A Theory of Abrupt Climate Changes: Their Genesis and Anatomy
We combine our ice-sheet and climate models to formulate a deductive theory of abrupt climate changes pertaining to Heinrich/Dansgaard–Oeschger (H/DO) cycles and the last deglaciation punctuated by the Younger Dryas (YD). Since they are all accompanied by ice-rafted debris, we posit their common ori...
Published in: | Geosciences |
---|---|
Main Author: | |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2022
|
Subjects: | |
Online Access: | https://doi.org/10.3390/geosciences12110391 |
id |
ftmdpi:oai:mdpi.com:/2076-3263/12/11/391/ |
---|---|
record_format |
openpolar |
spelling |
ftmdpi:oai:mdpi.com:/2076-3263/12/11/391/ 2023-08-20T04:07:14+02:00 A Theory of Abrupt Climate Changes: Their Genesis and Anatomy Hsien-Wang Ou agris 2022-10-24 application/pdf https://doi.org/10.3390/geosciences12110391 EN eng Multidisciplinary Digital Publishing Institute Climate https://dx.doi.org/10.3390/geosciences12110391 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 12; Issue 11; Pages: 391 abrupt climate change Heinrich events Dansgaard–Oeschger cycles bond cycles younger dryas ice-sheet instability maximum entropy production Text 2022 ftmdpi https://doi.org/10.3390/geosciences12110391 2023-08-01T07:01:18Z We combine our ice-sheet and climate models to formulate a deductive theory of abrupt climate changes pertaining to Heinrich/Dansgaard–Oeschger (H/DO) cycles and the last deglaciation punctuated by the Younger Dryas (YD). Since they are all accompanied by ice-rafted debris, we posit their common origin in the calving of the ice sheet due to a thermal switch at its bed, which naturally endows abruptness to these climate signals of the millennial timescale characteristics of the ice-mass balance. To distinguish the H/DO cycles, we differentiate the thermal triggers by geothermal-heat/surface-melt in the calving of inland/coastal ice, which provide their respective freshwater sources. Since surface-melt requires post-H warmth during the glacial, but is already operative in the Holocene, the DO cycles are encased within the H cycle during the glacial, but self-sustaining in the Holocene. They otherwise share the same time signature, thus resolving this seeming puzzle of commonality without invoking unknown climate forcing. The DO cycles transcend deglaciation to produce the observed sequence, but the calving-induced freshwater flux needs to be boosted by the rerouting of continental meltwater to cause YD. We discern a key process of an eddying ocean in its millennial adjustment toward maximum entropy production (MEP), which would melt the H-induced sea ice to cause an abrupt post-H warming followed by a gradual cooling that anchors the DO cycles to form the hierarchical Bond cycle. Since the modelled anatomies resemble the observed ones, our theory may provide a robust and unified account of abrupt climate changes. Text Ice Sheet Sea ice MDPI Open Access Publishing Geosciences 12 11 391 |
institution |
Open Polar |
collection |
MDPI Open Access Publishing |
op_collection_id |
ftmdpi |
language |
English |
topic |
abrupt climate change Heinrich events Dansgaard–Oeschger cycles bond cycles younger dryas ice-sheet instability maximum entropy production |
spellingShingle |
abrupt climate change Heinrich events Dansgaard–Oeschger cycles bond cycles younger dryas ice-sheet instability maximum entropy production Hsien-Wang Ou A Theory of Abrupt Climate Changes: Their Genesis and Anatomy |
topic_facet |
abrupt climate change Heinrich events Dansgaard–Oeschger cycles bond cycles younger dryas ice-sheet instability maximum entropy production |
description |
We combine our ice-sheet and climate models to formulate a deductive theory of abrupt climate changes pertaining to Heinrich/Dansgaard–Oeschger (H/DO) cycles and the last deglaciation punctuated by the Younger Dryas (YD). Since they are all accompanied by ice-rafted debris, we posit their common origin in the calving of the ice sheet due to a thermal switch at its bed, which naturally endows abruptness to these climate signals of the millennial timescale characteristics of the ice-mass balance. To distinguish the H/DO cycles, we differentiate the thermal triggers by geothermal-heat/surface-melt in the calving of inland/coastal ice, which provide their respective freshwater sources. Since surface-melt requires post-H warmth during the glacial, but is already operative in the Holocene, the DO cycles are encased within the H cycle during the glacial, but self-sustaining in the Holocene. They otherwise share the same time signature, thus resolving this seeming puzzle of commonality without invoking unknown climate forcing. The DO cycles transcend deglaciation to produce the observed sequence, but the calving-induced freshwater flux needs to be boosted by the rerouting of continental meltwater to cause YD. We discern a key process of an eddying ocean in its millennial adjustment toward maximum entropy production (MEP), which would melt the H-induced sea ice to cause an abrupt post-H warming followed by a gradual cooling that anchors the DO cycles to form the hierarchical Bond cycle. Since the modelled anatomies resemble the observed ones, our theory may provide a robust and unified account of abrupt climate changes. |
format |
Text |
author |
Hsien-Wang Ou |
author_facet |
Hsien-Wang Ou |
author_sort |
Hsien-Wang Ou |
title |
A Theory of Abrupt Climate Changes: Their Genesis and Anatomy |
title_short |
A Theory of Abrupt Climate Changes: Their Genesis and Anatomy |
title_full |
A Theory of Abrupt Climate Changes: Their Genesis and Anatomy |
title_fullStr |
A Theory of Abrupt Climate Changes: Their Genesis and Anatomy |
title_full_unstemmed |
A Theory of Abrupt Climate Changes: Their Genesis and Anatomy |
title_sort |
theory of abrupt climate changes: their genesis and anatomy |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2022 |
url |
https://doi.org/10.3390/geosciences12110391 |
op_coverage |
agris |
genre |
Ice Sheet Sea ice |
genre_facet |
Ice Sheet Sea ice |
op_source |
Geosciences; Volume 12; Issue 11; Pages: 391 |
op_relation |
Climate https://dx.doi.org/10.3390/geosciences12110391 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/geosciences12110391 |
container_title |
Geosciences |
container_volume |
12 |
container_issue |
11 |
container_start_page |
391 |
_version_ |
1774718729773383680 |