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20 papers included: tree ring records from Tasmania; evaluation of the relative importance of temperature and precipitation to major paleoenvironmental changes; link between volcanism and climate cooling; examination of decadel to century time-scale variability in the climate system; nonlinear time series analysis; deterministic chaos offers a new paradigm for understanding irregular fluctuations; summer temperature reconstructions from tree-ring chronologies; paleoclimatic data for Mexico; South American hydrology; El Nino events; and more.
A profound knowledge of the past climate is vital for our understanding of global warming. The past 2000 years are both the period which is of most relevance to the next century and that for which there is the most evidence. High-resolution proxy records for this period are available from a variety of sources. Five sections consider dendroclimatology, ice cores, corals, historical records, lake varves, and other indicators. The final two sections cover the histories of various forcing factors and attempt to bring together records from a variety of sources and provide explanations.