Unit 5 Seminar Carbon dioxide. The Carbon Cycle Carbon comes into the living world through the plants, algae, and bacteria that take in atmospheric carbon.

Slides:



Advertisements
Similar presentations
Your Name Your Title Your Organization (Line #1) Your Organization (Line #2) Global warming.: Matthieu BERCHER, Master M.I.G.S., University of Burgundy,
Advertisements

Greenhouse Effect How we stay warm. The Sun’s energy reaches Earth through Radiation (heat traveling through Space)
Essential Principles Challenge
Objective: Understand Causes, Effects and Solutions of Global Warming
+ YEAR 10 EARTH AND SPACE SCIENCE (ESS). + EARTH & SPACE SCIENCE 2 parts to the unit: EARTH – Global systems & SPACE – Origins of the universe We’re going.
1 THE CARBON CYCLE AND GLOBAL WARMING. 2 CARBON CYCLE Movement of carbon between the atmosphere, oceans, biosphere, and geosphere Movement of carbon between.
IB BIOLOGY 5.2 The greenhouse effect. The Carbon Cycle Carbon exists in many forms:  Atmospheric gases (CO2 and Methane- CH4)  Dissolved CO2 in aquatic.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Ozone & Greenhouse Effect. What is Ozone? Ozone is a molecule that occurs in the Stratosphere Ozone absorbs harmful UV rays from the sun O 3 + uv O 2.
Earth Science Chapter 11.2 Climate Change.
Global warming.
Geochemical Cycles Science Biological Processes Involved 1.Photosynthesis –Plants convert CO 2 and H 2 O into O 2 and sugar 6CO 2 + 6H 2 O + energy.
Causes Effects Solutions
May 10th, 2007 HW: Textbook- Read p , #’s 1-4 Do Now: Do you think that we need Earth to be warmed? Aim: What is the greenhouse effect and how.
24 Global Ecology. Figure 24.2 A Record of Coral Reef Decline.
Carbon Cycle Gr 9 Science. Carbon Cycle Fourth most abundant element in universe Building block of all living things Main Pathway– in and out of living.
Carbon Cycle The carbon cycle is the biogeochemical cycle by which carbon is exchanged between the biosphere and living organisms. Carbon is an essential.
THE CARBON CYCLE-part 3.
Cycling of Matter in Ecosystems. Biogeochemical Cycles Matter cannot be made or destroyed. All water and nutrients must be produced or obtained from chemicals.
NOTES 20 – The Carbon Cycle, The Greenhouse Effect, and Global Warming.
Global Warming.
Estimated major stores of carbon on the Earth The Carbon Cycle Carbon exists in many forms: Atmospheric gases (CO 2 and methane) Dissolved CO 2.
Choose a category. You will be given the answer. You must give the correct question. Click to begin.
What is Global Warming? How does it work? What can we do?
Global Warming by Alex Kiss. Natural Warmth The Earth’s surface is heated primarily by sunlight The Earth’s surface is heated primarily by sunlight It.
THE CARBON CYCLE.
 Journal: Compare and contrast the carbon cycle and the nitrogen cycle.
Chapter 13 Section 3 Global Warming Environmental Science Spring 2011.
Carbon Cycle. What is the Carbon Cycle? In the carbon cycle, carbon is transferred from inside the Earth to the atmosphere, oceans, crust, and to living.
 You have time for test corrections today and we will complete the FRQ for this Quizzam.  Logistics:  We are going through a Chapter a week, so do your.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
HUMAN IMPACT ON THE ENVIRONMENT Global Warming and Acid Rain.
The Green House Effect ISCI (1). The fate of solar radiation – 26% reflected back into space 20% clouds; 6% by atmosphere – 19% absorbed by clouds,
By Kathryn Boit.  an increase in the earth's atmospheric and oceanic temperatures widely predicted to occur due to an increase in the greenhouse effect.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
The Greenhouse Effect & Global Warming. The Greenhouse Effect The Earth’s average temperature is increasing.
Environmental Chemistry: Global Warming
Greenhouse Effect How we stay warm. The Sun’s energy reaches Earth through Radiation (heat traveling through Space)
Rapid warming is changing the global climate The scientific debate about global warming is over—cause of warming is still debated –Global temperature has.
Chapter 19 Global Change.
Greenhouse Effect How we stay warm.
You will be given the answer. You must give the correct question.
Greenhouse Effect How we stay warm.
Chapter 19 Global Change.
Global Change.
Chapter 29 How Do Ecosystems Work?.
Unit A: Energy and Matter Exchange in the Biosphere
Chapter 19 Global Change.
Greenhouse Effect How we stay warm.
Global Warming Noadswood Science, 2016.
Earth Science Chapter 11.2 Climate Change.
Climate Change CH 19.
Greenhouse Effect How we stay warm.
Greenhouse Effect How we stay warm.
Chapter 19 Global Change.
Warm-up Finish questions from energy budget activity 10.1 quiz.
Greenhouse Effect How we stay warm.
GLOBAL WARMING.
Chapter 15 Global Change.
Chapter 19 Global Change.
Human Impacts on Climate Change
Greenhouse Effect How we stay warm.
Nutrient Cycles in Nature Ch. 3-3
2/6 What is the greenhouse effect?.
THE CARBON CYCLE
The Earth in Balance.
THE CARBON CYCLE.
Chapter 19 Global Change.
NOTES 36 – The Carbon Cycle, The Greenhouse Effect, and Global Warming
Presentation transcript:

Unit 5 Seminar Carbon dioxide

The Carbon Cycle Carbon comes into the living world through the plants, algae, and bacteria that take in atmospheric carbon dioxide to perform photosynthesis. Animals obtain their carbon from these photosynthesizing organisms.

The Carbon Cycle The carbon cycle is completed when carbon moves back into the atmosphere in the form of carbon dioxide, which is produced naturally through two processes: –the respiration of living things –the decomposition of them following their death

The Carbon Cycle Figure 35.1 atmospheric CO 2 photosynthesis respiration animals plants dead organisms fossil fuels decomposition by bacteria and fungi burning of fossil fuels The carbon cycle Plants and other photosynthesizing organisms take in atmospheric carbon dioxide (CO 2 ) and convert or “fix” it into molecules that become part of the plant. The physical functioning or respiration of organisms converts the carbon in their tissues back into CO 2. Plants and animals die and are decomposed by fungi and bacteria. Some CO 2 results, which moves back into the atmosphere. Some of the carbon in the remains of dead organisms becomes locked up in carbon-based compounds such as coal or oil. The burning of these fossil fuels puts this carbon into the atmosphere in the form of CO 2. Source: Krogh, D. (2009). Biology: A Guide to the Natural World. Pearson Benjamin Cummings

The Carbon Cycle Carbon dioxide makes up a small but critical proportion of the Earth’s atmosphere. It is vital to life and greatly affects global temperature.

Global Warming

The Earth’s atmospheric temperature is increasing through the phenomenon known as global warming. Scientists can now state with at least 90 percent certainty that most of the global warming seen since 1950 has come about because of human activities – deforestation –emission of such gases as carbon dioxide and methane into the atmosphere.

Global Warming Global temperatures risen 0.74 o C since 1906 to 2005 Warming trend over last 50 years nearly twice that for the last 100 years

Growing Concentration of Atmospheric CO 2 Beginning of industrialization Carbon dioxide levels over the last 10,000 yearsA closer look at the last 250 years Source: Krogh, D. (2009). Biology: A Guide to the Natural World. Pearson Benjamin Cummings

The Greenhouse Effect CO 2 and methane are referred to as greenhouse gases –trap additional quantities of the heat that comes to the Earth from the sun. –lower energy radiation (heat) cannot penetrate layer of gases

The Greenhouse Effect Figure heat trapped greenhouse gases reflection of low-energy radiation (heat) high-energy sun rays Source: Krogh, D. (2009). Biology: A Guide to the Natural World. Pearson Benjamin Cummings

Global Warming Deforestation—today, primarily of tropical forests –puts CO 2 into the atmosphere directly, when trees are burned –results in less CO 2 being taken out of the atmosphere trees that are destroyed no longer take up CO 2 to perform photosynthesis.

Global Warming The Earth appears to have warmed by 0.74°C or about 1.3°F in the 100 years that ended in 2005, according to our most authoritative source on global warming, the Intergovernmental Panel on Climate Change (IPCC).

Disappearing Glaciers Figure Source: Krogh, D. (2009). Biology: A Guide to the Natural World. Pearson Benjamin Cummings

Global Warming In 2007, the panel predicted that, over the course of the twenty-first century, the Earth is likely to warm by an addition 1.8°C to 4.0°C, depending on the additional quantity of greenhouse gases put into the atmosphere.

Global Warming The consequences of this warming –a rise in sea levels –more intense tropical storms –less snow cover globally – permafrost that thaws to increasing depths.

Rise in Sea Level 6 meters (~20 ft) sea level rise No greenhouse gases reduction

Habitat Changes: Disappearing Arctic Ice Figure Source: Krogh, D. (2009). Biology: A Guide to the Natural World. Pearson Benjamin Cummings

Australian Passerine Birds Body Size Australia average surface temp risen more than 1 o F since 1900 Passerine body size decreased by 3.6% Individuals within a species are larger the closer to a pole Smaller birds now live somewhat closer to the South Pole Nutritional deficiencies not found Jacky winter

Habitat Changes Alpine mountain regions –Native plants and animals driven to higher elevations

Global Warming Global warming cannot be stopped, the IPCC said, but it can be lessened in accordance with future human activities. –Use less energy –Reduce fossil fuel use –Store CO 2 –Slow tropical rain forest destruction

Seminar Questions If there is strong evidence indicating that CO2 levels contribute to global warming, why is the United States opposed to any reductions? Is there any science supporting those who do not wish to reduce fossil fuel CO2 emissions? If we choose to reduce fossil fuel emissions significantly, how might we do so in a way that does not damage our economy?

Seminar Questions Is there a fair method globally to reduce CO2 emissions? Support your answer. If we decide to wait until the climate is clearly too warm for the human species, is there a technological quick fix? What can be done to monitor the situation?

Questions?