ALEX | Alabama Learning Exchange

Heat StudyJam

Classroom Resource Information

Title:

Heat StudyJam

URL:

http://studyjams.scholastic.com/studyjams/jams/science/energy-light-sound/heat.htm

Content Source:

Other
http://studyjams.scholastic.com/

Type:

Audio/Video

Overview:

The classroom resource provides a video that will describe the different ways heat can be transferred from the sun through the atmosphere, as well as other applications of heat transfer. There is also a short test that can be used to assess students' understanding.

Content Standard(s):

Science
SC2015 (2015)
Grade: 6
Earth and Space Science

13 ) Use models (e.g., diagrams, maps, globes, digital representations) to explain how the rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation that determine regional climates.

a. Use experiments to investigate how energy from the sun is distributed between Earth's surface and its atmosphere by convection and radiation (e.g., warmer water in a pan rising as cooler water sinks, warming one's hands by a campfire).

NAEP Framework

NAEP Statement::
E8.11a: The Sun is the major source of energy for phenomena on Earth's surface.

NAEP Statement::
E8.11b: It provides energy for plants to grow and drives convection within the atmosphere and oceans, producing winds, ocean currents, and the water cycle.

NAEP Statement::
E8.13a: Global patterns of atmospheric movement influence local weather.

NAEP Statement::
E8.13b: Oceans have a major effect on climate because water in the oceans holds a large amount of heat.

NAEP Statement::
P8.10a: Energy is transferred from place to place.

NAEP Statement::
P8.10b: Light energy from the Sun travels through space to Earth (radiation).

NAEP Statement::
P8.10c: Thermal energy travels from a flame through the metal of a cooking pan to the water in the pan (conduction).

NAEP Statement::
P8.10d: Air warmed by a fireplace moves around a room (convection).

NAEP Statement::
P8.10e: Waves (including sound and seismic waves, waves on water, and light waves) have energy and transfer energy when they interact with matter.

NAEP Statement::
P8.11a: A tiny fraction of the light energy from the Sun reaches Earth.

NAEP Statement::
P8.11b: Light energy from the Sun is Earth's primary source of energy, heating Earth surfaces and providing the energy that results in wind, ocean currents, and storms.

Unpacked Content

Scientific And Engineering Practices:

Developing and Using Models

Crosscutting Concepts: Systems and System Models

Disciplinary Core Idea: Earth's Systems

Evidence Of Student Attainment:

Students:

Explain by using models, how the rotation of Earth and unequal heating of its surface create patterns of atmospheric circulation that determine regional climates.
Explain by using models, how the rotation of Earth and unequal heating of its surface create patterns of oceanic circulation that determine regional climates.
Use experiments to investigate how energy from the sun is distributed between Earth's surface and its atmosphere by convection.
Use experiments to investigate how energy from the sun is distributed between Earth's surface and its atmosphere by radiation.

Teacher Vocabulary:

Model
Diagram
Map
Globe
Digital representation
Rotation
Heat
Pattern
Atmosphere
Atmospheric circulation
Ocean
Oceanic circulation
Climate
Regional climate
Radiation
Sun
Solar energy
Thermal energy
Water
Land
Ice
Temperature
Matter
Conduction
Latitude
Altitude
Geography
Geographic land distribution
Precipitation
Absorption
Landform
Atmospheric flow
Mountain
Rain shadow effect
Coriolis force
Fluid
Density
Salinity
Global ocean convection cycle
Landmass
Marine
Coast
Variation
Radiation
Electromagnetic wave
Space
Convection
Current
Liquid
Gas
Equator

Knowledge:

Students know:

Radiation from the sun (solar energy) introduces heat (thermal energy) into Earth's atmosphere, water, land, and ice.
Thermal energy exists in the atmosphere, water, land, and ice as represented by temperature.
Thermal energy moves from areas of high temperature to areas of lower temperature either through the movement of matter, via radiation, or via conduction of heat from warmer objects to cooler objects.
Absorbing or releasing thermal energy produces a more rapid change in temperature on land compared to in water.
Absorbing or releasing thermal energy produces a more rapid change in temperature in the atmosphere compared to either on land or in water so the atmosphere is warmed or cooled by being in contact with land or the ocean.
The rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation.
Patterns of atmospheric and oceanic circulation vary by latitude, altitude, and geographic land distribution.
Higher latitudes receive less solar energy per unit of area than do lower latitudes, resulting in temperature differences based on latitude.
A general latitudinal pattern in climate exists where higher average annual temperatures are found near the equator and lower average annual temperatures are at higher latitudes.
Latitudinal temperature differences are caused by more direct light (greater energy per unit of area) at the equator (more solar energy) and less direct light at the poles (less solar energy).
A general latitudinal pattern of drier and wetter climates caused by the shift in the amount of air moisture during precipitation from rising moisture-rich air and the sinking of dry air.
In general, areas at higher altitudes have lower average temperatures than do areas at lower altitudes. Because of the direct relationship between temperature and pressure, given the same amount of thermal energy, air at lower pressures (higher altitudes) will have lower temperatures than air at higher pressures (lower altitudes).
Features on the Earth's surface, such as the amount of solar energy reflected back into the atmosphere or the absorption of solar energy by living things, affect the amount of solar energy transferred into heat energy.
Landforms affect atmospheric flows (e.g., mountains deflect wind and/or force it to higher elevation, known as the rain shadow effect).
The geographical distribution of land limits where ocean currents can flow.
The Earth's rotation causes oceanic and atmospheric flows to curve when viewed from the rotating surface of Earth (Coriolis force).
Fluid matter (i.e., air, water) flows from areas of higher density to areas of lower density (due to temperature or salinity). The density of a fluid can vary for several different reasons (e.g., changes in salinity and temperature of water can each cause changes in density). Differences in salinity and temperature can, therefore, cause fluids to move vertically and, as a result of vertical movement, also horizontally because of density differences.
Ocean circulation is dependent upon the transfer of heat by the global ocean convection cycle, which is constrained by the Coriolis effect and the outlines of continents.
Because water can absorb more solar energy for every degree change in temperature compared to land, there is a greater and more rapid temperature change on land than in the ocean. At the centers of landmasses, this leads to conditions typical of continental climate patterns.
Climates near large water bodies, such as marine coasts, have comparatively smaller changes in temperature relative to the center of the landmass. Land near the oceans can exchange thermal energy through the air, resulting in smaller changes in temperature. At the edges of landmasses, this leads to marine climates.
Variations in density due to variations in temperature and salinity drive a global pattern of interconnected ocean currents.
Radiation is the transfer of heat energy by electromagnetic wave motion. The transfer of energy from the sun across nearly empty space is accomplished primarily by radiation.
Radiation from the sun (solar energy) introduces heat (thermal energy) into Earth's atmosphere, water, land, and ice.
Convection is the transfer of heat by a current and can occur in a liquid or a gas.
When air near the ground is warmed by heat radiating from Earth's surface. The warm air is less dense, so it rises. As it rises, it cools. The cool air is dense, so it sinks to the surface. This creates a convection current.
Convection is the most important way that heat travels in the atmosphere.
Convection in the atmosphere is responsible for the redistribution of heat from the warm equatorial regions to higher latitudes and from the surface upward.

Skills:

Students are able to:

Use a model of Earth and identify the relevant components of Earth's system, including inputs and outputs.
Describe the relationships between components of the model including how the rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation.
Articulate a statement that relates a given phenomenon to a scientific idea, including how the rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation.
Identify and describe the phenomenon under investigation, which includes how energy is distributed between Earth's surface and its atmosphere.
Identify and describe the purpose of the investigation, which includes providing evidence that energy from the sun is distributed between Earth's surface and its atmosphere by convection and radiation.
Collect and record data, according to the given investigation plan.
Evaluate the data to determine how energy from the sun is distributed between Earth's surface and its atmosphere by convection and radiation.

Understanding:

Students understand that:

Weather and climate are influenced by interactions involving sunlight, the ocean, the atmosphere, ice, landforms, and organisms. These interactions vary with latitude, altitude, and local and regional geography, all of which can affect oceanic and atmospheric flow patterns.
The ocean exerts a major influence on weather and climate by absorbing energy from the sun, releasing it over time, and globally redistributing it through ocean currents.
Radiation from the sun (solar energy) introduces heat (thermal energy) into Earth's atmosphere, water, land, and ice and is represented by temperature. Thermal energy moves from areas of high temperature to areas of lower temperature on Earth's surface and in its atmosphere either through radiation or convection.

AMSTI Resources:

AMSTI Module:
Understanding Weather and Climate (for both 13 and 13a)

Alabama Alternate Achievement Standards

AAS Standard:
SCI.AAS.6.13 - Use models to investigate how energy from the sun impacts Earth's surface; recognize that uneven heating of Earth's surface causes patterns in weather and climate. SCI.AAS.6.13a - Recognize that the sun's thermal energy is distributed throughout Earth's atmosphere by convection and radiation.

Tags:

conduction, convection, heat, heat transfer, radiation, reflection, thermal energy

License Type:

Custom Permission Type
See Terms: http://www.scholastic.com/terms.htm
For full descriptions of license types and a guide to usage, visit :
https://creativecommons.org/licenses

Accessibility

Comments

The test may be completed as a whole group or independently on student devices.

There is a printable available that includes a short synopsis of the video and definitions of the vocabulary words. This could be used as a notetaking sheet for students as they watch the video.

This resource provided by:

Author:

Hannah Bradley

ALEX Classroom Resource

Heat StudyJam