1 What Is Climate?

Total Page:16

File Type:pdf, Size:1020Kb

1 What Is Climate? Name Class Date CHAPTER 17 Climate SECTION 1 What Is Climate? National Science BEFORE YOU READ Education Standards After you read this section, you should be able to answer ES 1f, 1j, 3d these questions: • What is climate? • What factors affect climate? • How do climates differ around the world? What Is Climate? How is weather different from climate? Weather is STUDY TIP the condition of the atmosphere at a certain time. The Ask Questions As you read weather can change from day to day. In contrast, climate this section, write down any questions that you have. describes the average weather conditions in a region over When you fi nish reading, talk a long period of time. The climate of an area includes the about your questions in a area’s average temperature and amount of precipitation. small group. Different parts of the world have different climates. What Factors Affect Climate? Climate is mainly determined by temperature and pre- cipitation. Many factors affect temperature and precipi- tation, including latitude, wind patterns, landforms, and ocean currents. READING CHECK 1. List What are the two SOLAR ENERGY AND LATITUDE main things that determine Remember that the latitude of an area is its distance climate? north or south of the equator. In general, the temperature of an area depends on its latitude. Latitudes closer to the poles tend to have colder climates. Latitude affects tem- perature because latitude determines how much direct solar energy an area gets, as shown in the figure below. 4HESUNSRAYSTRAVELINPARALLEL STRAIGHTLINES 4HESUNSRAYSHITTHEEQUATOR ATNEARLYAANGLE4HE ENERGYISFOCUSEDONASMALL AREAOF%ARTH4HESMALLAREA ABSORBSALLOFTHEENERGY SO ITTENDSTOHAVEHIGH TAKE A LOOK TEMPERATURES 2. Explain Why do areas %QUATOR 4HESUNSRAYSHITTHEPOLESAT near the equator tend to ASMALLERANGLETHANATTHE EQUATOR4HEENERGYISSPREAD have high temperatures? OVERALARGERAREA%ACHPART OFTHEAREAABSORBSLESS ENERGY SOTHEAREATENDSTO HAVELOWTEMPERATURES Copyright © by Holt, Rinehart and Winston. All rights reserved. Interactive Textbook 325 Climate Name Class Date SECTION 1 What Is Climate? continued STANDARDS CHECK LATITUDE AND SEASONS ES 3d The sun is the major Most places in the United States have four seasons source of energy for phenomena during the year. However, some places in the world do on the earth’s surface, such as growth of plants, winds, ocean not have such large seasonal changes. For example, currents, and the water cycle. places near the equator have about the same tempera- Seasons result from variations in the amount of the sun’s energy tures and amounts of daylight all year. hitting the surface, due to the tilt Seasons happen because Earth is tilted on its axis by of the earth’s rotation on its axis and the length of the day. about 23.5°. This tilt affects how much solar energy an area gets as Earth orbits the sun. The figure below shows Word Help: major of great importance or how Earth’s tilt affects the seasons. large scale Winter During its winter, the Northern Hemisphere is tilted Word Help: energy away from the sun. It receives less the ability to make things direct sunlight than the Southern Hemisphere. Therefore, the North- happen ern Hemisphere experiences lower March 21 temperatures and shorter days. Word Help: phenomenon Spring any fact or event that December 21 June 21 can be sensed or described Winter scientifi cally (plural, Summer phenomena) September 22 Summer During its summer, the Fall Northern Hemisphere is tilted toward the 3. Explain Why don’t sun. It receives more direct sunlight than areas near the equator the Southern Hemisphere. Therefore, Areas near the equator do not tilt the Northern Hemisphere experiences toward or away from the sun very much. have large seasonal warmer temperatures and longer days. Therefore, they do not experience large changes in weather? changes in weather during the year. PREVAILING WINDS Prevailing winds are winds that blow mainly in one direction. The wind patterns on Earth are caused by the uneven heating of Earth’s surface. This uneven heating forms areas with different air pressures. Wind forms when air moves from areas of high pressure to areas of READING CHECK low pressure. 4. Identify What causes Prevailing winds affect climate and weather because wind to form? they move solar energy from one place to another. This can cause the temperature in one place to decrease and the temperature in another place to increase. Prevailing winds also affect the amount of precipita- tion an area gets. They can carry water vapor away from the oceans. The water vapor can condense and fall to the land somewhere far from the ocean. The figure on top of the next page shows the major prevailing winds on Earth. Notice that most prevailing winds blow from west to east or from east to west. Copyright © by Holt, Rinehart and Winston. All rights reserved. Interactive Textbook 326 Climate Name Class Date SECTION 1 What Is Climate? continued 90°N PolarPolar easterlies easterlies 60°N PrevailingPrevailing westerlies 30°N Trade windswinds Trade winds 0° Equator Trade windswinds Trade winds 30°S TAKE A LOOK PrevailingPrevailing westerlies 5. Read a Map In which 60°S direction do the Prevailing Westerlies blow? PolarPolar easterlies easterlies 90°S Wind direction TOPOGRAPHY The sizes and shapes of the land-surface features of a region form its topography. The topography of an area affects its climate because topography can affect temperature and precipitation. For example, elevation is a feature of topography that can have a large impact on temperature. Elevation is the height of an area above sea level. As elevation increases, temperature tends to decrease. READING CHECK Mountains can also affect precipitation. As air rises to 6. Describe In general, move over a mountain, it cools. The cool air condenses, how does elevation affect forming clouds. Precipitation may fall. This process temperature? causes the rain-shadow effect, which is illustrated in the figure below. Air rises to flow over mountains. The air cools as The air on this side of the mountain it rises, and water vapor can condense to form contains much less water vapor. As clouds. The clouds can release the water as pre- the air sinks down the side of the cipitation. Therefore, this side of the mountain mountain, it becomes warmer. The tends to be wetter, with more vegetation. warm air absorbs moisture from the land. Therefore, this side of the mountain tends to be drier and more desert-like. TAKE A LOOK 7. Explain Why do clouds form as air moves over a mountain? Copyright © by Holt, Rinehart and Winston. All rights reserved. Interactive Textbook 327 Climate Name Class Date SECTION 1 What Is Climate? continued LARGE WATER BODIES Large bodies of water can affect an area’s climate. Water absorbs and releases heat more slowly than land. This quality helps regulate the air temperature over the land nearby. This is why sudden temperature changes are READING CHECK not very common in areas near large bodies of water. 8. Explain Why aren’t An example of this effect is the climate of Michigan. sudden temperature Michigan is surrounded by the Great Lakes. It has more- changes common near large moderate temperatures than other places at the same bodies of water? latitude. However, the lakes also increase the humidity of the air. This can cause heavy snowfalls in the winter. OCEAN CURRENTS Surface currents can have a big effect on a region’s climate. Surface currents are paths of flowing water found near the surface of the ocean. As surface currents move, they carry warm or cool water to different places. Critical Thinking The temperature of the water affects the temperature of the air above it. For example, warm currents can heat the 9. Describe Processes Cool surface currents can surrounding air. cause the air above them to An example of the effects of ocean currents on climate become cooler. Explain how can be seen in Iceland. Iceland is an island near the Arctic this happens. Circle. The Gulf Stream, a warm surface current, flows past Iceland. The warm water in the Gulf Stream causes Iceland’s climate to be fairly mild. In contrast, the island of Greenland is at a similar latitude but is not affected by the Gulf Stream. Greenland’s climate is much colder than Iceland’s. Arctic Ocean North Europe America North Asia Pacific North Ocean Atlantic Ocean Africa Equator South America Indian Ocean Australia TAKE A LOOK South South Pacific Atlantic 10. Identify What kind Ocean Ocean of surface current is found off the East Coast of the Antarctica United States? Warm current Cold current Copyright © by Holt, Rinehart and Winston. All rights reserved. Interactive Textbook 328 Climate Name Class Date SECTION 1 What Is Climate? continued What Are the Different Climates Around the World? Earth has three major climate zones: tropical, temper- ate, and polar. The figure below shows where these zones are found. Polar 66.5°N Temperate 23.5°N Tropical Earth’s three major climate zones 0° are determined by latitude. Tropical TAKE A LOOK 23.5°S 11. Identify What Temperate determines Earth’s major climate zones? 66.5°S Polar Each climate zone has a certain range of temperatures. The tropical zone, near the equator, has the highest tem- peratures. The polar zones, located at latitudes above 66.5°, have the lowest temperatures. READING CHECK 12. Describe Which BIOMES climate zone has the highest Each climate zone contains several different kinds of temperatures? climates. The different climates are the result of topography, winds, and ocean currents. The different climates affect the organisms that live in an area. A large area with a certain climate and types of organisms is called a biome. READING CHECK 13. Identify Relationships How are biomes and climate related? Equator Polar ice Temperate grassland TAKE A LOOK Tundra Savanna 14.
Recommended publications
  • Rain Shadows
    WEB TUTORIAL 24.2 Rain Shadows Text Sections Section 24.4 Earth's Physical Environment, p. 428 Introduction Atmospheric circulation patterns strongly influence the Earth's climate. Although there are distinct global patterns, local variations can be explained by factors such as the presence of absence of mountain ranges. In this tutorial we will examine the effects on climate of a mountain range like the Andes of South America. Learning Objectives • Understand the effects that topography can have on climate. • Know what a rain shadow is. Narration Rain Shadows Why might the communities at a certain latitude in South America differ from those at a similar latitude in Africa? For example, how does the distribution of deserts on the western side of South America differ from the distribution seen in Africa? What might account for this difference? Unlike the deserts of Africa, the Atacama Desert in Chile is a result of topography. The Andes mountain chain extends the length of South America and has a pro- nounced influence on climate, disrupting the tidy latitudinal patterns that we see in Africa. Let's look at the effects on climate of a mountain range like the Andes. The prevailing winds—which, in the Andes, come from the southeast—reach the foot of the mountains carrying warm, moist air. As the air mass moves up the wind- ward side of the range, it expands because of the reduced pressure of the column of air above it. The rising air mass cools and can no longer hold as much water vapor. The water vapor condenses into clouds and results in precipitation in the form of rain and snow, which fall on the windward slope.
    [Show full text]
  • Hurricane Paths: Comparing Places with Different Prevailing Winds
    Name ___________________________ Hurricane Paths: Comparing Places with Different Prevailing Winds To understand where hurricanes usually start and what direction they usually move, it helps to have a clear mental image of the pattern of prevailing winds in the world. One way to get this image is to make a careful comparison of wind observations in several places. The diagrams on the right are examples of a special kind of graph called a wind rose. The number in the center indicates the percentage of time the air is calm (no wind). Each of the eight lines radiating away from the center shows the percentage of time the wind blows FROM that direction. Repeat: The lines point to the direction the wind is blowing FROM. Please answer the following questions. 1) According to the map above, Boston has calm air about 12% of the time; the percentage of time San Juan, Puerto Rico, has calm air is _____ . 2) In San Juan, the wind blows the largest percentage of time from the northeast; in Boston, the wind blows from the _________ more often than from any other direction. 3) Use the wind rose graphs on pages 2 and 3. To get an idea about the net zonal flow of air in each location, add up the total percentage of time the wind blows from the southwest, west, and northwest, and subtract the total percentage from the southeast, east, and northeast total percentage. The result is the net westerly component - it is a positive number if the flow is mainly westerly (from the west), and a negative number if the flow is easterly (from the east).
    [Show full text]
  • Prevailing Wind Park Energy Facility Draft Environmental Assessment
    Prevailing Wind Park Energy Facility Draft Environmental Assessment DOE/EA-2061 January 2019 Prevailing Wind Park Energy Facility Draft Environmental Assessment Bon Homme, Charles Mix, Hutchinson, and Yankton Counties, South Dakota U.S. Department of Energy Western Area Power Administration DOE/EA-2061 January 2019 Prevailing Wind Park Draft EA Table of Contents TABLE OF CONTENTS Page No. 1.0 INTRODUCTION ............................................................................................... 1-1 1.1 WAPA’s Purpose and Need ................................................................................. 1-3 1.2 Prevailing Wind Park’s Goals and Objectives ..................................................... 1-3 2.0 DESCRIPTION OF PROPOSED ACTION AND NO ACTION ALTERNATIVES ............................................................................................... 2-1 2.1 Proposed Action ................................................................................................... 2-1 2.1.1 Prevailing Wind Park Project ................................................................ 2-1 2.1.2 Project Life Cycle ................................................................................. 2-5 2.2 No Action Alternative .......................................................................................... 2-5 3.0 AFFECTED ENVIRONMENT ............................................................................ 3-1 3.1 Land Cover and Land Use ..................................................................................
    [Show full text]
  • FINAL REPORT Wind Assessment For: BANKSTOWN
    FINAL REPORT Wind Assessment for: BANKSTOWN COMPASS CENTRE 83-99 North Terrace & 62 The Mall, Bankstown Sydney, NSW 2200, Australia Prepared for: Fioson Pty Ltd L34, 225 George St Sydney NSW 2000 CPP Project: 8759 October 2016 Prepared by: Thomas Evans, Engineer Graeme Wood, Ph.D., Director CPP Project 8759 Executive Summary This report provides an opinion based qualitative assessment of the impact of the proposed Bankstown Compass Centre development on the local pedestrian-level wind environment. This assessment is based on knowledge of the local Bankstown wind climate and previous wind- tunnel test on similar buildings in the Bankstown area. The proposed development is taller than surrounding buildings. Wind speeds are expected to be higher around the outer corners of the development, though the podium roof will prevent significant wind effects occurring at street level. The environmental wind conditions at ground level around the proposed development are expected to be suitable for pedestrian standing from a comfort perspective and pass the distress criterion. Within the development, wind conditions are expected to be suitable for pedestrian standing or walking activities and pass the distress criterion under Lawson. For such a large development with several similar sized towers designed in such a complex manner, it would be recommended to quantify the wind conditions and confirm the qualitative findings using wind-tunnel testing. ii CPP Project 8759 DOCUMENT VERIFICATION Prepared Checked Approved Date Revision by by by 04/02/16 Final Report KF GSW GSW 10/02/16 Revision 1 KF GSW GSW 04/10/16 Amended design drawings TE GSW GSW 05/10/16 Amended Figure TE GSW GSW TABLE OF CONTENTS Executive Summary ...............................................................................................................................
    [Show full text]
  • T5.1 the Dynamics of Nova Scotia's Climate
    PAGE .............................................................. 94 ▼ T5.1 THE DYNAMICS OF NOVA SCOTIA’S CLIMATE The main features of Nova Scotia’s climate are am- MAJOR AIR MASSES ple and reliable precipitation, a fairly wide but not extreme temperature range, a late and short sum- Satellite photography, computer modelling, a greater mer, skies that are often cloudy or overcast, frequent knowledge of the structure of weather systems and a coastal fog and marked changeability of weather better understanding of the physical processes that from day to day. These features can be related to four control our weather have all led to a much-reduced basic factors: use of air-mass concepts. Air-mass theory is still 1. the prevailing westerly winds used descriptively, however, and is very useful to 2. the interactions between the three main air introduce people to the disciplines of meteorology masses which converge on the east coast and climatology. 3. Nova Scotia’s position astride the routes of the Much of the variability of the weather is caused by major eastward-moving storms the shifting positions of the three main air masses T5.1 4. the modifying influence of the sea that dominate the eastern seaboard. Continental The Dynamics of arctic air from the northwest is very dry and cold in Nova Scotia’s WIND SYSTEMS winter. Maritime polar air, moving in from the north Climate or northeast, has been somewhat warmed by its The basic eastward movement of the wind systems passage over the ocean and is cool and moist. Mari- (known as the westerlies) over North America is a time tropical air from the south or southwest is warm result of the general circulation of warm air from the and moist.
    [Show full text]
  • Global Wind Patterns
    NAME: _______________________________________________________________ PERIOD: ___________ DATE: _______EN GLOBAL WIND PATTERNS The most common wind direction is called the prevailing winds. When Columbus set sail for Asia (and “discovered” the Americas) he utilized the prevailing winds. He knew that at about 20° north latitude he would find dependable winds from the north-east which would carry his ships quickly westward across the Atlantic Ocean. On his return, he sailed northward to the zone of prevailing westerlies, that ferried him back to Europe. (See the diagram below.) These wind belts soon became the avenues of the triangular trade routes. Merchants from England sent manufactured items to Africa, where they were traded for negro slaves. The slaves were sailed across the Atlantic on the north-east trade winds. In the Americas, the slaves were traded for rum and cotton, which were shipped to England on the prevailing westerlies farther to the north. The rum and cotton were sold in England for a considerable profit to the owners and investors. The north-east trade winds and the mid-latitude westerlies are two zones of the world wide pattern of prevailing winds. 1. Why did Columbus sail south along Africa before he sailed west to the Americas? 2. What do we call winds from the most common wind direction? 3. Winds are heat flow by . If the Earth were not in motion, the world wide pattern of winds would be very simple. As this diagram shows, we would have two giant convection cells. Warm, moist air would rise at the equator and travel toward the poles.
    [Show full text]
  • Chapter 6 Climate
    Chapter 6 Climate Climate . Canada's climate is not as cold all year around as some may believe. In winter, temperatures fall below freezing point throughout most of Canada. But the south- western coast has a relatively mild climate. Along the Arctic Circle, mean temperatures are below freezing for seven months a year. Climate . During the summer months the southern provinces often experience high levels of humidity and temperatures that can surpass 30 degrees Celsius regularly. Western and south-eastern Canada experience high rainfall, but the Prairies are dry with 250 mm to 500 mm of rain every year. Weather/Climate . Weather – Is the result of the day-to-day conditions of the atmosphere. Climate – A long term pattern of weather – Climate Is The Weather + Weather + More Weather . Climate is what you expect, weather is what you get! Weather . Types of things given in a weather forecast: – Temperature Precipitation – Humidity Wind speed/direction – Cloud cover Air pressure Climate . Factors that affect climate (J.BLOWER); – Jet Stream (air masses) – Bodies of water – Latitude – Ocean Currents – Winds – Elevation – Relief . Note: Different parts of Canada have different climates. Factors that affect Climate A. Jet Stream (Air Masses) Air Masses -- is a large body of air that has similar temperature and moisture properties throughout. For example: Winds blowing from a cold region will bring cold temperature conditions to an area over which they pass Factors that affect Climate . B. Bodies of water – Water warms up more slowly than land and cools off more slowly – As a result of this, land near bodies of water are affected by the weather over these bodies of water.
    [Show full text]
  • FOSS Weather and Water Course Vocabulary/Glossary Terms Second Edition © 2014 Investigations Guide Vocabulary Investigation 1
    FOSS Weather and Water Course Vocabulary/Glossary Terms Second Edition © 2014 Investigations Guide Vocabulary Investigation 1: What Is Weather? Investigation 4: Convection air pressure convection climate convection cell forecast energy transfer humidity fluid meteorologist model meteorology precipitation Investigation 5: Heat Transfer prediction absorb severe weather climatologist temperature climatology weather differential heating wind evidence heat Investigation 2: Where’s the Air? latitude air radiant energy atmosphere radiation compress ray exosphere solar angle expand wave mass matter Investigation 6: Air Flow mesosphere air mass particle conduction permanent gas Coriolis effect pressure jet stream state land breeze stratosphere prevailing winds thermosphere sea breeze troposphere variable gas Investigation 7: Water in the Air weight condensation condensation nucleus Investigation 3: Air Pressure and Wind dew point atmospheric pressure evaporation bar precipitation barometer saturated density transpiration equilibrium isobar Investigation 8: Meteorology kinetic energy cold front millibar (mb) radiosonde warm front FOSS Weather and Water, Second Edition: Course Vocabulary/Glossary Terms 1 of 4 Investigation 9: The Water Planet El Niño groundwater gyre ocean current salinity water cycle Investigation 10: Climate over Time carbon dioxide carbon sequestration climate change emission global warming greenhouse effect greenhouse gas ice core infrared paleoclimatology pollutant FOSS Weather and Water, Second Edition: Course Vocabulary/Glossary
    [Show full text]
  • Climatology of Tropical Cyclones in New England and Their Impact at the Blue Hill Observatory, 1851-2012
    Climatology of Tropical Cyclones in New England and Their Impact at the Blue Hill Observatory, 1851-2012 Michael J. Iacono Blue Hill Meteorological Observatory Updated September 2013 Introduction Over the past four centuries, extreme hurricanes have occurred in New England at intervals of roughly 150 years, as evidenced by the three powerful storms of 1635, 1815, and 1938. Histories and personal accounts of these infamous hurricanes make for fascinating reading (Ludlum, 1963; Minsinger, 1988), and they serve as an important reminder of the devastating impact that tropical cyclones can have in the Northeast. Most tropical systems in New England are less damaging, but they can still disrupt our daily lives with strong winds, heavy rain, and flooding. This article, which updates an earlier report in the Blue Hill Observatory Bulletin (Iacono, 2001), will describe the climatology of all 250 tropical cyclones that have affected New England since the mid-19th century and will summarize their intensity, frequency, and specific meteorological impact at the Blue Hill Observatory. A hurricane is a self-sustaining atmospheric process in which sunlight, water, and wind combine to transfer energy from the tropics to higher latitudes. The uneven distribution of solar heating at the Earth’s surface ultimately drives much of our weather as the atmosphere continually circulates to equalize the tropical warmth and the polar cold. In the tropics, this process is normally tranquil and slow, brought about through the life cycles of individual thunderstorms, the prevailing winds, and ocean currents. However, under the right conditions very warm air and water in the tropics trigger the formation of the most efficient heat transfer mechanism available to the atmosphere: a hurricane.
    [Show full text]
  • Wind Environment Statement West Melbourne Waterfront Precinct
    WIND ENVIRONMENT STATEMENT WEST MELBOURNE WATERFRONT PRECINCT WC721-01F02(REV2)- WS REPORT 16 SEPTEMBER 2015 Prepared for: WMW Developments Pty Ltd C/- Perri Projects Level 10, 60 Albert Road South Melbourne VIC 3205 Attention: Ms Lucy Simms WINDTECH Consultants Pty Ltd ABN 72 050 574 037 Melbourne Office: Suite 218, 87 Gladstone Street, South Melbourne VIC 3205 Australia P +61 3 9329 5132 E [email protected] W www.windtech.com.au Sydney (Head Office) | Abu Dhabi | London | Melbourne | Mumbai | New York | Shanghai | Singapore DOCUMENT CONTROL Non- Reviewed & Issued Prepared By Instructed By Date Revision History Issued Authorised by Revision (initials) (initials) Revision (initials) 01/09/2015 Initial - 0 KP TR KP 08/09/2015 Comments - 1 KP TR KP 15/09/2015 Comfort Criteria - 2 KP TR KP 16/9/2015 Comments 3 KP TR KP The work presented in this document was carried out in accordance with the Windtech Consultants Quality Assurance System, which is based on International Standard ISO 9001. This document is issued subject to review and authorisation by the Team Leader noted by the initials printed in the last column above. If no initials appear, this document shall be considered as preliminary or draft only and no reliance shall be placed upon it other than for information to be verified later. This document is prepared for our Client's particular requirements which are based on a specific brief with limitations as agreed to with the Client. It is not intended for and should not be relied upon by a third party and no responsibility is undertaken to any third party without prior consent provided by Windtech Consultants Pty Ltd.
    [Show full text]
  • 16 Tropical Cyclones
    Copyright © 2017 by Roland Stull. Practical Meteorology: An Algebra-based Survey of Atmospheric Science. v1.02 16 TROPICAL CYCLONES Contents Intense synoptic-scale cyclones in the tropics are called tropical cyclones. As for all cyclones, trop- 16.1. Tropical Cyclone Structure 604 ical cyclones have low pressure in the cyclone center 16.2. Intensity & Geographic distribution 605 near sea level. Low-altitude winds also rotate cy- 16.2.1. Saffir-Simpson Hurricane Wind Scale 605 clonically (counterclockwise in the N. Hemisphere) 16.2.2. Typhoon Intensity Scales 607 around these storms and spiral in towards their cen- 16.2.3. Other Tropical-Cyclone Scales 607 ters. 16.2.4. Geographic Distribution and Movement 607 Tropical cyclones are called hurricanes over 16.3. Evolution 608 the Atlantic and eastern Pacific Oceans, the Carib- 16.3.1. Requirements for Cyclogenesis 608 bean Sea, and the Gulf of Mexico (Fig. 16.1). They 16.3.2. Tropical Cyclone Triggers 610 are called typhoons over the western Pacific. Over 16.3.3. Life Cycle 613 the Indian Ocean and near Australia they are called 16.3.4. Movement/Track 615 cyclones. In this chapter we use “tropical cyclone” 16.3.5. Tropical Cyclolysis 616 to refer to such storms anywhere in the world. 16.4. Dynamics 617 Comparing tropical and extratropical cyclones, 16.4.1. Origin of Initial Rotation 617 tropical cyclones do not have fronts while mid-lati- 16.4.2. Subsequent Spin-up 617 tude cyclones do. Also, tropical cyclones have warm 16.4.3. Inflow and Outflow 618 cores while mid-latitude cyclones have cold cores.
    [Show full text]
  • Hazard: High Winds High Wind Profile
    HAZARD: HIGH WINDS HIGH WIND PROFILE: Wind is essentially the movement of air in response to pressure differences. A pressure gradient force tends to start the flow of air from higher to lower pressure. The stronger the pressure gradient, the stronger the wind. As shown on Figure 28, wind speeds are graded on the Beaufort Scale from 0 (calm) to 12 (hurricane-75 mph). Normally, damage to trees occurs above number 8 (gale force-39 mph on the Beaufort Scale), while structural damage to buildings starts at number 9 (47 mph) with considerable damage to buildings and trees being uprooted at number 10 (55mph). Winds above this speed are seldom experienced inland with the exception of the passage of tornadoes and hurricanes. COUNTY PERSPECTIVE AND PROFILE: Garrett County is situated in the lower part of the westerly wind belt which extends from latitude 35 to latitude 60. Over time, prevailing winds in Garrett County are from the southwest in summer and the northwest in winter. This northwest wind flow in winter has a strong influence over the “Lake Effect” precipitation that brings snow to Garrett County while areas to the east receive little or no precipitation. In winter these winds are very strong and approach gale force on the Beaufort Scale on numerous days from November through April. In addition to strong winds associated with winter “Lake Effect” storms, Garrett County is also subject to high winds associated with thunderstorms and the occasional hurricane or tornado that passes through or near the county. Because of the prevalence of high wind conditions, the local planning committee has ranked high winds as a high risk in Garrett County.
    [Show full text]