The meaning of the ocean for the state in contemporary Taiwan since 1949: understanding state perceptions of the ocean through a historical approach

Kuang-Hao Hou

首页> 外文期刊>Australian journal of maritime & ocean affairs >The meaning of the ocean for the state in contemporary Taiwan since 1949: understanding state perceptions of the ocean through a historical approach

【24h】

The meaning of the ocean for the state in contemporary Taiwan since 1949: understanding state perceptions of the ocean through a historical approach

机译：1949年以来，海洋在当代台湾对国家的意义：通过历史方法了解国家对海洋的看法

获取原文

获取原文并翻译 | 示例

掌桥外文数据库（机构版） >>

开具论文收录证明 >>

文献代查 >>

页面导航

摘要
著录项
相似文献
相关主题

摘要

This study applies Philip Steinberg's models of perceptions of the ocean and his territorial political economics to interpret the ocean policy, marine laws and maritime acts of the Republic of China against the historical context of contemporary Taiwan. I outline the trajectory of the state's perception of the ocean. This perception has changed from that of the Indian Ocean Model into a Mediterranean-Freitian perception regarding the maritime activities of Taiwan after 1949. In the 1990s, the perception assimilated elements of the Mediterranean-Grotian style of perception from international maritime treaties. Moreover, the state absorbed elements of the Mediterranean-Seldenian type and the Micronesia Model. The experiences of current Taiwanese politics may help add a novel type or subtype of perceptions to Steinberg's existing classification.

机译：这项研究运用菲利普·斯坦伯格的海洋观及其领土政治经济学模型来解释当代台湾历史背景下的中华民国海洋政策，海洋法和海洋行为。我概述了该州对海洋的看法。这种看法已经从印度洋模式的看法转变为对1949年后台湾海事活动的地中海-弗利特主义的看法。在1990年代，这种看法吸收了国际海事条约中地中海-格鲁吉亚式的看法要素。此外，该州吸收了地中海-塞尔登式和密克罗尼西亚模型的元素。当前台湾政治的经验可能有助于在斯坦伯格的现有分类中添加新的类型或子类型的看法。

著录项

来源
《Australian journal of maritime & ocean affairs》 |2014年第4期|191-206|共16页
作者
Kuang-Hao Hou;
展开▼
作者单位

Graduate Institute of Marine Affairs, National Quemoy University, Kinmen, ROC (Taiwan);

展开▼
收录信息
原文格式 PDF
正文语种 eng
中图分类
关键词

相似文献

外文文献
中文文献
专利

1. Understanding the bias in surface latent and sensible heat fluxes in contemporary AGCMs over tropical oceans [J] . Zhou Xin, Ray Pallav, Barrett Bradford S., Climate dynamics . 2020,第11a12期

机译：在热带海洋上，了解当代AGCMS中表面潜热和明智的热量通量的偏差
2. U-Pb Dating, Oxygen and Hafnium Isotope Ratios of Zircon from Rocks of Oceanic Core Complexes at the Mid-Atlantic Ridge: Evidence for the Interaction of Contemporary and Ancient Crusts in the Spreading Center of the Ocean Floor [J] . Bortnikov N. S., Silantyev S. A., Bea F., Doklady Earth Sciences . 2019,第PTa2期

机译：Zircon的U-PB约会，氧气和铪同位素在大西洋核心复合物岩石中的岩石：当代和古代外壳在海底扩散中心相互作用的证据
3. Plastic pollution of the world’s seas and oceans as a contemporary challenge in ocean governance [J] . Marcus Haward Nature Communications . 2018,第1期

机译：世界海洋的塑料污染是海洋治理的当代挑战
4. Oceans '89 An International Conference Addressing Methods For Understanding The Global Ocean [C] . . 2001

机译：89年海洋大会国际会议，探讨了解全球海洋的方法
5. Oceans crossing: Factors contributing to the social and academic integration of Korean, Malaysian, and Taiwanese international undergraduate students at a research university. [D] . Pham, Hoa. 2013

机译：海洋跨越：在研究型大学中促进韩国，马来西亚和台湾国际本科学生的社会和学术融合的因素。
6. Plastic pollution of the world’s seas and oceans as a contemporary challenge in ocean governance [O] . Marcus Haward -1

机译：世界海洋的塑料污染是海洋治理的当代挑战
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. U.S. West Coast Shellfish Industry’s Perception of and Response to Ocean Acidification: Understanding an Ocean Stakeholder. [R] . Mabardy, B., Conway, F. D. L., Waldbusser, G. G., 2016

机译：美国西海岸贝类产业对海洋酸化的认识和应对：了解海洋利益相关者。

The meaning of the ocean for the state in contemporary Taiwan since 1949: understanding state perceptions of the ocean through a historical approach

摘要

著录项

相似文献

相关主题

期刊订阅