The Initiation of Modern "Soft Snowball" and "Hard Snowball" Climates in CCSM3. Part II: Climate Dynamic Feedbacks
This study investigates the climate dynamic feedbacks during a transition from the present climate to the extremely cold climate of a "Snowball Earth" using the Community Climate System Model, version 3 (CCSM3). With the land-sea distribution fixed to modern, it is found that by reducing s...
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ftpekinguniv:oai:localhost:20.500.11897/296882 2023-05-15T13:41:05+02:00 The Initiation of Modern "Soft Snowball" and "Hard Snowball" Climates in CCSM3. Part II: Climate Dynamic Feedbacks Yang, Jun Peltier, W. Richard Hu, Yongyun Yang, J (reprint author), 40 Gerrard St E,Apt 3308, Toronto, ON M5B 2E8, Canada. Univ Toronto, Dept Phys, Toronto, ON, Canada. Peking Univ, Lab Climate & Ocean Atmosphere Studies, Dept Atmospher & Ocean Sci, Sch Phys, Beijing 100871, Peoples R China. 40 Gerrard St E,Apt 3308, Toronto, ON M5B 2E8, Canada. 2012 https://hdl.handle.net/20.500.11897/296882 https://doi.org/10.1175/JCLI-D-11-00190.1 en eng journal of climate JOURNAL OF CLIMATE.2012,25,(8),2737-2754. 879913 0894-8755 http://hdl.handle.net/20.500.11897/296882 1520-0442 doi:10.1175/JCLI-D-11-00190.1 WOS:000302787300010 SCI EI SEA-ICE HEAT-TRANSPORT CARBON-CYCLE DEEP-TIME EARTH OCEAN ATMOSPHERE ENERGY CO2 CIRCULATIONS Journal 2012 ftpekinguniv https://doi.org/20.500.11897/296882 https://doi.org/10.1175/JCLI-D-11-00190.1 2021-08-01T09:23:10Z This study investigates the climate dynamic feedbacks during a transition from the present climate to the extremely cold climate of a "Snowball Earth" using the Community Climate System Model, version 3 (CCSM3). With the land-sea distribution fixed to modern, it is found that by reducing solar luminosity and/or carbon dioxide concentration: 1) the amount of atmospheric water vapor and its attendant greenhouse effect decrease with the logarithm of sea ice cover, thereby promoting the expansion of sea ice; 2) over the sea ice, the cloud radiative feedback is positive, thus enhancing sea ice advance; over the ocean, the cloud radiative feedback is first negative and then becomes positive as sea ice enters the tropics; and 3) the strength of the atmospheric Hadley cell and the wind-driven ocean circulation increases significantly in the Southern Hemisphere, inhibiting the expansion of sea ice into the tropics. Meanwhile, the North Atlantic Deep Water cell disappears and the Antarctic Bottom Water cell strengthens and expands to occupy almost the entire Atlantic basin. In the experiment with 6% less solar radiation and 70 ppmv CO2 compared to the control experiment with 100% solar radiation and 355 ppmv CO2 near the ice edge (28 degrees S latitude), the changes of solar radiation, CO2 forcing, water vapor greenhouse effect, longwave cloud forcing at the top of the model, and atmospheric and oceanic energy transport are -22.4, -6.2, -54.4, +6.2, and +16.3 W m(-2), respectively. Therefore, the major controlling factors in producing global ice cover are ice albedo feedback (Yang et al., Part I) and water vapor feedback. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000302787300010&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Meteorology & Atmospheric Sciences SCI(E) EI 19 ARTICLE 8 2737-2754 25 Journal/Newspaper Antarc* Antarctic North Atlantic Deep Water North Atlantic Sea ice Peking University Institutional Repository (PKU IR) Antarctic The Antarctic Journal of Climate 25 8 2737 2754 |
institution |
Open Polar |
collection |
Peking University Institutional Repository (PKU IR) |
op_collection_id |
ftpekinguniv |
language |
English |
topic |
SEA-ICE HEAT-TRANSPORT CARBON-CYCLE DEEP-TIME EARTH OCEAN ATMOSPHERE ENERGY CO2 CIRCULATIONS |
spellingShingle |
SEA-ICE HEAT-TRANSPORT CARBON-CYCLE DEEP-TIME EARTH OCEAN ATMOSPHERE ENERGY CO2 CIRCULATIONS Yang, Jun Peltier, W. Richard Hu, Yongyun The Initiation of Modern "Soft Snowball" and "Hard Snowball" Climates in CCSM3. Part II: Climate Dynamic Feedbacks |
topic_facet |
SEA-ICE HEAT-TRANSPORT CARBON-CYCLE DEEP-TIME EARTH OCEAN ATMOSPHERE ENERGY CO2 CIRCULATIONS |
description |
This study investigates the climate dynamic feedbacks during a transition from the present climate to the extremely cold climate of a "Snowball Earth" using the Community Climate System Model, version 3 (CCSM3). With the land-sea distribution fixed to modern, it is found that by reducing solar luminosity and/or carbon dioxide concentration: 1) the amount of atmospheric water vapor and its attendant greenhouse effect decrease with the logarithm of sea ice cover, thereby promoting the expansion of sea ice; 2) over the sea ice, the cloud radiative feedback is positive, thus enhancing sea ice advance; over the ocean, the cloud radiative feedback is first negative and then becomes positive as sea ice enters the tropics; and 3) the strength of the atmospheric Hadley cell and the wind-driven ocean circulation increases significantly in the Southern Hemisphere, inhibiting the expansion of sea ice into the tropics. Meanwhile, the North Atlantic Deep Water cell disappears and the Antarctic Bottom Water cell strengthens and expands to occupy almost the entire Atlantic basin. In the experiment with 6% less solar radiation and 70 ppmv CO2 compared to the control experiment with 100% solar radiation and 355 ppmv CO2 near the ice edge (28 degrees S latitude), the changes of solar radiation, CO2 forcing, water vapor greenhouse effect, longwave cloud forcing at the top of the model, and atmospheric and oceanic energy transport are -22.4, -6.2, -54.4, +6.2, and +16.3 W m(-2), respectively. Therefore, the major controlling factors in producing global ice cover are ice albedo feedback (Yang et al., Part I) and water vapor feedback. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000302787300010&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Meteorology & Atmospheric Sciences SCI(E) EI 19 ARTICLE 8 2737-2754 25 |
author2 |
Yang, J (reprint author), 40 Gerrard St E,Apt 3308, Toronto, ON M5B 2E8, Canada. Univ Toronto, Dept Phys, Toronto, ON, Canada. Peking Univ, Lab Climate & Ocean Atmosphere Studies, Dept Atmospher & Ocean Sci, Sch Phys, Beijing 100871, Peoples R China. 40 Gerrard St E,Apt 3308, Toronto, ON M5B 2E8, Canada. |
format |
Journal/Newspaper |
author |
Yang, Jun Peltier, W. Richard Hu, Yongyun |
author_facet |
Yang, Jun Peltier, W. Richard Hu, Yongyun |
author_sort |
Yang, Jun |
title |
The Initiation of Modern "Soft Snowball" and "Hard Snowball" Climates in CCSM3. Part II: Climate Dynamic Feedbacks |
title_short |
The Initiation of Modern "Soft Snowball" and "Hard Snowball" Climates in CCSM3. Part II: Climate Dynamic Feedbacks |
title_full |
The Initiation of Modern "Soft Snowball" and "Hard Snowball" Climates in CCSM3. Part II: Climate Dynamic Feedbacks |
title_fullStr |
The Initiation of Modern "Soft Snowball" and "Hard Snowball" Climates in CCSM3. Part II: Climate Dynamic Feedbacks |
title_full_unstemmed |
The Initiation of Modern "Soft Snowball" and "Hard Snowball" Climates in CCSM3. Part II: Climate Dynamic Feedbacks |
title_sort |
initiation of modern "soft snowball" and "hard snowball" climates in ccsm3. part ii: climate dynamic feedbacks |
publisher |
journal of climate |
publishDate |
2012 |
url |
https://hdl.handle.net/20.500.11897/296882 https://doi.org/10.1175/JCLI-D-11-00190.1 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic North Atlantic Deep Water North Atlantic Sea ice |
genre_facet |
Antarc* Antarctic North Atlantic Deep Water North Atlantic Sea ice |
op_source |
SCI EI |
op_relation |
JOURNAL OF CLIMATE.2012,25,(8),2737-2754. 879913 0894-8755 http://hdl.handle.net/20.500.11897/296882 1520-0442 doi:10.1175/JCLI-D-11-00190.1 WOS:000302787300010 |
op_doi |
https://doi.org/20.500.11897/296882 https://doi.org/10.1175/JCLI-D-11-00190.1 |
container_title |
Journal of Climate |
container_volume |
25 |
container_issue |
8 |
container_start_page |
2737 |
op_container_end_page |
2754 |
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1766145577841590272 |