| | The Climate of the Last Millennium |
| | 9,38 | | MB |
| | 45 | | stron |
| | 2380 | | ID | University of Massachusetts |
| | 2002 | | rok |
| | Introduction |
| | We are living in unusual times. Twentieth century climate was dominated by near universal warming |
| | with almost all parts of the globe experiencing temperatures at the end of the century that were |
| | significantly higher than when it began (Figure 6.1) (Parker et al. 1994; Jones et al. 1999). However |
| | the instrumental data provide only a limited temporal perspective on present climate. How unusual |
| | was the last century when placed in the longer-term context of climate in the centuries and millennia |
| | leading up to the 20th century? Such a perspective encompasses the period before large-scale |
| | contamination of the global atmosphere by human activities and global-scale changes in land- |
| | surface conditions. |
| | By studying the records of climate variability and forcing mechanisms in the recent past, it is |
| | possible to establish how the climate system varied under “natural” conditions, before anthropogenic |
| | forcing became significant. Natural forcing mechanisms will continue to operate in the 21st |
| | century, and will play a role in future climate variations, so regardless of how anthropogenic effects |
| | develop it is essential to understand the underlying background record of forcing and climate |
| | system response. |