How stable are twentieth-century calibration models? A high-resolution summer temperature reconstruction for the eastern Swiss Alps back to AD 1580 derived from proglacial varved sediments

被引:41
作者
Blass, Alex [1 ]
Grosjean, Martin
Troxler, Andrea
Sturm, Michael
机构
[1] Swiss Fed Inst Aquat Sci & Technol, CH-8600 Dubendorf, Switzerland
[2] NCCR Climate, CH-3012 Bern, Switzerland
[3] Univ Bern, Dept Phys Geog, CH-3012 Bern, Switzerland
关键词
late Holocene; varves; lake sediments; climate reconstruction; 'Little Ice Age'; glacier; Alps;
D O I
10.1177/0959683607073278
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
We found a significant positive correlation between local summer air temperature (May-September) and the annual sediment mass accumulation rate (MAR) in Lake Silvaplana (46 degrees N, 9 degrees E, 1800 in a.s.l.) during the twentieth century (r = 0.69, p < 0.001 for decadal smoothed series). Sediment trap data (2001-2005) confirm this relation with exceptionally high particle yields during the hottest summer of the last 140 years in 2003. On this base we developed a decadal-scale summer temperature reconstruction back to AD 1580. Surprisingly, the comparison of our reconstruction with two other independent regional summer temperature reconstructions (based on tree-rings and documentary data) revealed a significant negative correlation for the pre-1900 data (ie, late 'Little Ice Age'). This demonstrates that the correlation between MAR and summer temperature is not stable in time and the actualistic principle does not apple in this case. We suggest that different climatic regimes (modern/'Little Ice Age') lead to changing state conditions in the catchment and thus to considerably different sediment transport mechanisms. Therefore, we calibrated our MAR data with gridded early instrumental temperature series from AD 1760-1880 (r = - 0.48, p < 0.01 for decadal smoothed series) to properly reconstruct the late LIA climatic conditions. We found exceptionally low temperatures between AD 1580 and 1610 (0.75 degrees C below twentieth-century mean) and during the late Maunder Minimum from AD 1680 to 1710 (0.5 degrees C below twentieth-century mean). In general, summer temperatures did not experience major negative departures from the twentieth-century mean during the late 'Little Ice Age'. This compares well with the two existing independent regional reconstructions suggesting that the LIA in the Alps was mainly a phenomenon of the cold season.
引用
收藏
页码:51 / 63
页数:13
相关论文
共 51 条
[1]  
AUER I, 2006, IN PRESS INT J CLIMA
[2]  
Berner R.A., 1971, PRINCIPLES CHEM SEDI
[3]   The last 1300 years of environmental history recorded in the sediments of Lake Sils (Engadine, Switzerland) [J].
Blass, A ;
Anselmetti, FS ;
Grosjean, M ;
Sturm, M .
ECLOGAE GEOLOGICAE HELVETIAE, 2005, 98 (03) :319-332
[4]  
Blass A, 2003, ECLOGAE GEOL HELV, V96, pS59
[5]   A CRITICAL-REVIEW OF SEDIMENTATION TRAP TECHNIQUE [J].
BLOESCH, J ;
BURNS, NM .
SCHWEIZERISCHE ZEITSCHRIFT FUR HYDROLOGIE-SWISS JOURNAL OF HYDROLOGY, 1980, 42 (01) :15-55
[6]   Historical climatology in Europe -: The state of the art [J].
Brázdil, R ;
Pfister, C ;
Wanner, H ;
Von Storch, H ;
Luterbacher, J .
CLIMATIC CHANGE, 2005, 70 (03) :363-430
[7]   Influence of volcanic eruptions on Northern Hemisphere summer temperature over the past 600 years [J].
Briffa, KR ;
Jones, PD ;
Schweingruber, FH ;
Osborn, TJ .
NATURE, 1998, 393 (6684) :450-455
[8]   A 1052-year tree-ring proxy for Alpine summer temperatures [J].
Büntgen, U ;
Esper, J ;
Frank, DC ;
Nicolussi, K ;
Schmidhalter, M .
CLIMATE DYNAMICS, 2005, 25 (2-3) :141-153
[9]   Temperature and precipitation variability in the european Alps since 1500 [J].
Casty, C ;
Wanner, H ;
Luterbacher, J ;
Esper, J ;
Böhm, R .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2005, 25 (14) :1855-1880