Climate is regulated by complex interactions among components of the Earth system.

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.

There are 5 more fundamental concepts. See them all...

Hide

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 freshwater 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 more rapid climate change 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 regional differences in climates on Earth. Many climatic processes such as the greenhouse effect and the carbon cycle are the result of the 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

These ideas address some of the natural complexities of our climate system and build a foundation for the understanding of key components such as the carbon cycle, the greenhouse effect, and interactions and feedback loops. These topics are active areas of climate research and include important questions such as:

• 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 CO_2, and changes in circulation patterns.
• Why some past climate changes have been gradual and others abrupt.

On a more basic level, the processes covered in this principle can easily be observed, such as:

• Compared to air, water takes a long 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.

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.

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.

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

Just because a process is complex does not mean it needs to be complicated. Teaching these basic climate science topics may be best handled by an approach that allows depth over breadth. If students are able to address a single topic with sufficient depth, they can come to an understanding of nuances like feedback loops or deep ocean circulation. So a good tactic would be to set aside time to explore a topic and several facets within it. An important part of climate literacy is an appreciation for scientific complexity, and even young learners can comprehend that a seemingly simple and linear process can be quickly complicated by other factors.

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

Middle school

• Carbon Cycle Role Play - Carbon cycle activity to demonstrate how carbon moves throughout the atmosphere. The activity ends with a discussion of how humans impact the carbon cycle.
• What is Albedo? - In this lesson, students watch a 2-minute video explaining albedo. The video shows visualizations of albedo across Earth and how it can change. Students then interpret the images in the video and answer questions about albedo.
• 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.
• NOAA Ocean Odyssey: Ocean Currents - This lesson provides a demonstration and lesson focused on ocean currents. The demonstration of how cold water and warm water interact is a strong learning tool for the topic.

High school

• Global Warming: Carbon Dioxide and the Greenhouse Effect - This video segment demonstrates carbon dioxide's role in the greenhouse effect and explains how increasing concentrations of C02 in the atmosphere is contributing to global warming. The video includes an unusual demonstration of C02's heat-absorbing properties, using infrared film, a researcher's face, and a stream of C02 between them.
• Decoding Antarctica's Climate History - Antarctica's Climate Secrets - This 10 minute video builds connections between topics that are important in climate science such as: the impact of variations in Earth's orbit and wobble on it's axis on climate; how the cores being sampled fit into the bigger climate picture; connecting greenhouse gases to melting ice and sea level changes; the sensitivity of the ice melt / sea level rise relationship; and computer model simulations showing connections between ice sheets and sea level. The companion website provides resources, an extensive list of activities, teacher guides, posters, and more.10-minute
• 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.
• Students can explore feedback loops further with this data-rich activity that examines albedo and the rate of snowmelt in the Arctic, Arctic Climate Curriculum: Exploring Arctic Climate Data.

College

• 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 students' 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.