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Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene.

机译：从冰芯到人类世和更新世的矿物气溶胶（粉尘）记录中区域和全球气候变化的证据。

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作者
Aarons, Sarah Miranda.;
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作者单位

University of Michigan.;

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授予单位 University of Michigan.;
学科 Climate change.;Biogeochemistry.;Atmospheric sciences.;Geophysics.;Environmental geology.
学位 Ph.D.
年度 2016
页码 198 p.
总页数 198
原文格式 PDF
正文语种 eng
中图分类
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专利

1. Glacial/interglacial changes in mineral dust and sea-salt records in polar ice cores: Sources, transport, and deposition [J] . Fischer H, Siggaard-Andersen ML, Ruth U, Reviews of Geophysics . 2007,第1期

机译：极地冰芯中矿物尘埃和海盐记录的冰川/间冰层变化：来源，运输和沉积
2. Local vs global climate change-investigation of dust from deep ice cores [J] . A. Marcelli, D. Hampai, G. Cibin, Spectroscopy Asia . 2012,第3期

机译：局部与全球气候变化-深冰芯尘埃的调查
3. Local vs global climate change-investigation of dust from deep ice cores [J] . A.Marcelli, D.Hampai, G.Cibin, Spectroscopy Europe . 2012,第3期

机译：局部与全球气候变化-深冰芯尘埃的调查
4. LINKING AEROSOLS SOURCES TO CLIMATE CHANGE AND AIR POLLUTION IMPACTS—HOW GOOD ARE OUR GLOBAL AND REGIONAL MODELS? [C] . GREGORY R. CARMICHAEL International Seminar On Nuclear War And Planetary Emergencies . 2007

机译：将气溶胶源与气候变化和空气污染影响 - 我们的全球和区域模型有多好？
5. Aerosol-climate interactions: The role of convective plumes and vortices on the global mineral dust budget and convective-radiative interactions. [D] . Koch, Jacquelin. 2006

机译：气溶胶与气候的相互作用：对流羽流和涡流在全球矿物粉尘预算和对流-辐射相互作用中的作用。
6. A scaling theory for the size distribution of emitted dust aerosols suggests climate models underestimate the size of the global dust cycle [O] . Jasper F. Kok 2011

机译：排放粉尘气溶胶的尺寸分布的尺度理论表明气候模型低估了全球粉尘循环的大小
7. Glacial/interglacial changes in mineral dust and sea-salt records in polar ice cores: sources, transport, and deposition [O] . Fischer Hubertus, Siggaard-Andersen Marie-Louise, Ruth Urs, 2007

机译：极地冰芯中矿物尘埃和海盐记录的冰期/间冰期变化：来源，运输和沉积

Evidence of Regional and Global Climate Change in the Mineral Aerosol (Dust) Record from Ice Cores Through the Anthropocene and Pleistocene.

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