Simulation of inferior mirages observed at the Halligen Sea

Eberhard Tr#nkle

首页> 外文期刊>Applied optics >Simulation of inferior mirages observed at the Halligen Sea

【24h】

Simulation of inferior mirages observed at the Halligen Sea

机译：模拟在哈利根海观察到的下层海市ages楼

获取原文

获取原文并翻译 | 示例

掌桥外文数据库（机构版） >>

开具论文收录证明 >>

文献代查 >>

页面导航

摘要
著录项
相似文献
相关主题

摘要

Two unusual forms of inferior mirage are observed and photographed at the Halligen Sea. With heuristic analytic functions for the temperature profiles, numerical integration of the refraction differential equation on a flat earth is performed. The simulation shows that a double inferior mirage can appear if a light wind carries hot air from above dry sandbanks in the mud flats. Horizontal stripes can appear in the mirage image if a water channel crosses the line of sight between the observer and the object. # 1998 Optical Society of America OCIS codes: 010.0010, 010.4030, 120.6780.

机译：在哈利根海观察并拍摄了两种不同寻常的下海市rage楼。利用温度分布的启发式解析函数，可以对平整地面上的折射微分方程进行数值积分。模拟显示，如果轻风从泥滩的干燥沙洲上方运送热空气，则会出现双重劣质海市rage楼。如果水通道越过观察者与物体之间的视线，则海市rage楼图像中可能会出现水平条纹。＃1998美国光学学会OCIS代码：010.0010、010.4030、120.6780。

著录项

来源
《Applied optics》 |1998年第12期|共11页
作者
Eberhard Tr#nkle;
展开▼
作者单位

展开▼
收录信息
原文格式 PDF
正文语种 eng
中图分类光学;
关键词

相似文献

外文文献
中文文献
专利

1. Simulation of inferior mirages observed at the Halligen Sea [J] . Trankle E. Applied optics . 1998,第9期

机译：模拟在哈利根海观察到的下层海市ages楼
2. Simulation of the Inferior Mirage [J] . Mario Branca The Physics Teacher . 2010,第6期

机译：下海市age楼的模拟
3. Constraining Parameter Uncertainty in Simulations of Water and Heat Dynamics in Seasonally Frozen Soil Using Limited Observed Data [J] . Mousong Wu, Per-Erik Jansson, Xiao Tan, Water . 2016,第2期

机译：使用有限观测数据模拟季节性冻土中水和热动力学的约束参数不确定性
4. Predicted and observed settlements of a subsea rock installation - comparison between field measurements and FE simulations of soft North Sea clay [C] . M. Kahlstroem, R. Frossard, H. Mattsson International Symposium on Frontiers in Offshore Geotechnics . 2015

机译：预测和观察到的海底岩石沉降-现场测量与北海软黏土有限元模拟之间的比较
5. Interannual variation of the Polar Front in the East/Japan Sea: Observed data and numerical simulations. [D] . Choi, Byoung-Ju. 2004

机译：东/日本海极地锋的年际变化：观测数据和数值模拟。
6. Binaural Electric-Acoustic Interactions Recorded from the Inferior Colliculus of Guinea Pigs: The Effect of Masking Observed in the Central Nucleus of the Inferior Colliculus [O] . Heil Noh, Dong-Hee Lee 2012

机译：从豚鼠下睫状体记录的双耳电-声相互作用：观察在下睫状体中央核中掩蔽的影响
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。

Simulation of inferior mirages observed at the Halligen Sea

摘要

著录项

相似文献

相关主题

期刊订阅