Chapter 18 · Unit 6: Processes that Shape Earth · Segment 3

The Water Cycle

What moves Earth's water from place to place, what makes it change between solid, liquid and gas, and why can the same water end up in so many different places?

MS-ESS2-4 · assessesMS-ETS1-4 · assessesMS-ETS1-3 · assessesMS-ESS3-1 · supports Textbook pp. 232–243 1 presentation · 10 worksheets · 3 labs

Overview

Students figure out that Earth's water is never used up and never created: the same water moves between the ocean, the air, the land, the ground and living things, changing state as it goes. They work out which moves need water to gain energy from the Sun (evaporation, transpiration, melting, sublimation), which happen when water gives energy off as it cools (condensation, freezing, deposition), and which are powered by gravity (precipitation, runoff, infiltration, groundwater flow). They build and test a solar distiller, measure evaporation and transpiration in the schoolyard, and run a dice-driven model of water's many routes. The chapter closes the loop on Lesson 17's rock cycle: the Sun, not Earth's interior, does most of the work here, and it sets up Lesson 19's question of why water, including groundwater, is spread so unevenly.

Estimated class time: presentation about 127 minutes · worksheets about 415 minutes in total · labs 6 sessions. Seven class periods of about 50 minutes: two for the presentation and the first worksheets, three lab days (Lab 2 spans two short sessions on consecutive days and Lab 1 spans three short sessions), and two for synthesis, transfer and assessment. Lab 1 needs sunny windows or warm lamps, so check the weather and the room before scheduling. The sequence is tight: not every worksheet fits in class time, so assign W2, W3 or W5 as homework and choose W8 or W9 (or add an eighth period) as time allows.

Phenomenon

Snow in April, faucets in August

In early April the Sierra Nevada is buried under a snowpack that can be several meters deep. By late August the same slopes are bare granite and dry grass, and almost none of that snow is left. Yet in August, hundreds of kilometers away, canals in the Central Valley still carry water to farms, and wells in valley towns still pump water from hundreds of meters underground. The snow did not vanish. Something moved it, in stages, from the mountain tops to the valley floor, to the air, to the sea and to deep below the ground.

Notice and wonder prompts

  • Notice: the snow disappears in a few months, but there is no giant drain at the bottom of the mountain. Where could it go?
  • Wonder: how could water that fell as snow in the mountains end up hundreds of meters underground in the valley?
  • Wonder: what has to happen to snow before it can rise into the air, and what has to happen before it can fall back down?
  • Predict: of the snow that melts, what fraction reaches the ocean, and what fraction never gets there?

Learning targets

  • I can describe the main processes of the water cycle and name the change of state, if any, that each one involves.
  • I can explain how the Sun's energy and the force of gravity together drive the cycling of water, and say which processes each one powers.
  • I can use a particle model to explain why water evaporates well below its boiling point and why water vapor condenses when air cools or becomes saturated.
  • I can trace several different routes water can take through the ocean, atmosphere, land, groundwater and living things, and explain why the cycle has no fixed order.
  • I can use data from tests of a water-collecting design to decide what to change and improve it.

What shows the learning happened

  • A labeled water cycle model (W4) that shows at least two different routes, names the change of state at each step, and marks each process as Sun-driven, gravity-driven or caused by cooling.
  • A CER paragraph (W6) that uses a lake's water budget to argue that evaporation and releases, not a dam leak, explain a summer drop in its level.
  • A completed Lab 1 design log with output measurements for at least two design versions and a data-based decision about what to change next, plus a W9 design that combines the best-performing prototype features.
  • Evaporation-rate and transpiration measurements from Lab 2 with a written comparison of sun versus shade.
  • A Lab 3 route record and class-data analysis that ranks the reservoirs by how long water tends to stay in them.
  • A mastery quiz (W10) score showing the student can match processes to energy sources and changes of state.

Key vocabulary 12 terms

water cycleThe continuous movement of water among the ocean, the atmosphere, the land, the ground and living things, with water changing between solid, liquid and gas along the way. The Sun's energy and gravity keep it moving.A hydrologist uses the water cycle to explain how rain that fell in the mountains can show up in a valley well years later.
water vaporWater in its gas state. It is invisible. Clouds, fog and the mist above a kettle are not vapor; they are tiny liquid droplets or ice crystals you can see.On a humid day the air over the bay holds far more water vapor than the air over the desert, even though both look clear.
evaporationThe change of liquid water into water vapor at the surface of the liquid. It happens at any temperature because the fastest-moving molecules at the surface can escape, so a puddle dries without ever boiling.Evaporation from the reservoir was high during the heat wave, so the water level dropped even though no water was released.
transpirationThe movement of water from a plant's roots up to its leaves, where it evaporates inside the leaf and escapes through tiny pores called stomata as water vapor.A single large tree can move hundreds of liters of water into the air by transpiration on a hot summer day.
condensationThe change of water vapor into liquid water. It happens when air cools or becomes saturated, so that vapor molecules slow down and cling together, usually on a surface or on tiny particles in the air. Condensation releases energy to the surroundings.Condensation on the inside of the tent wall overnight came from the campers' own breath.
crystallization (freezing and deposition)The change of water into solid ice. Liquid water freezing into ice is one kind; water vapor turning directly into ice crystals, as frost or snowflakes, is another kind that scientists call deposition. Both release energy to the surroundings.The frost on the windshield formed by deposition: water vapor became ice crystals without ever being liquid.
sublimationThe change of ice directly into water vapor without melting first. It is why snow can shrink on a cold, dry, sunny day even though the temperature stays below freezing.Part of the Sierra snowpack is lost to sublimation each winter, so not all of the snow becomes stream water.
precipitationWater that falls from clouds to Earth's surface as rain, snow, sleet or hail, pulled down by gravity once droplets or ice crystals have grown heavy enough.Most of California's precipitation arrives between November and March, which is why reservoirs and snowpack matter so much.
runoffWater that flows across the land surface, downhill under gravity, into streams, rivers, lakes and eventually the ocean.After the storm, runoff from the paved parking lot reached the creek in minutes, while the forest soil soaked its share up.
infiltrationThe soaking of water from the surface down into the ground through the spaces in soil and rock, also driven by gravity.Infiltration was slow in the clay field but fast in the sandy field, so the two fields flooded very differently.
groundwaterWater that fills the tiny connected spaces, called pores, between grains of soil, sand, gravel and rock below the surface. It moves slowly and can stay underground for years to thousands of years.The well draws groundwater from about 150 meters down, and the water it pumps may have fallen as rain centuries ago.
aquiferA body of sediment or rock with enough connected pore space, and enough water in it, to supply a well or a spring.The Central Valley aquifer system supplies a large share of the water that valley farms and towns use in a dry year.

Standards alignment

California NGSS, Grade 7 Preferred Integrated Course Model. Each entry says whether this chapter's work assesses the performance expectation, gives practice toward it, or supports it as background; the resource lists below repeat this for every worksheet and lab.

MS-ESS2-4Assesses: developing and using a model of water cycling powered by sunlight and gravityCA Grade 6

Develop a model to describe the cycling of water through Earth’s systems driven by energy from the sun and the force of gravity.

This is a California Grade 6 performance expectation in the Preferred Integrated model, so seventh graders are revisiting it; the textbook places it here. Students develop conceptual models (W4, the W10 synthesis, Lab 3) and work with a physical model and field evidence (Lab 1, Lab 2) of water changing state and moving through Earth's systems, and explain which moves the Sun powers and which gravity powers. Quantitative latent heat is not assessed.

Assessment boundary: A quantitative understanding of the latent heats of vaporization and fusion is not assessed.

MS-ETS1-4Assesses: generating data from a model for iterative testing and modification, through Lab 1CA Grade 6-8

Develop a model to generate data for iterative testing and modification of a proposed object, tool, or process such that an optimal design can be achieved.

In Lab 1 students build a working solar distiller, measure its output, change one feature, retest and record the result over two rounds; the design log and output data are evidence for this PE. Elsewhere in the chapter the PE is practiced, not assessed.

MS-ETS1-3Assesses: analyzing test data from several designs to combine their best features, through W9CA Grade 6-8

Analyze data from tests to determine similarities and differences among several design solutions to identify the best characteristics of each that can be combined into a new solution to better meet the criteria for success.

W9 assesses this PE: students analyze side-by-side test data from six solar still prototypes, identify the best characteristic of each, and combine them into a new design. The Lab 1 class results table and the slide 22 design-data task practice the same move.

MS-ESS3-1Supports: groundwater as an unevenly distributed resourceCA Grade 7

Construct a scientific explanation based on evidence for how the uneven distributions of Earth’s mineral, energy, and groundwater resources are the result of past and current geoscience processes.

Aquifers, infiltration and the California connection slides give students the background they need for Lesson 19's explanation of why groundwater resources are distributed unevenly; this chapter does not assess the explanation itself.

Science and engineering practices

  • Developing and Using Models. Students draw a water cycle model with multiple routes (W4), trace routes from evidence cards (W8), run a dice-driven systems model that generates class data (Lab 3), and build physical models of evaporation and condensation (Labs 1 and 2).
  • Planning and Carrying Out Investigations. In Lab 2 students decide where to place evaporation trays and transpiration bags, control what they can, and collect measurements over a day in the schoolyard.
  • Analyzing and Interpreting Data. Students compute evaporation rates, compare distiller outputs across the class, and turn Lab 3 tallies into estimates of how long water stays in each reservoir (W5, Labs 1-3).
  • Constructing Explanations and Designing Solutions. Students argue in CER form from a lake's water budget (W6), and improve solar still designs from test data (their own in Lab 1, a prototype test report in W9).

Disciplinary core ideas

  • ESS2.C The Roles of Water in Earth's Surface Processes. The whole chapter: water moves among reservoirs by evaporation, transpiration, condensation, crystallization, precipitation, runoff, infiltration and groundwater flow, driven by sunlight and gravity.
  • ETS1.B Developing Possible Solutions. Students test solar distiller designs and use the results to improve them; the fog-catcher story shows the same test-and-modify loop at full scale.
  • ETS1.C Optimizing the Design Solution. Students compare class designs, identify the features that raised output, and propose a combined design (Lab 1, W9).

Crosscutting concepts

  • Energy and Matter. Every change of state is tracked as water gaining energy (from the Sun) or giving energy off (as it cools); gravity moves the matter downhill. The amount of water is conserved as it cycles.
  • Systems and System Models. Students treat the ocean, atmosphere, snowpack, rivers, soil, plants and aquifers as connected parts of one system, and judge what each model shows and leaves out.
  • Cause and Effect. Students reason from causes (heating, cooling, saturation, gravity) to effects (a drying puddle, dew on a cold can, a flowing spring) and back.

Presentation 26 slides

The Water Cycle: the Sun lifts it, gravity brings it back. Original, editable slides with speaker notes: a phenomenon opener, learning targets, the chapter's concepts with diagrams, vocabulary in context, 3 checks for understanding, 2 discussion prompts, an application task, a misconception check, a synthesis and an exit ticket.

Worksheets 10 of 10

Ten different tasks, one per instructional blueprint. Each has a student PDF (low ink, US Letter), an editable DOCX, an HTML preview, and a separate teacher answer key with reasoning.

First page of Twelve Places, One Cycle: An Evidence Jigsaw on Sun, Cooling and Gravity
Worksheet 8 · Collaborative investigation

Twelve Places, One Cycle: An Evidence Jigsaw on Sun, Cooling and Gravity

I can use evidence from many places on Earth to sort water cycle processes by their driver, trace several different routes a water molecule could take, and defend the idea that the cycle has no fixed order.

55 minjigsawPracticeCollaborationDiscussionData analysis MS-ESS2-4 · practice
First page of Design Challenge: A Solar Still That Runs on the Water Cycle
Worksheet 9 · Transfer and design

Design Challenge: A Solar Still That Runs on the Water Cycle

I can analyze test data from several solar still prototypes, combine their best features into an improved design, plan the next test, and justify my choices with the criteria, the constraints and the science of evaporation, condensation and gravity.

50 minpairsExtensionEngineering designData analysisWriting MS-ETS1-3 · assessesMS-ETS1-4 · practiceMS-ESS2-4 · supports

Collaborative labs 3 of 3

Three different investigation approaches. Each has a teacher guide (purpose, materials with quantities, estimated cost, prep, safety, procedure, expected observations, debrief, answer key, assessment criteria, accessibility adaptations, low-cost alternative) and a student recording sheet.

First page of the Build, Test, Improve: a Solar Distiller That Runs on Sunlight and Gravity recording sheet
Lab 1 · Engineering design challenge

Build, Test, Improve: a Solar Distiller That Runs on Sunlight and Gravity

How can you change a simple solar still so it turns more salt water into fresh water in a day, and how will your test data tell you whether the change helped?

Groups of 43 sessions120 min activityEst. 10 to 20 per classLarge clear bowl or clear food-storage container, about 2 to 3 L, at least 20 cm acrossSmall cup, shorter than the bowl is deep (a 100 mL plastic cup or a clean yogurt cup)Plastic wrap MS-ETS1-4 · assessesMS-ETS1-3 · practiceMS-ESS2-4 · practice
First page of the Reading the Schoolyard: Evaporation and Transpiration in Sun and Shade recording sheet
Lab 2 · Classroom field investigation

Reading the Schoolyard: Evaporation and Transpiration in Sun and Shade

How much faster does water leave an open tray, and a living plant, in full sun than in shade, and what does that tell us about what powers the upward half of the water cycle?

Groups of 42 sessions65 min activityEst. 8 to 15 per classIdentical shallow trays, about 20 to 30 cm across (aluminum baking pans, plastic food-container lids with a rim, or plant saucers)Measuring cup or 500 mL bottle for filling the traysRuler marked in millimeters MS-ESS2-4 · practice
First page of the Roll the Dice: Where Does a Water Molecule Go, and How Long Does It Stay? recording sheet
Lab 3 · Collaborative systems modeling

Roll the Dice: Where Does a Water Molecule Go, and How Long Does It Stay?

If you follow one water molecule through a chance-based model of the water cycle, where does it spend most of its time, which processes move it, and how well does the model match Earth's real reservoirs?

Groups of 31 session42 min activityEst. 0 to 15 per classStation signs printed from the station rules table (one per reservoir, large type)Six-sided diceRecording sheet MS-ESS2-4 · assesses

Teacher guidance

Suggested sequence (7 steps)
  1. Period 1: Presentation slides 1-9 (phenomenon, where water is, evaporation and transpiration). W1 phenomenon worksheet at the start; W2 vocabulary for homework. Set up Lab 2 trays and bags in the last 20 minutes so they run overnight.
  2. Period 2: Collect Lab 2 measurements first (25 minutes). Then slides 10-14 (cooling, condensation, crystallization, sublimation; discussion of what clouds are made of).
  3. Period 3: Slides 15-18 (gravity's half: precipitation, runoff, infiltration, aquifers, the California connection). W3 reading and W4 diagram worksheet.
  4. Period 4: Lab 1 session 1: build the first solar distiller, start it under light, record the design. Slides 19-20 (energy accounting and residence times) while stills run.
  5. Period 5: Lab 1 session 2: measure the first run, change one feature, restart. Lab 3 dice model in the second half; W5 data worksheet for homework.
  6. Period 6: Lab 1 session 3: final measurements and the class comparison table. Slides 21-24 (routes discussion, design-data task, fog catchers, misconception). W6 CER and W7 misconception repair.
  7. Period 7: W8 collaborative stations or jigsaw, W9 transfer challenge, slides 25-26 synthesis and exit ticket. W10 mastery quiz the following day.

Materials overview: Clear bowls or food containers, small cups, plastic wrap, rubber bands, small pebbles or coins, table salt, food coloring, a desk lamp with a warm (incandescent or halogen) bulb if the room lacks sun, shallow trays, zip-top bags, string, rulers, a 10 mL syringe or small graduated cylinder, dice, printed station cards, and optional colored beads. Everything is available from a grocery or hardware store; the three labs together cost an estimated 20 to 50 dollars per class, mostly in reusable items.

Common misconceptions (6)
“Water has to boil before it can turn into a gas, so lakes and puddles only evaporate when it is very hot.”
Why it happens: The only time most students have watched liquid become gas on purpose is a boiling pot. Evaporation from a puddle is invisible and slow.
Correction: At any temperature, some surface molecules move fast enough to escape; evaporation is just faster when it is warmer, windier or drier. Boiling is a special case where bubbles of vapor form inside the liquid.
“Clouds, fog and the cloud above a kettle are water vapor.”
Why it happens: Everyday language calls the visible white cloud 'steam' or 'vapor', and vapor itself cannot be seen, so the visible thing gets the name.
Correction: Water vapor is an invisible gas. What you can see in a cloud, in fog, or above a kettle is liquid droplets (or ice crystals) that have already condensed.
“The water on the outside of a cold can leaked through the metal from inside.”
Why it happens: The droplets appear only on cold containers that are full of liquid, so the liquid inside looks like the obvious source.
Correction: The droplets are water vapor from the surrounding air that condensed on the cold surface. A sealed, empty, cold can sweats just the same, and a warm full can does not.
“The water cycle is one loop in a fixed order: ocean to cloud to rain to river to ocean.”
Why it happens: Almost every diagram students have seen draws a single circle with four arrows.
Correction: Water can skip places and repeat places: rain can evaporate before it hits the ground, groundwater can feed a river or flow straight to the sea, snow can sublimate, and a molecule can spend a week in the air or thousands of years in the ocean or an aquifer.
“Groundwater sits in underground lakes and rivers, like caves full of water.”
Why it happens: The word 'water' plus 'underground' brings to mind the only underground water students have seen in pictures: cave pools.
Correction: Nearly all groundwater fills the tiny pores between grains of sand, gravel and rock, like water held in a sponge. It moves slowly through connected pores; an aquifer is a layer that holds enough of it to supply a well.
“Condensation and freezing are 'powered by' the Sun or by gravity, just like the other steps.”
Why it happens: The chapter's framing that the Sun and gravity drive the whole cycle gets applied to every single step.
Correction: Condensation and crystallization happen when water loses energy as it cools (or when air becomes saturated). The Sun and gravity drive the cycle as a whole, including lifting the moist air that later cools, but these two changes are water giving energy off, not taking it in.
Differentiation suggestions (5)
  • Multilingual learners: Provide a bilingual process card that pairs each process name with its change of state and an icon (arrow up for Sun-driven, arrow down for gravity-driven, snowflake for cooling). Allow labeling of the W4 model in the home language first, then in English. Pre-teach 'vapor', 'pore' and 'saturated' with physical objects: a sponge, a cold can, a sealed jar.
  • Students who need more support: Give a partially completed water cycle model with the reservoirs drawn and the arrows blank, and a word bank of the nine processes. In Lab 3, let them move the token with a partner and record only the place names, adding process names in the debrief. Use the sentence starters in the W1 scaffold and the two-column organizer in the W6 scaffold.
  • Students ready for extension: Ask them to add residence times to their W4 model and defend the ordering, to design a Lab 3 rule change for a drought year or a warmer climate and predict how the class data would shift, or to estimate how large a solar still would need to be to supply one person's drinking water from their Lab 1 rate.
  • Students who need movement or alternative output: Lab 3 is physical by design: students walk between stations. For written tasks, accept a narrated route recording, a labeled photo of a physical model, or a short video explanation of the sweating can. Lab 2's outdoor measurements can be the main evidence for the investigation target.
  • Students with limited access to outdoor space or sunlight: Lab 2 can run on an indoor windowsill versus a shaded shelf, and Lab 1 can run under a warm desk lamp. The data will be smaller but the comparisons still work; the labs' accessibility and low-cost notes say so.
Accuracy notes: where the textbook simplifies (11)
  • Transpiration: the lesson's section 1 says liquid water leaves the leaf through the stomata and then evaporates. In plants, water evaporates from cell surfaces inside the leaf and exits the stomata already as vapor, which is what the lesson's own concept spread says. We teach the vapor-exits version.
  • Crystallization: the lesson uses one word for both liquid-to-solid (freezing) and gas-to-solid changes. Scientists call the gas-to-solid change deposition (frost, many snowflakes). We keep the textbook term because it is also the NGSS wording and add the two precise terms. Ice crystals are built from water molecules, not from 'atoms' as the lesson states.
  • 'Powered by the Sun or gravity': the concept spread says every one of the nine processes is powered by one of the two. Condensation and crystallization are not; they happen when water vapor gives off energy as it cools, often in rising, expanding air, or when air becomes saturated. The Sun and gravity drive the cycle as a whole. We say so on the slides and in the misconception list.
  • The 90 percent (evaporation) and 10 percent (transpiration) split for atmospheric moisture is a rough estimate; a very small share also comes from sublimation of ice and snow, which the lesson never names. We teach 'roughly nine tenths' and add sublimation as a real pathway.
  • Clouds: the lesson summary says clouds can be made of 'crystallized water vapor that has condensed', which muddles the two changes. Clouds are made of liquid droplets, ice crystals, or both; water vapor itself is invisible.
  • Freezing temperature: the lesson ties crystallization to the air dropping below the freezing point. Being below 0 °C is necessary but not sufficient; cloud droplets often stay liquid (supercooled) far below 0 °C until a particle or an ice crystal starts freezing. We avoid stating a temperature rule.
  • Raindrop sizes in the lesson's precipitation figure (2 mm, 5 mm) are not labeled as diameters or radii, and published breakup sizes vary. We teach only the shape pattern: small drops are round, larger falling drops flatten underneath because air pushes up on them, very large drops break apart; raindrops are not teardrop-shaped.
  • Fog catchers: the lesson says smaller holes and finer material collect the most water. Research shows a best balance rather than 'smaller is always better': a nearly solid surface makes fog flow around it. Our design-data task and W9 use test data that show the trade-off.
  • Atacama figures (population, rainfall, 'for the first time', the 1950s student) are dated or simplified; the inventor is usually described as the Chilean scientist and professor Carlos Espinosa Arancibia. We do not test these details.
  • Residence times (how long water typically stays in a reservoir) are not in the lesson. The values we use, about nine days in the atmosphere, months in rivers, years to centuries in lakes, years to thousands of years in groundwater, and thousands of years in the ocean, are approximate estimates that vary by source, and the slides say so.
  • California figures: the Sierra snowpack supplies roughly 30 percent of the state's water in a typical year by the state's own estimate, and parts of the San Joaquin Valley have sunk by several meters over the past century as groundwater was pumped out faster than it was replaced. Both are stated as approximate and are not quiz items.

Review status: reviewed · 2026-10-19 · Resumed after both authors were interrupted: W8 q2's example routes broke the sheet's own rule (two pairs shared four cards); rewrote it with three routes that share at most two cards per pair, one avoiding the ocean. Presentation estimatedMinutes (127) equals the pacing sum and every bullet is within 110 characters. Science fixes: slide 4 bar and caption (lakes, rivers, soil, air and living things hold about 0.02 percent of Earth's water, not 0.1); lake residence time is years to centuries (slide 20, Lab 3 table and key, accuracy notes); slide 19 no longer credits condensation for mild cloudy nights; slide 23 fog forms from moist air chilled over a cold ocean; W3 calls the sun and gravity two drivers rather than two forces, says evaporated water returns to the air rather than 'to the sea', and says pumps lift water uphill rather than only over ridges; W7 rule no longer says gravity never heats. Keys and arithmetic re-solved for all ten worksheets and three labs; distiller data in slide 22, W9 and Lab 1 checked. Fixed: W10 points (synthesis now 8, equal to items 1-6; total 25); W5 q10 ratio (3.3 to 4.4 times); W9 basin described as about 1 cm of water so its outputs are physically realistic, and the 58 C water is no longer called safe to touch; Lab 1 q9 example (the basic still already has the pebble, and 6 to 11 mL is not a doubling) and q5 scale range; Lab 3 driver and roll-share statements recomputed from the rule probabilities; W4 Route 2 no longer sends groundwater from the field uphill to the spring on the far side. Originality: a 6-word scan against the lesson text found echoes in ten strings (including the W10 snowy-city scene, which repeated the textbook opener's wording); all rewritten. W3 passage trimmed from 734 to 685 words. Standards: caGrade added to every lab standards entry (6 for MS-ESS2-4, 6-8 for ETS1); chapter role for MS-ETS1-3 raised to assesses to match W9, which meets the PE as written; MS-ESS2-4 notes state the Grade 6 placement throughout. Consistency: evidenceOfLearning, threeDimensions and fourteen slide links corrected to describe the worksheets as written (W6 is a lake water-budget CER, not the Sierra phenomenon; W5 has no reservoir shares; W8 has no contrail card); lab cost total corrected to an estimated 20 to 50 dollars; pacing now says not every worksheet fits seven periods. Safety: Lab 1 adds a teacher-only rule for warm water above 50 C; Lab 2 plant warning made accurate and the soil-drying suggestion no longer uses an oven. Labs remain physically untested, as their model limitations say; all datasets are labeled simulated.

Source references

Verified against the student edition of Bring Science Alive! 7th Grade Integrated (Student Edition). Printed page numbers appear in the book; PDF pages are the physical pages of the 524-page scan (printed + 36). The textbook is not reproduced on this site.

SectionPrinted pagesPDF pagesUsed for
Introduction: the kayaker, Sun energy versus Earth's interior, the four spheres232, 233268, 269Framing that the Sun, not Earth's interior, supplies most of the energy; the NGSS box listing MS-ESS2-4 and MS-ETS1-4.
1. Heating and the Water Cycle: evaporation and transpiration234, 235270, 271Particle model of evaporation, no starting point, transpiration and stomata, the 90/10 estimate, the sweat analogy; slides 6-9 and Lab 2.
2. Cooling and the Water Cycle: condensation and crystallization236, 237272, 273Condensation onto particles, energy released, the cold-window example, crystallization and frost; slides 10-14.
3. Gravity and the Water Cycle: precipitation, runoff, infiltration, groundwater238, 239274, 275Droplet growth and air resistance, runoff, infiltration, pores, aquifers and groundwater flow to the ocean; slides 15-18 and the aquifer layers diagram.
Key Science Concept: Global Processes in the Water Cycle240, 241276, 277The nine named processes including melting and groundwater flow; the basis for Lab 3's stations and the energy-accounting slide.
4. Designing a Fog Catcher: Atacama fog nets and iterative testing242, 243278, 279Fog as a ground-level cloud, droplets merging and draining by gravity, iterative testing with input and output data; slide 23, Lab 1 and W9.
Lesson Summary243279Checking that every summary idea is covered by a target; identified the muddled 'crystallized water vapor that has condensed' sentence recorded in accuracyNotes.

External references used for accuracy checks

  • Evaporation and the Water Cycle (U.S. Geological Survey, Water Science School): Evaporation below boiling, the approximate 90 percent share from open water, and sublimation as a minor source.
  • Condensation and the Water Cycle (U.S. Geological Survey, Water Science School): Clouds forming as rising air cools; energy released during condensation.
  • Aquifers and Groundwater (U.S. Geological Survey, Water Science School): Groundwater as water in pore spaces, the water table, and aquifers that supply wells.
  • The water cycle (National Oceanic and Atmospheric Administration (NOAA)): Deposition and sublimation as pathways; the simple loop as a useful but incomplete model.
  • Transport of Water and Solutes in Plants (Biology 2e, section 30.5) (OpenStax, Rice University): Water evaporates inside the leaf and leaves through stomata as vapor; stomata regulate the rate.
  • Snow Surveys and Water Supply Forecasting (California Department of Water Resources): The April 1 snowpack measurement and the approximate 30 percent share of the state's water supply.
  • How to get fresh water out of thin air (MIT News, Massachusetts Institute of Technology): Fog nets collect about 2 percent of fog water; finer meshes can collect more, but fog flows around near-solid surfaces.

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