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An experimental regional scale climate simulation laboratory. Year 1 progress letter

机译：实验区域规模气候模拟实验室。 1年级进度信

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1. Multi-Year Simulations and Experimental Seasonal Predictions for Rainy Seasons in China by Using a Nested Regional Climate Model (RegCM_NCC) Part Ⅱ: The Experimental Seasonal Prediction [J] . DING YIHUI, LIU YIMING, SHI XUELI, Advances in Atmospheric Sciences . 2006,第4期

机译：基于嵌套区域气候模型（RegCM_NCC）的中国雨季的多年模拟和试验性季节预报第二部分：试验性季节预报
2. Multi-Year Simulations and Experimental Seasonal Predictions for Rainy Seasons in China by Using a Nested Regional Climate Model (RegCM_NCC) Part Ⅱ: The Experimental Seasonal Prediction [J] . 大气科学进展（英文版） . 2006,第004期

机译：基于嵌套区域气候模型（RegCM_NCC）的中国雨季的多年模拟和试验性季节预报第二部分：试验性季节预报
3. Multi-year Simulations and Experimental Seasonal Predictions for Rainy Seasons in China by Using a Nested Regional Climate Model (RegCM_NCC). Part Ⅰ: Sensitivity Study [J] . DING Yihui, SHI Xueli, LIU Yiming, Advances in Atmospheric Sciences . 2006,第3期

机译：基于嵌套区域气候模型（RegCM_NCC）的中国雨季的多年模拟和实验季节预测。第一部分：敏感性研究
4. Progress in Fast, Accurate Multi-scale Climate Simulations [C] . W. D. Collins, H. Johansen, K. J. Evans, International Conference on Computational Science . 2015

机译：快速，准确的多尺度气候模拟进展
5. Peatland carbon cycle responses to hydrological change at time scales from years to centuries: Impacts on model simulations and regional carbon budgets. [D] . Sulman, Benjamin N. 2012

机译：泥炭地碳循环对水文变化的响应时间跨度为数年至数百年：对模型模拟和区域碳预算的影响。
6. Ensemble of European regional climate simulations for the winter of 2013 and 2014 from HadAM3P-RM3P [O] . Nathalie Schaller, Sarah N. Sparrow, Neil R. Massey, 2018

机译：HadAM3P-RM3P在2013年和2014年冬季进行的欧洲区域气候模拟汇总
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. Experimental regional scale climate simulation laboratory. Year 1 progress letter. [R] . 1993

机译：实验区域尺度气候模拟实验室。 1年级进度信。

An experimental regional scale climate simulation laboratory. Year 1 progress letter

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