Theoretical study on behavior of the Earth system in the snowball Earth phenomena
Theoretical study on behavior of the Earth system in the snowball Earth phenomena
批准号:
12640419
负责人:
TAJIKA Eiichi
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
项目状态:
已结题
起止时间:
2000 至 2001
中文摘要
元古界低纬冰川的证据表明,在这些时期,整个地球表面可能被冰雪覆盖。在这项研究中,我用理论模型对这种“雪球地球现象”进行了研究。根据主导过程及其特征时间尺度,将雪球地球现象划分为四个阶段。我发现,启动雪球地球现象需要一个关键条件。在这种情况下,进入大气-海洋系统的二氧化碳净输入通量(=火山作用导致的二氧化碳脱气率、有机碳的风化速率-有机碳的埋藏率)几乎为零。因此,雪球地球现象的发生是由于碳循环系统内CO2通量的不平衡造成的。过去的微弱太阳可能是元古界雪球地球现象重复的原因。然而,根据气候系统和碳循环系统的分析,元古界土壤生物活性降低导致的化学风化效率降低,应该完全抵消了太阳光度降低的影响。利用新元古代海水碳同位素记录的变化建立的碳同位素物质平衡模型表明,冰期前有机碳埋藏率变得很大。这表明大气中二氧化碳的消耗速率增加,这可能是新元古代雪球地球现象的始作俑者。
英文摘要
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.
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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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共 7 条
Study of physical conditions for climate mode of terrestrial water-rich planets in the extrasolar planetary systems
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批准号:22540434
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项目类别:Grant-in-Aid for Scientific Research (C)
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资助金额:$2.75万
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财政年份:2010
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负责人:TAJIKA Eiichi
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依托单位:
Reconstruction and system analyses of the global events of the Earth during the Paleoproterozoic
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批准号:18340128
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项目类别:Grant-in-Aid for Scientific Research (B)
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资助金额:$6.25万
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财政年份:2006
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负责人:TAJIKA Eiichi
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依托单位:
Study of snowball Earth events and rise of the atmospheric oxygen based on geologicalg survey of glacial sediments of the Paleoproterozoic
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批准号:14403004
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项目类别:Grant-in-Aid for Scientific Research (B)
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资助金额:$8.32万
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财政年份:2002
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负责人:TAJIKA Eiichi
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依托单位:
海外基金