Teaching about climate interactions is supported by six key concepts:
a. Earth's climate is influenced by interactions involving the sun, ocean, atmosphere, clouds, ice, land, and life. Climate varies by region as a result of local differences in these interactions.
b. Covering 70% of Earth's surface, the ocean exerts a major control on climate by dominating Earth's energy and water cycles. It has the capacity to absorb large amounts of solar energy. Heat and water vapor are redistributed globally through density-driven ocean currents and atmospheric circulation. Changes in ocean circulation caused by tectonic movements or large influxes of fresh water from melting polar ice can lead to significant and even abrupt changes in climate, both locally and on global scales.
c. The amount of solar energy absorbed or radiated by Earth is modulated by the atmosphere and depends on its composition. Greenhouse gases— such as water vapor, carbon dioxide, and methane— occur naturally in small amounts and absorb and release heat energy more efficiently than abundant atmospheric gases like nitrogen and oxygen. Small increases in carbon dioxide concentration have a large effect on the climate system.
d. The abundance of greenhouse gases in the atmosphere is controlled by biogeochemical cycles that continually move these components between their ocean, land, life, and atmosphere reservoirs. The abundance of carbon in the atmosphere is reduced through seafloor accumulation of marine sediments and accumulation of plant biomass and is increased through deforestation and the burning of fossil fuels as well as through other processes.
e. Airborne particulates, called "aerosols," have a complex effect on Earth's energy balance: they can cause both cooling, by reflecting incoming sunlight back out to space, and warming, by absorbing and releasing heat energy in the atmosphere. Small solid and liquid particles can be lofted into the atmosphere through a variety of natural and manmade processes, including volcanic eruptions, sea spray, forest fires, and emissions generated through human activities.
f. The interconnectedness of Earth's systems means that a significant change in any one component of the climate system can influence the equilibrium of the entire Earth system. Positive feedback loops can amplify these effects and trigger abrupt changes in the climate system. These complex interactions may result in climate change that is more rapid and on a larger scale than projected by current climate models.
Earth's climate is governed by several different types of processes.
Oceanic, atmospheric, biologic and geologic processes all drive the climate system and result in a regional differences in climates on Earth. Many climatic processes such as the greenhouse effect and the carbon cycle are the result of interplay between the "spheres" of the Earth system (atmosphere, cryosphere, geosphere, biosphere). Feedbacks between various components work to exacerbate or mitigate changes to the climate.
Climate cycles, feedbacks, and interplay between causes and effects
- How aerosols play a role in the changing climate. These small airborne particles have both a cooling and warming effect and originate from both natural and human-caused sources.
- How feedbacks in the climate system contribute to the effects of increasing atmospheric CO2.
- How oceanic processes are integral in the distribution of heat, absorption of CO2, and changes in circulation patterns.
- Why some past climate changes have been gradual and others abrupt.
- Compared to air, water takes a longer time to warm up or cool down.
- A cloudy night will be warmer than a clear night (if all other factors remain equal).
- The overall climate of a region is not solely determined by its latitude, but is also influenced by factors such as proximity to oceans or mountain ranges.
Helping students understand these ideas
The natural greenhouse effect is a common area of misunderstanding. Educators should strive to explain this concept in a way that is as simple as possible, but is still accurate.
- Most of the Sun's energy that reaches Earth's surface is short wave radiation, which warms the surface and is transformed into long-wave infrared that radiates back toward space.
- Most of the gases in the atmosphere do not trap the outgoing radiation.
- However, greenhouse gases in the atmosphere such as water vapor, carbon dioxide, methane, and nitrogen oxides are very powerful in absorbing the outgoing radiation and re-radiating it in all directions.
- The re-radiation of energy causes the lower atmosphere to warm, and in turn warms Earth's land surface and oceans.
Attempts to oversimplify the greenhouse effect can be counter-productive and further confuse learners. For younger students the mental model of how the natural greenhouse effect is like a "blanket" that keeps heat under the covers may be appropriate, but a key difference is that a blanket retains heat that is generated by your body (or the Earth, in the analogy). In reality, the heat energy is originally coming from the Sun, not from the Earth.
By high school and certainly college students should have a clearer understanding of the mechanics of the greenhouse effect. This concept is essential to understanding how human activities are impacting the climate system.
Full comprehension of the carbon cycle requires an understanding of biogeochemical systems. Students also have to understand the different time scales at which carbon exchange takes place in the different reservoirs. Learning about the carbon cycle lays an important foundation to the understanding of the impact of burning fossil fuels. As shown in the famous Harvard Private Universe study, students struggle to build the connection between mass production through photosynthesis and carbon uptake, the burial of biomass, and fossil fuels - all these concepts are part of the carbon cycle.
The terminology of positive and negative feedback in a system can often lead to misunderstanding because the words 'positive' and 'negative' have other meanings. It is clearer to use the term 'self-reinforcing cycle' to describe the way that positive feedback can amplify the initial input. Negative feedback can be termed a 'self-dampening cycle.'
Bringing these ideas into your classroom
Another strategy for teaching these principles is the Earth systems science approach. This method teaches students about the "spheres" of the Earth system: the atmosphere, cryosphere, geosphere, and biosphere. An Earth systems approach is an effective way to illustrate the interplay between different components of Earth and that processes do not occur in isolation. Learn more and find specific examples from the InTeGrate project: Teach Systems Thinking or Incorporating Systems Thinking in the Classroom.
Teaching materials from the CLEAN collection
- Carbon Cycle Animation is an easy way to introduce younger students to the ways that carbon moves through plants, animals, soil, and the atmosphere.
- Understanding Albedo explores the heat-trapping qualities of certain gases, and how thermal energy carried by ocean currents can influence on local climates around the world.
- Heating it Up: The Chemistry of the Greenhouse Effect is part of a sequence of activities about climate change. Suitable for high school as well.
- This short Greenhouse Effect Video from atmospheric scientist Scott Denning gives a candid and entertaining explanation of how greenhouse gases in Earth's atmosphere warm our planet. This video could also be useful as professional development for teachers.
- Ocean Currents and Sea Surface Temperature students access sea surface temperature and wind speed data from a NASA site, plot and compare data, draw conclusions, and link them to the topic of global climate change.
- Carbon on the Move is a 3-part lab activity where students investigate the global carbon cycle and study the effects of specific feedback loops.
- A slide show and case study from the New York Times shows one example of a self-reinforcing feedback occurring today, As Permafrost Thaws, Scientists Study the Risks.
- Students can explore feedbacks further with this data-rich activity that examines albedo and the rate of snowmelt in the Arctic, Arctic Climate Curriculum: Exploring Arctic Climate Data.
Related Pedagogic Methods:
- Understanding the Carbon Cycle: A Jigsaw Approach offers an interactive way for students to investigate and communicate the roles of carbon throughout the Earth.
- Students can visualize how 8 different greenhouse gases absorb energy with the Greenhouse Gases - IR Spectra animation.
- Gulf Stream Heat Budget and Europe's Mild Climate is a role-playing activity where students determine whether the Gulf Stream is responsible for keeping northern Europe warm. They consider the potential future of the Gulf Stream if polar ice were to continue melting.
- Students can build a simplified computer model in Modeling the Oceanic Thermohaline Circulation with STELLA, and examine the impacts of varying the initial reservoirs, temperature changes, and freshwater pulses. The activity will challenge student's expectations that only complex behaviors come out of complex systems and models.
- In Sediments and the Global Carbon Cycle, students learn about the role of sedimentary rocks in long-term carbon storage and relevance to global warming. It also introduces students to the use of carbon isotopes for paleoenvironmental interpretations.
- Exploring the Link between Hurricanes and Climate using GCM Results - Students examine global climate model output and consider the potential impact of global warming on tropical cyclone initiation and evolution.
Find activities and visuals for teaching this topic
Carbon and Climate - an educational website with a carbon cycle applet for modeling your own projection on carbon emissions and future carbon sinks.
McCaffrey & Buhr, 2008: Clarifying Climate Confusion.- journal article in Physical Geography about common misconceptions in climate science.