Vaisala Visualization. November 2010 Petteri Leppänen

Size: px
Start display at page:

Download "Vaisala Visualization. November 2010 Petteri Leppänen"

Transcription

1 Vaisala Visualization November 2010 Petteri Leppänen

2 Roads Web visualization offering sales price Road Weather Advisor Road Weather Observer Road Weather Navigator 2.0 RWDSS customer value Page 2 / date / name / Internal use / Vaisala

3 Road Weather Advisor Includes easy to set alarms Page 3 / date / name / Internal use / Vaisala

4 Road Weather Observer Page 4 / date / name / Internal use / Vaisala

5 Archiving for Navigator Page 5 / date / name / Internal use / Vaisala

6 Differences between the products Single station view (camera image, main parameters, configurable graph) Outcomes based messages Simple alert management Supports more than five stations Map view (station status, parameters) Thermal map Station summary list, Camera wall Forecast texts from service providers Timer slider (controls map, list and wall) Animated playback of map layers Historical data available Single-click PDF reports and data exports Advanced alert management Advisor Observer Navigator Page 6 / date / name / Internal use / Vaisala

7 Single site view with observed data Page 7 / date / name / Internal use / Vaisala

8 Forecaster generated texts show up in drop down boxes Page 8 / date / name / Internal use / Vaisala

9 Vaisala Solution (Icebreak) Icebreak is a mathematical model capable of simulating the changes in pavement temperature and state using information about the forecast location and forecasted atmospheric conditions. Icebreak s capacity to provide tactical and strategic information (i.e. nowcasts and forecasts) about the ever changing road weather conditions supports the planning and execution of maintenance activities. Page 9 / date / name / Internal use / Vaisala

10 Vaisala Solution (Icebreak) A fundamental element of good weather and road condition forecasts is accurate assessment of the environment and pavement at the beginning of the forecast period. Vaisala s Icebreak model and RWIS serve as a foundation for accurate, timely road weather predictions Icebreak setup techniques help ensure that forecast accuracy is maximized. Additional products, such as Thermal Mapping, can be used augment and support pavement forecasting. Page 10 / date / name / Internal use / Vaisala

11 Icebreak Input Requirements Initial Road Weather Conditions Client Site Metadata Forecast Data Icebreak Navigator Display Page 11 / date / name / Internal use / Vaisala

12 Icebreak Client Site Data Location of forecast site (latitude, longitude) Elevation As-built properties of the pavement Road versus bridge Asphalt versus concrete Subsurface layer properties (type and thickness) Number and depth of sensors Surface roughness length A height which aids in understanding the impact of roughness elements such as trees or buildings on the wind. Sky view factor Used to gauge the obstructions on the forecast site. Obstructions impact the amount of radiation received at the site location. Each of these factors is essential in predicting the evolution of pavement conditions; however, a number of road weather providers don t attempt to account for all of these parameters. Page 12 / date / name / Internal use / Vaisala

13 Icebreak Initial Condition Inputs Properly assessing the initial atmospheric and road conditions is extremely important for forecast accuracy. Weather and road condition information can be used to initialize both NWP models* and Icebreak For Icebreak, the main source of initial conditions comes from RWIS Icebreak input data for initial conditions Weather Air temperature Dew point temperature Wind speed Precipitation status/intensity Road Pavement temperature Subsurface temperature(s) Pavement condition (i.e., dry, wet, icy, etc.) * NWP models rely mainly on weather and soil condition parameters Page 13 / date / name / Internal use / Vaisala

14 Icebreak Weather Forecast Inputs Atmospheric forecast data is used to help drive Icebreak Icebreak input forecast data Air temperature Dew point temperature Wind speed Precipitation status/intensity Cloud cover Page 14 / date / name / Internal use / Vaisala

15 Icebreak Output Pavement temperature Pavement condition Subsurface temperatures Air temperature Dew point temperature Wind speed Precipitation status friction in close future Page 15 / date / name / Internal use / Vaisala

16 IceNet Delivery Icebreak forecast (pavement temp) Observed Pavement Temperature Page 16 / date / name / Internal use / Vaisala

17 Coupling Icebreak Predictions and Thermal Mapping Icebreak will provide forecasts at point locations (typically RWIS sites) In cases where roads have been thermally mapped, Icebreak forecasts can be extrapolated to other sections of the roadway to provide an understanding of what is occurring between stations or forecast points* Extrapolated Forecast Forecast point Extrapolated Forecast *This can be done in none-precipitation situations during nighttime hours Page 17 / date / name / Internal use / Vaisala

18 Summary Icebreak is capable of supporting year-round maintenance activities by providing prognostic information regarding pavement temperature and conditions. Icebreak can support tactical and/or strategic decision making process. Data from RWIS are leveraged by Icebreak for effective pavement predictions. Site specific characteristics are used to enhance Icebreak forecasts Icebreak can be driven by Vaisala or third party supplied weather forecasts. Page 18 / date / name / Internal use / Vaisala

19 Time slider function allows you to browse into the future all data shown is then forecast values, color codes etc Page 19 / date / name / Internal use / Vaisala

20 Single site view when forecasts are available Now Page 20 / date / name / Internal use / Vaisala

21 Comparing critical values of your choice Page 21 / date / name / Internal use / Vaisala

22 Road surface nearly dry with some chemical present Road surface now wet with chemical present (melted snow) Snow overwhelmed treatment and settles on road Snow melted again back to wet roads with chemical present Page 22 / date / name / Internal use / Vaisala

23 Road surface wet with active chemical present note embedded sensor gives freezing temperature below RST Freezing temperature now above sub zero RST hence ICE forms on the road New treatment restores wet roads with sufficient chemical to lower freezing temperature Page 23 / date / name / Internal use / Vaisala

24 Introduction to Thermal Mapping Page 24 / date / name / Internal use / Vaisala

25 Depth Temperature Sky View Rural Proximity to water Wind Road Surface Cloud Temperature Traffic Volume Road construction Humidity Altitude Tunnels Urban Page 25 / date / name / Internal use / Vaisala Road surface Bridges Air temperature

26 Factors affecting Road Surface Temperature Static Sky View Urban environment Rural environment Proximity to water/sea Bridges Tunnels/Underpasses Road construction Road surfaces Altitude Road Surface Temperature Variable Cloud Humidity / Dew Point Wind speeds Depth temperature Air Temperature Traffic volumes Page 26 / date / name / Internal use / Vaisala

27 Factors affecting Road Surface Temperature No one factor has complete control Sky View 70% of the variability However construction has massive impact Page 27 / date / name / Internal use / Vaisala

28 Variable factors can have different affects Clear skies Day Allow sunshine on the road giving it extra heat Night allows heat to escape fast dropping temperatures quickly Wind Calm Cold air sinks next to surface creating cold layer, heat is drawn out of the road more quickly. Windy warmer air aloft bought down to the surface warms the road/stops heat loss. Traffic Rush hour traffic makes location a warm site lots of extra heat Sunday morning can mean location suddenly becomes colder than usual. Page 28 / date / name / Internal use / Vaisala

29 Modelling Road Surface Temperature (RST) RST is the final product No one factor dictates what it is or will become Static Factors are always the same so drop out of the equation once a site is known (Thermal Mapping shows this for a whole network). Variable Factors need more care and attention Models are written to take into account heat balance equations Page 29 / date / name / Internal use / Vaisala

30 What forecasters do Site specific forecasts verified by observed data RST model run by specifying key weather variables Air Temperature Dew Point Cloud Cover Wind Speed Precipitation Each has a significant effect on the RST at the site Final output is an estimation of RST at that site throughout 24 hr period Page 30 / date / name / Internal use / Vaisala

31 What Vaisala do Thermally Map the road to identify how fixed variable effect the RST on average conditions Damped Cloudy/windy/rainy Extreme Clear/still/dry Intermediate somewhere in between the two Output is a repeatable temperature variation measurement across the whole network based upon all fixed factors. Weather variables are held fixed by choosing similar characteristic nights to survey on. Results different by category, cold spots tend to stay the same but not always. Temperature variations most noticeable under Extreme conditions Page 31 / date / name / Internal use / Vaisala

32 Put them together Forecasters cover the variable factors Vaisala cover the Fixed factors By combining the two you can get a representation of all factors in one Time Step Thermal Maps How does it work? Page 32 / date / name / Internal use / Vaisala

33 Using Thermal Fingerprints Warmer location Average Network Temperature Colder location Page 33 / date / name / Internal use / Vaisala

34 Using Thermal Fingerprints, how repreentative is one point measurement only? Page 34 / date / name / Internal use / Vaisala

35 Forecast Thermal Maps can also be animated Page 35 / date / name / Internal use / Vaisala

36 Animated radar on same screen Page 36 / date / name / Internal use / Vaisala

37 Other forecast relevant map layers available on demand Air Temperature GLD360 Lightning Data Page 37 / date / name / Internal use / Vaisala

38 Traffic Counting Page 38 / date / name / Internal use / Vaisala

39 Alert Function for visibility Page 39 / date / name / Internal use / Vaisala

40 Alert Setting for Slippery Conditions Page 40 / date / name / Internal use / Vaisala

41 Alert Setting for High Winds Page 41 / date / name / Internal use / Vaisala

42 Your total solution for weather management Technology Services End-user applications Measurement instrumentation Communication solutions System design User interface Product services Observation services 24/7 customer commitment Data quality monitoring Customer Training Road weather prediction Ice and snow warning Wind warning Fog warning Route Optimization Rain warning Thermal Mapping Page 42 / date / name / Internal use / Vaisala

43 We are ready are you? Page 43 / date / name / Internal use / Vaisala

44 Page 44 / date / name / Internal use / Vaisala Thank you

ROAD WEATHER AND WINTER MAINTENANCE

ROAD WEATHER AND WINTER MAINTENANCE Road Traffic Technology ROAD WEATHER AND WINTER MAINTENANCE METIS SSWM WMi ROAD WEATHER STATIONS ADVANCED ROAD WEATHER INFORMATION SYSTEM MAINTENANCE DECISION SUPPORT SYSTEM WINTER MAINTENANCE PERFORMANCE

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

EXPLANATION OF WEATHER ELEMENTS AND VARIABLES FOR THE DAVIS VANTAGE PRO 2 MIDSTREAM WEATHER STATION

EXPLANATION OF WEATHER ELEMENTS AND VARIABLES FOR THE DAVIS VANTAGE PRO 2 MIDSTREAM WEATHER STATION EXPLANATION OF WEATHER ELEMENTS AND VARIABLES FOR THE DAVIS VANTAGE PRO 2 MIDSTREAM WEATHER STATION The Weather Envoy consists of two parts: the Davis Vantage Pro 2 Integrated Sensor Suite (ISS) and the

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

CHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles

CHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles CHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles I. Air Temperature: Five important factors influence air temperature: A. Insolation B. Latitude C. Surface types D. Coastal vs. interior

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

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

The Water Cycle Now You See It, Now You Don t

The Water Cycle Now You See It, Now You Don t The Water Cycle Now You See It, Now You Don t Unit: Salinity Patterns & the Water Cycle l Grade Level: Elementary l Time Required: Introduction - 30 min. - Activity as groups 45min Wrap Up 20 min l Content

More information

Pavement Management System Overview

Pavement Management System Overview TABLE OF CONTENTS The Home Screen... 3 The Gutter... 4 Icons... 4 Quick Links... 5 Miscellaneous... 6 PMS Menus... 7 Setup Menu... 7 Construction Setup... 7 1. Material Codes... 8 2. Standard Sections...

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

UNIT VII--ATMOSPHERIC STABILITY AND INSTABILITY

UNIT VII--ATMOSPHERIC STABILITY AND INSTABILITY UNIT VII--ATMOSPHERIC STABILITY AND INSTABILITY The stability or instability of the atmosphere is a concern to firefighters. This unit discusses how changes in the atmosphere affect fire behavior, and

More information

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

Empirical study of the temporal variation of a tropical surface temperature on hourly time integration Global Advanced Research Journal of Physical and Applied Sciences Vol. 4 (1) pp. 051-056, September, 2015 Available online http://www.garj.org/garjpas/index.htm Copyright 2015 Global Advanced Research

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

Read and study the following information. After reading complete the review questions. Clouds

Read and study the following information. After reading complete the review questions. Clouds Name: Pd: Read and study the following information. After reading complete the review questions. Clouds What are clouds? A cloud is a large collection of very tiny droplets of water or ice crystals. The

More information

Basic Climatological Station Metadata Current status. Metadata compiled: 30 JAN 2008. Synoptic Network, Reference Climate Stations

Basic Climatological Station Metadata Current status. Metadata compiled: 30 JAN 2008. Synoptic Network, Reference Climate Stations Station: CAPE OTWAY LIGHTHOUSE Bureau of Meteorology station number: Bureau of Meteorology district name: West Coast State: VIC World Meteorological Organization number: Identification: YCTY Basic Climatological

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

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

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

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

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

Seasonal & Daily Temperatures. Seasons & Sun's Distance. Solstice & Equinox. Seasons & Solar Intensity Seasonal & Daily Temperatures Seasons & Sun's Distance The role of Earth's tilt, revolution, & rotation in causing spatial, seasonal, & daily temperature variations Please read Chapter 3 in Ahrens Figure

More information

Grade 4 Standard 1 Unit Test Water Cycle. Multiple Choice. 1. Where is most water found on Earth? A. in glaciers B. in lakes C. in rivers D.

Grade 4 Standard 1 Unit Test Water Cycle. Multiple Choice. 1. Where is most water found on Earth? A. in glaciers B. in lakes C. in rivers D. Grade 4 Standard 1 Unit Test Water Cycle Multiple Choice 1. Where is most water found on Earth? A. in glaciers B. in lakes C. in rivers D. in oceans 2. What source of energy evaporates the most water from

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

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

Heat and Temperature: Front End Evaluation Report. Joshua Gutwill. October 1999 Heat and Temperature: Front End Evaluation Report Joshua Gutwill October 1999 Keywords: 1 Heat and Temperature Front End Evaluation Report October 28, 1999 Goal:

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

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

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

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

How does snow melt? Principles of snow melt. Energy balance. GEO4430 snow hydrology 21.03.2006. Energy flux onto a unit surface:

How does snow melt? Principles of snow melt. Energy balance. GEO4430 snow hydrology 21.03.2006. Energy flux onto a unit surface: Principles of snow melt How does snow melt? We need energy to melt snow/ ice. GEO443 snow hydrology 21.3.26 E = m L h we s K = ρ h = w w we f E ρ L L f f Thomas V. Schuler t.v.schuler@geo.uio.no E energy

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

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

SECTION 623 CONCRETE BONDING COMPOUND, EPOXY MORTAR AND EPOXY POLYMER CONCRETE OVERLAY SECTION 623.10 CONCRETE BONDING COMPOUND.

SECTION 623 CONCRETE BONDING COMPOUND, EPOXY MORTAR AND EPOXY POLYMER CONCRETE OVERLAY SECTION 623.10 CONCRETE BONDING COMPOUND. SECTION 623 CONCRETE BONDING COMPOUND, EPOXY MORTAR AND EPOXY POLYMER CONCRETE OVERLAY SECTION 623.10 CONCRETE BONDING COMPOUND. 623.10.1 Description. This work shall consist of preparing the surface,

More information

CONDENSATION IN REFRIDGERATED BUILDINGS

CONDENSATION IN REFRIDGERATED BUILDINGS CONDENSATION IN REFRIDGERATED BUILDINGS By: Steve Salisbury Nov. 10, 2010 (revised Nov. 14, 2013) Introduction The following discussion reviews the basic causes of condensation in refrigerated buildings

More information

8.5 Comparing Canadian Climates (Lab)

8.5 Comparing Canadian Climates (Lab) These 3 climate graphs and tables of data show average temperatures and precipitation for each month in Victoria, Winnipeg and Whitehorse: Figure 1.1 Month J F M A M J J A S O N D Year Precipitation 139

More information

EA Technology (UK) EA Technology (UK) NEDL (UK)

EA Technology (UK) EA Technology (UK) NEDL (UK) Optimising Customer Information and the Fault Management Process D C Newis L Roberts John Barnett EA Technology (UK) EA Technology (UK) NEDL (UK) SUMMARY Electricity companies are under increasing pressure

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

Southern AER Atmospheric Education Resource

Southern AER Atmospheric Education Resource Southern AER Atmospheric Education Resource Vol. 9 No. 5 Spring 2003 Editor: Lauren Bell In this issue: g Climate Creations exploring mother nature s remote control for weather and Climate. g Crazy Climate

More information

Section 1 The Earth System

Section 1 The Earth System Section 1 The Earth System Key Concept Earth is a complex system made up of many smaller systems through which matter and energy are continuously cycled. What You Will Learn Energy and matter flow through

More information

MiSP WEATHER WIND SPEED AND DIRECTION Teacher Guide, L1 L3. Introduction

MiSP WEATHER WIND SPEED AND DIRECTION Teacher Guide, L1 L3. Introduction MiSP WEATHER WIND SPEED AND DIRECTION Teacher Guide, L1 L3 Introduction This MiSP unit can be included in a standard weather and climate unit. Some teachers may like it as part of the introduction. Others

More information

6.4 Taigas and Tundras

6.4 Taigas and Tundras 6.4 Taigas and Tundras In this section, you will learn about the largest and coldest biomes on Earth. The taiga is the largest land biome and the tundra is the coldest. The taiga The largest land biome

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

WEATHER, CLIMATE AND ADAPTATIONS OF ANIMALS TO CLIMATE

WEATHER, CLIMATE AND ADAPTATIONS OF ANIMALS TO CLIMATE 7 WEATHER, CLIMATE AND ADAPTATIONS OF ANIMALS TO CLIMATE TEXTBOOK QUESTIONS AND ANSWERS Q.1. Why weather changes so frequently? Ans. All changes in the weather are caused by the sun. The movement of the

More information

Kindergarten Seasons and Weather Assessment

Kindergarten Seasons and Weather Assessment Kindergarten Seasons and Weather Assessment 1a. Circle the pictures that represent the four seasons: snowman going to a teacher harvest fruits colorful flowers the beach 1b. Write the name of the season

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

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

SAFNWC/MSG Cloud type/height. Application for fog/low cloud situations

SAFNWC/MSG Cloud type/height. Application for fog/low cloud situations SAFNWC/MSG Cloud type/height. Application for fog/low cloud situations 22 September 2011 Hervé LE GLEAU, Marcel DERRIEN Centre de météorologie Spatiale. Lannion Météo-France 1 Fog or low level clouds?

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 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

Fog and low cloud ceilings in the northeastern US: climatology and dedicated field study

Fog and low cloud ceilings in the northeastern US: climatology and dedicated field study Fog and low cloud ceilings in the northeastern US: climatology and dedicated field study Robert Tardif National Center for Atmospheric Research Research Applications Laboratory 1 Overview of project Objectives:

More information

Managing Extreme Weather at Transport for London. ARCC Assembly - 12 June 2014 Helen Woolston, Transport for London Sustainability Coordinator

Managing Extreme Weather at Transport for London. ARCC Assembly - 12 June 2014 Helen Woolston, Transport for London Sustainability Coordinator Managing Extreme Weather at Transport for London ARCC Assembly - 12 June 2014 Helen Woolston, Transport for London Sustainability Coordinator Slide list (wont show) Long Term Climate Change 1. What TfL

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

Web Portal Step by Step

Web Portal Step by Step Web Portal Step by Step Topics Getting Started The Dashboard General Information Weather Data Widgets Charting Settings Setting Up My Web Bridge Sharing My Weather Viewing A Friends Weather Weather Select

More information

Improved Meteorological Measurements from Merchant Ships. Peter K. Taylor and Elizabeth C. Kent Southampton Oceanography Centre, UK

Improved Meteorological Measurements from Merchant Ships. Peter K. Taylor and Elizabeth C. Kent Southampton Oceanography Centre, UK Improved Meteorological Measurements from Merchant Ships Peter K. Taylor and Elizabeth C. Kent Southampton Oceanography Centre, UK Summary What Merchant Ship observations do we have? Why improve the Merchant

More information

Please see the Seasonal Changes module description.

Please see the Seasonal Changes module description. Overview Children will measure and graph the precipitation on the playground throughout the year using a rain gauge. Children will also observe satellite images of clouds and begin to investigate how clouds

More information

NIGHT RADIATIVE COOLING The effect of clouds and relative humidity Mike Luciuk

NIGHT RADIATIVE COOLING The effect of clouds and relative humidity Mike Luciuk NIGHT RADIATIVE COOLING The effect of clouds and relative humidity Mike Luciuk We ve all experienced that chilly feeling after sunset on a clear calm night. It seems unusually cold, and, in the winter

More information

ENVIRONMENTAL STRUCTURE AND FUNCTION: CLIMATE SYSTEM Vol. II - Low-Latitude Climate Zones and Climate Types - E.I. Khlebnikova

ENVIRONMENTAL STRUCTURE AND FUNCTION: CLIMATE SYSTEM Vol. II - Low-Latitude Climate Zones and Climate Types - E.I. Khlebnikova LOW-LATITUDE CLIMATE ZONES AND CLIMATE TYPES E.I. Khlebnikova Main Geophysical Observatory, St. Petersburg, Russia Keywords: equatorial continental climate, ITCZ, subequatorial continental (equatorial

More information

Chapter 2, Lesson 5: Changing State Melting

Chapter 2, Lesson 5: Changing State Melting Chapter 2, Lesson 5: Changing State Melting Key Concepts Melting is a process that causes a substance to change from a solid to a liquid. Melting occurs when the molecules of a solid speed up enough that

More information

California Standards Grades 9 12 Boardworks 2009 Science Contents Standards Mapping

California Standards Grades 9 12 Boardworks 2009 Science Contents Standards Mapping California Standards Grades 912 Boardworks 2009 Science Contents Standards Mapping Earth Sciences Earth s Place in the Universe 1. Astronomy and planetary exploration reveal the solar system s structure,

More information

Water & Climate Review

Water & Climate Review Water & Climate Review 1. The cross section below shows the direction of air flowing over a mountain. Points A and B are at the same elevation on opposite sides of the mountain. 4. The graph below shows

More information

Overview of the IR channels and their applications

Overview of the IR channels and their applications Ján Kaňák Slovak Hydrometeorological Institute Jan.kanak@shmu.sk Overview of the IR channels and their applications EUMeTrain, 14 June 2011 Ján Kaňák, SHMÚ 1 Basics in satellite Infrared image interpretation

More information

U s e r M a n u a l. Avalanche Warning Service Eduard-Wallnoefer-Platz 3 A-6020 Innsbruck. Weather stations. 1 The map window: Version 12/2015

U s e r M a n u a l. Avalanche Warning Service Eduard-Wallnoefer-Platz 3 A-6020 Innsbruck. Weather stations. 1 The map window: Version 12/2015 Avalanche Warning Service Eduard-Wallnoefer-Platz 3 A-6020 Innsbruck U s e r M a n u a l Weather stations In this database you will find all available weather stations from currently participating avalanche

More information

Geography affects climate.

Geography affects climate. KEY CONCEPT Climate is a long-term weather pattern. BEFORE, you learned The Sun s energy heats Earth s surface unevenly The atmosphere s temperature changes with altitude Oceans affect wind flow NOW, you

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

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

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

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

BECAUSE WEATHER MATTERS UBIMET

BECAUSE WEATHER MATTERS UBIMET UBIMET Weather Information and Alert Systems for Railroads UBIMET because weather matters One of the largest private weather services in Europe Provides severe weather warnings for more than 1 million

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

HAY MOISTURE & WEATHER:

HAY MOISTURE & WEATHER: HAY MOISTURE & WEATHER: IMPLICATIONS FOR HAY HARVEST Paul Brown Extension Specialist, Biometeorlogy University of Arizona Harvest Losses vs. Moisture From Collins & Owens, 1995 Losses During Haymaking

More information

a) species of plants that require a relatively cool, moist environment tend to grow on poleward-facing slopes.

a) species of plants that require a relatively cool, moist environment tend to grow on poleward-facing slopes. J.D. McAlpine ATMS 611 HMWK #8 a) species of plants that require a relatively cool, moist environment tend to grow on poleward-facing slopes. These sides of the slopes will tend to have less average solar

More information

Order of the Weather Experiments

Order of the Weather Experiments Order of the Weather Experiments 1. Staying Dry Towel in bottle--student i. Magic Air Pushing the stick down-- Student ii. Air Power Water in funnel--teacher 2. Tipping the Scale Weighing air--student

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

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

Cumulifor m clouds develop as air slowly rises over Lake Powell in Utah.

Cumulifor m clouds develop as air slowly rises over Lake Powell in Utah. Cumulifor m clouds develop as air slowly rises over Lake Powell in Utah. Figure 6.1 Dew forms on clear nightswhen objects on the surface cool to a temperature below the dew point. If these beads of water

More information

In most cases problem images are caused by the environment. Here are some of the most common issues:

In most cases problem images are caused by the environment. Here are some of the most common issues: PROBLEM IMAGES In most cases problem images are caused by the environment. Here are some of the most common issues: Rain, snow, & condensation will distort images Light levels can change the apparent color

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

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

Fog and Cloud Development. Bows and Flows of Angel Hair

Fog and Cloud Development. Bows and Flows of Angel Hair Fog and Cloud Development Bows and Flows of Angel Hair 1 Ch. 5: Condensation Achieving Saturation Evaporation Cooling of Air Adiabatic and Diabatic Processes Lapse Rates Condensation Condensation Nuclei

More information

Solvent Cementing Instructions For Plastic Pipe & Fittings

Solvent Cementing Instructions For Plastic Pipe & Fittings Solvent Cementing Instructions For Plastic Pipe & Fittings Description Solvent cementing is the process of fusing plastic pipe and fittings by the use of an adhesive containing a suitable active solvent

More information

Water Cycle Unit Test

Water Cycle Unit Test Name: Multiple Choice (2 pts each): 1. What is the source of energy for all parts of the water cycle? A. Wind B. The Ocean C. Soil D. The Sun 2. Which of the following processes would result in water pollution?

More information

THIRD GRADE WEATHER 1 WEEK LESSON PLANS AND ACTIVITIES

THIRD GRADE WEATHER 1 WEEK LESSON PLANS AND ACTIVITIES THIRD GRADE WEATHER 1 WEEK LESSON PLANS AND ACTIVITIES WATER CYCLE OVERVIEW OF THIRD GRADE WATER WEEK 1. PRE: Comparing the different components of the water cycle. LAB: Contrasting water with hydrogen

More information

ATM S 111, Global Warming: Understanding the Forecast

ATM S 111, Global Warming: Understanding the Forecast ATM S 111, Global Warming: Understanding the Forecast DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 1: OCTOBER 1, 2015 Outline How exactly the Sun heats the Earth How strong? Important concept

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

The Clouds Outside My Window. National Weather Service NOAA

The Clouds Outside My Window. National Weather Service NOAA The Clouds Outside My Window National Weather Service NOAA The Clouds Out My Window Written and illustrated by John Jensenius My window With help from Owlie Skywarn 1 The Clouds Outside My Window Whether

More information

Please be sure to save a copy of this activity to your computer!

Please be sure to save a copy of this activity to your computer! Thank you for your purchase Please be sure to save a copy of this activity to your computer! This activity is copyrighted by AIMS Education Foundation. All rights reserved. No part of this work may be

More information

EMERGENCY ACTION PLAN. for

EMERGENCY ACTION PLAN. for EMERGENCY ACTION PLAN for Facility Name: Facility Address: DATE PREPARED: / / EMERGENCY PERSONNEL NAMES AND PHONE NUMBERS EMERGENCY COORDINATOR: Name: Phone: ( ) AREA MONITORS (If applicable): Area: Name:

More information

(Walter Glogowski, Chaz Shapiro & Reid Sherman) INTRODUCTION

(Walter Glogowski, Chaz Shapiro & Reid Sherman) INTRODUCTION Convection (Walter Glogowski, Chaz Shapiro & Reid Sherman) INTRODUCTION You know from common experience that when there's a difference in temperature between two places close to each other, the temperatures

More information

Technical Note A007 Modbus Gateway Vantage Pro2 25/09/2009 Rev. A 1 de 7

Technical Note A007 Modbus Gateway Vantage Pro2 25/09/2009 Rev. A 1 de 7 1 de 7 1. Introduction This Technical Note explains how to configure the Modbus Gateway for Vantage Pro2. The Modbus Gateway allows the easy connection of a PLC (Programmable Logic Controller), RTU (Remote

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

Summary This lesson will introduce the concept of the water cycle by using a simple demonstration.

Summary This lesson will introduce the concept of the water cycle by using a simple demonstration. Partnerships Implementing Engineering Education Worcester Polytechnic Institute Worcester Public Schools Supported by: National Science Foundation Weather: 4.H.3 Water Cycle Grade Level 4 Sessions Seasonality

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

Wireless Soil Moisture and Weather Monitoring System Caipos

Wireless Soil Moisture and Weather Monitoring System Caipos Wireless Soil Moisture and Weather Monitoring System Caipos System Overview Soil moisture and weather monitoring systems Caipos System Overview Caipos consists of base station, sensors and web application.

More information

HEATING OF DOMESTIC OUTDOOR SWIMMING POOLS

HEATING OF DOMESTIC OUTDOOR SWIMMING POOLS HEATING OF DOMESTIC OUTDOOR SWIMMING POOLS INTRODUCTION 1. There are no general EU regulations and standards for outdoor swimming pool heating. Local regulations in the member countries are covering most

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

Weather stations: Providing business critical information

Weather stations: Providing business critical information Weather stations: Providing business critical information As a nation, the U.S. consumes seven percent of the globe s energy, making it the largest energy user in the world by a considerable margin. Weather

More information

Minnesota Comprehensive Assessments-Series III

Minnesota Comprehensive Assessments-Series III Not for student use. Minnesota Comprehensive Assessments-Series III Science Item Sampler Script Grade 8 S ARE NOT SECURE TEST MATERIALS. THIS ITEM SAMPLER SCRIPT MAY BE COPIED OR DUPLICATED. MINNESOTA

More information

Floods are too much water on normally dry land. Rivers can flood after heavy rain has fallen over a long period of time. River flooding can last

Floods are too much water on normally dry land. Rivers can flood after heavy rain has fallen over a long period of time. River flooding can last Floods are too much water on normally dry land. Rivers can flood after heavy rain has fallen over a long period of time. River flooding can last weeks or longer. River floods usually occur slowly enough

More information

Driving in Fog, Rain and Wind for School Bus Drivers. Reference Guide and Test

Driving in Fog, Rain and Wind for School Bus Drivers. Reference Guide and Test Driving in Fog, Rain and Wind for School Bus Drivers Reference Guide and Test Introduction Every school year bus drivers are faced with adverse driving conditions. Pounding rain storms, wet slippery roads,

More information

Atmospheric Stability & Cloud Development

Atmospheric Stability & Cloud Development Atmospheric Stability & Cloud Development Stable situations a small change is resisted and the system returns to its previous state Neutral situations a small change is neither resisted nor enlarged Unstable

More information

ORANGE PUBLIC SCHOOLS OFFICE OF CURRICULUM AND INSTRUCTION OFFICE OF SCIENCE. GRADE 6 SCIENCE Post - Assessment

ORANGE PUBLIC SCHOOLS OFFICE OF CURRICULUM AND INSTRUCTION OFFICE OF SCIENCE. GRADE 6 SCIENCE Post - Assessment ORANGE PUBLIC SCHOOLS OFFICE OF CURRICULUM AND INSTRUCTION OFFICE OF SCIENCE GRADE 6 SCIENCE Post - Assessment School Year 2013-2014 Directions for Grade 6 Post-Assessment The Grade 6 Post-Assessment is

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

IBM Big Green Innovations Environmental R&D and Services

IBM Big Green Innovations Environmental R&D and Services IBM Big Green Innovations Environmental R&D and Services Smart Weather Modelling Local Area Precision Forecasting for Weather-Sensitive Business Operations (e.g. Smart Grids) Lloyd A. Treinish Project

More information