2500 Years of European Climate Variability and Human Susceptibility

@article{Bntgen20112500YO,
  title={2500 Years of European Climate Variability and Human Susceptibility},
  author={Ulf B{\"u}ntgen and Willy Tegel and Kurt Nicolussi and Michael McCormick and David C. Frank and Valerie Trouet and Jed O. Kaplan and Franz Herzig and Karl Uwe Heussner and Heinz Wanner and J{\"u}rg Luterbacher and Jan Esper},
  journal={Science},
  year={2011},
  volume={331},
  pages={578 - 582}
}
Variability of central European temperature and precipitation shows correlations with some major historical changes. Climate variations influenced the agricultural productivity, health risk, and conflict level of preindustrial societies. Discrimination between environmental and anthropogenic impacts on past civilizations, however, remains difficult because of the paucity of high-resolution paleoclimatic evidence. We present tree ring–based reconstructions of central European summer… 

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References

SHOWING 1-10 OF 79 REFERENCES

Atlantic Forcing of Persistent Drought in West Africa

TLDR
It is found that intervals of severe drought lasting for periods ranging from decades to centuries are characteristic of the monsoon and are linked to natural variations in Atlantic temperatures, indicating that themonsoon is capable of longer and more severe future droughts.

The climatic interpretation of pan-European signature years in oak ring-width series

Large-scale signature years, in which oak growth across much of northern Europe varies consistently, are identified. Postulating that the likely cause of such widespread departures in growth is

Assessing the spatial signature of European climate reconstructions

Much progress has recently been made in reconstructing European temperature variabil- ity over centuries to millennia. In contrast, there are only a few attempts at long-term precipitation and/or

Adjustment for proxy number and coherence in a large‐scale temperature reconstruction

Proxy records may display fluctuations in climate variability that are artifacts of changing replication and interseries correlation of constituent time‐series and also from methodological

Atlantic hurricanes and climate over the past 1,500 years

TLDR
The statistical model indicates that the medieval peak, which rivals or even exceeds (within uncertainties) recent levels of activity, results from the reinforcing effects of La-Niña-like climate conditions and relative tropical Atlantic warmth.

Historical Climatology In Europe – The State Of The Art

This paper discusses the state of European research in historical climatology. This field of science and an overview of its development are described in detail. Special attention is given to the

Climate and the Collapse of Maya Civilization

TLDR
A seasonally resolved record of titanium shows that the collapse of Maya civilization in the Terminal Classic Period occurred during an extended regional dry period, punctuated by more intense multiyear droughts centered at approximately 810, 860, and 910 A.D.

Summer temperature variations in the European Alps, A.D. 755-2004

Abstract Annually resolved summer temperatures for the European Alps are described. The reconstruction covers the a.d. 755–2004 period and is based on 180 recent and historic larch [Larix decidua

Cultural Responses to Climate Change During the Late Holocene

TLDR
Four case studies drawn from New and Old World civilizations document societal responses to prolonged drought, including population dislocations, urban abandonment, and state collapse.
...