Session 1, Unit 1 Course Overview. Introduction Course – ENV 7335 Air Quality Modeling Instructor – Yousheng Zeng, Ph.D., P.E. Prerequisite – ENV 7331.

Slides:



Advertisements
Similar presentations
AIR POLLUTION AND METEOROLOGY
Advertisements

Ozone Wind 3rd Quarter- 6th Grade Science Jeopardy- Test #1
Section 2: The Planetary Boundary Layer
Circulation in the atmosphere
Chapter 17 Study Guide Answers
EOSC 112: THE FLUID EARTH ATMOSPHERIC STRUCTURE AND DYNAMICS Atm12 Read: Kump et al. Chap.3, p ; Chap.4, p Objectives: 1.To describe how.
The Atmosphere: Climate and Weather John Todd 6 lecture mini-series.
Module 9 Atmospheric Stability MCEN 4131/ Preliminaries I will be gone next week, Mon-Thur Tonight is design night, 7:30ish, meet in classroom.
M ETEOROLOGY : T HE S CIENCE OF W EATHER Key variables for determining Earth’s weather Rotation of the Earth Revolution of the Earth Radiation received.
ENAC-SSIE Laboratoire de Pollution de l'Air The Atmospheric Layers.
Introduction to the ISC Model Marti Blad NAU College of Engineering.
Riddles What happens when you throw a yellow rock into a purple stream? What starts with a T, ends with a T, and has T in it?
The Atmosphere Chapter 22.
 What is pressure?  Pressure is accumulative force of gas particles   High Energy gas (HOT) has lots of movement, therefore.
Ch 17 - The Atmosphere Vocab Charts (Example) WordDefinitionPicture Weather the state of the atmosphere at a given time and place.
Wind Science 101: I. Overview of Wind Patterns Eugene S. Takle Professor Department of Agronomy Department of Geological and Atmospheric Science Director,
1 The Wind. 2 3 The origin of wind The earth is unevenly heated by the sun resulting in the poles receiving less energy from the sun than the equator.
Chapter 7 cover. Figure 7.1 Figure 7.2 Figure mb/km 115G150 knots.
Movement of Air in Earth’s Atmosphere. What is wind? The movement of air from an area of higher pressure to an area of lower pressure. The movement of.
Planetary Atmospheres, the Environment and Life (ExCos2Y) Revision Chris Parkes Rm 455 Kelvin Building.
Chapter 9: Weather Factors
Preview Section 1 Characteristics of the Atmosphere
Class #14 Wednesday, September 30 Class #14: Wednesday, September 30 Chapters 6 and 7 Thermal Circulation, Scales of Motion, Global Winds 1.
Unit 3 Earth’s Atmosphere Big Idea: Earth’s atmosphere is a mixture of gases that interacts with solar energy.
Essential Question: Why does sinking air cause areas of high pressure?
Introduction to Modeling – Part II
The Atmosphere By : Jennifer Drinkard. Atmospheric gases Our atmosphere is made up of mainly Nitrogen, Oxygen, and Carbon Dioxide, but it also contains.
Atmosphere Test Review
Unit 4 Vocabulary The Atmosphere. 1. Storm surge – abnormal rise of the sea along a shore as a result of strong winds 2. local winds – winds causes by.
Notes Points Chapter 22.3 Notes
5.01 Heating and Cooling of the Atmosphere
17.1 The Atmosphere. Unit 7: Atmosphere, Weather, and Climate  Weather – the state of the atmosphere at a given time vs. vs.  Climate – weather over.
1. The atmosphere 2 © Zanichelli editore 2015 Characteristics of the atmosphere 3 © Zanichelli editore 2015.
Atmosphere. What makes up our atmosphere?  Nitrogen  Oxygen  Argon.
Chapter 17 continued  The horizontal movement of air from high pressure to low pressure  Moderates surface temperatures  Distributes moisture 
Meteorology for modeling AP Marti Blad PhD PE. Meteorology Study of Earth’s atmosphere Weather science Climatology and study of weather patterns Study.
Chapter 22 Test Review The Atmosphere.
Intro to Modeling – Terms & concepts Marti Blad, Ph.D., P.E. ITEP
Presentation by: Alex Hezik – Atmosphere, Weather, and Climate Layers of the Atmosphere troposphere: moderates flow of energy to Earth; where weather.
ATMOSPHERE OBJECTIVE 1 1.What are the structural components of the
Characteristics of the Atmosphere Atmospheric Heating Global Winds and Local Winds Air Pollution Terms to Know
Isobars and wind barbs sea level pressure. factors affecting wind wind is the result of horizontal differences in pressure air flows from higher to lower.
Ch.22 Atmosphere. Composition 78% nitrogen 21% oxygen 0.9% argon 0.1&other gasses.
Unit 4 Study Guide The Atmosphere. PART 1 a.Weather - constantly changing, refers to the state of the atmosphere at any given place and time. b. Climate.
Atmosphere-ocean interactions Exchange of energy between oceans & atmosphere affects character of each In oceans –Atmospheric processes alter salinity.
Importance of the Atmosphere Earth's atmosphere is a mixture of gases that surrounds Maintains balance of heat Protects life forms from sun’s rays 1 1.
Key Concepts 1 Earth’s atmosphere formed as Earth cooled and chemical and biological processes took place. Earth’s atmosphere consists of nitrogen, oxygen,
Atmosphere Air Pressure Local Winds Global Winds Instruments
Chapter 17 Study Guide Answers
5.01 Heating and Cooling of the Atmosphere
Unit 2 BASICS OF FLIGHT MECHANICS
The Atmosphere and Climate
Temperature Changes With Earth’s Atmosphere
Temperature Changes With Earth’s Atmosphere
Atmosphere and Weather
5.01 Heating and Cooling of the Atmosphere
EARTH’S ATMOSPHERE (AIR).
1. The condition of the atmosphere at a particular time and place
Air Weather Patterns Atmosphere Energy Transfer
Unit 7: Atmosphere Notes
Air Weather Patterns Atmosphere Energy Transfer
A mixture of gases surrounding the Earth.
5.01 Heating and Cooling of the Atmosphere
Introduction to Modeling – Part II
The Atmosphere.
Do Now What are the layers of the atmosphere?
The Atmosphere Chapter 17.
The Atmosphere Chapter 17.
Chapter 5 Ecosystems and the Physical Environment
Isobars and wind barbs sea level pressure.
Presentation transcript:

Session 1, Unit 1 Course Overview

Introduction Course – ENV 7335 Air Quality Modeling Instructor – Yousheng Zeng, Ph.D., P.E. Prerequisite – ENV 7331 or equivalent

Course Objectives Understand air pollution meteorology and theory of atmospheric dispersion modeling Be able to perform an air quality modeling analysis using the most common regulatory model – ISC3 Understand the regulatory requirements related to air quality modeling analysis Become knowledgeable of other air quality models

Course Materials Textbook – “Atmospheric Dispersion Modeling Compliance Guide” with CD-ROM by Schnelle & Dey McGraw Hill, 1999 Other materials available on the Internet ISC3 Program and Manual BPIP Program and Manual Other relevant information

Course Outline Session 1 Introduction/Course overview Basic meteorological principles Session 2 Air pollution climatology Turbulence and the mixing process Session 3 The dispersion model Dispersion coefficients

Course Outline Session 4 Plume rise The effect of averaging time, multiple sources, and receptors Session 5 Modeling in the presence of dispersion ceilings SCREEN3, ISCPC, and midterm review Session 6 Chimney, building, and terrain effects Midterm exam

Course Outline Session 7 Chimney design The ISC3 Model Session 8 ISC3 practical issues and the BPIP program Regulatory procedures and PSD modeling Session 9 Other important models – ISC-PRIME, AERMOD, CALPUFF, UAM, CAMx Final review

Course Outline Session 10 Modeling accidental releases Final exam Modeling exercise due Modeling project report due

Course Work Study problems at the end of each chapter in the textbook Modeling exercise use the ISCPC model in the textbook CD-ROM 20 practice problems in Appendix E Earn credit by turning in answers for 10 of them (even or odd numbers) to demonstrate completion of the exercise Midterm exam Final exam

Course Work Modeling Project EPA ISCST3 model and BPIP program Multiple sources Buildings and terrain Receptor grid 1 year met data Modeling report

Grading Midterm exam20 points Final exam30 points Modeling exercise10 points Modeling Project40 points Total100 points

Communication Course website: All students should send me a short at so that I can distribute announcement/materials if

Session 1, Unit 2 Basic meteorological principles

Atmosphere Composition Near surface (tropospheric air)  Nitrogen:78.08%  Oxygen:20.95%  Argon:0.9%  Contributors to atmospheric absorptive properties H 2 O:Variable CO 2 :332 ppm CH 4 :1.65 ppm N 2 O:0.33 ppm O 3 : ppm

Atmosphere Vertical temperature profile Troposphere Stratosphere Mesosphere Thermosphere

Energy Balance Radiation Occurs when an electron drops to a lower level of energy Blackbody radiation  Emissivity of a blackbody at 6000 K (the sun)  Emissivity of a blackbody at 300 K (the earth) Energy balance Day vs. night Local energy balance/out of balance Global energy balance Greenhouse effect

Scales of Atmospheric Motion Microscale Mesoscale Synoptic (cyclonic scale) Macroscale

General Circulation General energy balance controls large scale air movement Air circulation if the earth did not turn General circulation Rotation of the earth – Coriolis force General circulation pattern

Geostrophic Layer m height Two forces Horizontal pressure gradient Coriolis force Undisturbed constant air flow – Geostrophic wind

Planetary Boundary Layer Surface to 500 m high Three forces Horizontal pressure gradient Coriolis force Frictional force due to earth’s surface roughness Different wind from geostrophic wind Speed – retarded by friction Direction – altered due to force balance Urban/mountain vs. smooth surface Surface layer – from surface to 50 m high

Impact of Fixed Geographic Features Sea breeze Valley wind Drainage wind Flow patterns due to topographical features