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
Format: Book Part
Language:English
Published: Open Book Publishers 2020
Subjects:
Ice
Online Access:https://dx.doi.org/10.17863/cam.81060
https://www.repository.cam.ac.uk/handle/1810/333643
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spelling ftdatacite:10.17863/cam.81060 2024-02-04T10:01:06+01:00 Ice ... Dowdeswell, Julian 2020 https://dx.doi.org/10.17863/cam.81060 https://www.repository.cam.ac.uk/handle/1810/333643 en eng Open Book Publishers open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 3705 Geology 13 Climate Action 14 Life Below Water Chapter chapter Book chapter BookChapter 2020 ftdatacite https://doi.org/10.17863/cam.81060 2024-01-05T09:42:30Z 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 DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
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. ...
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://dx.doi.org/10.17863/cam.81060
https://www.repository.cam.ac.uk/handle/1810/333643
genre Ice
permafrost
Sea ice
genre_facet Ice
permafrost
Sea ice
op_rights open.access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.81060
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