheric Physics / 22
13 Credits and exam How to earn credits: The short presentations in the last lecture are obligatory in order to take the oral exam The oral exam lasts 25 minutes You need to obtain at least grade 4 (60% of the points) for credits to be awarded The course yields 3 ECTS credit points Ulrike Lohmann (IACETH) Atmospheric Physics / 22
14 Textbook Lohmann, U., Lüönd, F. and Mahrt, F., An Introduction to Clouds: From the Microscale to Climate, Cambridge Univ. Press, 391 pp., Online available from the moodle platform (complete and as individual chapters for the lectures) Hard copies available either from Cambridge Univ. Press or Amazon (cheaper) Purchasing the hard copy maybe useful if you consider also taking the MSc course Cloud Dynamics Also the ETH green library has a total of 10 copies which can only be borrowed by students subscribed to this course. These copies can be loaned for the whole semester. Ulrike Lohmann (IACETH) Atmospheric Physics / 22
15 Course outline Sep 19: Introduction Sep 26: Thermodynamics - part I Oct 03: Thermodynamics - part II flipped Oct 10: Atmospheric dynamics Oct 17: Radiation and optical properties Oct 24: Mixing and convection - flipped Oct 31: Atmospheric aerosols Nov 07: Formation of cloud droplets flipped Nov 14: Microphysics of warm clouds Nov 21: Microphysics of cold clouds - flipped Nov 28: Precipitation Dec 05: Storms - flipped Dec 12: Applied cloud and aerosol physics Dec 19: Lecture wrap-up - flipped Ulrike Lohmann (IACETH) Atmospheric Physics / 22
16 Importance of clouds Definition: A cloud is an aggregate of cloud droplets or ice crystals, or a combination of both, suspended in air. Clouds are a major factor in the Earth s radiation budget, reflecting sunlight back to space and trapping infrared radiation emitted by the Earth s surface. Clouds deliver water from the atmosphere to the Earth s surface as rain or snow hydrological cycle Clouds scavenge gaseous and particulate materials and return them to the surface (wet deposition). Clouds provide a medium for aqueous-phase chemical reactions and production of secondary species. Updrafts and downdrafts associated with clouds largely determine the vertical redistribution of trace species, temperature and moisture. Ulrike Lohmann (IACETH) Atmospheric Physics / 22
17 Cloud types Cumulus (Cu): vertical development Stratus (St): layered cloud Cirrus (Ci): high altitude ice clouds 10 cloud types in 4 families 1 : Low base with vertical extent: Cu, Cb, Ns Low base and layered (0-2 km): St, Sc Mid level clouds (2-7 km): As, Ac High altitude ice clouds (5-13 km): Ci, Cs, Cc Sources for individual cloud types: Karlsruher Wolkenatlas: and Lohmann et al. (2016) 1 heights refer to mid latitudes Ulrike Lohmann (IACETH) Atmospheric Physics / 22
18 Introduction Outline Big picture Cloud types according to WMO Appendix Summary of different cloud types Fig. 1.3 (Lohmann et al., 2016) Ulrike Lohmann (IACETH) Atmospheric Physics / 22
19 Your task Take 1-2 minutes and work in groups of three. Which cloud do you see on the picture? Try to name them. Put it on the blackboard in the right family and justify your choice Ulrike Lohmann (IACETH) Atmospheric Physics / 22
20 Global mean energy budget [W m 2 ] Solar reflected 100 TOA Incoming solar 340 Imbalance 1 Thermal outgoing 239 Atmosphere Solar reflected by clouds, aerosol and gases Solar down surface 185 Solar absorbed 79 Thermal outgoing Atmospheric Greenhouse window gases Earth`s surface Imbalance 1 Absorbed solar 161 Sensible heat 20 Latent heat 84 Up surface 398 Down surface 342 Fig (Lohmann et al., 2016) Ulrike Lohmann (IACETH) Atmospheric Physics / 22
21 Seasonal mean cloud cover Ulrike Lohmann (IACETH) Atmospheric Physics / 22
22 Introduction Outline Big picture Cloud types according to WMO Appendix Cloud radiative effect (CRE) & precipitation IPCC, AR5, Fig. 7.7: Annual mean CRE ( ) from CERES satellite data and precipitation ( ) from GPCP (Boucher et al., 2013) Ulrike Lohmann (IACETH) Atmospheric Physics / 22
Importance of clouds. climate. ocean. radiation. life. hydrological cycle. latent heat + loading. clouds & precip + aerosols.
Importance of clouds climate life ocean radiation hydrological cycle clouds & precip + aerosols latent heat + loading dynamics electricity aqueous chemistry Ulrike Lohmann (IACETH) Physics and Dynamics
Name(s) Period Date. Earth s Energy Budget: How Is the Temperature of Earth Controlled?
Name(s) Period Date 1 Introduction Earth s Energy Budget: How Is the Temperature of Earth Controlled? As you learned from the reading, the balance between incoming energy from the sun and outgoing energy
Implications of Sulfate Aerosols on Clouds, Precipitation and Hydrological Cycle
Implications of Sulfate Aerosols on Clouds, Precipitation and Hydrological Cycle Source: Sulfate aerosols are produced by chemical reactions in the atmosphere from gaseous precursors (with the exception
REMOTE SENSING OF THE ATMOSPHERE AND OCEANS
EAS 6145 SPRING 2007 REMOTE SENSING OF THE ATMOSPHERE AND OCEANS Instructor: Prof. Irina N. Sokolik office 2258, phone 404-894-6180 isokolik@eas.gatech.edu Meeting Time: Mondays: 3:05-4:25 PM Wednesdays:
Clouds on Mars Cloud Classification
Lecture Ch. 8 Cloud Classification Descriptive approach to clouds Drop Growth and Precipitation Processes Microphysical characterization of clouds Complex (i.e. Real) Clouds Examples Curry and Webster,
1. Weather and climate.
Lecture 31. Introduction to climate and climate change. Part 1. Objectives: 1. Weather and climate. 2. Earth s radiation budget. 3. Clouds and radiation field. Readings: Turco: p. 320-349; Brimblecombe:
Polar regions Temperate Regions Tropics High ( cirro ) 3-8 km 5-13 km 6-18 km Middle ( alto ) 2-4 km 2-7 km 2-8 km Low ( strato ) 0-2 km 0-2 km 0-2 km
Clouds and Climate Clouds (along with rain, snow, fog, haze, etc.) are wet atmospheric aerosols. They are made up of tiny spheres of water from 2-100 m which fall with terminal velocities of a few cm/sec.
Earth s Energy Budget: How Is the Temperature of Earth Controlled?
1 NAME Investigation 2 Earth s Energy Budget: How Is the Temperature of Earth Controlled? Introduction As you learned from the reading, the balance between incoming energy from the sun and outgoing energy
Precipitation. GEOG/ENST 2331 Lecture 12 Ahrens: Chapter 7
Precipitation GEOG/ENST 2331 Lecture 12 Ahrens: Chapter 7 Last lecture! Atmospheric stability! Condensation! Cloud condensation nuclei (CCN)! Types of clouds Precipitation! Why clouds don t fall! Terminal
ATMOSPHERIC RADIATIVE TRANSFER Fall 2009 EAS 8803
ATMOSPHERIC RADIATIVE TRANSFER Fall 2009 EAS 8803 Instructor: Prof. Irina N. Sokolik Office 3104, phone 404-894-6180 isokolik@eas.gatech.edu Meeting Time: Tuesdays/Thursday: 1:35-2:55 PM Meeting place:
Global Climate Change
Global Climate Change Definition of Climate According to Webster dictionary Climate: the average condition of the weather at a place over a period of years exhibited by temperature, wind velocity, and
Week: Dates: 3/2 3/20 Unit: Climate
clementaged.weebly.com Name: EVEN Period: Week: 28 30 Dates: 3/2 3/20 Unit: Climate Monday Tuesday Wednesday Thursday Friday 2 O 3 E *Vocabulary *Water in the Atmosphere and Clouds Notes *Cloud Drawings
The 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
CLIM-111/PHYS-111 Introduction to the Fundamentals of Atmospheric Science CLIM-112/PHYS-112 Lab
CLIM-111/PHYS-111 Introduction to the Fundamentals of Atmospheric Science CLIM-112/PHYS-112 Lab An overview of the Earth s atmosphere, its history, and the fundamental physical and chemical processes which
Mon Oct 20. Today: radiation and temperature (cont) sun-earth geometry energy balance >> conceptual model of climate change Tues:
Mon Oct 20 Announcements: bring calculator to class from now on > in-class activities > midterm and final Today: radiation and temperature (cont) sun-earth geometry energy balance >> conceptual model of
8. Clouds and Climate
8. Clouds and Climate 1. Clouds (along with rain, snow, fog, haze, etc.) are wet atmospheric aerosols. They are made up of tiny spheres of water from 2-100 m which fall with terminal velocities of a few
Wednesday, September 8, 2010 Infrared Trapping the Greenhouse Effect
Wednesday, September 8, 2010 Infrared Trapping the Greenhouse Effect Goals to look at the properties of materials that make them interact with thermal (i.e., infrared, or IR) radiation (absorbing and reemitting
9 Condensation. Learning Goals. After studying this chapter, students should be able to:
9 Condensation Learning Goals After studying this chapter, students should be able to: 1. explain the microphysical processes that operate in clouds to influence the formation and growth of cloud droplets
ATMOS 5140 Lecture 1 Chapter 1
ATMOS 5140 Lecture 1 Chapter 1 Atmospheric Radiation Relevance for Weather and Climate Solar Radiation Thermal Infrared Radiation Global Heat Engine Components of the Earth s Energy Budget Relevance for
Climate Change: Global Warming Claims
Climate Change: Global Warming Claims Background information (from Intergovernmental Panel on Climate Change): The climate system is a complex, interactive system consisting of the atmosphere, land surface,
Introduction to Atmosphere, Ocean, and Climate Dynamics
12.003 Introduction to Atmosphere, Ocean, and Climate Dynamics Instructor Paul O Gorman, 54-1712 pog@mit.edu Teaching Assistant Elezhan Zhakiya (e.zhakiya@gmail.com) Webpage http://www.mit.edu/~pog/12.003
What does a raindrop look like as it is falling? A B C
What does a raindrop look like as it is falling? A B C As the raindrop falls, it bumps into air molecules, flattening out the bottom of the drop! Force or air resistance Force of gravity Water can be in
GEOGRAPHY AND HISTORY
GEOGRAPHY AND HISTORY YEAR 1, PART 1 www.vicensvives.es Contents 01 Our planet Earth 02 The representation of the Earth: maps 03 The Earth s relief 04 Rivers and seas 05 Weather and climate 06 Climates
NATS 1750 Lecture. Wednesday 28 th November Pearson Education, Inc.
NATS 1750 Lecture Wednesday 28 th November 2012 Processes that lift air Orographic lifting Elevated terrains act as barriers Result can be a rainshadow desert Frontal wedging Cool air acts as a barrier
GEOG 1010 B. Come to the PASS workshop with your mock exam complete. During the workshop you can work with other students to review your work.
It is most beneficial to you to write this mock midterm UNDER EXAM CONDITIONS. This means: Complete the midterm in 70 minutes. Work on your own. Keep your notes and textbook closed. Attempt every question.
Meteorological Satellite Image Interpretations, Part III. Acknowledgement: Dr. S. Kidder at Colorado State Univ.
Meteorological Satellite Image Interpretations, Part III Acknowledgement: Dr. S. Kidder at Colorado State Univ. Dates EAS417 Topics Jan 30 Introduction & Matlab tutorial Feb 1 Satellite orbits & navigation
Pd: Date: Page # Describing Weather -- Lesson 1 Study Guide
Name: Pd: Date: Page # Describing Weather -- Lesson 1 Study Guide Rating Before Learning Goals Rating After 1 2 3 4 Describe weather. 1 2 3 4 1 2 3 4 List and define the variables used to describe weather.
Weather Forecasts and Climate AOSC 200 Tim Canty. Class Web Site: Lecture 27 Dec
Weather Forecasts and Climate AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Climate Natural Variations Feedback Mechanisms Lecture 27 Dec 4 2018 1 Climate
Name 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
GEOGRAPHY EYA NOTES. Weather. atmosphere. Weather and climate
GEOGRAPHY EYA NOTES Weather and climate Weather The condition of the atmosphere at a specific place over a relatively short period of time Climate The atmospheric conditions of a specific place over a
NATS 101 Section 13: Lecture 11. Clouds
NATS 101 Section 13: Lecture 11 Clouds Cloud Classification Luke Howard (English naturalist) developed a system in 1803 that employed Latin words to describe clouds as they appear to a ground observer.
- matter-energy interactions. - global radiation balance. Further Reading: Chapter 04 of the text book. Outline. - shortwave radiation balance
(1 of 12) Further Reading: Chapter 04 of the text book Outline - matter-energy interactions - shortwave radiation balance - longwave radiation balance - global radiation balance (2 of 12) Previously, we
ATMOSPHERIC SCIENCE-ATS (ATS)
Atmospheric Science-ATS (ATS) 1 ATMOSPHERIC SCIENCE-ATS (ATS) Courses ATS 150 Science of Global Climate Change Credits: 3 (3-0-0) Physical basis of climate change. Energy budget of the earth, the greenhouse
Climate Dynamics (PCC 587): Feedbacks & Clouds
Climate Dynamics (PCC 587): Feedbacks & Clouds DARGAN M. W. FRIERSON UNIVERSITY OF WASHINGTON, DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 6: 10-14-13 Feedbacks Climate forcings change global temperatures directly
Earth Energy Budget Pre-lab
Science Unit: Lesson 3: Climate Change Earth Energy Budget Pre-lab School year: 2008/2009 Developed for: Developed by: Grade level: Duration of lesson: Notes: Shaughnessy Elementary School, Vancouver School
Planetary Atmospheres: Earth and the Other Terrestrial Worlds Pearson Education, Inc.
Planetary Atmospheres: Earth and the Other Terrestrial Worlds 10.1 Atmospheric Basics Our goals for learning: What is an atmosphere? How does the greenhouse effect warm a planet? Why do atmospheric properties
Energy Balance and Temperature. Ch. 3: Energy Balance. Ch. 3: Temperature. Controls of Temperature
Energy Balance and Temperature 1 Ch. 3: Energy Balance Propagation of Radiation Transmission, Absorption, Reflection, Scattering Incoming Sunlight Outgoing Terrestrial Radiation and Energy Balance Net
Energy Balance and Temperature
Energy Balance and Temperature 1 Ch. 3: Energy Balance Propagation of Radiation Transmission, Absorption, Reflection, Scattering Incoming Sunlight Outgoing Terrestrial Radiation and Energy Balance Net
4/25/18. Precipitation and Radar GEF4310 Cloud Physics. Schedule, Spring Global precipitation patterns
Precipitation and Radar GEF4310 Cloud Physics Trude Storelvmo, Dept. of Geoscience, U. of Oslo Spring 2018 Schedule, Spring 2018 Week # Monday (exercises) Wednesday (lectures) 3 (15/1) No class (17/1)
Clouds and Rain Unit (3 pts)
Name: Section: Clouds and Rain Unit (Topic 8A-2) page 1 Clouds and Rain Unit (3 pts) As air rises, it cools due to the reduction in atmospheric pressure Air mainly consists of oxygen molecules and nitrogen
Text: Lutgens and Tarbuck, The Atmosphere (14 th ed.), Quick Start: Preparing Effectively for Each Class
Montgomery College, Rockville AOSC100 Weather and Climate (CRN#31633) Syllabus Spring 2019 Text: Lutgens and Tarbuck, The Atmosphere (14 th ed.), 2019 Instructor: Bill Krayer, Adjunct Professor Office:
How to display RGB imagery by SATAID
How to display RGB imagery by SATAID Akihiro SHIMIZU Meteorological Satellite Center (MSC), Japan Meteorological Agency (JMA) Ver. 2015110500 RGB imagery on SATAID SATAID software has a function of overlapping
Introduction to Climate ~ Part I ~
2015/11/16 TCC Seminar JMA Introduction to Climate ~ Part I ~ Shuhei MAEDA (MRI/JMA) Climate Research Department Meteorological Research Institute (MRI/JMA) 1 Outline of the lecture 1. Climate System (
The troposphere is the layer closest to Earth s surface. Extends from 9-16 km above Earth s Surface It contains most of the mass of the atmosphere.
Chapter 11 The atmosphere is the blanket of gases surrounding Earth that contains about 78% nitrogen, 21% oxygen, and 1% other gases such as argon, carbon dioxide, and water vapor The atmosphere is classified
Chapter 5: Forms of Condensation and Precipitation. Copyright 2013 Pearson Education, Inc.
Chapter 5: Forms of Condensation and Precipitation Water vapor's role in the Earth's weather is major. Its the product of evaporation. It is lifted up, condenses and forms clouds. It is also a greenhouse
Clouds & Mission for NASA
Clouds & Mission for NASA Name: Danielle Leavitt Estimated Time: 1 hr. 10 min. + Daily NASA Observations Content Area(s): Science Grade Level(s): 4th Number of Students: 30 Stage 1- Desired Results Established
Name 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
Moisture, Clouds, and Precipitation: Clouds and Precipitation. Dr. Michael J Passow
Moisture, Clouds, and Precipitation: Clouds and Precipitation Dr. Michael J Passow What Processes Lift Air? Clouds require three things: water vapor, a condensation nucleus, and cooling Cooling usually
Geoscience 106 syllabus (fall offering)
Geoscience 106 syllabus (fall offering) Environmental Geology Class meetings: Three 50-minute meetings per week, typically MWF 9:55-10:45 A.M. Classroom: AB20 Weeks Hall Textbook: Environmental Geology
Mon April 17 Announcements: bring calculator to class from now on (in-class activities, tests) HW#2 due Thursday
Mon April 17 Announcements: bring calculator to class from now on (in-class activities, tests) HW#2 due Thursday Today: Fundamentals of Planetary Energy Balance Incoming = Outgoing (at equilibrium) Incoming
Lecture 7: The Monash Simple Climate
Climate of the Ocean Lecture 7: The Monash Simple Climate Model Dr. Claudia Frauen Leibniz Institute for Baltic Sea Research Warnemünde (IOW) claudia.frauen@io-warnemuende.de Outline: Motivation The GREB
ESE / GE 148a: Introduction to Climate. Organizational Details - I
ESE / GE 148a: Introduction to Climate Organizational Details - I TA: Tim Merlis and Zhihong Tan Tim is a graduate student in Environmental Science and Engineering and is currently working on climate dynamics
SHAPING OUR FUTURE: THE CLIMATE CHALLENGE KS3 LESSON 1 TEACHER GUIDE HOW IS OUR CLIMATE CHANGING?
SHAPING OUR FUTURE: THE CLIMATE CHALLENGE KS3 LESSON 1 TEACHER GUIDE HOW IS OUR CLIMATE CHANGING? KS3 LESSON 1 TEACHER GUIDE HOW IS OUR CLIMATE CHANGING? Learning objective: To understand, through the
Moisture, Clouds, and Precipitation Earth Science, 13e Chapter 17
Moisture, Clouds, and Precipitation Earth Science, 13e Chapter 17 Stanley C. Hatfield Southwestern Illinois College Changes of state of water, H 2 O Water is the only substance in atmosphere that exists
Earth: the Goldilocks Planet
Earth: the Goldilocks Planet Not too hot (460 C) Fig. 3-1 Not too cold (-55 C) Wave properties: Wavelength, velocity, and? Fig. 3-2 Reviewing units: Wavelength = distance (meters or nanometers, etc.) Velocity
Weather Notes. Chapter 16, 17, & 18
Weather Notes Chapter 16, 17, & 18 Weather Weather is the condition of the Earth s atmosphere at a particular place and time Weather It is the movement of energy through the atmosphere Energy comes from
Electromagnetic Radiation. Radiation and the Planetary Energy Balance. Electromagnetic Spectrum of the Sun
Radiation and the Planetary Energy Balance Electromagnetic Radiation Solar radiation warms the planet Conversion of solar energy at the surface Absorption and emission by the atmosphere The greenhouse
Three-dimensional (3-D) radiative transfer codes are mainly used in cloud studies (e.g., LES models) and vegetation studies.
Lecture 5. Composition and structure of the Earth s atmosphere. Basic properties of gases, aerosols, and clouds that are important for radiative transfer modeling. Objectives: 1. Structure of the Earth
Lecture 3. Background materials. Planetary radiative equilibrium TOA outgoing radiation = TOA incoming radiation Figure 3.1
Lecture 3. Changes in planetary albedo. Is there a clear signal caused by aerosols and clouds? Outline: 1. Background materials. 2. Papers for class discussion: Palle et al., Changes in Earth s reflectance
Climate Dynamics (PCC 587): Clouds and Feedbacks
Climate Dynamics (PCC 587): Clouds and Feedbacks D A R G A N M. W. F R I E R S O N U N I V E R S I T Y O F W A S H I N G T O N, D E P A R T M E N T O F A T M O S P H E R I C S C I E N C E S D A Y 7 : 1
The Structure and Motion of the Atmosphere OCEA 101
The Structure and Motion of the Atmosphere OCEA 101 Why should you care? - the atmosphere is the primary driving force for the ocean circulation. - the atmosphere controls geographical variations in ocean
An Introduction to Earth s Climate
LIVE INTERACTIVE LEARNING @ YOUR DESKTOP An Introduction to Earth s Climate Presented by: Dr. Lisa Gardiner Thursday, March 25, 2010 An Introduction to Earth s Climate A web seminar for the NSTA community
student pretest Stewardship Project middle school (Grades 7-8)
student pretest Stewardship Project middle school (Grades 7-8) 1. True or False. Solar energy is radiant energy carried through the sun s heat and light. 2. Yes or No. Does solar energy dissipate as it
Chapter 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
ATOC 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
Layers of the Earth, Ozone Layer and Spheres of the Earth
Layers of the Earth, Ozone Layer and Spheres of the Earth Importance of the Atmosphere: Earth s atmosphere is a thin layer of air that forms a protective covering around the planet, without which days
ASTRONOMY 2212 The Solar System: Planets, small bodies and new worlds Fall 2017
ASTRONOMY 2212 The Solar System: Planets, small bodies and new worlds Fall 2017 Class Meetings: Tuesday & Thursday 11:40 12:55 Class Location: Space Sciences Building Room 105 Instructor: Philip Nicholson
Let s make a simple climate model for Earth.
Let s make a simple climate model for Earth. What is the energy balance of the Earth? How is it controlled? ó How is it affected by humans? Energy balance (radiant energy) Greenhouse Effect (absorption
- global radiative energy balance
(1 of 14) Further Reading: Chapter 04 of the text book Outline - global radiative energy balance - insolation and climatic regimes - composition of the atmosphere (2 of 14) Introduction Last time we discussed
Weather, 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,
Weather is the of the Earth s atmosphere at a place and time. It is the movement of through the atmosphere o Energy comes from the
Weather Notes Weather Weather is the of the Earth s atmosphere at a place and time It is the movement of through the atmosphere o Energy comes from the The sun is the force that weather The sun s energy
Chapter 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
9/13/2012. 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
Meteorology Curriculum Maps Unit 1: Basic Concepts of Meteorology Unit 2: The Atmosphere in Motion
Meteorology Curriculum Maps Unit 1: Basic Concepts of Meteorology Unit 2: The Atmosphere in Motion NOTE: Meteorology is a one semester course designed for students interested in understanding the complex
Our Atmosphere as seen from the bottom of it near Grand Pre, NS. Info modified from various sources by TWebb HHS
Our Atmosphere as seen from the bottom of it near Grand Pre, NS Info modified from various sources by TWebb HHS Properties of the Atmosphere A) Mobility B) Expansion (MOST important!) C) Compression These
IV. Atmospheric Science Section
EAPS 100 Planet Earth Lecture Topics Brief Outlines IV. Atmospheric Science Section 1. Introduction, Composition and Structure of the Atmosphere Learning objectives: Understand the basic characteristics
Variability in Global Top-of-Atmosphere Shortwave Radiation Between 2000 And 2005
Variability in Global Top-of-Atmosphere Shortwave Radiation Between 2000 And 2005 Norman G. Loeb NASA Langley Research Center Hampton, VA Collaborators: B.A. Wielicki, F.G. Rose, D.R. Doelling February
ESM 186 Environmental Remote Sensing and ESM 186 Lab Syllabus Winter 2012
ESM 186 Environmental Remote Sensing and ESM 186 Lab Syllabus Winter 2012 Instructor: Susan Ustin (slustin@ucdavis.edu) Phone: 752-0621 Office: 233 Veihmeyer Hall and 115A, the Barn Office Hours: Tuesday
GARP 0102 Earth Radiation Balance (Part 1)
Class 8: Earth s Radiation Balance I (Chapter 4) 1. Earth s Radiation Balance: Sun, Atmosphere, and Earth s Surface as a System 2. Electromagnetic Radiation: Shortwave vs. longwave radiation (Page 69-71)
Climate Modeling Research & Applications in Wales. John Houghton. C 3 W conference, Aberystwyth
Climate Modeling Research & Applications in Wales John Houghton C 3 W conference, Aberystwyth 26 April 2011 Computer Modeling of the Atmosphere & Climate System has revolutionized Weather Forecasting and
Weather. Describing Weather
Weather Describing Weather What is weather? Weather is the atmospheric conditions, along with short-term changes, of a certain place at a certain time. Have you ever been caught in a rainstorm on what
Weather and climate. reflect. what do you think? look out!
reflect You re going on vacation in a week and you have to start thinking about what clothes you re going to pack for your trip. You ve read the weather reports for your vacation spot, but you know that
https://ipass.lsrhs.net/school/ipass/assignmentsheet.html?m=8... Earth Sci (1) (Lab) Sanders-Fleming BLOCK: 4 12/03/ /21/2016
Earth Sci (1) (Lab) Sanders-Fleming BLOCK: 4 12/03/2015 01/21/2016 ES1 B4 Weather 14 Jan 2016 Date What it is Due Date Thr 12/03/2015 In class today: Foucault Pendulum Lab Concept: Proving earth's rotation
Chapter 6 Clouds. Cloud Development
Chapter 6 Clouds Chapter overview Processes causing saturation o Cooling, moisturizing, mixing Cloud identification and classification Cloud Observations Fog Why do we care about clouds in the atmosphere?
Global warming and Extremes of Weather. Prof. Richard Allan, Department of Meteorology University of Reading
Global warming and Extremes of Weather Prof. Richard Allan, Department of Meteorology University of Reading Extreme weather climate change Recent extreme weather focusses debate on climate change Can we
Earth and Space Science. Teacher s Guide
Earth and Space Science Teacher s Guide WALCH PUBLISHING Table of Contents To the Teacher............................................................. vi Classroom Management....................................................
Assessment Schedule 2017 Earth and Space Science: Demonstrate understanding of processes in the atmosphere system (91414)
NCEA Level 3 Earth and Space Science (91414) 2017 page 1 of 6 Assessment Schedule 2017 Earth and Space Science: Demonstrate understanding of processes in the atmosphere system (91414) Evidence Statement
5) 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
Next quiz: this Friday, questions. Plus more on Wednesday.
Next quiz: this Friday, 10-20 questions from Plus more on Wednesday. Chapter 19: 1, 6, 7, 8, 10, 11, 15, 16, 29, 20, 21, 27, 42, 46 Chapter 20: 1, 2, 7, 13, 14, 16, 19, 20, 34, 37, 40, 41, 42, 43, 47,
Climate Roles of Land Surface
Lecture 5: Land Surface and Cryosphere (Outline) Climate Roles Surface Energy Balance Surface Water Balance Sea Ice Land Ice (from Our Changing Planet) Surface Albedo Climate Roles of Land Surface greenhouse
Precipitation Processes. Precipitation Processes 2/24/11. Two Mechanisms that produce raindrops:
Precipitation is any form of water that falls from a cloud and reaches the ground. How do cloud drops grow? Chapter 7 When air is saturated with respect to a flat surface it is unsaturated with respect
Energy, Temperature, & Heat. Energy, Temperature, & Heat. Temperature Scales 1/17/11
Energy, Temperature, & Heat Energy is the ability to do work (push, pull, lift) on some form of matter. Chapter 2 Potential energy is the potential for work (mass x gravity x height) Kinetic energy is
Mid High Latitude Cirrus Precipitation Processes. Jon Sauer, Dan Crocker, Yanice Benitez
Mid High Latitude Cirrus Precipitation Processes Jon Sauer, Dan Crocker, Yanice Benitez Department of Chemistry and Biochemistry, University of California, San Diego, CA 92093, USA *To whom correspondence
Monday 7 October 2013, Class #15
Monday 7 October 2013, Class #15 Concepts for Today (Basics for Thermodynamics) Weather versus climate Lapse Rate (Adiabatic Lapse Rate) Ideal Gas Law Adiabatic Processes Potential Temperature Hydrostatic
Introduction. Effect of aerosols on precipitation: - challenging problem - no agreement between the results (quantitative and qualitative)
Introduction Atmospheric aerosols affect the cloud mycrophysical structure & formation (observations, numerical studies) An increase of the aerosol particles: - increases CCN concentrations - decreases
Torben Königk Rossby Centre/ SMHI
Fundamentals of Climate Modelling Torben Königk Rossby Centre/ SMHI Outline Introduction Why do we need models? Basic processes Radiation Atmospheric/Oceanic circulation Model basics Resolution Parameterizations
Atmospheric 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
Explain the parts of the water cycle that are directly connected to weather.
Name: Pd: Date: Page # Describing Weather -- Lesson 1 Study Guide Rating Before Learning Goals Rating After 1 2 3 4 Describe weather. 1 2 3 4 1 2 3 4 List and define the variables used to describe weather.
Meteorology. I. The Atmosphere - the thin envelope of gas that surrounds the earth.
Meteorology I. The Atmosphere - the thin envelope of gas that surrounds the earth. A. Atmospheric Structure - the atmosphere is divided into five distinct layers that are based on their unique characteristics.
Radiation Conduction Convection
Lecture Ch. 3a Types of transfers Radiative transfer and quantum mechanics Kirchoff s law (for gases) Blackbody radiation (simplification for planet/star) Planck s radiation law (fundamental behavior)