Temperature WEATHER AND CLIMATE. Temperature refers to the degree of hotness or coldness of the air It varies throughout the day in a place The temperature.

Slides:



Advertisements
Similar presentations
Geography Sec 1 E learning Lesson
Advertisements

Unit 3-4: Air Pressure.
Chapter 10 Atmosphere and Air Pressure The sun provides heat and energy for the Earth. The angle at which sunlight strikes Earth’s surface is called.
Lesson 1: How Does Uneven Heating of Earth Affect Weather?
Mr. Fetch’s Earth Science Classroom. Temperature – a measurement of heat Temperature is a factor of particle motion. Faster moving particles create more.
A Stevenson screen or instrument shelter is a screen to shield meteorological instruments against precipitation and direct heat radiation from outside.
Earth’s Motions, Solar Radiation, and the Seasons
Why the Earth has seasons  Earth revolves in elliptical path around sun every 365 days.  Earth rotates counterclockwise or eastward every 24 hours.
Atmosphere & Climate Change
Thermal Energy.
Atmosphere, Weather and Climate
Lesson Overview 4.1 Climate.
Elements of Weather & Climate
What creates different climates in Canada and what impact does climate have on human activity? The Climates of Canada.
Weather and Climate.
Measuring the weather. Weather and Climate How do you measure the weather?
Thermal Energy Transfers
Air Pressure and Winds Notebook Page 78
Weather Variables.
1 1 Temperature and Thermal Energy Temperature and energy Glencoe: Chapter 9 – Section 1: pages
Chapter 17 Notes: The Atmosphere. What is the Atmosphere? The atmosphere can be defined as the portion of planet earth that contains gas. Weather can.
At ppt Air Pressure CH 15 Prentice Hall p
Weather Temporary behavior of atmosphere (what’s going on at any certain time) Small geographic area Can change rapidly.
THE ENERGY BALANCE AT SURFACE Net Radiation + Sensible Heat + Latent Heat + Ground Heating = 0 1 st LAW OF THERMODYNAMICS (CONSERVATION OF ENERGY): Energy.
Heat in the CH 15 Prentice Hall p CH 15 Prentice Hall p At ppt Atmosphere.
Meteorology Ch 3 Jeopardy
Copyright © 2013 Pearson Education, Inc. The Atmosphere: An Introduction to Meteorology, 12 th By: Lutgens and Tarbuck Lectures by: Heather Gallacher,
Class #2: Seasonal and daily variations in temperature
Atmosphere and Climate ChangeSection 1 Climate average weather conditions in an area over a long period of time. determined by factors that include: latitude,
Objectives Explain the difference between weather and climate.
Backward Forward Home Exit III. How do temperatures change over time and over place? 1. What are some common records of temperature? Mean daily temperatureMean.
Two characteristics of Climate that are most important: 1) The average temperature over the year 2) The annual temperature range (difference between the.
EOY Revision Form 4- Geography 1. The difference between the maximum and minimum temperatures recorded for a place during a period of one day is called.
World Climate Patterns Earth’s Movement in Space.
End Show Slide 1 of 26 Copyright Pearson Prentice Hall 4-1 Climate.
Weather and Climate. How many people know what the weather is going to be the next three days? How do you know? Can you predict the weather?
Section 1: Atmosphere and Climate Change
Climate and Climate Change Environmental Science Spring 2011.
Climate and Climate Change. Lesson 1 Factors Affecting Climate.
WEATHER AND CLIMATE TEMPERATURE. TOPIC 1 - TEMPERATURE Essential QuestionsDefinitionsLearning outcomes A.What is the difference between weather and climate?
Bellringer. Climate Climate is the average weather conditions in an area over a long period of time. – determined by a variety of factors including: latitude,
Day one Chapter 13 Atmosphere and Climate Change
Lesson Overview Lesson OverviewClimate Chapter 4 Ecosystems and Communities 4.1 Climate.
14.1 – Defining Climate. Climatology Study of Earth’s climate and the factors that affect past, present, and future climate changes Long-term weather.
Climate -Climate is the average weather conditions in an area over a long period of time. -Climate is determined by a variety of factors that include latitude,
When people say that it is going to rain, or that it is cold outside, what is the “it” that they are talking about? The “it” refers to the atmosphere.
Factors that Affect Climate Weather is the short term (day to day) conditions of the atmosphere which include: Temperature Temperature Precipitation.
Atmosphere & Climate Change Chapter 13, Section 1: Climate & Climate Change Standards: SCSh2a,b, 3c, 4a, 6a, d.
Thermal Energy & Heat 1.Temperature – The measure of the average kinetic energy of the particles that make up a substance. 2.Temperature Scales – Fahrenheit,
Heat. Nature of Heat Heat is the transfer of energy (every in transit) from one body to another due to the temperature difference between the two bodies.
Chapter 4: Ecosystems & Communities Starting with … Climate (4.1)
DAY ONE Chapter 13 Atmosphere and Climate Change Section 1: Climate and Climate Change.
Factors affecting Temperature
Thermal Energy.
1. Climate Climate is the average weather conditions in an area over a long period of time. Climate is determined by a variety of factors that include.
Unit 2, lesson 2 Temperature
Lesson Overview 4.1 Climate.
Understanding Heat Transfer: Conduction, Convection and Radiation
How does the weather affect your life. What is the weather like today
4.1 Climate Lesson Overview
AIR TEMPERATURE.
Lesson Overview 4.1 Climate.
Lesson Overview 4.1 Climate.
Climate Chapter 4.1.
Lesson Overview 4.1 Climate.
Lesson Overview 4.1 Climate.
Lesson Overview 4.1 Climate.
What creates different climates in Canada and what impact does climate have on human activity? The Climates of Canada.
Lesson Overview 4.1 Climate.
Lesson Overview 4.1 Climate.
Presentation transcript:

Temperature WEATHER AND CLIMATE

Temperature refers to the degree of hotness or coldness of the air It varies throughout the day in a place The temperature rises and falls as the Earth rotates from west to east and it rises during the day and falls at night It also varies from place to place Temperature gets cooler as we go to higher grounds Places nearer the Equator are warmer throughout the year than places farther away from it Elements of Weather: Temperature

Singapore What is the reason for Singapore’s hot climate? Elements of Weather: Temperature

Factors Affecting Temperature 1. Latitude Due to angle of incidence, the sun’s ray travels a shorter distance through the atmosphere and the solar radiation is concentrated on a smaller area These places experience uniform temperatures annually due to the tilt of the earth on its axis and cause these places to face the sun and receive the same radiation all year round. Places at lower latitudes are always hotter than those at higher latitudes

Factors Affecting Temperature 2. Altitude Temperature falls as altitude increases at a rate of 6.5°C/1000m (known as the Normal lapse rate) Air is less dense at higher altitudes -> absorb less long wave radiation -> lower temperatures

Measuring Temperature Air temperature is measured with a thermometer The scale is in degree Celsius (OC) Daily maximum temperature refers to the highest temperature reading for the day Daily minimum temperature refers to the lowest temperature reading for the day Glass tube Mercury or alcohol

Measuring Temperature Maximum temperature is measured by the maximum thermometer It consists of a glass tube containing mercury and a metal index When temperature rises, the mercury expands and pushes the metal index upwards When temperature falls and the mercury contracts, the metal index stays in place

Measuring Temperature The minimum thermometer works in the same way to measure the lowest temperature reading, but contains alcohol instead of mercury The maximum and minimum thermometer, which is also called the U-shaped thermometer, can measure both maximum and minimum temperatures

Six’s Thermometer Six’s Thermometer/U-shaped thermometer left bulbright bulb metal index vacuum alcohol mercury right bulb

Six’s Thermometer When temp increases, both alcohol and mercury expand alcohol in the left limb forces the mercury towards the right limb the mercury pushes the index up in the right limb part of the alcohol in the right limb vaporises and moves into the vacuum end of the index closest to the mercury gives the maximum temperature

Six’s Thermometer When temp decreases, both alcohol and mercury contract alcohol vapour in the right bulb liquifies so that the mercury now flows in the opposite direction and pushes the up the metal index in the left limb end of the index closest to the mercury gives the minimum temperature

Diurnal temperature range Average temperature range Mean monthly temperature Annual range of temperature Mean annual temperature Calculating Temperatures

The mean daily temperature is the average temperature of a place on any one day Formula Mean daily temperature = Daily maximum Daily minimum temperature + temperature 2 The daily temperature range is the difference between the maximum and minimum temperatures recorded in a day Formula Daily temperature range = Daily maximum Daily minimum temperature - temperature Calculating Temperatures

The mean monthly temperature is the average temperature of a place in a month Formula Mean monthly temperature = Sum of mean daily temperatures for the month Number of days in the month The mean annual temperature is the average temperature in a place within a year Formula Mean annual temperature = Sum of mean monthly temperatures in the year 2

Calculating Temperatures The annual temperature range is the difference between the maximum and minimum mean monthly temperatures recorded in a year Formula Annual temperature range = Maximum Minimum mean monthly - mean monthly temperature temperature

Elements of Weather: Temperature Isotherms: lines joining places of equal temperature

Elements of Weather: Temperature Line graph:

Stevenson Screen Instruments used to measure temperature are usually placed in a Stevenson Screen Maximum and minimum thermometers or six’s thermometer and a wet and dry bulb thermometer are kept in the SS. Barometer can also be kept in SS

Stevenson Screen It is made of wood ✓ wood is a poor conductor of heat It is painted white ✓ white paint reflects light so that the box does not heat up excessively Its is a raised 1.2 metres above ground ✓ to minimise the effect heat radiating from the ground

Stevenson Screen The sides and doors have louvres ✓ to allow free air movement in and out of the box direct heat of the Sun It has a double-layered roof with intervening air space ✓ to reduce excessive heating inside the box as air is a good insulator ✓ Where should a stevenson screen be sited?