The Arctic Ocean Curriculum Unit was created by the Arctic Research Consortium of the United States with funding from the North Pacific Research Board. This project aimed to update and revise existing Arctic Ocean-related lesson plans originally created by PolarTREC program teacher alumni. The format used lends itself to the changes in education - providing student-facing slide decks that allow
By rolling a die, students will simulate a molecule of carbon’s movement with in the carbon cycle. This is a fun, active way to introduce students to the carbon cycle and/or to review the cycle and identify carbon sinks and sources.
Students experience the carbon cycle as CO2 molecules or as stored carbon and travel the path of
Oceanography is the study of the ocean. It covers a wide range of topics from marine life to the geology of the sea floor to the physical properties of the ocean. Physical oceanographers study the physical components of the ocean including light, waves, tides, currents and the composition of sea water. The physical properties of the ocean can
This activity works best for students who don't have a lot of lab experience and learn best through hands on activities. It allows them to not only investigate an aspect of global warming (rising sea levels), they will also get practice with making predictions and writing a hypothesis as well as understanding basic scientific concepts such as water
The students will bury ice (frozen in various shapes such as flat slabs, wedges, & lumps) at varying depths and under the various substrates and vegetation covers.
The students will record the ambient temperature and how long it takes the various ice shapes with the various coverings to melt. Students will observe and record results.
The students will
This lesson answers the question: How does ice floating on the ocean act as it melts?
Objective
* Students will learn about temperature, salinity and their effect on density.
* Students will learn that ocean currents are caused by differences in densities as a result of temperature and salinity. These differences allow ocean currents to circulate water