Computer Simulation of the Influence on Sea Ice Concentration Caused by Sea Surface Temperature and Sea Level Pressure

机译：海面温度和海平面压力对海冰浓度影响的计算机模拟

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In this paper, focusing on the Northwest Passage, we looked into the relevance between sea surface temperature(SST), sea level pressure(SLP) and the reducing amount of annual sea ice concentration (May minus September) based on the NSST daily average data from NASA MODISA, SLP monthly average data from NCEP and AMSR-E sea ice concentration product with the resolution of 6.25 kilometers from the year 2002 to 2010.

机译：在本文中，我们着眼于西北航道，根据NSST日平均数据研究了海表温度（SST），海平面压力（SLP）和年度海冰浓度减少量（5月减9月）之间的相关性。来自NASA MODISA的SLP来自NCEP和AMSR-E海冰浓缩产品的月平均数据，从2002年到2010年的分辨率为6.25公里。

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《Computing, Measurement, Control and Sensor Network (CMCSN), 2012 International Conference on》|2012年|p.261- 264|共4页
会议地点 Taiyuan(CN)
作者
Sijia Zou; Lidaling Yi;
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正文语种 eng
中图分类计算机网络;
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1. The Met Office Hadley Centre sea ice and sea surface temperature data set, version 2: 1. Sea ice concentrations [J] . Holly A. Titchner, Nick A. Rayner Journal of Geophysical Research, D. Atmospheres: JGR . 2014,第6期

机译：大都会办公室哈德利中心海冰和海面温度数据集，版本2：1.海冰浓度
2. VARIATIONS OF SEA SURFACE TEMPERATURE AND SEA LEVEL PRESSURE OVER PACIFIC AND INDIAN OCEANS AND THEIR INFLUENCE ON COLD SUMMER IN EAST ASIA [J] . 沙文钰, 蔡剑平气象学报：英文版 . 1993,第002期

机译：太平洋和印度洋海面温度和海平面压力的变化及其对东亚寒冷夏季的影响
3. Interannual Tropical Pacific Sea Surface Temperatures and TheirRelation to Preceding Sea Level Pressures in the NCAR CCSM2 [J] . Anderson BT, Maloney E Journal of Climate . 2006,第6期

机译：NCAR CCSM2的年际热带太平洋海表温度及其与先前海平面压力的关系
4. Computer Simulation of the Influence on Sea Ice Concentration Caused by Sea Surface Temperature and Sea Level Pressure [C] . Sijia Zou, Lidaling Yi International Conference on Computing, Measurement, Control and Sensor Network . 2012

机译：海面温度和海平面压力影响对海冰浓度影响的计算机模拟
5. Atlantic sea surface temperature variability and its relationship to overlying air temperature, sea level pressure, and 500 MB teleconnections [D] . Marshall, Mary Louise. 1994

机译：大西洋海表温度的变化及其与上层气温，海平面压力和500 MB远程连接的关系
6. Inter-relationship between subtropical Pacific sea surface temperature Arctic sea ice concentration and North Atlantic Oscillation in recent summers [O] . Young-Kwon Lim, Richard I. Cullather, Sophie M. J. Nowicki, -1

机译：近期夏季亚热带太平洋海表温度北极海冰浓度和北大西洋涛动之间的相互关系
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。
8. Climatic Atlas of Seasonal and Annual Arctic Sea-Level Pressures, Slp Anomalies,and Sea-Ice Concentrations, 1953-1988 [R] . Mysak, L. A., Wang, J. 1991

机译：1953 - 1988年季节性和年度北极海平面压力，slp异常和海冰浓度的气候图集

Computer Simulation of the Influence on Sea Ice Concentration Caused by Sea Surface Temperature and Sea Level Pressure

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