C267: Climate Change

C267 Climate Change is a Western Governors University course that teaches future and current science teachers the science behind a changing climate, from how the system works to what the evidence shows.

WGU's program guides place the course in its science education degrees, including the M.A. Science Education (Secondary Chemistry), at three competency units.

The description covers how the climate system works, what makes climate change on different time scales, how climate has changed in the past and how scientists use models, observations and theory to project future climate.

Students often find the course demanding because it sits across several sciences at once. You need enough physics for energy balance, enough chemistry for ocean acidity and enough Earth science for past climates, and then you must explain all of it in plain language.

What C267 Covers

The official description groups the course into a handful of big questions. Each one is a likely focus for an assessment task:

Key Concepts Explained

The Greenhouse Effect and Energy Balance

Earth absorbs sunlight and radiates heat back to space as infrared. Greenhouse gases absorb some of that outgoing infrared and re-emit it, warming the lower atmosphere. Adding more of these gases tips the balance, so the planet warms until outgoing energy matches incoming energy again.

Feedbacks

A feedback amplifies or dampens an initial change. Ice-albedo feedback is the classic amplifier: warming melts reflective ice, darker ocean or land absorbs more sunlight, and warming increases further.

Ocean Acidification

The ocean absorbs part of the carbon dioxide we emit. Dissolved CO2 forms carbonic acid, which lowers pH and reduces the carbonate ions that corals and shellfish use to build shells and skeletons. This is chemistry a secondary teacher can demonstrate in class.

Typical Assignments and How to Approach Them

WGU assesses competency through performance assessments (written tasks scored against a rubric) or objective assessments (exams). Check your course page for the current format. Work in this subject typically looks like this:

How Today's Change Differs from Past Cycles

The course asks you to explain how present-day change differs from earlier natural cycles. This is where many answers go wrong, either by ignoring past change or by assuming it makes today's warming unremarkable.

Three lines of reasoning make the comparison clear:

• Rate. Glacial cycles unfolded over thousands of years; the current warming is happening over decades.
• Cause. Orbital cycles explain the timing of ice ages, but they do not account for the recent rise, which matches the increase in greenhouse gases from human activity.
• Fingerprints. The pattern of change, such as a warming lower atmosphere alongside a cooling upper atmosphere, points to greenhouse gases rather than a brighter Sun.

Teaching Climate Change in the Classroom

C267 sits in a teacher preparation program, so explanations that work for school students are a real advantage. Climate change is also a topic where students arrive with strong opinions, partial information and sometimes anxiety.

A few approaches help keep lessons scientific and constructive:

• Start with data. Let students read temperature or carbon dioxide records and describe the trends themselves before any discussion of causes.
• Separate science from policy. What is happening and why is a scientific question; what to do about it involves values and politics.
• Use models students can test. A simple jar experiment on warming, or a graph of sea ice, makes abstract ideas concrete.
• End with agency. Showing how communities adapt and reduce emissions avoids leaving students with only bad news.

Even when a task does not ask for teaching ideas directly, writing as someone who could explain the concept to a class tends to produce clearer, better organized answers.

Where Students Get Stuck

• Confusing weather and climate. A cold week is weather. Climate is the long-term average, usually over 30 years or more.
• Listing evidence without mechanism. Saying sea level is rising is not enough; explain thermal expansion and melting land ice.
• Overstating certainty or uncertainty. Describe what is well established and where projections vary, without exaggeration.
• Using unreliable sources. Rely on scientific agencies and peer-reviewed work, not opinion pieces.

Study Tips for C267

• Draw the climate system as a diagram with arrows for energy flows; it makes every later topic easier.
• Keep a table of each line of evidence, what it measures and what it shows.
• Practice explaining one concept, such as acidification, as you would to a high school class.
• Read each rubric aspect and label the matching section of your work.

How We Help with C267

Send the task instructions, rubric, any data sets or articles provided and evaluator comments from earlier attempts. A writer with a science background prepares a model explanation, helps you interpret graphs, or reviews your draft for scientific accuracy and clarity.

GradeEssays is independent of Western Governors University. Our work is tutoring and reference material: use it to understand the science, then write and submit your own work under WGU's academic integrity rules. We never log in to student portals. Every order is written from scratch, with free revisions within the scope of your original request.