Accurate near surface air temperature measurements are necessary to gauge large‐scale ecological responses to global climate change

Adam Terando; Elsa Youngsteadt; Emily Meineke; Sara Prado

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Accurate near surface air temperature measurements are necessary to gauge large‐scale ecological responses to global climate change

机译：准确的近地表气温测量对于衡量对全球气候变化的大规模生态响应是必要的

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Linked Article : https://doi.org/10.1002/ece3.3965

机译：链接的文章：https://doi.org/10.1002/ece3.3965

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《Ecology and Evolution》 |2018年第11期|共2页
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Adam Terando; Elsa Youngsteadt; Emily Meineke; Sara Prado;
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中图分类生物科学;
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2. Climate change impact of livestock CH4 emission in India: Global temperature change potential (GTP) and surface temperature response [J] . Kumari Shilpi, Hiloidhari Moonmoon, Kumari Nisha, Ecotoxicology and Environmental Safety . 2018,第jana期

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3. Spatial Patterns and Frequency of Unforced Decadal-Scale Changes in Global Mean Surface Temperature in Climate Models [J] . Middlemas Eleanor A., Clement Amy C. Journal of Climate . 2016,第17期

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4. CHANGES IN PERMAFROST LANDSCAPES UNDER GLOBAL CHANGE Ecological responses to variations in land use and climate [C] . B. C. FORBES NATO advanced research workshop on permafrost response on economic development, environmental security and natural resources . 2001

机译：全球变化生态反应下的永久冻土景观的变化对土地利用和气候的变化
5. Assessing forest responses to climate change, and, Resolving productivity measurements across spatial scales. [D] . Boisvenue, Celine. 2007

机译：评估森林对气候变化的反应，以及解决跨空间尺度的生产力测量。
6. Accurate near surface air temperature measurements are necessary to gauge large‐scale ecological responses to global climate change [O] . Adam Terando, Elsa Youngsteadt, Emily Meineke, 2018

机译：准确的近地表气温测量对于衡量对全球气候变化的大规模生态响应是必要的
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。

Accurate near surface air temperature measurements are necessary to gauge large‐scale ecological responses to global climate change

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