Ice

With an average surface temperature of 15°C (and rising), much of our planet is inhospitable to ice. Today, less than 2% of Earth’s water exists in a frozen form, locked up in glaciers and ice sheets, sea ice and permafrost. This ‘cryosphere’ is critically important for controlling global sea level...

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Bibliographic Details
Main Author: Dowdeswell, Julian
Other Authors: Tortell, Philippe
Format: Book Part
Language:English
Published: Open Book Publishers 2020
Subjects:
Ice
Online Access:https://www.repository.cam.ac.uk/handle/1810/333643
https://doi.org/10.17863/CAM.81060
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spelling ftunivcam:oai:www.repository.cam.ac.uk:1810/333643 2024-01-14T10:07:34+01:00 Ice Dowdeswell, Julian Tortell, Philippe 2020-04 application/pdf https://www.repository.cam.ac.uk/handle/1810/333643 https://doi.org/10.17863/CAM.81060 eng eng Open Book Publishers Earth 2020 https://www.repository.cam.ac.uk/handle/1810/333643 doi:10.17863/CAM.81060 Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ 37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 3705 Geology 13 Climate Action 14 Life Below Water Book chapter 2020 ftunivcam https://doi.org/10.17863/CAM.81060 2023-12-21T23:23:49Z With an average surface temperature of 15°C (and rising), much of our planet is inhospitable to ice. Today, less than 2% of Earth’s water exists in a frozen form, locked up in glaciers and ice sheets, sea ice and permafrost. This ‘cryosphere’ is critically important for controlling global sea level and the distribution of the planet’s fresh water, yet it has always existed in a rather perilous state. In contrast, the ice caps on Mars and the frozen surface of Jupiter’s moon, Europa, enjoy a much colder and more stable existence. To understand the impacts of climate change on Earth’s cryosphere, it is necessary to examine the different components of our icy world separately, for each has its own sensitivity to local and global forces. Book Part Ice permafrost Sea ice Apollo - University of Cambridge Repository
institution Open Polar
collection Apollo - University of Cambridge Repository
op_collection_id ftunivcam
language English
topic 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3705 Geology
13 Climate Action
14 Life Below Water
spellingShingle 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3705 Geology
13 Climate Action
14 Life Below Water
Dowdeswell, Julian
Ice
topic_facet 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3705 Geology
13 Climate Action
14 Life Below Water
description With an average surface temperature of 15°C (and rising), much of our planet is inhospitable to ice. Today, less than 2% of Earth’s water exists in a frozen form, locked up in glaciers and ice sheets, sea ice and permafrost. This ‘cryosphere’ is critically important for controlling global sea level and the distribution of the planet’s fresh water, yet it has always existed in a rather perilous state. In contrast, the ice caps on Mars and the frozen surface of Jupiter’s moon, Europa, enjoy a much colder and more stable existence. To understand the impacts of climate change on Earth’s cryosphere, it is necessary to examine the different components of our icy world separately, for each has its own sensitivity to local and global forces.
author2 Tortell, Philippe
format Book Part
author Dowdeswell, Julian
author_facet Dowdeswell, Julian
author_sort Dowdeswell, Julian
title Ice
title_short Ice
title_full Ice
title_fullStr Ice
title_full_unstemmed Ice
title_sort ice
publisher Open Book Publishers
publishDate 2020
url https://www.repository.cam.ac.uk/handle/1810/333643
https://doi.org/10.17863/CAM.81060
genre Ice
permafrost
Sea ice
genre_facet Ice
permafrost
Sea ice
op_relation https://www.repository.cam.ac.uk/handle/1810/333643
doi:10.17863/CAM.81060
op_rights Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.17863/CAM.81060
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