Understanding the Comparing Climates Gizmo Answer Key
The Gizmo simulations from ExploreLearning are cloud-based educational tools used in middle and high school science classes. The Comparing Climates Gizmo specifically lets students manipulate variables like latitude, elevation, and proximity to water to observe how those factors affect temperature and precipitation patterns. When teachers assign it as homework or lab work, students and parents naturally look for a Comparing Climates Gizmo Answer Key to check their work or understand concepts they found confusing during the simulation. I used these simulations in a classroom setting for several years, so I can speak to how they actually function and where people typically run into trouble. The interface looks straightforward at first, but there are a few mechanics that trip up students every single semester.
What the Comparing Climates Gizmo Answer Key Actually Covers
The answer key isn't a single document with predetermined values. The Gizmo generates randomized data each time you run the simulation, so the exact numbers will vary between student sessions. What remains consistent are the relationships and patterns you're supposed to discover. Here's what you should be seeing when you work through it correctly:
- Latitude effect: As latitude increases (moving toward the poles), annual temperature decreases. This is a fairly linear relationship until you get above 60 degrees, where the curve flattens slightly.
- Elevation effect: Temperature drops roughly 6.5°C per 1,000 meters of elevation gain. This is the standard environmental lapse rate, and the Gizmo models it accurately.
- Proximity to water: Cities near large bodies of water show smaller temperature ranges between summer and winter compared to continental interior cities at the same latitude.
- Ocean current influence: Warm currents raise coastal temperatures; cold currents lower them. This is often the trickiest concept for students because it requires understanding both latitude position AND current direction simultaneously.
- precipitation patterns: Windward sides of mountains receive more precipitation than leeward sides due to orographic lift. The Gizmo shows this through the rain shadow effect on the downwind side.
If your data doesn't align with these patterns, something is wrong with how you're setting up the simulation, not with the simulation itself. The biggest issue I see students making is not controlling variables properly. The Gizmo lets you change multiple factors at once, which ruins the cause-and-effect analysis the assignment is supposed to teach. You need to change only one variable while holding everything else constant. Set a baseline city, record the data, then change exactly one thing and compare. Another mistake is reading the data tables without looking at the visual representation. The Gizmo provides both a climate graph and a data table for each city. The graph shows monthly temperature and precipitation visually, while the table gives you exact numbers. Cross-referencing both helps catch errors. If the graph shows a wet summer but the table says dry, something got mixed up.
Get the Full Details

I ran into a specific edge case that confused an entire class once. When students placed two cities at the same latitude but one was on the leeward side of a mountain range and the other windward, the precipitation difference was dramatic, but the temperature readings were nearly identical. Several students thought the simulation had broken because the numbers looked too similar. The workaround was to extend the observation period and compare annual totals rather than monthly snapshots. The rain shadow effect is more pronounced in cumulative precipitation data than in any single month's reading. Once they switched to annual totals, the pattern became obvious. Here's the step-by-step process I recommend:
- Open the Gizmo and select the data collection mode first, not the exploration mode. Data collection locks variables and makes it easier to compare systematically.
- Set City A at your baseline coordinates. Record all temperature and precipitation data before touching anything else.
- Change only the variable you're testing. If studying elevation, keep latitude and proximity to water identical and only adjust elevation.
- Record City B's data in a side-by-side table. Don't rely on memory to compare the two sets.
- Repeat for each variable: latitude, elevation, distance from water, ocean current type, and mountain barrier presence.
- After collecting all data, use the summary table feature to generate your final comparison chart. This auto-formats everything and catches calculation errors.
Download and Access Information
The Gizmo simulations require a subscription through ExploreLearning. Individual student licenses run approximately $35 to $50 per year, while classroom packs are available through school districts. Some teachers provide class access codes that students can use without individual subscriptions. If you're looking for a free Comparing Climates Gizmo Answer Key, you won't find an official one from ExploreLearning since the randomized nature of the simulation makes a static answer key impractical. However, the pattern-based guidance above covers what any legitimate answer key would contain. Third-party answer key sites exist, but most of them are outdated or contain incorrect values because they were generated from a single randomized run. The numbers on those pages won't match your simulation results. I've seen students lose points because they copied answers from a site that used different randomization seeds. It's better to work through the patterns yourself using the framework I outlined.
Pitfalls and Limitations to Be Aware Of
The Gizmo is a model, not a perfect representation of reality. It simplifies several complex atmospheric processes. For example, it treats ocean currents as binary warm or cold without accounting for current strength variability. It also doesn't model microclimate effects, urban heat islands, or seasonal wind patterns like monsoons. Students should understand that the Gizmo shows idealized relationships, not every real-world exception. Another limitation is the sample size. The Gizmo typically uses about 20 representative cities worldwide. That's enough to establish general patterns, but it won't capture regional anomalies. A city like Quito, Ecuador sits near the equator but has a cool climate due to extreme elevation. The Gizmo can demonstrate this, but the small dataset means students might not encounter enough high-elevation equatorial cities to generalize the pattern confidently. If you need more rigorous climate data for advanced analysis, I'd recommend supplementing the Gizmo with actual climate databases like the World Climate database from the University of Cornell or the NOAA climate normals dataset. Those provide real observational data for thousands of stations worldwide and can fill gaps the Gizmo leaves open.
