...
  • 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>Climatic Change >The 'Little Ice Age': Local and global perspectives - Preface
【24h】

The 'Little Ice Age': Local and global perspectives - Preface

机译：“小冰河时代”：本地和全球视角-前言

获取原文
获取原文并翻译 | 示例
           
页面导航
  • 摘要
  • 著录项
  • 相似文献
  • 相关主题

摘要

This volume of Climatic Change is devoted to the study of tile climate of the last 1000 years, with a major emphasis on the last few centuries. The timespan encompasses what has been referred to as the "Little Ice Age" (Bradley, 1992). This term was originally coined by glaciologists, with reference to the most recent major glacial advance of the Holocene (Bradley and Jones, 1993). Although other such advances in different parts of the world may not have been synchronous, the term "Little Ice Age" has come to be associated with the period of a widespread foreward movement of European glaciers between about 1450 to 1850, as well as with relatively cooler temperatures. The issue of whether or not this concept is appropriate, is a major theme of many of the papers included in this volume. The main geographical focus here is on the North Atlantic and European sectors. Much more is known about the climate history from these regions than other parts of the world. The wealth of knowledge available thus enables different types of proxy climate evidence to be intercompared, and extensive climate calibration of these data is possible using early instrumental observations which extend back to the mid-to-late eighteenth century. Another focus of this special issue is the climate of Iceland, and its climatological links with Greenland, and the western half of Europe. A provocative introductory chapter (Ogilvie and J6nsson) considers the origins and usage of the term "Little Ice Age", and also discusses whether this concept has, ill fact, outlived its usefulness as an accurate description of the general climate of ca. 1600 to 1900. This paper also outlines early Icelandic and Scandinavian research on the history of climate, as well as aspects of the present-day climate of Iceland.
机译：气候变化量致力于研究过去1000年的瓷砖气候，主要侧重于最近几个世纪。时间跨度包含了所谓的“小冰河时代”（Bradley，1992）。这个术语最初是由冰川学家根据全新世的最新主要冰川进展创造的（Bradley and Jones，1993）。尽管在世界各地的其他类似进步可能未同步进行，但“小冰河时代”一词已与大约1450至1850年间欧洲冰川广泛前移的时期有关，并且与温度较低。这个概念是否合适的问题是本卷中许多论文的主题。这里的主要地理重点是北大西洋和欧洲地区。这些地区对气候历史的了解要比世界其他地区多得多。因此，可用的丰富知识可以对不同类型的代理气候证据进行比较，并且可以使用可追溯到18世纪中后期的早期仪器观测对这些数据进行广泛的气候校准。本期特刊的另一个重点是冰岛的气候，以及与格陵兰岛和欧洲西半部的气候联系。引人入胜的介绍性章节（Ogilvie和J6nsson）考虑了“小冰河时代”一词的起源和用法，并讨论了这个概念是否事实上已经超过了其对ca总体气候的准确描述的用处。 1600年至1900年。本文还概述了冰岛人和斯堪的纳维亚人对气候历史的早期研究，以及当今冰岛气候的各个方面。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱：kefu@zhangqiaokeyan.com

京公网安备：11010802029741号 ICP备案号：京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有

  • 客服微信

  • 服务号