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Radiative Transfer Diversity and Its Influence on the Response of the Hydrological Cycle in Climate Models

机译：辐射转移多样性及其对气候模型水文循环响应的影响

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作者
Kramer, Ryan Joseph.;
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作者单位

University of Miami.;

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授予单位 University of Miami.;
学科
学位 Ph.D.
年度 2018
页码 132 p.
总页数 132
原文格式 PDF
正文语种 eng
中图分类 AAI13419103;
关键词
Hydrological cycle; Radiative feedbacks; Radiative forcing; Radiative kernels;

机译：水文循环;辐射反馈;辐射强迫;辐射仁;

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专利

1. Radiative Constraints on the Hydrological Cycle in an Idealized Radiative-Convective Equilibrium Model [J] . Takahashi K Journal of the Atmospheric Sciences . 2009,第1期

机译：理想的辐射对流平衡模型中水文循环的辐射约束
2. Insolation-control on the Late Cretaceous hydrological cycle and tropical African climate-global climate modelling linked to marine climate records [J] . Floegel S, Wagner T Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences . 2006,第1a3期

机译：与海洋气候记录相关的白垩纪晚期水文周期的日照控制和热带非洲气候-全球气候模拟
3. Response of a coupled chemistry-climate model to changes in aerosol emissions: Global impact on the hydrological cycle and the tropospheric burdens of OH, ozone, and NOx [J] . Lamarque JF, Kiehl JT, Hess PG, Geophysical Research Letters . 2005,第16期

机译：化学-气候耦合模型对气溶胶排放变化的响应：对水文循环和OH，臭氧和NOx对流层负担的全球影响
4. Evaluating the hydrological responses to climate change over a large basin with a hydrological-vegetation coupling model [C] . XINGGUO MO, SUXIA LIU, ZHONGHUI LIN Hydrological modelling and integrated water resources management in ungauged mountainous watershed . 2008

机译：利用水文植被耦合模型评估大流域对气候变化的水文响应
5. Interactions between nitrogen and hydrological cycles: Implications for river nitrogen responses to climate and land use with the model LM3-TAN [D] . Lee, Minjin. 2015

机译：氮与水文循环之间的相互作用：LM3-TAN模型对河流氮对气候和土地利用的响应的意义
6. A Framework for Effective Use of Hydroclimate Models in Climate-Change Adaptation Planning for Managed Habitats with Limited Hydrologic Response Data [O] . Rachel A. Esralew, Lorraine Flint, James H. Thorne, -1

机译：在水文响应数据有限的情况下在受管理生境的气候变化适应规划中有效利用水文气候模型的框架
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。

Radiative Transfer Diversity and Its Influence on the Response of the Hydrological Cycle in Climate Models

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