Theoretical study on behavior of the Earth system in the snowball Earth phenomena
雪球地球现象中地球系统行为的理论研究
基本信息
- 批准号:12640419
- 负责人:
- 金额:$ 0.9万
- 依托单位:
- 依托单位国家:日本
- 项目类别:Grant-in-Aid for Scientific Research (C)
- 财政年份:2000
- 资助国家:日本
- 起止时间:2000 至 2001
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
Evidence for low-latitude glaciations during the Proterozoic suggests that the entire surface of the Earth may have been covered with ice and snow in these periods. In this study, I investigated such "snowball Earth Phenomena" with theoretical models.The snowball Earth phenomena will be divided into four stages by dominant processes and their characteristic timescale. I found that there is a critical condition required for an initiation of the snowball Earth phenomena. At that condition, a net input flux of CO2 into the atmosphere-ocean system (=CO2 degassing rate due to volcanism + weathering rate of organic carbon - burial rate of organic carbon) becomes nearly zero. Therefore, the snowball Earth phenomena is occurred owing to imbalance of CO2 fluxes within the carbon cycle system.The faint sun in the past may have been responsible for the repetition of snowball Earth phenomena during the Proterozoic. According to the analysis of the climate system and the carbon cycle system, however, an effect of lower luminosity of the sun should have been cancelled out completely by an effect of lower efficiency of chemical weathering rate due to lower soil biological activity during the Proterozoic. Therefore, the faint young sun may not have been the cause for the snowball Earth phenomena.The carbon isotope mass balance model which uses variation of carbon isotope record of seawater during the Neoproterzoic suggests that organic carbon burial rate became very large just before the glaciations. This indicates increases in the consumption rate of atmospheric CO2, which may have initiated the snowball Earth phenomena during the Neoproterozoic.
元古代低纬度冰川作用的证据表明,在这些时期,地球的整个表面可能都被冰雪覆盖。在这项研究中,我用理论模型研究了这种“雪球地球现象”。根据主导过程及其特征时间标度,将雪球地球现象分为四个阶段。我发现雪球地球现象的开始需要一个临界条件。在这种情况下,大气-海洋系统的CO2净输入通量(=火山作用导致的CO2脱气速率+有机碳风化速率-有机碳埋藏速率)接近于零。因此,雪球地球现象的发生是由于碳循环系统内CO2通量的不平衡。过去微弱的太阳可能是元古代雪球地球现象反复出现的原因。然而,根据气候系统和碳循环系统的分析,元古代土壤生物活性较低,化学风化速率效率较低,应完全抵消了太阳亮度较低的影响。因此,微弱的年轻太阳可能不是雪球地球现象的原因。利用新元古代海水碳同位素记录变化的碳同位素质量平衡模型表明,在冰期之前,有机碳埋藏率变得非常大。这表明大气中二氧化碳消耗速率的增加,这可能是新元古代雪球地球现象的起源。
项目成果
期刊论文数量(12)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Eiichi Tajila: "Modeling the snowball Earth phenomena"Mathematical Sciences. 38. 76-83 (2000)
Eiichi Tajila:“模拟雪球地球现象”数学科学。
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Eiichi Tajika: "Proterozoic Snowball Earth : Effect of faint young Sun on the climate of the Earth"Proceedings of ISAS Lunar and Planetary Science Symposium. 34. 45-48 (2001)
Eiichi Tajika:“元古代雪球地球:微弱的年轻太阳对地球气候的影响”ISAS 月球和行星科学研讨会论文集。
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Eiichi Tajika: "Proterozoic Snowball Earth : Effect of faint young Sun on the climate of the Earth"Proceedings of ISAS Lunar and Planetary Science. Symposium, 34. 45-48 (2001)
Eiichi Tajika:“元古代雪球地球:微弱的年轻太阳对地球气候的影响”ISAS 月球与行星科学论文集。
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田近英一: "スノーボール・アース現象のモデリング"数理科学. 38. 76-83 (2000)
Eiichi Tajika:“雪球地球现象的建模”《数学科学》38. 76-83 (2000)。
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田近英一: "スノーボール・アース現象"日本惑星科学会誌. 11(印刷中). (2002)
Eiichi Tajika:“雪球地球现象”日本行星科学学会杂志 11(出版中)。
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TAJIKA Eiichi其他文献
TAJIKA Eiichi的其他文献
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{{ truncateString('TAJIKA Eiichi', 18)}}的其他基金
Study of physical conditions for climate mode of terrestrial water-rich planets in the extrasolar planetary systems
太阳系外富含类水行星气候模式的物理条件研究
- 批准号:
22540434 - 财政年份:2010
- 资助金额:
$ 0.9万 - 项目类别:
Grant-in-Aid for Scientific Research (C)
Reconstruction and system analyses of the global events of the Earth during the Paleoproterozoic
古元古代地球全球事件重建与系统分析
- 批准号:
18340128 - 财政年份:2006
- 资助金额:
$ 0.9万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Study of snowball Earth events and rise of the atmospheric oxygen based on geologicalg survey of glacial sediments of the Paleoproterozoic
基于古元古代冰川沉积物地质调查的雪球地球事件与大气氧含量上升研究
- 批准号:
14403004 - 财政年份:2002
- 资助金额:
$ 0.9万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
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EAGER: An Oasis for Surface Life on the Ocean of Snowball Earth
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2041491 - 财政年份:2020
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464393-2014 - 财政年份:2014
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University Undergraduate Student Research Awards
EAGER: Microbial Successions in the Aftermath of a Snowball Earth Event
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- 批准号:
1048974 - 财政年份:2010
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Continuous Geomagnetic Field Records During Snowball Earth: Critical Tests of Cryogenian Uniformitarianism
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0739105 - 财政年份:2008
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Collaborative Research: Biogeochemistry of Neoproterozoic Snowball Earth and Its Aftermath in South China
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0719493 - 财政年份:2007
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$ 0.9万 - 项目类别:
Standard Grant