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This work is supported by the National Science Foundation’s
Directorate for Education and Human Resources TUES-1245025, IUSE-
1612248, IUSE-1725347, and IUSE-1914915. Questions, contact education-AT-unavco.org
THERMAL EXPANSION OF WATER
An Important Contributor to Sea-Level Rise
Version: Jan 16, 2019
THERMAL EXPANSION
• Thermal expansion refers to
the tendency of matter to
change shape, area, and
volume in response to a
change in temperature.
• When a substance is heated,
the molecules begin to
vibrate and move more, and
maintain a larger
separation. This results in
the molecules taking up
greater volume.
WATER EXPANDS AS IT WARMS
THERMAL EXPANSION OF WATER
• As the ocean warms,
the density decreases.
Thus even at constant
mass the volume of the
ocean increases when
warmed.
• Thermal expansion
occurs at all ocean
temperatures and is a
major contributor to
sea-level changes.
THE MAJORITY OF ADDITIONAL ENERGY IN THE
EARTH’S CLIMATE SYSTEM IS STORED IN THE OCEANS
• Ocean warming
dominates the total
energy change
inventory.
Plot of energy accumulation in ZJ (1 ZJ =
1021 J) within distinct components of the
Earth’s climate system relative to 1971 and
from 1971 to 2010 unless otherwise
indicated (IPCC 2014).

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Overview of Thermal Expansion

  • 1. This work is supported by the National Science Foundation’s Directorate for Education and Human Resources TUES-1245025, IUSE- 1612248, IUSE-1725347, and IUSE-1914915. Questions, contact education-AT-unavco.org THERMAL EXPANSION OF WATER An Important Contributor to Sea-Level Rise Version: Jan 16, 2019
  • 2. THERMAL EXPANSION • Thermal expansion refers to the tendency of matter to change shape, area, and volume in response to a change in temperature. • When a substance is heated, the molecules begin to vibrate and move more, and maintain a larger separation. This results in the molecules taking up greater volume.
  • 3. WATER EXPANDS AS IT WARMS
  • 4. THERMAL EXPANSION OF WATER • As the ocean warms, the density decreases. Thus even at constant mass the volume of the ocean increases when warmed. • Thermal expansion occurs at all ocean temperatures and is a major contributor to sea-level changes.
  • 5. THE MAJORITY OF ADDITIONAL ENERGY IN THE EARTH’S CLIMATE SYSTEM IS STORED IN THE OCEANS • Ocean warming dominates the total energy change inventory. Plot of energy accumulation in ZJ (1 ZJ = 1021 J) within distinct components of the Earth’s climate system relative to 1971 and from 1971 to 2010 unless otherwise indicated (IPCC 2014).

Editor's Notes

  1. https://en.wikipedia.org/wiki/Thermal_expansion Image: https://upload.wikimedia.org/wikipedia/commons/a/ac/Thermal_expansion_cartoon.jpg (This file is licensed under the Creative Commons Attribution 4.0 International license.) Figure shows an example of a cold liquid (left) and hot liquid (right).
  2. Water expands as it warms and shrinks as it cools. Water is unusual in that it also expands when it turns to ice. Water is densest at ~4 degrees Celsius. Modified from http://janison.cyriljackson.wa.edu.au/Janison/Science/Physics2A2B/Physics2B/0_West1-2B/content/cell2_effects_heat/html/cc2_01.html#
  3. http://www.ipcc.ch/ipccreports/tar/wg1/411.htm Image: https://commons.wikimedia.org/wiki/File:Thermal_expansion_cartoon.jpg
  4. Energy in > energy out in the Earth system, which is leading to climate warming. This graph shows that ocean warming dominates the surplus energy change inventory. http://www.climatechange2013.org/images/figures/WGI_AR5_FigBox3.1-1.jpg IPCC=Intergovernmental Panel on Climate Change IPCC2014: Ocean warming dominates the total energy change inventory, accounting for roughly 93% on average from 1971 to 2010 (high confidence). The upper ocean (0–700 m) accounts for about 64% of the total energy change inventory. Melting ice (including Arctic sea ice, ice sheets, and glaciers) accounts for 3% of the total, and warming of the continents 3%. Warming of the atmosphere makes up the remaining 1%. “Ocean warming (heat-content change) dominates, with the upper ocean (light blue, above 700 m) contributing more than the mid-depth and deep ocean (dark blue, below 700 m; including below 2000 m estimates starting from 1992). Ice melt (light grey; for glaciers and ice caps, Greenland and Antarctic ice sheet estimates starting from 1992, and Arctic sea ice estimate from 1979 to 2008); continental (land) warming (orange); and atmospheric warming (purple; estimate starting from 1979) make smaller contributions. Uncertainty in the ocean estimate also dominates the total uncertainty (dot-dashed lines about the error from all five components at 90% confidence intervals).“