首页> 外文OA文献 >Controlling atmospheric forcing parameters of global ocean models: sequential assimilation of sea surface Mercator-Ocean reanalysis data

【2h】

Controlling atmospheric forcing parameters of global ocean models: sequential assimilation of sea surface Mercator-Ocean reanalysis data

机译：控制全球海洋模型的大气强迫参数：海面墨卡托 - 海洋再分析资料的顺序同化

代理获取

本网站仅为用户提供外文OA文献查询和代理获取服务，本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文，但由于OA文献来源多样且变更频繁，仍可能出现获取不到、文献不完整或与标题不符等情况，如果获取不到我们将提供退款服务。请知悉。

页面导航

著录项
引文网络
相似文献
相关主题

著录项

作者
C. Skandrani; J.-M. Brankart; N. Ferry; J. Verron; P. Brasseur; B. Barnier;
展开▼
作者单位

展开▼
年度 2009
总页数
原文格式 PDF
正文语种
中图分类

相似文献

外文文献
中文文献
专利

1. Controlling atmospheric forcing parameters of global ocean models: sequential assimilation of sea surface Mercator-Ocean reanalysis data [J] . Ocean Science Discussions . 2009,第4期

机译：控制全球海洋模型的大气强迫参数：海面Mercator-Ocean再分析数据的顺序同化
2. Controlling atmospheric forcing parameters of global ocean models: sequential assimilation of sea surface Mercator-Ocean reanalysis data [J] . Ocean Science Discussions . 2009,第3期

机译：控制全球海洋模型的大气强迫参数：海面Mercator-Ocean再分析数据的顺序同化
3. Controlling atmospheric forcing parameters of global ocean models: sequential assimilation of sea surface Mercator-Ocean reanalysis data [J] . C.Skandrani, J.-M.Brankart, N.Ferry, Ocean science . 2009,第4期

机译：控制全球海洋模型的大气强迫参数：海面Mercator-Ocean再分析数据的顺序同化
4. CONTROL OF A FREE-SURFACE BAROTROPIC MODEL OF THE BAY OF BISCAY BY ASSIMILATION OF SEALEVEL DATA IN PRESENCE OF ATMOSPHERIC FORCINGS [C] . Lamouroux, J., De Mey, Symposium on 15 years of Progress in Radar Altimetry . 2006

机译：存在大气强迫的海量数据同化控制比斯开湾的自由表面正压模式
5. Lagrangian measurements and low -dimensional models for oceanographic and atmospheric data assimilation. [D] . Buehner, Mark. 2000

机译：海洋和大气数据同化的拉格朗日测量和低维模型。
6. Spontaneous abrupt climate change due to an atmospheric blocking–sea-ice–ocean feedback in an unforced climate model simulation [O] . Sybren Drijfhout, Emily Gleeson, Henk A. Dijkstra, 2013

机译：在非强迫气候模型模拟中由于大气阻塞-海冰-海洋反馈而导致的自然自发突变
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。

Controlling atmospheric forcing parameters of global ocean models: sequential assimilation of sea surface Mercator-Ocean reanalysis data

著录项

引文网络

相似文献

相关主题

期刊订阅