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Contiguous US summer maximum temperature and heat stress trends in CRU and NOAA Climate Division data plus comparisons to reanalyses

机译：Cru和Noaa气候划分数据加上Reanalyses的比较，连续的美国夏季最高温度和热应激趋势

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Richard Grotjahn; Jonathan Huynh;
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年度 2018
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1. Contiguous US summer maximum temperature and heat stress trends in CRU and NOAA Climate Division data plus comparisons to reanalyses [J] . Richard Grotjahn, Jonathan Huynh Scientific reports. . 2018,第1期

机译：CRU和NOAA气候司数据中连续的美国夏季最高温度和热应力趋势以及与重新分析的比较
2. Assessing surface heat fluxes in atmospheric reanalyses with a decade of data from the NOAA Kuroshio Extension Observatory [J] . Dongxiao Zhang, Meghan F. Cronin, Caihong Wen, Journal of Geophysical Research, C. Oceans: JGR . 2016,第9期

机译：利用NOAA黑潮延伸观测站的十年数据评估大气再分析中的表面热通量
3. Comments on "Global and Regional Comparison of Daily 2-m and 1000-hPa Maximum and Minimum Temperatures in Three Global Reanalyses" [J] . S. Brands, J. M. Gutierrez, A. S. Cofino, Journal of Climate . 2012,第22期

机译：评论“在三项全球再分析中每日2 m和1000-hPa最高和最低温度的全球和区域比较”
4. The Effect of High Summer Temperatures on Emergency Hospital Admissions in Switzerland: A Comparison to Heat-Related Mortality [C] . Martina S. Ragettli, Ana M. Vicedo-Cabrera, Benjamin Fluckiger, Joint annual meeting of the International Society of Exposure Science and the International Society for Environmental Epidemiology . 2018

机译：夏季高温对瑞士急诊入院的影响：与热相关死亡率的比较
5. Climate-Human Health Vulnerability: Identifying Relationships between Maximum Temperature and Heat-Related Illness across North Carolina, USA [D] . Kovach, Margaret Mae. 2015

机译：气候-人类健康脆弱性：确定美国北卡罗来纳州的最高温度和与热有关的疾病之间的关系
6. Contiguous US summer maximum temperature and heat stress trends in CRU and NOAA Climate Division data plus comparisons to reanalyses [O] . Richard Grotjahn, Jonathan Huynh -1

机译：CRU和NOAA气候司数据中连续的美国夏季最高温度和热应力趋势以及与重新分析的比较
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。

Contiguous US summer maximum temperature and heat stress trends in CRU and NOAA Climate Division data plus comparisons to reanalyses

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