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Our climate, our change - using digital learning objects to present the complex science of global climate change

机译：我们的气候，我们的变化 - 使用数字学习对象来呈现全球气候变化的复杂科学

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Martin Brian; Mahaffy Peter;
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年度 2010
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原文格式 PDF
正文语种 eng
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入库时间 2022-08-20 21:03:42

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1. A review of recent developments in climate change science. Part II: The global-scale impacts of climate change [J] . Gosling S.N., Warren R., Arnell N.W., Progress in Physical Geography . 2011,第4期

机译：回顾气候变化科学的最新发展。第二部分：气候变化对全球的影响
2. The climate change dilemma: big science, the globalizing of climate and the loss of the human scale [J] . Heymann Matthias Regional Environmental Change . 2019,第6期

机译：气候变化的困境：科学大，气候全球化和人类规模的丧失
3. The climate change dilemma: big science, the globalizing of climate and the loss of the human scale [J] . Heymann Matthias Regional Environmental Change . 2019,第6期

机译：气候变化困境：大科学，气候全球化和人类规模的丧失
4. ENHANCING GLOBAL CLIMATE DATA EXCHANGE TO BETTER MONITOR CLIMATE CHANGE AND EMPOWER POLICY MAKERS, SCIENTISTS AND THE COMMUNITY [C] . Muhammad Shafiq, Bernardo Santos, Ana Alexandra Pérez, IAC;International Astronautical Congress . 2011

机译：加强全球气候数据交换，以更好地监测气候变化和企业政策制定者，科学家和社区
5. Communicating climate change: Climate rhetorics and discursive tipping points in United States global warming science and public policy. [D] . Besel, Richard D. 2007

机译：传达气候变化：美国全球变暖科学和公共政策中的气候言论和论点。
6. Climate Change and Food Security Special Feature: Global food security under climate change [O] . Josef Schmidhuber, Francesco N. Tubiello 2007

机译：气候变化与粮食安全专刊：气候变化下的全球粮食安全
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. Global Climate Change Impacts in the United States: Unified Synthesis Product. Report by the U.S. Climate Change Science Program and the Subcommittee on glabl Change Research [R] . 2009

机译：全球气候变化对美国的影响：统一合成产品。美国气候变化科学计划和小组委员会关于glabl变化研究的报告

Our climate, our change - using digital learning objects to present the complex science of global climate change

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