Winds. Winds on a weather map are represented by wind barbs; e.g., Notes:

Size: px
Start display at page:

Download "Winds. Winds on a weather map are represented by wind barbs; e.g., Notes:"

Transcription

1 Winds Winds on a weather map are represented by wind barbs; e.g., flag half flag pennant wind direction The wind is blowing from the side with the flags and pennants (think an arrow with feathers) Speeds are given by: pennant: 50 knots flag: 10 knots half flag: 5 knots = 75 knots

2 Winds Winds on a weather map are represented by wind barbs; e.g., flag half flag pennant wind direction The wind is blowing from the side with the flags and pennants (think an arrow with feathers) Speeds are given by: 1 knot = 1 nautical mile hr = 1.15 mile hr = 1.85 km hr = 0.51 m s

3 The Station Model The data reported at a weather station looks like (in simplified form): wind (15 knots) temperature precipitation pressure dew point 63 pressure trend cloud cover

4 The Station Model The data reported at a weather station looks like (in simplified form): wind (15 knots) Winds use the same scale as before; i.e., pennant: 50 knots flag: 10 knots half flag: 5 knots

5 The Station Model The data reported at a weather station looks like (in simplified form): temperature dew point 63 In the US, the temperature and dew point temperature are given in o F. Everywhere else it's o C.

6 The Station Model The data reported at a weather station looks like (in simplified form): precipitation Precipitation types are represented by symbols: light rain moderate rain heavy rain ** ** light snow * moderate snow freezing rain and others...see Appendix C (or wikipedia)

7 The Station Model The data reported at a weather station looks like (in simplified form): cloud cover Shading of the station dot shows the extent of cloud cover: clear half coverage full coverage (overcast) etc...see Appendix C for details

8 The Station Model The data reported at a weather station looks like (in simplified form): pressure trend The trend line shows the change in pressure over the past 3 hours: steady (no change) falling rising falling, then rising etc...

9 The Station Model The data reported at a weather station looks like (in simplified form): pressure The pressure is shown using a three-digit code; i.e.,: mb mb mb

10 The Station Model The data reported at a weather station looks like (in simplified form): pressure The rule of thumb is If the three-digit code is less than 500: Add a 10 in front and a decimal before the last digit hpa If the code is greater than 500: Add a 9 in front and a decimal before the last digit hpa

11 Upper Levels (e.g., 500 mb) Data at upper levels is similar, but with a couple of changes: temperature height dew point depression 23

12 Upper Levels (e.g., 500 mb) Data at upper levels is similar, but with a couple of changes: dew point depression 23 Instead of the dew point temperature, we get the dew-point depression, defined as: depression = temperature dew point temperature

13 Upper Levels (e.g., 500 mb) Data at upper levels is similar, but with a couple of changes: temperature dew point depression Somewhat inexplicably, the temperature and dew point depression are given in o C. (Remember the surface temperature was o F.)

14 Upper Levels (e.g., 500 mb) Data at upper levels is similar, but with a couple of changes: height Instead of pressure, we get the height of the surface, in units of decameters (or 10 m) m

15 Frontal Symbols front warm front stationary front for the, warm and occluded fronts, the symbols show the direction of motion occluded front

16 Frontal Symbols warm front warm front stationary front for the, warm and occluded fronts, the symbols show the direction of motion occluded front

17 Frontal Symbols warm warm front warm front stationary front for the, warm and occluded fronts, the symbols show the direction of motion occluded front

18 Frontal Symbols warm warm warm front warm front stationary front for the, warm and occluded fronts, the symbols show the direction of motion occluded front

19 Frontal Symbols warm warm warm er front warm front stationary front occluded front for the, warm and occluded fronts, the symbols show the direction of motion

Weather Map Symbols, Abbreviations, and Features

Weather Map Symbols, Abbreviations, and Features Weather Map Symbols, Abbreviations, and Features Table of Contents 1. Symbols... 2 Pressure Systems/Fronts... 2 Precipitation... 3 Wind Speed... 4 Center pressures (on Surface Maps)... 4 2. Abbreviations...

More information

Basics of weather interpretation

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

More information

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

Chapter 3: Weather Map. Weather Maps. The Station Model. Weather Map on 7/7/2005 4/29/2011 Chapter 3: Weather Map Weather Maps Many variables are needed to described weather conditions. Local weathers are affected by weather pattern. We need to see all the numbers describing weathers at many

More information

Name: OBJECTIVES Correctly define: WEATHER BASICS: STATION MODELS: MOISTURE: PRESSURE AND WIND: Weather

Name: OBJECTIVES Correctly define: WEATHER BASICS: STATION MODELS: MOISTURE: PRESSURE AND WIND: Weather Name: OBJECTIVES Correctly define: air mass, air pressure, anemometer, barometer, cyclone, dew point, front, isobar, isotherm, meteorology, precipitation, psychrometer, relative humidity, saturated, transpiration

More information

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

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

More information

SIXTH GRADE WEATHER 1 WEEK LESSON PLANS AND ACTIVITIES

SIXTH 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 information

7613-1 - Page 1. Weather Unit Exam Pre-Test Questions

7613-1 - 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 information

Activity 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 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 information

Weather Help - NEXRAD Radar Maps. Base Reflectivity

Weather 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 information

Air Masses and Fronts

Air Masses and Fronts Air Masses and Fronts Air Masses The weather of the United States east of the Rocky Mountains is dominated by large masses of air that travel south from the wide expanses of land in Canada, and north from

More information

How to analyze synoptic-scale weather patterns Table of Contents

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

More information

WEATHER AND CLIMATE practice test

WEATHER 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 information

Activity 4 Clouds Over Your Head Level 1

Activity 4 Clouds Over Your Head Level 1 Activity 4 Clouds Over Your Head Level 1 1 Objectives: Students will become familiar with the four main types of clouds: stratus, cirrus, cumulus, and cumulonimbus and their characteristics. Students will

More information

CGC1D1: Interactions in the Physical Environment Factors that Affect Climate

CGC1D1: Interactions in the Physical Environment Factors that Affect Climate Name: Date: Day/Period: CGC1D1: Interactions in the Physical Environment Factors that Affect Climate Chapter 12 in the Making Connections textbook deals with Climate Connections. Use pages 127-144 to fill

More information

UNIT 6a TEST REVIEW. 1. A weather instrument is shown below.

UNIT 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 information

Clouds/WX Codes. B.1 Introduction

Clouds/WX Codes. B.1 Introduction Clouds/WX Codes B.1 Introduction This appendix provides the necessary tables and specific instructions to enter Clouds/Wx at the Surface Data screen. This guidance assumes no previous knowledge of synoptic

More information

WeatherBug Vocabulary Bingo

WeatherBug Vocabulary Bingo Type of Activity: Game: Interactive activity that is competitive, and allows students to learn at the same time. Activity Overview: WeatherBug Bingo is a fun and engaging game for you to play with students!

More information

Analyze Weather in Cold Regions and Mountainous Terrain

Analyze Weather in Cold Regions and Mountainous Terrain Analyze Weather in Cold Regions and Mountainous Terrain Terminal Learning Objective Action: Analyze weather of cold regions and mountainous terrain Condition: Given a training mission that involves a specified

More information

Stability 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. 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 information

WEATHER THEORY Temperature, Pressure And Moisture

WEATHER THEORY Temperature, Pressure And Moisture WEATHER THEORY Temperature, Pressure And Moisture Air Masses And Fronts Weather Theory- Page 77 Every physical process of weather is a result of a heat exchange. The standard sea level temperature is 59

More information

The Anatomy of a Forecast

The Anatomy of a Forecast The Anatomy of a Forecast The Met Service issues forecasts for sky condition, precipitation probability, wind, seas state and temperature on a routine basis. Because the weather is always changing, the

More information

Cloud Development and Forms. LIFTING MECHANISMS 1. Orographic 2. Frontal 3. Convergence 4. Convection. Orographic Cloud. The Orographic Cloud

Cloud 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 information

If wispy, no significant icing or turbulence. If dense or in bands turbulence is likely. Nil icing risk. Cirrocumulus (CC)

If wispy, no significant icing or turbulence. If dense or in bands turbulence is likely. Nil icing risk. Cirrocumulus (CC) Cirrus (CI) Detached clouds in the form of delicate white filaments or white patches or narrow bands. These clouds have a fibrous or hair like appearance, or a silky sheen or both. with frontal lifting

More information

ASOS GUIDE FOR PILOTS

ASOS GUIDE FOR PILOTS ASOS GUIDE FOR PILOTS INTRODUCTION... 1 NOTICES TO AIRMEN... 1 SYSTEM DESCRIPTION... 2 WEATHER OBSERVATION ELEMENTS... 3 DATA NOT AUTOMATICALLY PROVIDED BY ASOS... 7 MISSING DATA AND NON EVENT DATA...

More information

How do I measure the amount of water vapor in the air?

How do I measure the amount of water vapor in the air? How do I measure the amount of water vapor in the air? Materials 2 Centigrade Thermometers Gauze Fan Rubber Band Tape Overview Water vapor is a very important gas in the atmosphere and can influence many

More information

Convective Clouds. Convective clouds 1

Convective Clouds. Convective clouds 1 Convective clouds 1 Convective Clouds Introduction Convective clouds are formed in vertical motions that result from the instability of the atmosphere. This instability can be caused by: a. heating at

More information

How do Scientists Forecast Thunderstorms?

How do Scientists Forecast Thunderstorms? How do Scientists Forecast Thunderstorms? Objective In the summer, over the Great Plains, weather predictions often call for afternoon thunderstorms. While most of us use weather forecasts to help pick

More information

National Meteorological Library and Archive

National Meteorological Library and Archive National Meteorological Library and Archive Fact sheet No. 11 Interpreting weather charts Weather systems On a weather chart, lines joining places with equal sea-level pressures are called isobars. Charts

More information

Severe 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 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 information

Mixing Heights & Smoke Dispersion. Casey Sullivan Meteorologist/Forecaster National Weather Service Chicago

Mixing Heights & Smoke Dispersion. Casey Sullivan Meteorologist/Forecaster National Weather Service Chicago Mixing Heights & Smoke Dispersion Casey Sullivan Meteorologist/Forecaster National Weather Service Chicago Brief Introduction Fire Weather Program Manager Liaison between the NWS Chicago office and local

More information

Gold Seal Online Ground School www.onlinegroundschool.com

Gold Seal Online Ground School www.onlinegroundschool.com Weather Charts and Reports Relating to weather reports: Ceiling Lowest layer of broken or overcast clouds IFR Ceilings less than 1,000 feet or visibilities less than three statute miles MVFR Ceilings between

More information

MIAMI-SOUTH FLORIDA National Weather Service Forecast Office http://www.weather.gov/miami

MIAMI-SOUTH FLORIDA National Weather Service Forecast Office http://www.weather.gov/miami MIAMI-SOUTH FLORIDA National Weather Service Forecast Office http://www.weather.gov/miami November 2014 Weather Summary Cooler and Drier than Normal December 1, 2014: Cooler than normal temperatures was

More information

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

2. The map below shows high-pressure and low-pressure weather systems in the United States. 1. Which weather instrument has most improved the accuracy of weather forecasts over the past 40 years? 1) thermometer 3) weather satellite 2) sling psychrometer 4) weather balloon 6. Wind velocity is

More information

Make a Cloud Finder. How to Fold the Cloud Finder: Play the Weather Word Game:

Make a Cloud Finder. How to Fold the Cloud Finder: Play the Weather Word Game: Make a Cloud Finder Make a Cloud Finder. The pattern is included here. Learn the names of the beautiful clouds that may appear in the sky where you live. Color your Cloud Finder, and cut it out on the

More information

FOR 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! 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 information

[7] SD3.1 The student demonstrates an understanding of cycles influenced by energy from the

[7] SD3.1 The student demonstrates an understanding of cycles influenced by energy from the Cloud Types Levels Overview: During this project, students learn about different types of clouds and determine which type of cloud is most commonly overhead in their area over a period of four weeks. Objectives:

More information

Chapter 7 Stability and Cloud Development. Atmospheric Stability

Chapter 7 Stability and Cloud Development. Atmospheric Stability Chapter 7 Stability and Cloud Development Atmospheric Stability 1 Cloud Development - stable environment Stable air (parcel) - vertical motion is inhibited if clouds form, they will be shallow, layered

More information

Partnerships Implementing Engineering Education Worcester Polytechnic Institute Worcester Public Schools

Partnerships 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 information

Cloud seeding. Frequently Asked Questions. What are clouds and how are they formed? How do we know cloud seeding works in Tasmania?

Cloud seeding. Frequently Asked Questions. What are clouds and how are they formed? How do we know cloud seeding works in Tasmania? What are clouds and how are they formed? Clouds are composed of water droplets and sometimes ice crystals. Clouds form when air that is rich in moisture near the Earth s surface rises higher into the atmosphere,

More information

Anticyclones, depressions, hot & drought, cold & snow

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

More information

Clouds, Fog, & Precipitation

Clouds, Fog, & Precipitation firecatching.blogspot.com Kids.brittanica.com Clouds and fog are physically the same just location is different Fog is considered a stratus cloud at or near the surface What does one see when looking at

More information

RE: James vs. ABC Company Greentown, NJ D/A: February 20, 2011

RE: James vs. ABC Company Greentown, NJ D/A: February 20, 2011 PO Box 7100 Hackettstown, NJ 07840 Phone: 1 800 427 3456 Fax: 908-850-8664 http://www.weatherworksinc.com June 16, 2012 Attn: John Doe Law Offices of John Doe 123 Fourth Street Smithtown, NJ 04506 RE:

More information

Chapter 10 Weather. Weather in Antarctica is characterized by extremes: extreme temperatures, extreme

Chapter 10 Weather. Weather in Antarctica is characterized by extremes: extreme temperatures, extreme Field Manual for the U.S. Antarctic Program Chapter 10 Weather Figure 10-1: Storm approaching. (photo by Tim Cully) Weather in Antarctica is characterized by extremes: extreme temperatures, extreme winds,

More information

How To Understand The Weather Patterns In Tallahassee, Florida

How To Understand The Weather Patterns In Tallahassee, Florida PATTERN RECOGNITION OF SIGNIFICANT SNOWFALL EVENTS IN TALLAHASSEE, FLORIDA Jeffery D. Fournier and Andrew I. Watson NOAA/National Weather Service Weather Forecast Office Tallahassee, Florida Abstract Skew-T

More information

Name: Date: LAB: Dew Point and Cloud Formation Adapted from Exploration in Earth Science, The Physical Setting, United Publishing Company, Inc.

Name: Date: LAB: Dew Point and Cloud Formation Adapted from Exploration in Earth Science, The Physical Setting, United Publishing Company, Inc. Name: _ Date: LAB: Dew Point and Cloud Formation Adapted from Exploration in Earth Science, The Physical Setting, United Publishing Company, Inc. Introduction: Cumulus clouds are our puffy fair weather

More information

How To Find Out If The Winds From The Oak Ridge Site Are Calm

How To Find Out If The Winds From The Oak Ridge Site Are Calm EVALUATING THE WIND DATA FROM THE AUTOMATED SURFACE OBSERVING SYSTEM IN OAK RIDGE, TENNESSEE - IS KOQT THE CALMEST SITE IN THE US? Thomas E. Bellinger, CCM Y-12 National Security Complex Oak Ridge, Tennessee

More information

5. Why does the weather near cities tend to be cloudier and wetter than in rural areas?

5. Why does the weather near cities tend to be cloudier and wetter than in rural areas? Name: Date: 1. Today weather forecasting is better because of the use of A. barometers. B. telescopes. C. satellites. D. anemometers. 2. The letter H is the weather symbol for A. hail storms. B. humidity.

More information

Humidity, Condensation, Clouds, and Fog. Water in the Atmosphere

Humidity, Condensation, Clouds, and Fog. Water in the Atmosphere Humidity, Condensation, Clouds, and Fog or Water in the Atmosphere The Hydrologic Cycle Where the Water Exists on Earth Evaporation From the Oceans and Land The Source of Water Vapor for the Atmosphere

More information

Clouds and What They Mean

Clouds and What They Mean Vocabulary and Writing Worksheet 1. Choose the best vocabulary word for each sentence and write it in the blank. dew point evaporation fog gas precipitation relative humidity a. Relative humidity refers

More information

Safe Operating Procedure

Safe Operating Procedure Safe Operating Procedure (Revised 11/11) OPACITY OF EMISSIONS FROM COMBUSTION SOURCES (For assistance, please contact EHS at (402) 472-4925, or visit our web site at http://ehs.unl.edu/) The University

More information

Chapter 6 - Cloud Development and Forms. Interesting Cloud

Chapter 6 - Cloud Development and Forms. Interesting Cloud Chapter 6 - Cloud Development and Forms Understanding Weather and Climate Aguado and Burt Interesting Cloud 1 Mechanisms that Lift Air Orographic lifting Frontal Lifting Convergence Localized convective

More information

J4.1 CENTRAL NORTH CAROLINA TORNADOES FROM THE 16 APRIL 2011 OUTBREAK. Matthew Parker* North Carolina State University, Raleigh, North Carolina

J4.1 CENTRAL NORTH CAROLINA TORNADOES FROM THE 16 APRIL 2011 OUTBREAK. Matthew Parker* North Carolina State University, Raleigh, North Carolina J4.1 CENTRAL NORTH CAROLINA TORNADOES FROM THE 16 APRIL 2011 OUTBREAK Matthew Parker* North Carolina State University, Raleigh, North Carolina Jonathan Blaes NOAA/National Weather Service, Raleigh, North

More information

This chapter discusses: 1. Definitions and causes of stable and unstable atmospheric air. 2. Processes that cause instability and cloud development

This 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 information

Introduction to the forecasting world Jukka Julkunen FMI, Aviation and military WS

Introduction to the forecasting world Jukka Julkunen FMI, Aviation and military WS Boundary layer challenges for aviation forecaster Introduction to the forecasting world Jukka Julkunen FMI, Aviation and military WS 3.12.2012 Forecast for general public We can live with it - BUT Not

More information

Reference Guide. Vantage PRO2 Quick

Reference Guide. Vantage PRO2 Quick 3465 Diablo Avenue, Hayward, CA 94545-2778 U.S.A. 510-732-9229 Fax: 510-732-9188 E-mail: info@davisnet.com www.davisnet.com Vantage PRO2 Quick Reference Guide Part Number: 07395.235 Rev C (1/6/2012) 2012

More information

P3.8 INTEGRATING A DOPPLER SODAR WITH NUCLEAR POWER PLANT METEOROLOGICAL DATA. Thomas E. Bellinger

P3.8 INTEGRATING A DOPPLER SODAR WITH NUCLEAR POWER PLANT METEOROLOGICAL DATA. Thomas E. Bellinger P3.8 INTEGRATING A DOPPLER SODAR WITH NUCLEAR POWER PLANT METEOROLOGICAL DATA Thomas E. Bellinger Illinois Emergency Management Agency Springfield, Illinois 1. INTRODUCTION A Doppler sodar owned by the

More information

Guy Carpenter Asia-Pacific Climate Impact Centre, School of energy and Environment, City University of Hong Kong

Guy Carpenter Asia-Pacific Climate Impact Centre, School of energy and Environment, City University of Hong Kong Diurnal and Semi-diurnal Variations of Rainfall in Southeast China Judy Huang and Johnny Chan Guy Carpenter Asia-Pacific Climate Impact Centre School of Energy and Environment City University of Hong Kong

More information

IMPACT OF SAINT LOUIS UNIVERSITY-AMERENUE QUANTUM WEATHER PROJECT MESONET DATA ON WRF-ARW FORECASTS

IMPACT OF SAINT LOUIS UNIVERSITY-AMERENUE QUANTUM WEATHER PROJECT MESONET DATA ON WRF-ARW FORECASTS IMPACT OF SAINT LOUIS UNIVERSITY-AMERENUE QUANTUM WEATHER PROJECT MESONET DATA ON WRF-ARW FORECASTS M. J. Mueller, R. W. Pasken, W. Dannevik, T. P. Eichler Saint Louis University Department of Earth and

More information

Formation & Classification

Formation & 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 information

Clouds. 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 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 information

Tabelle MOS Vorhersage-Parameter

Tabelle MOS Vorhersage-Parameter Tabelle MOS Vorhersage-Parameter Element number Name Description Unit 1005 T Air temperature C*10 1000 T5cm Temperature at 5 cm above ground C*10 1006 Td Dew point temperature C*10 1001 DD Wind direction

More information

UNIT IV--TEMPERATURE-MOISTURE RELATIONSHIP

UNIT IV--TEMPERATURE-MOISTURE RELATIONSHIP UNIT IV--TEMPERATURE-MOISTURE RELATIONSHIP Weather is the most variable and often the most critical determinant of fire behavior. This is the first of several units that will deal with weather and its

More information

Climates are described by the same conditions used to describe

Climates are described by the same conditions used to describe 58 The Causes of Climate R E A D I N G Climates are described by the same conditions used to describe weather, such as temperature, precipitation, and wind. You now know that oceans have an important effect

More information

Glaciogenic Cloud Seeding to Increase Orographic Precipitation Bruce A. Boe bboe@weathermod.com Director of Meteorology

Glaciogenic Cloud Seeding to Increase Orographic Precipitation Bruce A. Boe bboe@weathermod.com Director of Meteorology Glaciogenic Cloud Seeding to Increase Orographic Precipitation Bruce A. Boe bboe@weathermod.com Director of Meteorology Weather Modification, Inc. Fargo, North Dakota, USA www.weathermodification.com Content

More information

Hurricanes. Characteristics of a Hurricane

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

More information

Comparison of visual observations and automated ceilometer cloud reports at Blindern, Oslo. Anette Lauen Borg Remote sensing MET-Norway

Comparison of visual observations and automated ceilometer cloud reports at Blindern, Oslo. Anette Lauen Borg Remote sensing MET-Norway Comparison of visual observations and automated ceilometer cloud reports at Blindern, Oslo Anette Lauen Borg Remote sensing MET-Norway A test of our ceilometer data To fully exploit our new ceilometer

More information

Technical Support Document For The May 2, 2008 Exceptional Event

Technical Support Document For The May 2, 2008 Exceptional Event Technical Support Document For The May 2, 2008 Exceptional Event Prepared by the Technical Services Program Air Pollution Control Division June 9, 2009 2 Table of Contents: 1.0 Introduction... 4 2.0 Ambient

More information

Temperature affects water in the air.

Temperature 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 information

Aircraft incident to SE-KPE during approach to the Malmö/Sturup airport, M county, Sweden, on 03 December 1999

Aircraft incident to SE-KPE during approach to the Malmö/Sturup airport, M county, Sweden, on 03 December 1999 Aircraft incident to SE-KPE during approach to the Malmö/Sturup airport, M county, Sweden, on 03 December 1999 Micro-summary: On approach, this Saab 340 was hit by lightning, causing dual generator electrical

More information

Temperature and Humidity

Temperature and Humidity Temperature and Humidity Overview Water vapor is a very important gas in the atmosphere and can influence many things like condensation and the formation of clouds and rain, as well as how hot or cold

More information

APPENDIX C METEOROLOGICAL STATION DATA

APPENDIX C METEOROLOGICAL STATION DATA ONONDAGA LAKE PDI: PHASE VI DATA SUMMARY REPORT FINAL APPENDIX C METEOROLOGICAL STATION DATA P:\Honeywell -SYR\446092 - Phase VI PDI\09 Reports\9.5 Final Report\Final\PDI VI Summary Report_FINAL_8-2011.doc

More information

1. a. Surface Forecast Charts (USA and Ontario and Quebec) http://www.rap.ucar.edu/weather/

1. a. Surface Forecast Charts (USA and Ontario and Quebec) http://www.rap.ucar.edu/weather/ COMPUTER ASSISTED METEOROLOGY Frank Pennauer This contribution gives the available computer data sources, how to access them and use this data for predicting Soaring weather conditions will be discussed

More information

Mid latitude Cyclonic Storm System. 08 _15 ab. jpg

Mid latitude Cyclonic Storm System. 08 _15 ab. jpg Mid latitude Cyclonic Storm System 08 _15 ab. jpg Mid Latitude Cyclone Storm System (MLCSS) It has several names. Cyclone, Cyclonic Storm, Cyclonic System, Depression. Cyclonic Storms are the weather maker

More information

Temperature. PJ Brucat

Temperature. 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 information

In a majority of ice-crystal icing engine events, convective weather occurs in a very warm, moist, tropical-like environment. aero quarterly qtr_01 10

In a majority of ice-crystal icing engine events, convective weather occurs in a very warm, moist, tropical-like environment. aero quarterly qtr_01 10 In a majority of ice-crystal icing engine events, convective weather occurs in a very warm, moist, tropical-like environment. 22 avoiding convective Weather linked to Ice-crystal Icing engine events understanding

More information

Lecture 1: A Brief Survey of the Atmosphere

Lecture 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 information

Weather Merit Badge Workbook

Weather Merit Badge Workbook Merit Badge Workbook This workbook can help you but you still need to read the merit badge pamphlet. The work space provided for each requirement should be used by the Scout to make notes for discussing

More information

Purpose: To determine the dew and point and relative humidity in the classroom, and find the current relative humidity outside.

Purpose: To determine the dew and point and relative humidity in the classroom, and find the current relative humidity outside. Lab Exercise: Dew Point and Relative Humidity Purpose: To determine the dew and point and relative humidity in the classroom, and find the current relative humidity outside. Relative humidity is a measure

More information

Activity: Clouds, Air Pressure and Temperature

Activity: Clouds, Air Pressure and Temperature Activity: Clouds, Air Pressure and Temperature Materials A clean, clear, dry plastic 2-liter or larger beverage bottle with cap, thin liquid crystal temperature strip (available in aquarium supply stores),

More information

A.4 SEVERE WEATHER PLAN

A.4 SEVERE WEATHER PLAN Page 1 of 5 A.4 SEVERE WEATHER PLAN 1.0 Purpose 1.1 The purpose of this Severe Weather Response Plan is to minimize the impact on the University from a severe weather incident 2.0 Applicability 2.1 This

More information

Weather Theory. Chapter 11. Introduction

Weather Theory. Chapter 11. Introduction Chapter 11 Weather Theory Introduction Weather is an important factor that influences aircraft performance and flying safety. It is the state of the atmosphere at a given time and place, with respect to

More information

Storms Short Study Guide

Storms 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 information

Air Temperature With Flow Over a Mountain

Air Temperature With Flow Over a Mountain Air Temperature With Flow Over a Mountain WHAT YOU SHOULD LEARN IN THIS EXERCISE: Identify how air temperature changes when wind flow encounters topography. BACKGROUND INFORMATION Program In the program

More information

Weather Forecasting. DELTA SCIENCE READER Overview... 103 Before Reading... 104 Guide the Reading... 105 After Reading... 114

Weather Forecasting. DELTA SCIENCE READER Overview... 103 Before Reading... 104 Guide the Reading... 105 After Reading... 114 Weather Forecasting T ABLE OF CONTENTS ABOUT DELTA SCIENCE MODULES Program Introduction................... iii Teacher s Guide..................... iv Delta Science Readers................ vi Equipment

More information

Precipitation forms from water droplets or ice crystals.

Precipitation forms from water droplets or ice crystals. KEY CONCEPT Water falls to Earth s surface as precipitation. BEFORE, you learned Water moves between Earth's surface and the atmosphere Water vapor condenses into clouds NOW, you will learn How precipitation

More information

4.12 Improving wind profiler data recovery in non-uniform precipitation using a modified consensus algorithm

4.12 Improving wind profiler data recovery in non-uniform precipitation using a modified consensus algorithm 4.12 Improving wind profiler data recovery in non-uniform precipitation using a modified consensus algorithm Raisa Lehtinen 1, Daniel Gottas 2, Jim Jordan 3, Allen White 2 1 Vaisala Inc, Boulder, Colorado,

More information

6 th Grade Science Assessment: Weather & Water Select the best answer on the answer sheet. Please do not make any marks on this test.

6 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 information

Early Season Northwest Flow Snowfall Event 28 October 2008

Early Season Northwest Flow Snowfall Event 28 October 2008 Early Season Northwest Flow Snowfall Event 28 October 2008 Scott Krentz NOAA/National Weather Service Greer, SC 1. Introduction A post frontal northwest flow snowfall event affected the mountains of North

More information

QUALITY ASSURANCE IN ROAD OPERATIONS AND MAINTENANCE THE CONSULTANT S POINT OF VIEW WINTER MAINTENANCE

QUALITY ASSURANCE IN ROAD OPERATIONS AND MAINTENANCE THE CONSULTANT S POINT OF VIEW WINTER MAINTENANCE QUALITY ASSURANCE IN ROAD OPERATIONS AND MAINTENANCE THE CONSULTANT S POINT OF VIEW WINTER MAINTENANCE INTRODUCTION 1 The Finnish Transport Agency s Performance Based Maintenance Contract Model is approved

More information

1 AOS 452 Lab 1: Meteorological data decoding and forecast preparation

1 AOS 452 Lab 1: Meteorological data decoding and forecast preparation 1 AOS 452 Lab 1: Meteorological data decoding and forecast preparation This semester we will be using a variety of programs and software specific to meteorology. The first program we will focus on is:

More information

Water, Phase Changes, Clouds

Water, 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 information

CLIMATE, WATER & LIVING PATTERNS THINGS

CLIMATE, WATER & LIVING PATTERNS THINGS CLIMATE, WATER & LIVING PATTERNS NAME THE SIX MAJOR CLIMATE REGIONS DESCRIBE EACH CLIMATE REGION TELL THE FIVE FACTORS THAT AFFECT CLIMATE EXPLAIN HOW THOSE FACTORS AFFECT CLIMATE DESCRIBE HOW CLIMATES

More information

FORENSIC WEATHER CONSULTANTS, LLC

FORENSIC WEATHER CONSULTANTS, LLC SAMPLE, CONDENSED REPORT DATES AND LOCATIONS HAVE BEEN CHANGED FORENSIC WEATHER CONSULTANTS, LLC Howard Altschule Certified Consulting Meteorologist 1971 Western Avenue, #200 Albany, New York 12203 518-862-1800

More information

ATMS 310 Jet Streams

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

More information

Synoptic Meteorology I: Meteorological Data and an Introduction to Synoptic Analysis. 2, 4 September 2014

Synoptic Meteorology I: Meteorological Data and an Introduction to Synoptic Analysis. 2, 4 September 2014 Synoptic Meteorology I: Meteorological Data and an Introduction to Synoptic Analysis Types of Meteorological Observations 2, 4 September 2014 There exist three primary types of meteorological observations:

More information

Tephigrams: What you need to know

Tephigrams: What you need to know Tephigrams: What you need to know Contents An Introduction to Tephigrams...3 Can be as complicated as you like!...4 What pilots need to know...5 Some fundamentals...6 Air...6 Why does the air cool as it

More information

For further information, and additional background on the American Meteorological Society s Education Program, please contact:

For 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 information

SECTION 2 3 OPERATION OF INSTRUMENTS AND CONTROLS. Lights, Wipers and Defogger

SECTION 2 3 OPERATION OF INSTRUMENTS AND CONTROLS. Lights, Wipers and Defogger OPERATION OF INSTRUMENTS AND CONTROLS Lights, Wipers and Defogger SECTION 2 3 Headlights and turn signals................................... 92 Emergency flashers..........................................

More information

Note taker: Katherine Willingham (NSSL)

Note taker: Katherine Willingham (NSSL) SMART-R Event Log IOP 3 Project: Debris Flow Project Lat: 34.200610 Lon: -118.350563 Alt: 712 ft. Truck HD: 193 deg Date/Time SR1 ready for operation: 12 December 2240 UTC Site: BUR Airport, Burbank CA

More information

What Causes Climate? Use Target Reading Skills

What Causes Climate? Use Target Reading Skills Climate and Climate Change Name Date Class Climate and Climate Change Guided Reading and Study What Causes Climate? This section describes factors that determine climate, or the average weather conditions

More information