Road Weather: The Science Behind What You Know

Similar documents
Road Weather: Pavement Forecasting

5.2 (HUMIDITY) WEATHER EARTH SCIENCE

1st Annual Southwest Ohio Snow Conference April 8, 2010 Abner F. Johnson, Office of Maintenance - RWIS Coordinator

7. The weather instrument below can be used to determine relative humidity.

Chapter 5: Weather. Only Section 1: What is Weather?

Temp 54 Dew Point 41 Relative Humidity 63%

1. Base your answer to the following question on the weather map below, which shows a weather system that is affecting part of the United States.

Clouds and Rain Unit (3 pts)

February 11, Weather and Water Investigation 6 Day 6

CLIMATE. UNIT TWO March 2019

Weather. Describing Weather

Weather. Describing Weather

GEOGRAPHY EYA NOTES. Weather. atmosphere. Weather and climate

WONDERING ABOUT WEATHER

Weather Maps. Name:& & &&&&&Advisory:& & 1.! A&weather&map&is:& & & & 2.! Weather&fronts&are:& & & & & &

latent heat/humidity

MOISTURE IN THE ATMOSPHERE MEGA PACKET

Weather - is the state of the atmosphere at a specific time & place

Questions. Making Better Weather-Based Management Decisions. Dual Polarization 5/1/2018

Weather & Atmospheric Variables Review

The Water Cycle. Water in the Atmosphere AOSC 200 Tim Canty. Class Web Site:

Water in the Atmosphere

Weather Part I- Weather Variables

Forecasting Weather: Air Masses and Fronts

Unit 5 Lesson 3 How is Weather Predicted? Copyright Houghton Mifflin Harcourt Publishing Company

Page 1. Name:

Weather, Atmosphere and Meteorology

Weather is the state or condition of the atmosphere at a given location for a brief time period.

5) The amount of heat needed to raise the temperature of 1 gram of a substance by 1 C is called: Page Ref: 69

ROAD PAVEMENT TEMPERATURES AND THEIR IMPACT ON TRAVEL DURING SNOW STORMS. Donald M. Moore, NOAA/NWS, Billings, MT; and R. J.

Three things necessary for weather are Heat, Air, Moisture (HAM) Weather takes place in the Troposphere (The lower part of the atmosphere).

WATER IN THE ATMOSPHERE

Name Class Date. 3. In what part of the water cycle do clouds form? a. precipitation b. evaporation c. condensation d. runoff

17 th Annual Snow & Ice Symposium Columbus, OH. Snow & Ice Management Association Copyright 2014 SALT BRINE & SNOW AND ICE CONTROL.

Atmosphere L AY E RS O F T H E AT MOSPHERE

Vantage Pro Technical Reference

III. Section 3.3 Vertical air motion can cause severe storms

Weather and Climate. An Introduction

Weather 101 Brad Jakubowski Doane College Water

Forecasting Local Weather

Pd: Date: Page # Describing Weather -- Lesson 1 Study Guide

Multiple Choice (2 Points Each)

Chapter Introduction. Weather. Patterns. Forecasts Chapter Wrap-Up

Station A. 1. In the Northern Hemisphere, the general direction of the flow of the jet stream is toward the: a. north b. east c.

Name 28-MAY-08. FA RP 1 Mr. Chase. 1. Which weather-station model shows an air pressure of millibars?

Fronts. Direction of Front

How Can You Predict Weather Changes?

COMPOSITION OF THE ATMOSPHERE

1/2/2016 WEATHER DEFINITION

Copyright 2015 Edmentum All rights reserved.

Unit: Weather Study Guide

UNIT 12: THE HYDROLOGIC CYCLE

Weather and climate. reflect. what do you think? look out!

above the land to be warmer, causing convection currents because of the difference in air pressure.

2nd Grade. Earth's Water. Slide 1 / 111 Slide 2 / 111. Slide 3 / 111. Slide 4 / 111. Slide 5 (Answer) / 111. Slide 5 / 111. Role of Water on Earth

Science Chapter 13,14,15

Weather. A. atmosphere is a layer of gases that wrap around the Earth like a blanket.

Earth/Space Systems and Cycles (SOL 4.6)

A) usually less B) dark colored and rough D) light colored with a smooth surface A) transparency of the atmosphere D) rough, black surface

Practical Atmospheric Analysis

Introduction. Sunny Partly Cloudy Cloudy. Flurries Snow Ice. Showers Thunderstorms Rain. High Pressure Low Pressure FRONTS. Cold Warm Stationary

Goal 2.5. The Atmosphere

Understanding Michigan snowfall. Jim Keysor - NWS Gaylord

Module 11: Meteorology Topic 5 Content: Weather Maps Notes

Condensation, Evaporation, Weather, and the Water Cycle

Introduction to Weather Moisture in the Air Vapor Pressure and Dew Point

PLOTTING WEATHER DATA to perform a SURFACE ANALYSIS

Ch 7 Weather Practice Questions

What do you think of when someone says weather?

MTO s Road Weather Information System (RWIS)

Climate versus Weather

Probabilistic Decision-Making and Weather Assessment

EGYPTIAN AMERICAN INTERNATIONAL SCHOOL Elementary Science Department TERM 4 GRADE 4. Revision. 1. Weather ( ) 1. Is too little precipitation.

Topic 1 The Atmosphere and Atmospheric Variables

1. Which weather map symbol is associated with extremely low air pressure? A) B) C) D) 2. The diagram below represents a weather instrument.

Guided Notes Weather. Part 1: Weather Factors Temperature Humidity Air Pressure Winds Station Models

Air Mass. 1. Air Mass : Large body of Air with similar temperature and humidity (or moisture) ; 4 types

Multiple Choice Identify the choice that best completes the statement or answers the question.

Laboratory Exercise #7 - Introduction to Atmospheric Science: The Seasons

also known as barometric pressure; weight of the air above the surface of the earth; measured by a barometer air pressure, high

Name Date Hour Table. Chapter 12-AP Lesson One

4 Changes in Climate. TAKE A LOOK 2. Explain Why is more land exposed during glacial periods than at other times?

Science 1206 Chapter 1 - Inquiring about Weather

1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures?

Weather. science centers. created by: The Curriculum Corner.

according to and water. High atmospheric pressure - Cold dry air is other air so it remains close to the earth, giving weather.

GEOGRAPHY AND HISTORY

Name Class Date STUDY GUIDE FOR CONTENT MASTERY

Evaporation - Water evaporates (changes from a liquid to a gas) into water vapor due to heat from the Sun.

Federal Maintenance Decision Support System (MDSS) Prototype Update

Using an Artificial Neural Network to Predict Parameters for Frost Deposition on Iowa Bridgeways

A) B) C) D) 2) The diagrams below show the phases of the Moon as viewed by an observer in New York State at different times in August.

Jessica M. Rathke* and Renee A. McPherson Oklahoma Climatological Survey, University of Oklahoma, Norman, Oklahoma 2. DATA. 2.1.

Meteorology. I. The Atmosphere - the thin envelope of gas that surrounds the earth.

Mr. Lanik Practice Test Name:

Average Weather In March For Fukuoka, Japan

Guided Notes Weather. Part 2: Meteorology Air Masses Fronts Weather Maps Storms Storm Preparation

4 Forecasting Weather

Warm Up 1: Atmosphere LT I can describe dew point, condensation nuclei and explain the difference between relative and absolute humidity.

NATS 1750 Lecture. Wednesday 28 th November Pearson Education, Inc.

Transcription:

The Weather Road Weather: The Science Behind What You Know Jon Tarleton Global Roads Marketing Manager Meteorologist Jon.tarleton@vaisala.com Page 2 / date / name / Internal use / Vaisala Weather and Our Pavement How can we measure the pavement temperature? Page 3 / date / name / Internal use / Vaisala Page 4 / date / name / Internal use / Vaisala Pavement Forecasting One key to pavement forecasting is accurately forecasting the weather above the road. I know what you are thinking Page 5 / date / name / Internal use / Vaisala Page 6 / date / name / Internal use / Vaisala 1

What Affects the Pavement? Back in the good old days. Air Above the Pavement Sun or Solar Radiation Moisture Heat Beneath the Pavement They said it was going to snow today. It s Cloudy, and the bank says 32º Time to go to work!!! Page 7 / date / name / Internal use / Vaisala Page 8 / date / name / Internal use / Vaisala Thermodynamics 101 Example To understand how the air impacts our pavement we must understand how heat transfers from objects. Every object is in a constant state of temperature change. 70 68 65 70 65 Page 9 / date / name / Internal use / Vaisala Page 10 / date / name / Internal use / Vaisala The greater the exposed surface area the faster the change. Another consideration is the material of the object. A bridge made of metal and concrete transfers heat very well, and therefore accelerates the temperature change. Page 11 / date / name / Internal use / Vaisala Page 12 / date / name / Internal use / Vaisala 2

Density and Composition Affect Rate of Change. Misconception of Wind Chill Wind Chill ONLY effects the human body and not other objects. Wind Chill Factor was created by meteorologists to give people an idea of how cold it feels outside. Concrete Asphalt Page 13 / date / name / Internal use / Vaisala Page 14 / date / name / Internal use / Vaisala When does the wind impact the pavement? Why is one curve different than the other? During times of air temperature change, the wind is blowing in colder temperatures, so the wind can help cool the pavement. Page 15 / date / name / Internal use / Vaisala Page 16 / date / name / Internal use / Vaisala Solar Radiation Pavement Temp vs. Air Temp Pavement Temp Cloud Cover Air Temp Page 17 / date / name / Internal use / Vaisala Page 18 / date / name / Internal use / Vaisala 3

During a typical sunny day the temperature can be rising about 10º every hour, or 1.5 º every 10 min between 7am and Noon. Temp Pavement Temperature Curve 100 80 60 Pavement Temp 40 20 0 2am Page 19 / date / name / Internal use / Vaisala 6am Time Noon 4pm Greatest change in temperature Page 20 / date / name / Internal use / Vaisala A brief cloud cover for 30 minutes before Noon could cause a forecast produced at Noon to be off by as much as 8-10º. Sun in Winter Elevation and Pavement At higher elevations there is less atmosphere for the sun s rays to penetrate, so solar heating is greater the higher the elevation. Even in the middle of January the sun has an affect on our pavement temperature. Page 21 / date / name / Internal use / Vaisala Page 22 / date / name / Internal use / Vaisala Moisture Two Forms are Important to the Pavement Water Vapor Precipitation Dewpoint is one of the most important variables to monitor before and during a winter storm. However, dewpoint is probably one of the least understood concepts in weather, so we will start with a little Dewpoint 101. Page 23 / date / name / Internal use / Vaisala Page 24 / date / name / Internal use / Vaisala 4

Dewpoint: The temperature to which air must be cooled for saturation to occur. An Example If you cooled the air Temperature 40 40 Dewpoint 30 to the dewpoint 35 Condensation 30 Occurs!!! When the temperature reaches the dew point, it causes water molecules in the air to form into water droplets Page 25 / date / name / Internal use / Vaisala on a surface. The Soda Can Effect On a hot day when you take a soda can outside the soda can sweats. Why? Air Temperature 88 Because the soda can Dewpoint 60 is colder than the dewpoint outside. Can temperature 35 Air around the can is cooled causing water vapor in the air to condense on the can s surface, just like water vapor condensing on dust particles in the air to form clouds. Page 26 / date / name / Internal use / Vaisala Why is Dewpoint important? Dewpoint gives you a measure of how moist or dry an airmass is. Remember that when the temperature and dewpoint are equal at the ground, we have condensation at the ground. This is a dry airmass This is a moist airmass Temp. 30 Temp. 30 Dew point 15 Dewpoint 27 So, the larger the spread between the temperature and the dew point, the drier the air. When temperature and dew point are the same, relative humidity= 100%, but this does not mean we have precipitation. To produce precipitation, we need condensation to occur well above the ground. That is where we need temperature to equal the dewpoint, or where the relative humidity is 100%. Page 27 / date / name / Internal use / Vaisala Page 28 / date / name / Internal use / Vaisala RWIS can be used to show the formation of frost. Criteria for Frost: Recent rain or melting snow Clear skies overnight Light winds (helps to have southerly direction) Must haves: Pavement temperature must drop below freezing Pavement temperature must be equal to or less than dew point. Black Ice or road frost example from Sioux City Iowa Spring of 2000. Tem mperature (F) 50 40 30 20 10 0 6pm Midnight 5am 7am Time Pavement Air Temp Dewpoint Page 29 / date / name / Internal use / Vaisala Page 30 / date / name / Internal use / Vaisala 5

Why does radar sometimes show snow everywhere but it is not snowing out the window? One common weather feature that can be misleading to view on Radar is Virga. What is Virga? Dry Air As the snow falls from the clouds it falls into the drier air near the surface which causes the snowflakes to evaporate before they reach the ground. Virga Page 31 / date / name / Internal use / Vaisala Page 32 / date / name / Internal use / Vaisala How does this look on radar? Classic Doughnut Hole On Radar, it will appear there is snow nearby, and sometimes it will even look like snow is all around the radar but not at the radar site. Remember that radar sees moisture. It can not tell whether it is reaching the ground. Page 33 / date / name / Internal use / Vaisala Page 34 / date / name / Internal use / Vaisala Affects of Precipitation Dew Point and Falling Temps. The harder the rain or snow is falling, the more it increases cooling. 33 As soon as it begins to rain or snow some of the moisture begins to evaporate. Evaporation is a cooling process. If the air is dry the evaporation rate is high causing a lot of cooling. (Common in the winter) Page 35 / date / name / Internal use / Vaisala 45 34 Page 36 / date / name / Internal use / Vaisala Temp. 30 Dew point 25 Pavements will cool faster! Temp. 30 Dew point 29 6

Subsurface Temperature Uses for Sub-surface Sensor: The main use for the sub-surface probe is input to the pavement temperature forecast model. Pavement Weather Center use pavement model as a piece of information to determine the flow of heat into or out of the pavement surface. Page 37 / date / name / Internal use / Vaisala Page 38 / date / name / Internal use / Vaisala Sub-surface is key when pavement temperatures are near freezing, especially during late fall and spring snow storms. Measuring Current Pavement Temperature With a warm sub-surface, pavement temps may drop at first, but heat under the road will help melt any snow or ice that accumulates. 40º 33º Vehicle Mounted Pavement Sensor Page 39 / date / name / Internal use / Vaisala Page 40 / date Road / name / Internal Weather use / Vaisala Information Systems (RWIS) Installed Pavement Sensors Mobile Temperature Sensors Placed directly in the road to measure pavement temperature. Still most accurate way to measure pavement temperature. System archives data for later analysis. a s Extremely popular because of cost and ease of use. Allows user to see entire road not just one spot. Not as accurate. ate Page 41 / date / name / Internal use / Vaisala Page 42 / date / name / Internal use / Vaisala 7

Non-Intrusive Sensors Forecasting the Pavement Non-Intrusive is a very popular method for all road devices. In science we call measuring something from a distance remote sensing. Benefits of sensors: Lower installation costs/cost to maintain Safer for service and install Accuracy similar to in-road sensors Page 43 / date / name / Internal use / Vaisala Page 44 / date / name / Internal use / Vaisala With pavement forecasts we can t do regional forecasts! Pavement forecasts are site specific Page 45 / date / name / Internal use / Vaisala Page 46 / date / name / Internal use / Vaisala Creating a Pavement Forecast 1. Make a forecast for atmosphere above a road. 2. Input into a pavement model along with: Current pavement trend Subsurface temperature 3. Model then can create a 24 hour pavement temperature forecast, knowing everything we just discussed. Summary A lot of variables effect pavement Air Sun Moisture Heat Beneath Difficult to monitor without the help of a pavement model. Many ways to measure pavement temperature re all are good, but some are better. Page 47 / date / name / Internal use / Vaisala Page 48 / date / name / Internal use / Vaisala 8

Summary Remember our fundamental question: When will I have to prevent the road from becoming hazardous? And the excuses as to why we can do it without any help: It is too expensive We can do it on our own it is not that hard. We don t have all that money like a DOT. A pavement forecast solves our fundamental question. Questions? Jon Tarleton Global Roads Marketing Manager Meteorologist Page 49 / date / name / Internal use / Vaisala 9