Monthly, seasonal and annual temperature reconstructions for Central Europe derived from documentary evidence and instrumental records since AD 1500

被引:160
作者
Dobrovolny, Petr [1 ]
Moberg, Anders [2 ]
Brazdil, Rudolf [1 ]
Pfister, Christian [3 ]
Glaser, Ruediger [4 ]
Wilson, Rob [5 ]
van Engelen, Aryan [6 ]
Limanowka, Danuta [7 ]
Kiss, Andrea [8 ]
Halickova, Monika [1 ]
Mackova, Jarmila [1 ]
Riemann, Dirk [4 ]
Luterbacher, Juerg [9 ]
Boehm, Reinhard [10 ]
机构
[1] Masaryk Univ, Inst Geog, CS-61137 Brno, Czech Republic
[2] Stockholm Univ, Dept Phys Geog & Quaternary Geol, S-10691 Stockholm, Sweden
[3] Univ Bern, Hist Inst, Bern, Switzerland
[4] Univ Freiburg, Inst Phys Geog, Freiburg, Germany
[5] Univ St Andrews, Sch Geog & Geosci, St Andrews, Fife, Scotland
[6] Royal Netherlands Meteorol Inst, NL-3730 AE De Bilt, Netherlands
[7] Inst Meteorol & Water Management, Krakow, Poland
[8] Univ Szeged, Dept Phys Geog & Geoinformat, Szeged, Hungary
[9] Univ Giessen, Dept Geog Climatol Climate Dynam & Climate Change, Giessen, Germany
[10] Cent Inst Meteorol & Geodynam, Vienna, Austria
基金
瑞典研究理事会;
关键词
NORTHERN-HEMISPHERE; HISTORICAL CLIMATOLOGY; TIME-SERIES; VARIABILITY; DENDROCLIMATOLOGY; INFORMATION; EXTREMES; DENSITY; TRENDS; WINTER;
D O I
10.1007/s10584-009-9724-x
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Monthly temperature series for Central Europe back to AD 1500 are developed from documentary index series from Germany, Switzerland and the Czech Republic (1500-1854) and 11 instrumental temperature records (1760-2007). Documentary evidence from the Low Countries, the Carpathian Basin and Poland are used for cross-checking for earlier centuries. The instrumental station records are corrected for inhomogeneities, including insufficient radiation protection of early thermometers and the urban heat island effect. For overlapping period (1760-1854), the documentary data series correlate with instrumental temperatures, most strongly in winter (86% explained variance in January) and least in autumn (56% in September). For annual average temperatures, 81% of the variance is explained. Verification statistics indicate high reconstruction skill for most months and seasons. The last 20 years (since 1988) stand out as very likely the warmest 20-year period, accounting for the calibration uncertainty and decreases in proxy data quality before the calibration period. The new reconstruction displays a previously unobserved long-term decrease in DJF, MAM and JJA temperature variability over last five centuries. Compiled monthly, seasonal and annual series can be used to improve the robustness of gridded large-scale European temperature reconstructions and possible impact studies. Further improvement of the reconstruction would be achieved if documentary data from other European countries are further developed.
引用
收藏
页码:69 / 107
页数:39
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