MS-ESS2-4 • Grades 6–8

Water Properties & Ice

Water is one of the most unusual substances on Earth — it exists naturally in all three states, absorbs and releases heat more slowly than almost any other material, and behaves differently depending on whether it freezes from ocean water or breaks off a glacier.

Water Facts Booklet & Heat Capacity

Water's unique properties — especially its high heat capacity — are what make Earth's climate livable. Oceans absorb enormous amounts of heat in summer and release it slowly in winter, moderating temperatures far more than land surfaces do.

Water facts booklet organizer

Water Facts Booklet

A student booklet covers key water properties including chemical formula, states of matter, density, and surface tension.

Water facts booklet example page showing heat capacity

Heat Capacity Page

One booklet page focuses on heat capacity — why oceans warm and cool more slowly than land, and how this drives coastal climates.

Why water's heat capacity matters for climate

Water absorbs about four times more heat per degree than most land surfaces. This is why coastal cities have milder, more stable temperatures than inland cities at the same latitude — the ocean is constantly absorbing and releasing heat, smoothing out the extremes. Ocean currents driven by this heat difference are one of the primary forces that distribute warmth around the planet.

Three States of Water

Water is the only substance found naturally in all three states on Earth's surface. Understanding the transitions between states — and the energy required for each — is essential for understanding both the water cycle and weather processes.

Three states of water and phase transitions A triangle diagram showing solid ice, liquid water, and water vapor with labeled arrows showing all six phase transitions between them. Water vapor Gas state Ice Solid state Liquid water Liquid state Deposition Sublimation Condensation Evaporation Melting Freezing

Sea Ice vs. Icebergs

Sea ice and icebergs are both frozen water — but they form differently, consist of different types of water, and play different roles in Earth's climate system.

Sea ice vs icebergs Side-by-side comparison of sea ice as a thin frozen ocean surface layer, and an iceberg showing approximately 10% above and 90% below the waterline. Sea Ice Forms from frozen ocean water Ice layer (1 to 3 meters thick) Salt water ocean below Salt water; forms and melts seasonally Reflects sunlight; regulates Earth's temperature Iceberg Chunk of freshwater glacier ice ~10% above ~90% below sea level Fresh water; breaks off glaciers (calving) Most mass hidden below the surface

Sea Ice vs. Iceberg Venn Organizer

A three-flap Venn organizer gives students a structured way to compare sea ice and icebergs — recording what is unique to each and what they share in the overlapping center section.

Sea ice vs iceberg three-flap Venn organizer

Sea Ice

  • Salt water
  • Thin flat layer
  • Seasonal — melts in summer
  • Reflects sunlight

Iceberg

  • Fresh water
  • Large floating mass
  • 90% below surface
  • Breaks off glaciers
MS-ESS2-4 • MS-ESS2-5 • MS-ESS2-6 • Grades 6–8

Want the Complete Weather & Climate Unit?

This page is one part of a full NGSS-aligned unit covering the hydrologic cycle, atmospheric layers, air pressure, fronts, storms, humidity, temperature, climate patterns, and more — with hands-on experiments, foldable organizers, vocabulary tools, and Check for Understanding pages throughout.

View the Full Unit on TPT