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Temperature and precipitation trends in California: Global warming and Pacific Ocean influences

机译：加利福尼亚的温度和降水趋势：全球变暖和太平洋的影响

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《AMS annual meeting》|2011年|1-15|共15页
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Steve LaDochy; Pedro Ramirez; Dan Killam; Ann Bui; William Patzert; JoshWillis;
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1. 热带太平洋海表温度年际变化对降水季节内振荡的影响 [J] . 李薇, 宇如聪, 张学洪大气科学进展（英文版） . 2001,第003期
2. Influence of local and remote sea surface temperatures on precipitation as inferred from changes in boundary-layer moisture convergence and moist thermodynamics over global oceans. [J] . Sud YC, Walker GK, Zhou YP, Quarterly Journal of the Royal Meteorological Society . 2008,第630期

机译：根据全球海洋边界层水分收敛和湿热力学的变化推论，局部和偏远海面温度对降水的影响。
3. The IOD-ENSO precursory teleconnection over the tropical Indo-Pacific Ocean: dynamics and long-term trends under global warming [J] . YUAN Dongliang, HU Xiaoyue, XU Peng, 中国海洋湖沼学报（英文版） . 2018,第001期

机译：IOD-ENSO热带印度洋-太平洋上的先兆遥相关：全球变暖下的动力学和长期趋势
4. The IOD-ENSO precursory teleconnection over the tropical Indo-Pacific Ocean： dynamics and long-term trends under global warming [J] . 袁东亮, 胡晓悦, 徐鹏, 海洋湖沼学报（英文） . 2018,第001期

机译：热带印度洋-太平洋上的IOD-ENSO前兆遥相关：全球变暖下的动力学和长期趋势
5. Potential Vineyard Evapotranspiration (ET) Due to Global Warming: Comparison of Vineyard ET at Three Locations in California Differing in Mean Seasonal Temperatures [C] . L.E. Williams International Horticultural Congress on Science and Horticulture for People . 2012

机译：由于全球变暖，潜在的葡萄园蒸散（et）：葡萄园等在加州三个地点的比较平均季节性温度
6. Questions Raised by the Global Warming Hiatus: The Predictability of Tropical Pacific Decadal Variability and Subsurface Warming of the Tropical Atlantic Ocean [D] . Ramesh, Nandini. 2018

机译：全球变暖中断提出的问题：热带太平洋年代际变率的可预测性和热带大西洋的地下变暖
7. Prolonged California aridity linked to climate warming and Pacific sea surface temperature [O] . Glen M. MacDonald, Katrina A. Moser, Amy M. Bloom, -1

机译：加利福尼亚州长期干旱与气候变暖和太平洋海表温度有关
8. 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。

Temperature and precipitation trends in California: Global warming and Pacific Ocean influences

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