describe, in general terms, how thermal energy is transferred through the atmosphere (i.e., global wind patterns, jet stream, Coriolis effect, weather systems) and through the hydrosphere (i.e., ocean currents, large bodies of water) from latitudes of net radiation surplus to latitudes of net radiation deficit, resulting in a variety of climatic zones (e.g., analyze static and animated satellite images)
Standard detail
D.STSK2A
Depth 3Parent ID: A7C5E3C32C8C425DA964D51E7E09DBBAStandard set: Grade 10 - Science 10 (2014)
Original statement
Quick facts
- Statement code
- D.STSK2A
- List ID
- a
- Standard ID
- A21655C2F47047A7A184463F0B411032
- Subject
- Science (1996, 2003, 2006, 2014)
- Grades
- 10
- Ancestor IDs
- A7C5E3C32C8C425DA964D51E7E09DBBAC3EFC796435341FD826A039821B395740F682F859DB84271A55D5AC8B419634D
- Source document
- Alberta Programs of Study
- License
- CC BY 4.0 US