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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F10%3A00044264%21RIV11-MSM-14310___
rdf:type
n11:Vysledek skos:Concept
dcterms:description
Future climate change will likely in%22uence the frequency and intensity of weather extremes. As such events are by de!nition rare, long records are required to understand their characteristics, drivers, and consequences on ecology and society. Herein we provide a unique perspective on regional-scale temperature extremes over the past millennium, using three tree-ring maximum latewood density (MXD) chronologies from higher elevations in the European Alps. We verify the tree-ring-based extremes using documentary evidences from Switzerland, the Czech Republic, and Central Europe that allowed the identi!cation of 44 summer extremes over the 1550-2003 period. These events include cold temperatures in 1579, 1628, 1675, and 1816, as well as warm ones in 1811 and 2003. Prior to 1550, we provide new evidence for cold (e.g., 1068 and 1258) and warm (e.g., 1333) summers derived from the combined MXD records and thus help to characterize high-frequency temperature variability during medieval times. Future climate change will likely in%22uence the frequency and intensity of weather extremes. As such events are by de!nition rare, long records are required to understand their characteristics, drivers, and consequences on ecology and society. Herein we provide a unique perspective on regional-scale temperature extremes over the past millennium, using three tree-ring maximum latewood density (MXD) chronologies from higher elevations in the European Alps. We verify the tree-ring-based extremes using documentary evidences from Switzerland, the Czech Republic, and Central Europe that allowed the identi!cation of 44 summer extremes over the 1550-2003 period. These events include cold temperatures in 1579, 1628, 1675, and 1816, as well as warm ones in 1811 and 2003. Prior to 1550, we provide new evidence for cold (e.g., 1068 and 1258) and warm (e.g., 1333) summers derived from the combined MXD records and thus help to characterize high-frequency temperature variability during medieval times.
dcterms:title
Five centuries of Central European temperature extremes reconstructed from tree-ring density and documentary evidence Five centuries of Central European temperature extremes reconstructed from tree-ring density and documentary evidence
skos:prefLabel
Five centuries of Central European temperature extremes reconstructed from tree-ring density and documentary evidence Five centuries of Central European temperature extremes reconstructed from tree-ring density and documentary evidence
skos:notation
RIV/00216224:14310/10:00044264!RIV11-MSM-14310___
n3:aktivita
n6:R
n3:aktivity
R
n3:cisloPeriodika
10
n3:dodaniDat
n12:2011
n3:domaciTvurceVysledku
n13:6007929 n13:1593552
n3:druhVysledku
n16:J
n3:duvernostUdaju
n10:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
259349
n3:idVysledku
RIV/00216224:14310/10:00044264
n3:jazykVysledku
n17:eng
n3:klicovaSlova
temperature extremes maximum latewood density documentary evidence European Alps Central Europe palaeoclimatology
n3:klicoveSlovo
n9:temperature%20extremes%20maximum%20latewood%20density%20documentary%20evidence%20European%20Alps%20Central%20Europe%20palaeoclimatology
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[5C00FFA48370]
n3:nazevZdroje
Global and Planetary Change
n3:obor
n8:DG
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
7
n3:rokUplatneniVysledku
n12:2010
n3:svazekPeriodika
72
n3:tvurceVysledku
Brázdil, Rudolf Battipaglia, Giovanna Esper, Jan Pfister, Christian Frank, David Büntgen, Ulf Dobrovolný, Petr
n3:wos
000280040300009
s:issn
0921-8181
s:numberOfPages
10
n15:organizacniJednotka
14310