HS-ESS2-2 | Feedbacks in Earth’s Systems
Analyze geoscience data to make the claim that one change to Earth’s surface can create feedbacks that cause changes to Earth’s systems.
Clarification statement: Examples should include climate feedbacks, such as how an increase in greenhouse gases causes a rise in global temperatures that melts glacial ice, which reduces the amount of sunlight reflected from Earth’s surface, increasing surface temperatures and further reducing the amount of ice. Examples could also be taken from other system interactions, such as how the loss of ground vegetation causes an increase in water runoff and soil erosion; how dammed rivers increase groundwater recharge, decrease sediment transport, and increase coastal erosion; or how the loss of wetlands causes a decrease in local humidity that further reduces the wetland extent.
Assessment
What assessment of HS-ESS2-2 might look like on a NY state exam.
Performance Level Descriptions
PLDs communicate the knowledge and skills expected of students to demonstrate proficiency in each Learning Standard. NYS assessments classify student performance into one of five levels.
Vocabulary
Terms from the Earth & Space Science Glossary that come from this standard or from the released exam questions that assess it.
- absorption
- atmosphere
- climate feedback
- climate system
- coastal erosion
- costs and benefits
- dammed rivers
- design solution
- Earth
- Earth materials
- Earth’s surface
- Earth’s systems
- electromagnetic radiation
- feedback
- geoscience data
- glacial ice
- global temperatures
- greenhouse gases
- ground vegetation
- groundwater recharge
- humidity
- ice
- model
- negative feedback
- new technologies
- observations
- ocean
- positive feedback
- radiation
- reflection
- river
- runoff
- sediment transport
- soil erosion
- surface temperature
- system feedback
- wetland extent
- wetland loss
- wetlands
- abyssal plain – Aug 2026
- acid mine drainage – Jan 2026
- acid rain – June 2026
- acidic – Jan 2026
- aerosols – June 2026
- air pollution – Jan 2026
- albedo – Sample 2024
- anomaly – June 2025
- arable land – June 2025
- atmospheric composition – Jan 2026
- banded iron formations – Jan 2026
- basin – Aug 2026
- bedrock – Jan 2026
- biodiversity – Jan 2026
- biomass – June 2025
- biomass fuel – June 2025
- biosphere – June 2026, Jan 2026
- black smokers – Jan 2026
- carbon – June 2025
- carbon cycle – June 2025
- carbon dioxide – Jan 2026, June 2025
- carbon sinks – June 2025
- carbon uptake – June 2025
- chemical weathering – June 2026
- climate change – Aug 2026, Jan 2026
- coastal flooding – June 2025
- conservation – June 2025
- cryosphere – Sample 2024
- decomposition – June 2025
- deforestation – Jan 2026, Aug 2025
- density – Sample 2024
- deposition – Aug 2026, Aug 2025, June 2025
- desertification – Aug 2026
- dredging – June 2025
- eddies – Aug 2026
- emissions – June 2026, June 2025
- energy and mineral resources – Jan 2026
- energy flow – June 2026
- erosion – Aug 2026, Jan 2026, Aug 2025, June 2025
- eruption column – Aug 2026
- evaporation – June 2025
- fossil fuels – June 2025
- free oxygen – Jan 2026
- fresh water – Jan 2026, Aug 2025, June 2025
- geologic time – Jan 2026
- geosphere – June 2026, Jan 2026, Sample 2024
- ghost forest – June 2025
- glacial melting – June 2025
- glaciers – Jan 2026, June 2025
- gorge – Aug 2025
- groundwater – Jan 2026, June 2025
- groundwater contamination – Jan 2026
- habitats – June 2025
- human activity – June 2025
- hydrosphere – June 2026, Jan 2026, Sample 2024
- hydrothermal vents – Jan 2026
- ice sheet – Jan 2026
- ice-core data – June 2025
- inorganic carbon – June 2025
- iron – Jan 2026
- land bridge – Jan 2026
- land use – Aug 2025
- livestock – June 2025
- mantle – Sample 2024
- mass – Aug 2026, Jan 2026
- mass extinction – Jan 2026
- megafires – June 2025
- methane – Jan 2026
- microfossils – Jan 2026
- minerals – Jan 2026
- mining – June 2026, Jan 2026
- mountain – June 2025
- natural disaster – June 2025
- ocean circulation – Aug 2026
- open pit mine – Jan 2026
- overgrazing – June 2025
- oxygen – Jan 2026
- Pangea – Sample 2024
- photosynthesis – June 2025
- physical weathering – June 2026
- plant cover – Aug 2025
- Polar Easterlies – Sample 2024
- Polar Front Jet Stream – Sample 2024
- pollutants – Jan 2026
- pollution – Jan 2026
- precipitation – Aug 2026, Jan 2026
- rate of erosion – Aug 2025
- reflectivity – Sample 2024
- salinity – Jan 2026, June 2025, Sample 2024
- salt front – June 2025
- saltwater intrusion – June 2025
- sea ice – Sample 2024
- sea level – Jan 2026, June 2025, Sample 2024
- sediment – Aug 2026, Aug 2025
- sedimentary rock – Jan 2026
- soil – Aug 2025, June 2025
- solar energy – June 2026
- solar radiation – June 2026
- storm surge – June 2025
- stromatolites – Jan 2026
- subduction zone – Sample 2024
- submarine volcano – Aug 2026
- subsidence – Jan 2026
- surface ocean currents – Aug 2026
- tailings – Jan 2026
- temperature anomaly – June 2025
- urbanization – Aug 2025
- volcanic eruptions – June 2026
- volcano – Aug 2026, June 2026
- water flux – Sample 2024
- water quality – June 2025
- water vapor – Aug 2026
- weather conditions – June 2025
- weathering – June 2025
- wildfire – June 2025
- greenhouse effect – implied by "how an increase in greenhouse gases causes a rise in global temperatures"
Resources
Examples and discussion of resources for the learning, teaching, and assessment of HS-ESS2-2.
NGSS Dimensions
Performance expectation HS-ESS2-2 was developed using the following elements from the NRC document A Framework for K-12 Science Education:
- Analyzing and interpreting data: Analyze data using tools, technologies, and/or models (e.g., computational, mathematical) in order to make valid and reliable scientific claims or determine an optimal design solution.
- Earth Materials and Systems: Earth’s systems, being dynamic and interacting, cause feedback effects that can increase or decrease the original changes.
- Weather and climate: The foundation for Earth’s global climate systems is the electromagnetic radiation from the sun, as well as its reflection, absorption, storage, and redistribution among the atmosphere, ocean, and land systems, and this energy’s re-radiation into space.
- Stability and change: Feedback (negative or positive) can stabilize or destabilize a system.
- Influence of engineering, technology, and science on society and the natural world: New technologies can have deep impacts on society and the environment, including some that were not anticipated. Analysis of costs and benefits is a critical aspect of decisions about technology.