13.2 Energy Systems.

Slides:



Advertisements
Similar presentations
Energy in the Earth System
Advertisements

Heat Transfer, Greenhouse Effect, Ozone Layer Notes
In the Atmosphere Thermal Energy Transfer. Temperature and Thermal Energy TEMPERATURE - a measure of the average kinetic energy of the individual particles.
Handout (yellow) Solar Energy and the Atmosphere Standard 3 Objective 1 Indicators a, b, and c Standard 3 Objectives 1, 2, and 3 Workbook Pages 3,
Solar Energy & the Atmosphere
Key Words radiation budget electromagnetic spectrum albedo Understand the concept of radiation and heat exchange Outline factors that control incoming.
Energy Flow Through Our Ecosystem
 What does a car need to run?  What does an ipod need to work?  What do we need to survive?  If all these things need a power/energy source, what is.
Objectives Explain how radiant energy reaches Earth.
Climate Long time, Large Area. Weather short term, small area.
Unit 3 Lesson 3 Energy Transfer
The Atmosphere: Energy Transfer & Properties Weather Unit Science 10.
Warm Up 3/6/08 More solar energy reaches the equatorial regions than the polar regions because the equatorial regions a. are covered by a greater area.
13.2 Energy Systems.
Heat Transfer in the Atmosphere Essential Question: How is heat transferred in the atmosphere?
Energy in Ecosystems ALL LIVING THINGS USE ENERGY The earth is SOLAR POWERED! The source of all energy for ecosystems is the Sun.
Chapter 22 Section 2 Handout
Weather and Climate Unit Investigative Science. * All materials are made of particles (atoms and molecules), which are constantly moving in random directions.
Earth’s Energy Budget. Modes of Energy Travel Heat Energy can be transferred in three specific ways: Heat Energy can be transferred in three specific.
In this presentation you will: explore the impact of the Sun’s energy Impact of the Sun’s Energy Next >
ENERGY MOVEMENT THROUGH ECOSYSTEMS Section 1.11 Section 13.2.
Where does the flow of energy in an ecosystem begin? The sun provides the radiant energy necessary for all the organisms in an ecosystem. Autotrophs (or.
AOS 100: Weather and Climate
Unit 9 Section 2: Solar Energy and the Atmosphere
3.1 Heat Transfer in the Atmosphere
Unit 3 Lesson 2 Energy Transfer
Understanding Heat Transfer: Conduction, Convection and Radiation
Radiation, Conduction, Convection
Earth's Energy and Radiation By: May-Lynn Fortune & Maesey Phillips
Understanding Heat Transfer: Conduction, Convection and Radiation
Food Chains, Food Webs, and the Transfer of Energy
Heat in the Atmosphere.
Energy in Ecosystems.
The Sun.
What is Energy? Energy – the ability to do work
Unit 3 Lesson 2 Energy Transfer
Chapter 2; Section 2 Atmospheric Heating
ENERGY IN THE BIOSPHERE
Energy in the Atmosphere
II)Convection in the Mantle
Earth’s Energy Budget.
Solar Energy and the Atmosphere
Chapter 1.10 Energy in Ecosystems
The Atmosphere Weather and Climate
Earth’s Energy Budget.
Energy Transfer in the Atmosphere
The Earth’s energy balance
Understanding Heat Transfer: Conduction, Convection and Radiation
Chapter 2; Section 2 Atmospheric Heating
Energy in the Atmosphere
Weather & Climate.
The Atmosphere and Weather
Earth’s Energy Balance
Section 2: Solar Energy and the Atmosphere
Heating the Atmosphere
Atmospheric Heating Notes
Weather dynamics Day 2 – Heat Science 10.
Chapter 2; Section 2 Atmospheric Heating
Earth’s Energy Balance
Understanding Heat Transfer: Conduction, Convection and Radiation
What Causes Weather? 2009.
Unit 3 Lesson 2 Energy Transfer
Understanding Heat Transfer, Conduction, Convection and Radiation
Energy Flow On Earth.
Do Now Do work sheet.
Solar Energy and the Atmosphere
Energy Movement Through Ecosystems
Understanding Heat Transfer: Conduction, Convection and Radiation
The Sun is the source of energy for the Earth.
Presentation transcript:

13.2 Energy Systems

How Energy is Transferred Energy (heat or light) is transferred in one of the following ways: Radiation Convection Advection Conduction

Radiation The transfer of energy by electromagnetic (light) waves (electromagnetic spectrum) Does not require a medium to travel through (i.e. can travel through a vacuum) Travels in straight lines Is emitted (given off) by all matter The only form of energy given to us by the sun.

Solar Energy Where does it come from? produced by nuclear fusion reactions in the sun How does Solar Energy reach Earth? Radiant energy travels in waves of different energy levels, collectively known as the Electromagnetic Spectrum In order from lowest to highest energy level: Radio Microwave Infrared Visible Ultraviolet X-rays Gamma

Electromagnetic Spectrum

Convection transfer of energy by vertical movement of particles in a fluid (liquid/gas) as the particles gain energy they move faster, take up more space, become less dense, and then can rise through the fluid they are in this can create convection currents this method of heat transfer is very important to weather

Advection Transfer of energy through the collision of particles in a liquid or gas Energy moves horizontally

Conduction the transfer of energy which occurs when a particle with high energy hits a particle with lower energy energy is passed through an object from atom to atom only occurs in solids, since the particles must be close together for frequent collisions to occur readily

What energy is needed to survive on Planet Earth? Hint:

Albedo When solar energy strikes an object, some of the energy is absorbed and some is reflected Albedo is a measurement of the percentage of light which a material will reflect Polar Ice Cap – High or Low? Answer: High Black Roof – High or Low? Answer: Low Bare Soil – High or Low? The higher the albedo, the less energy absorbed.

Heat Capacity: A measure of how much heat a substance must absorb to increase its temperature by 1⁰ C. If a substance absorbs a lot of heat, yet its temperature rises slowly, then it has a high heat capacity. Think of the Yoho Lake & a sandy beach in the summer. they both absorb the same amount of heat The water stays cold because it can absorb a lot of heat without its temperature rising, the sand on the other hand gets very hot.

Heat Sink An object which absorbs energy and becomes warmer. A substance with a high heat capacity makes a good heat sink. Water has a high heat capacity and so is a good heat sink, while rocks have a low heat capacity.

Absorption and Reflection Solar energy entering the atmosphere can be either absorbed or reflected. Both absorption and reflection can occur with the air, clouds and the earth’s surface. approximately 70% in total is absorbed 44% heat the Earth’s land surface and air 25% heat the water and evaporate some water 1% creates wind Less than 1% is used for photosynthesis approximately 30 % is reflected (air 6%, clouds 20%, earth 4%) 30% of the sun’s rays are reflected back and do not reach the Earth 44% of the sun’s rays heat the Earth’s land surface and air 25% heat the water and evaporate some of the water 1% creates wind Less than 1% is used by Photosynthesis.

Why is Solar Energy Important? all forms of life on earth are dependent on solar energy for life needed for plants to grow and to keep earth warm enough for survival Reminder: less than 1% is used by Photosynthesis. PHOTOSYNTHESIS – The process by which green plants use sunlight to produce sugar. CO2 + 2H2O + sunlight ---> O2 + (C6H12O6)n + H2O or... carbon dioxide + water + sunlight ---> oxygen + carbohydrate + water

ENERGY MOVEMENT IN ECOSYSTEMS Chapter 1.11 Chapter 1.11

FOOD WEB – a series of interlocking food chains Of the less than 1% (0.023%), how does the energy disperse throughout food chains and food webs. When talking about food webs and energy, new terms are used to describe producers and consumers/decomposers. FOOD WEB – a series of interlocking food chains When talking about food webs and energy, new terms are used to describe producers and consumers / decomposers

AUTOTROPHS Plants or algae which make their own food using the sun’s energy through photosynthesis. Previously called producers.

HETEROTROPHS Animals, fungi and bacteria that must eat or decompose plants or animals ( and their waste) to get their energy. Previously called consumers / decomposers

WHY NEW TERMS? Each of the feeding levels ( consumer, primary consumer, secondary consumer ) is called a trophic level. Every time something is consumed in a food chain, energy is passed along. However, less and less energy is passed on each time because some of the energy is used for life processes (maintaining body temperature, digestion, growing, movement, etc)

ECOLOGICAL PYRAMID Number of Organisms Decreases Third Trophic level Secondary Consumers Available Energy Decreases Second Trophic Level Primary Consumers First Trophic Level Producers Energy from the Sun

With these new terms and previous old terms we can place labels on organisms within food chains and food webs. Lets look at Handout: Energy loss in a food chain

Energy Loss in Food Chains

ENERGY LOSS IN A FOOD CHAIN The higher the trophic level in the food chain, the more energy is lost. Consuming plants, which are the lowest trophic level, allows for the least amount of energy to be lost.

A SIMPLE FOOD WEB

More Complex Food Web

HOMEWORK TEXT PAGE 39 QUESTIONS: #1-6, 9,10