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



Similar documents
2015 Annual Operating Plan Fire Weather Forecasts and Services NWS Chicago/Romeoville

6.9 A NEW APPROACH TO FIRE WEATHER FORECASTING AT THE TULSA WFO. Sarah J. Taylor* and Eric D. Howieson NOAA/National Weather Service Tulsa, Oklahoma

Stability and Cloud Development. Stability in the atmosphere AT350. Why did this cloud form, whereas the sky was clear 4 hours ago?

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

Seasonal Temperature Variations

Studying Topography, Orographic Rainfall, and Ecosystems (STORE)

Name Period 4 th Six Weeks Notes 2015 Weather

Convective Clouds. Convective clouds 1

Atmospheric Stability & Cloud Development

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

Fundamentals of Climate Change (PCC 587): Water Vapor

Lab 10. Solar and Wind Power

IBM Big Green Innovations Environmental R&D and Services

How to analyze synoptic-scale weather patterns Table of Contents

UNIT VII--ATMOSPHERIC STABILITY AND INSTABILITY

Heat Transfer. Energy from the Sun. Introduction

Fog and Cloud Development. Bows and Flows of Angel Hair

Air Masses and Fronts

How do Scientists Forecast Thunderstorms?

ATM S 111, Global Warming: Understanding the Forecast

Identification and Prevention of Frost or Freeze Damage By Linda Reddick, Kingman Area Master Gardener

Temperature and Humidity

WEATHER THEORY Temperature, Pressure And Moisture

Project Title: Quantifying Uncertainties of High-Resolution WRF Modeling on Downslope Wind Forecasts in the Las Vegas Valley

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

Use of numerical weather forecast predictions in soil moisture modelling

1. a. Surface Forecast Charts (USA and Ontario and Quebec)

WEATHER AND CLIMATE practice test

CONTENTS PAGE: 1. EU-UNAWE Mission Statement 3 2. CAPS Life Skills Programme of Assessment 4 5-6

Project 16 - PLAYING THE STOCK MARKET FOR GAIN OR LOSS

Chapter 6 - Cloud Development and Forms. Interesting Cloud

Geography affects climate.

4.3. David E. Rudack*, Meteorological Development Laboratory Office of Science and Technology National Weather Service, NOAA 1.

Estimating Firn Emissivity, from 1994 to1998, at the Ski Hi Automatic Weather Station on the West Antarctic Ice Sheet Using Passive Microwave Data

Basics of weather interpretation

Chapter 7 Stability and Cloud Development. Atmospheric Stability

Climate and Weather. This document explains where we obtain weather and climate data and how we incorporate it into metrics:

Heat and Temperature: Front End Evaluation Report. Joshua Gutwill. October 1999

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

Empirical study of the temporal variation of a tropical surface temperature on hourly time integration

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

THE HUMIDITY/MOISTURE HANDBOOK

Texas Department of Public Safety Texas Division of Emergency Management. Texas State Operations Center

AIRCRAFT PERFORMANCE Pressure Altitude And Density Altitude

Use of Decision Support Tools for Bushfire Risk Management in NSW

Optimum Solar Orientation: Miami, Florida

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

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

Monsoon Variability and Extreme Weather Events

Technical Attachment. The National Weather Service Estimated Actual Velocity Radar Tool. Ken Falk WFO Shreveport, Louisiana

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

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

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

Seasonal & Daily Temperatures. Seasons & Sun's Distance. Solstice & Equinox. Seasons & Solar Intensity

Analyzing Weather Data

Best Practices for Managing Heat Stress in Feedyard Cattle

Temperature affects water in the air.

FIRST GRADE 1 WEEK LESSON PLANS AND ACTIVITIES

CHAPTER 3. The sun and the seasons. Locating the position of the sun

P1.2 NUMERICAL SIMULATION OF LONG DISTANCE TRANSPORTATION OF VOLCANO ASH FROM PINATUBO

Cool Spaces. earth-wise guide to. green strategies: light strategies: Keep Austin Cool

The Balance of Power in the Earth-Sun System

The human body core temperature is constant around 37.1±1.0 o C ( degree Fahrenheit = degree Celsius )

(Walter Glogowski, Chaz Shapiro & Reid Sherman) INTRODUCTION

A Mariner s Guide to Marine Weather Services Great Lakes

ES 106 Laboratory # 6 MOISTURE IN THE ATMOSPHERE

FOR SUBSCRIBERS ONLY! - TRIAL PASSWORD USERS MAY NOT REPRODUCE AND DISTRIBUTE PRINTABLE MATERIALS OFF THE SOLPASS WEBSITE!

The Ideal Gas Law. Gas Constant. Applications of the Gas law. P = ρ R T. Lecture 2: Atmospheric Thermodynamics

Follow That Hurricane!

GENERAL WATERING & CARE GUIDE

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

Partnerships Implementing Engineering Education Worcester Polytechnic Institute Worcester Public Schools

Chapter 6: Cloud Development and Forms

HAY MOISTURE & WEATHER:

Improved Warnings for Natural Hazards: A Prototype System for Southern California

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

URGENT - WEATHER MESSAGE NATIONAL WEATHER SERVICE MELBOURNE FL 402 AM EST MON JAN

WeatherBug Vocabulary Bingo

Climate Models: Uncertainties due to Clouds. Joel Norris Assistant Professor of Climate and Atmospheric Sciences Scripps Institution of Oceanography

Joint Polar Satellite System (JPSS)

Principles of Rice Drying How does rice dry?

How Do Oceans Affect Weather and Climate?

Activity 1: 2 butter cartons, scissors, cling film, thermometer, water, a sunny spot and a shady spot.

CARBON THROUGH THE SEASONS

Glaciogenic Cloud Seeding to Increase Orographic Precipitation Bruce A. Boe Director of Meteorology

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

39th International Physics Olympiad - Hanoi - Vietnam Theoretical Problem No. 3

NOAA s National Weather Service Milwaukee/Sullivan

Page 1. Weather Unit Exam Pre-Test Questions

Weather Help - NEXRAD Radar Maps. Base Reflectivity

SKEW-T, LOG-P DIAGRAM ANALYSIS PROCEDURES

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

Analyze Weather in Cold Regions and Mountainous Terrain

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

Transcription:

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 fire/land managers At Chicago since December 2000 Shreveport, LA Northern Indiana

National Weather Service Federal Agency NOAA (National Oceanic & Atmospheric Administration) DOC (Department of Commerce) Mission, protection of life and property Staffed 24/7/365 Fire weather forecasts vary by office, by season and by local user needs

Outline Mixing Heights/Soundings 1700 FT Forecast Mixing Temperature Seasonal Affects on Mixing Heights Transport Winds/Ventilation/Dispersion Afternoon dip in relative humidity Red Flag Warnings/Fire Weather Watches Surface Wind definition

Mixing Heights The height to which smoke will rise before spreading out (inversion = mixing height) Layer of stable air where temperatures warm with increasing height Acts as a lid, severely limiting amount of vertical motion

Mixing Heights Expressed in FT AGL (feet above ground level) Typically will be very low at night, usually less than 1000 ft, sometimes at the surface, due to surface cooling 1700 Feet Minimum height most users want before burning Depends on location, size, fuel type, etc., of burn site

Mixing Heights Generally, an easy parameter to forecast, in terms of data availability Multiple computer forecast models Multiple forecasts levels & heights Hourly forecast data available from some models Forecast accuracy dependent on many factors Cloud cover and temperatures Data plotted and referred to as soundings

Difficult to Observe/Verify Weather Balloons Twice a day, early morning & early evening Roughly 80 locations spread out across the country

Difficult to Observe/Verify Weather sensors on aircraft Clustered around large airports/metro areas Only available to federal agencies

Observed Weather Balloon Sounding from Davenport, IA

Observed Aircraft Sounding

Observed Sounding with Dewpoint

Lowest Levels

Mixing Height Lifting in the afternoon then falling at night

1700 FT Mixing Temperature When the observed surface temperature equals the 1700 FT forecast mixing temperature, it can be estimated that the mixing height is now near or passing through 1700 feet. Used as a rough estimate by field personnel Local conditions such as bodies of water, terrain, rural vs. urban areas, may have impacts

1700 FT Mixing Temperature If the 1700 FT forecast mixing temperature is equal to or less than the forecast high/maximum temperature, then the mixing height is forecast to reach 1700 feet or higher Max temp forecast, 65 degrees Max mixing height forecast, 4500 ft 1700 ft forecast mixing temperature, 58 degrees When your surface temperature reaches 58 degrees, the mixing height is forecast to be near 1700 ft

1700 FT Mixing Temperature If the 1700 FT forecast mixing temperature is higher/warmer than the forecast high/maximum temperature, then the mixing height is NOT forecast to reach 1700 feet Max temp forecast, 55 degrees Max mixing height, 1500 ft 1700 ft forecast mixing temperature, 58 degrees Your surface temperature would have to reach 58 degrees for a 1700 ft mixing height, but the forecast high temperature is only 55 degrees

1700 FT Mixing Temperature IMPORTANT! This is only a forecast! Forecasts can and do change! Unexpected cloud cover could keep temperatures lower than expected and thus not reach the 1700 ft mixing temperature or even the expected max/high temperature. Result: Much lower mixing heights Temperatures may warm to or above the 1700 ft forecast mixing temperature, pushing the mixing height well above 1700 ft. Result: Much higher mixing heights

1700 FT Mixing Temperature Hourly weather graphs of mixing heights available on-line from many NWS offices, which will show height in feet vs. time Provides detailed information for specific grid points 1700 ft forecast mixing temperature still an important tool/parameter in the field and can help determine whether mixing height graphs are on track

NWS On-Line Hourly Weather Graph

Mixing Heights Seasonal Affects Duration of sunlight Mixing heights reach 1700 FT earlier and stay above 1700 FT longer Potential for mixing heights to reach higher, several thousand feet At the same time, vegetation is greening up

Shaded area is available time above 1700 feet Spring

Shaded area is available time above 1700 feet Late Spring

Shaded area is available time above 1700 feet Summer

Shaded area is available time above 1700 feet Fall

Shaded area is available time above 1700 feet Late Fall

Transport Winds Average wind speed and direction in the mixed layer The mixed layer is the surface to the mixing height Example, the mixing height is 2000 feet, and the transport winds are South at 15 mph. This means that the average wind speed between the surface and 2,000 feet is 15 mph FROM the south

Transport Winds/Mixed Layer

Ventilation Rate/Dispersion Multiplication of the mixing height in feet and the transport winds in knots Units differ based on user needs The larger the number, the better the ventilation NWS forecasts typically display highest number or Vent Rate Max for a 12 hour period Important to remember this Max may only last a few hours

Ventilation Rate/Dispersion IMPORTANT, descriptors are determined by the users! Forecasters only provide/create the numbers. Range/descriptors below used by Chicago area fire/land managers Poor, < 40,000 knot feet Fair, 40,000 to 60,000 knot feet Good, 60,000 to 100,000 knot feet Very Good, 100,000 to 150,000 knot feet Excellent, > 150,000 knot feet

Ventilation Rate/Dispersion High mixing height with light transport winds 8,000 feet with an east wind 10 knots, 80,000 Smoke column will go straight up Tilted slightly by direction of light winds Low mixing height with strong transport winds 2,000 feet with a south wind 35 knots, 70,000 Smoke column will not rise very high Tilted strongly by direction of winds

Sudden Drop In Humidity

How Low will RH drop?

Fire Weather Watches/Red Flag Warnings A fire weather watch/red flag warning is issued when a combination of dry fuels and weather conditions create extreme fire danger and/or fire behavior Watches issued in the 18 to 96 hour time frame Warnings issued up to 48 hours Criteria differ by NWS office/local user needs NWS Chicago Criteria Sustained 20 foot winds of 20 mph or higher Afternoon relative humidity less than 25% 10 hour fuel moisture at 8% or less for one day

Important note on Winds Surface winds in meteorology are defined as a 10 meter wind (roughly 33 feet) If the forecast doesn t specifically say, 20 foot wind, then assume it is at 10 meters NWS Chicago uses a standard 20% reduction 10 meter wind is 10 mph, 20 foot wind is 8 mph Strong cold air advection could be less, 15% Strong warm air advection, could be more, 25%

Thank you casey.sullivan@noaa.gov