The Climate of the Arctic
The Climate of the Arctic
复制标题
DOI:
10.1007/978-3-319-21696-6
复制
发表时间:
2003
期刊:
影响因子:
--
通讯作者:
R. Przybylak
中科院分区:
文献类型:
--
作者:
R. Przybylak
At the end of the nineteenth century, researchers put forward the hypothesis that the Polar regions may play the key role in shaping the global climate. This supposition then found full confirmation in empirical and model research conducted in recent decades. The intensification of global warming after about 1975 brought into focus the physical causes of this phenomenon. The first climate models, created at that time, and analyses of long observation series consistently showed that the Polar regions are the most sensitive to climate changes. This aroused the interest of numerous researchers, who thought that the examination of the processes taking place in these regions might help determine the mechanisms responsible for the ‘workings’ of the global climate system. The urgent need to better recognize these processes in the Polar regions was probably the main impulse behind the organization of the fourth International Polar Year (IPY) in 2007–2008. The success of this international scientific effort also influenced the decision to continue the greater than usual activity in the coming years, after the official end of the fourth IPY (International Polar Initiative, http://internationalpolarinitiative. org/IPIabout. html). The first edition of this book was published in 2003, just before the birth of the idea for that fourth IPY. Since that time, interest in the study of the Arctic climate has significantly increased, due–among other reasons–to the dramatic changes in the environment observed in the Arctic following the large-scale warming of the area (more that 1 C above the long-term mean) that began in the mid-1990s. The most spectacular change was observed in sea ice characteristics (extent and thickness). Suffice to say, that in 2007 and 2012, a record minimum sea ice was noted during September in the Arctic Ocean. The previously mentioned unprecedented level of interest in the Arctic climate resulted in the publishing of many new important papers, books, reports, etc., of which the majority have been taken into account in this new edition of the Climate of the Arctic. The primary aim of the 11 chapters of this publication is to present the current state of knowledge of:(1) the Arctic climate in the second half of the twentieth century and its main drivers (Chaps. 1, 2, 3, 4, 5, 6, 7, 8, and 9), and (2) changes in the Arctic climate over the last 10–11,000 years (Chaps. 10 and 11). In view of the