Students develop and test a hypothesis about how albedo affects temperature.

In this activity, students will analyze past and future eclipse data and orbital models to determine why we don’t experience eclipses every month.

Examine (daytime) surface temperature and solar radiation received at locations found near similar latitudes using NASA Data.

Students explore positive feedback effects of changing albedo from melting Arctic sea ice.

In this activity, students make a claim about the cause of ocean currents and then develop a model to explain the role of temperature and density in deep ocean currents.  This lesson is modified from "Visit to an Ocean Planet" Caltech and NASA/Jet Propulsion Laboratory.

The ocean's surface is not level, and sea levels change in response to changes in chemistry and temperature. Sophisticated satellite measurements are required for scientists to document current sea level rise.