Global Warming: Anthropogenic Effects. Systems and Loops A system: a group of independent parts working together as a whole (e.g. human body) Positive.

Slides:



Advertisements
Similar presentations
Dynamics of Climate Change
Advertisements

The Anthropogenic Greenhouse Effect. Anthropogenic: resulting from a human influence Increase of GH gases through human sources is causing an enhanced.
1 The Greenhouse Effect Natural and Anthropogenic.
Weather Review Row 1Row 2Row 3Row 4 Row 5 Row 6Row
Greenhouse Effect How we stay warm. The Sun’s energy reaches Earth through Radiation (heat traveling through Space)
Factors that Influence Climate
Key Words radiation budget electromagnetic spectrum albedo Understand the concept of radiation and heat exchange Outline factors that control incoming.
1 THE CARBON CYCLE AND GLOBAL WARMING. 2 CARBON CYCLE Movement of carbon between the atmosphere, oceans, biosphere, and geosphere Movement of carbon between.
Carbon Cycle VOCABULARY: – Carbon-Greenhouse Effect – Carbon Cycle-Photosynthesis – Consumers-Producers – Decomposers-Respiration – Fossil Fuels.
Chapter 8 – Dynamics of Climate Change
DAILY REVIEW #7 21.Describe 4 different ways that the Sun/Earth relationship changes that have an impact on Earth’s climate. 22. In general, what are.
Key Idea #18 The sun is the major source of energy for events that occur on the surface of the Earth.
S6E2.c. relate the tilt of earth to the distribution of sunlight through the year and its effect on climate.
Chapter 17 Chapter Review Place these notes into your notebook.
By: Kelsey Lewis, Kimmy Parks, Tyler Tucker, Ashley Sun.
Heating of the Atmosphere
Climate Change UNIT 3 Chapter 7: Earth’s Climate System
Geochemical Cycles.
The Greenhouse Effect (8.6). The Greenhouse Effect  How does the climate system trap energy to keep Earth warm?  Gases in the atmosphere absorbed the.
Copyright © 2005 Pearson Education, Inc., publishing as Benjamin Cummings 18 Global Climate Change Part A PowerPoint ® Slides prepared by Jay Withgott.
THE GREENHOUSE EFFECT Greenhouse Gases:  chemical compounds in the atmosphere that trap heat  they retain a proportion of the sun’s heat through the.
Atmosphere & Weather All About Winds.
Key Idea #14 There is a relationship between the warming of the Earth’s atmosphere by the sun and convection within the atmosphere and oceans.
Weather Review. Air Masses Air Mass – A large body of air through which temperature and moisture are the same. Types 1. Continental – formed over land.
UNIT 4:. Lesson 1 – Greenhouse Effect  Introduction to climate and climate change  Greenhouse Effect.
The Atmosphere Preview Section 2 Atmospheric Heating Concept Mapping.
Carbon is an element It is part of oceans, air, rocks, soil and all living things. Carbon doesn’t stay in one place.
THERMAL ENERGY TRANSFER NOTES. THERMAL ENERGY Total amount of energy in an object’s moving molecules. Heat--flow of thermal energy from a warmer object.
Heating of the Atmosphere Chapter 15 Section 2 Mrs. Mannel Earth Science.
ATMOSPHERIC HEATING Day 1. All matter is made of atoms Matter: anything that has mass and occupies space Atom: the smallest particle of a substance that.
Atmosphere & Weather All About Winds. Energy Transfer in the Atmosphere Earth’s energy is provided by the SUN. Energy is important to us because it… 1.Drives.
How does variability in the earth’s physical structure affect the transformations of energy? - albedo of different “spheres”; clouds What is the physical.
Climate Change. Natural Processes That Change Climates  Volcanic Eruptions  The presence of volcanic aerosols (ash, dust, and sulfur-based aerosols),CO.
Atmospheric Heating Radiation Conduction Convection.
The Greenhouse Effect. Greenhouse Effect Radiation from the sun easily penetrates the layer of gases surrounding the Earth (the atmosphere) Some of this.
Aim: How do increased carbon dioxide concentrations on our planet affect life?
Greenhouse Effect How we stay warm. The Sun’s energy reaches Earth through Radiation (heat traveling through Space)
Climate Factors of Climate El Nino Topography Greenhouse Effect
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
The Greenhouse Effect.
Greenhouse Effect How we stay warm.
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
Greenhouse Effect How we stay warm.
Climate Change Carbon Cycle.
Greenhouse Effect How we stay warm.
Greenhouse Effect and Global Warming
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
Energy Transfer in the Climate System
Energy Transfer in the Climate System
Greenhouse Gases & Human Activitites
Greenhouse the effect.
Greenhouse Effect How we stay warm.
Energy Transfer in the Climate System
Greenhouse Effect How we stay warm.
Unit #11: Ecology (Part 5) GEOCHEMICAL CYCLES and CHANGES IN ECOSYSTEMS Ms. Day AP Biology.
The Atmosphere and Weather
Wind circulation through the atmosphere
Section 2 Atmospheric Heating.
THE GREENHOUSE EFFECT Greenhouse Gases:
Warm-up Finish questions from energy budget activity 10.1 quiz.
Greenhouse Effect How we stay warm.
Atmosphere & Weather All About Winds.
Atmosphere & Weather All About Winds.
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
Greenhouse Effect How we stay warm.
2/6 What is the greenhouse effect?.
The Earth in Balance.
Greenhouse.
Climate.
OCEANS And CLIMATE.
Presentation transcript:

Global Warming: Anthropogenic Effects

Systems and Loops A system: a group of independent parts working together as a whole (e.g. human body) Positive Feedback Loop: Part of a systems output is fed back to input and increases effects of interacting parts

Negative Feedback Loops Decrease the effects of interacting parts to maintain equilibrium. To prevent, slow or reverse changes. Keep Homeostatic levels.

Energy Transfer Conduction –Transfer of thermal energy between 2 objects –E.g. metal pot on stove transfers heat from element to water in pot Convection –Transfer of thermal energy by highly energized molecules moving from one place to another. Fluid create currents –E.g. ocean currents, wind currents Radiation –Transfer of thermal energy from the sun to the earth. Electromagnetic radiation can travel through the vacuum of space heating up our planet

Energy Transfer In Oceans Warmer surface water –Heated by radiation –Less dense because warmer water so stays at surface until current takes it N then the air cools it and it sinks (convection) –Moves quickly at surface Cold dense deep water –Moves slowly at bottom of ocean –Pushes warm water our of the way as it sinks –More salty and dense

Ocean currents: Conveyor belts of energy

Cycles of weather El Nino –Heavy rains –Warmer than normal –Warm air brought by Jet streams across the Pacific La Nina –Dry, drought –Cooler than normal –Warm air & cool moisture pushed away from North America Periodic warming & cooling of a huge mass of sea water. Impacts weather in N. America.

El Nino & La Nina

Green House Gases 90% of atmosphere made of N2 and O2. They don’t absorb infrared radiation Water 1-4% CO % Water Vapour –Most abundant greenhouse gas –Not increasing in amount. Humans don’t release more of it

CO2 and Methane Carbon Dioxide –Main source: Animal respiration –Main human source  combustion of fossil fuels and fires –Main sink is plants and photosynthesis –**Deforestation** removes sink factors Methane –Main source  bacteria that breakdown waste matter –Main source  bogs and swamp lands- increase in decomposing matter –Sink  can be collected & used as a fuel –Sink  start eating Kangaroo instead of cow.

Anthropogenic Effects Anthropogenic Greenhouse Effect –Since 1750 humans have increase CO2 levels mostly from burning fossil fuels –Deforestation & Agriculture –Industrial activities –Methane has increase 1045 ppb –CO2 has increase 104 ppb