Free Printable WorksheetScienceGrade 9Science CurriculumNGSS HS-ESS2-4

9.123 Winds and Global Circulation Worksheet

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Worksheet Overview & Skills Covered

Core academic competencies and curriculum alignment

This Physical Science with Earth and Science Science worksheet provides structured practice on 9.123 Winds and Global Circulation. Students are guided through targeted exercises that build foundational understanding, computational accuracy, and critical thinking skills.

Winds and Global Circulation: MCQ focus: connect uneven heating, pressure gradients, Coriolis effect, convection, and global wind belts. Aligned to NGSS high school Physical Science, Earth and Space Science, and Engineering Design; NRC/DCI; SEP/CCC; CCSS math/literacy connections; selected CA NGSS, NYSSLS, Florida CPALMS, and Texas TEKS references NGSS HS-ESS2-4 - NGSS-aligned Winds and Global Circulation: NGSS: HS-ESS2-4; NRC/DCI: ESS2.D; SEP/CCC: Models / Systems; Common: RST.9-10.7; State refs: CA/NYSSLS same HS-ESS PE family; FL SC.912.E.7; TX Earth Systems 112.49.

Whether you are an educator preparing classroom handouts, a tutor reinforcing weekly topics, or a parent supporting homeschool learning, this printable resource gives students the deliberate practice required to achieve subject fluency and master state standards.

Grade

Physical Science with Earth and Science

Subject

Science

Domain

Science Curriculum

Formats

PDF & DOCX

Sample Practice Problems

Preview the types of problems and questions covered in this worksheet

Below are sample questions representative of the exercises included on this worksheet and related 9.123 Winds and Global Circulation skill assessments:

Problem 1Difficulty: Mastery

Which statement best describes global circulation as an Earth system rather than a list of separate wind names?

AGlobal winds are random surface events that do not affect climate patterns.

BHeating, pressure gradients, convection, Coriolis deflection, and wind belts interact to move energy and moisture.

CCoriolis alone determines climate, so heating and pressure can be ignored.

DEach wind belt forms independently and has no connection to pressure or heating.

Solution & Explanation:Global circulation is a connected system. Uneven heating drives pressure and convection patterns, Earth's rotation deflects motion, and the resulting winds redistribute heat and moisture.

Problem 2Difficulty: Mastery

Use the model-labeling image for this question. A blank global circulation map already shows pressure belts at 0 degrees, 30 degrees, 60 degrees, and 90 degrees. Which set of labels would best complete the model?

AHigh pressure at every latitude because air is always sinking.

BLow at 0 degrees, high at 30 degrees, low at 60 degrees, high at 90 degrees.

CHigh at 0 degrees, low at 30 degrees, high at 60 degrees, low at 90 degrees.

DLow pressure at every latitude because air is always rising.

Solution & Explanation:Global circulation models usually show equatorial lows, subtropical highs, subpolar lows, and polar highs. Those belts connect vertical air motion to surface winds.

Problem 3Difficulty: Mastery

Which variable is least necessary in a basic model explaining global wind belts?

AOcean salinity differences between basins.

BCoriolis deflection from Earth's rotation.

CUneven solar heating by latitude.

DPressure gradients between belts.

Solution & Explanation:A basic wind-belt model needs uneven heating, convection, pressure gradients, and Coriolis deflection. Ocean salinity can affect ocean circulation, but it is not a core driver of atmospheric wind belts.

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QWhat grade level and standards does this worksheet align with?

This worksheet is designed specifically for Physical Science with Earth and Science Science students. It aligns with educational standard NGSS HS-ESS2-4 (NGSS: HS-ESS2-4; NRC/DCI: ESS2.D; SEP/CCC: Models / Systems; Common: RST.9-10.7; State refs: CA/NYSSLS same HS-ESS PE family; FL SC.912.E.7; TX Earth Systems 112.49.).