Tree-rings and people - different views on the 1540
Megadrought. Reply to Buntgen et al. 2015

u 2015

Tree-rings and people - different views on the 1540 Megadrought. Reply to Buntgen et al. 2015

PFISTER, Christian; Otakar WETTER; Rudolf BRÁZDIL; Petr DOBROVOLNÝ; R. GLASER et al.

Základní údaje

Originální název

Tree-rings and people - different views on the 1540 Megadrought. Reply to Buntgen et al. 2015

Autoři

Vydání

DORDRECHT, 8 s. 2015

Nakladatel

SPRINGER

Další údaje

Jazyk

angličtina

Typ výsledku

Účelové publikace

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 3.344

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/15:00081169

Organizační jednotka

Přírodovědecká fakulta

ISSN

DOI

https://doi.org/10.1007/s10584-015-1429-8

UT WoS

000357037700002

Klíčová slova anglicky

drought; warmer; heat

Štítky

AKR

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 23. 6. 2020 09:37, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

Büntgen et al. (2015; hereinafter B15) present the result of new research which question the results of Wetter et al. 2014, (hereinafter W14) and Wetter et al. (2013, hereinafter W13)regarding European climate in 1540. B15 conclude from tree-ring evidence that the results based on documentary data of W14 probably overstated the intensity and duration of the 1540 drought event. W14 termed it Megadrought because of its extreme duration and spatial extent compared to other drought events in central Europe, although they note that the term is generally used for decadal rather than for single-year droughts (Seneviratne et al. 2012). We take the opportunity to recall the following issues. Firstly, when dealing with drought the complexity of this phenomenon should be kept in mind. Meteorological drought defined as a large negative precipitation anomaly during a certain period can trigger agricultural, hydrological, groundwater and socioeconomic droughts. Lloyd-Hughes (2013] and references cited herein) concluded that any workable objective definition of drought does not exist. To quantify droughts, various indices based on precipitation, temperature and evapotranspiration are used such as the Standardized Precipitation Index (SPI), Standardized Precipitation Evapotranspiration Index (SPEI), Z-index and PDSI. Their calculation depends on different periods (seasons, combination of months) and so different indices may classify the same drought episode differently (e.g. Brázdil et al.2014).

Návaznosti

GA13-04291S, projekt VaV

Název: Rekonstrukce hydro-klimatických podmínek jara a léta posledního milénia v České republice na základě dubové standardní chronologie

Investor: Grantová agentura ČR, Rekonstrukce hydro-klimatických podmínek jara a léta posledního milénia v České republice na základě šířky letokruhů dubu

GA13-19831S, projekt VaV

Název: Hydrometeorologické extrémy na jižní Moravě odvozené z dokumentárních pramenů

Investor: Grantová agentura ČR, Hydrometeorologické extrémy na jižní Moravě odvozené z dokumentárních pramenů

Citovat

PFISTER, Christian; Otakar WETTER; Rudolf BRÁZDIL; Petr DOBROVOLNÝ; R. GLASER; Juerg LUTERBACHER; SI. SENEVIRATNE; E. ZORITA; MJ. ALCOFORADO; M. BARRIENDOS; U. BIEBER; KH. BURMEISTER; C. CAMENISCH; A. CONTINO; U. GRUNEWALD; J. HERGET; I. HIMMELSBACH; T. LABBÉ; Danuta LIMANÓWKA; L. LITZENBURGER; Andrea KISS; Oldřich KOTYZA; O. NORDLI; K. PRIBYL; D. RETSO; D. RIEMANN; Christian ROHR; W. SIEGFRIED; JL. SPRING; J. SODERBERG; S. WAGNER a JP. WERNER. Tree-rings and people - different views on the 1540 Megadrought. Reply to Buntgen et al. 2015. DORDRECHT: SPRINGER, 2015, 8 s. ISSN 0165-0009. Dostupné z: https://doi.org/10.1007/s10584-015-1429-8.

@misc{1315991,
   author = {Pfister, Christian and Wetter, Otakar and Brázdil, Rudolf and Dobrovolný, Petr and Glaser, R. and Luterbacher, Juerg and Seneviratne, SI. and Zorita, E. and Alcoforado, MJ. and Barriendos, M. and Bieber, U. and Burmeister, KH. and Camenisch, C. and Contino, A. and Grunewald, U. and Herget, J. and Himmelsbach, I. and Labbé, T. and Limanówka, Danuta and Litzenburger, L. and Kiss, Andrea and Kotyza, Oldřich and Nordli, O. and Pribyl, K. and Retso, D. and Riemann, D. and Rohr, Christian and Siegfried, W. and Spring, JL. and Soderberg, J. and Wagner, S. and Werner, JP.},
   address = {DORDRECHT},
   doi = {https://doi.org/10.1007/s10584-015-1429-8},
   keywords = {drought; warmer; heat},
   language = {eng},
   location = {DORDRECHT},
   publisher = {SPRINGER},
   title = {Tree-rings and people - different views on the 1540 Megadrought. Reply to Buntgen et al. 2015},
   url = {https://link.springer.com/article/10.1007/s10584-015-1429-8},
   year = {2015}
}

TY  - GEN
ID  - 1315991
AU  - Pfister, Christian - Wetter, Otakar - Brázdil, Rudolf - Dobrovolný, Petr - Glaser, R. - Luterbacher, Juerg - Seneviratne, SI. - Zorita, E. - Alcoforado, MJ. - Barriendos, M. - Bieber, U. - Burmeister, KH. - Camenisch, C. - Contino, A. - Grunewald, U. - Herget, J. - Himmelsbach, I. - Labbé, T. - Limanówka, Danuta - Litzenburger, L. - Kiss, Andrea - Kotyza, Oldřich - Nordli, O. - Pribyl, K. - Retso, D. - Riemann, D. - Rohr, Christian - Siegfried, W. - Spring, JL. - Soderberg, J. - Wagner, S. - Werner, JP.
PY  - 2015
TI  - Tree-rings and people - different views on the 1540 Megadrought. Reply to Buntgen et al. 2015
PB  - SPRINGER
CY  - DORDRECHT
KW  - drought
KW  - warmer
KW  - heat
UR  - https://link.springer.com/article/10.1007/s10584-015-1429-8
N2  - Büntgen et al. (2015; hereinafter B15) present the result of new research which question the results of Wetter et al. 2014, (hereinafter W14) and Wetter et al. (2013, hereinafter W13)regarding European climate in 1540. B15 conclude from tree-ring evidence that the results based on documentary data of W14 probably overstated the intensity and duration of the 1540 drought event. W14 termed it Megadrought because of its extreme duration and spatial extent compared to other drought events in central Europe, although they note that the term is generally used for decadal rather than for single-year droughts (Seneviratne et al. 2012). We take the opportunity to recall the following issues. Firstly, when dealing with drought the complexity of this phenomenon should be kept in mind. Meteorological drought defined as a large negative precipitation anomaly during a certain period can trigger agricultural, hydrological, groundwater and socioeconomic droughts. Lloyd-Hughes (2013] and references cited herein) concluded that any workable objective definition of drought does not exist. To quantify droughts, various indices based on precipitation, temperature and evapotranspiration are used such as the Standardized Precipitation Index (SPI), Standardized Precipitation Evapotranspiration Index (SPEI), Z-index and PDSI. Their calculation depends on different periods (seasons, combination of months) and so different indices may classify the same drought episode differently (e.g. Brázdil et al.2014).
ER  -

PFISTER, Christian; Otakar WETTER; Rudolf BRÁZDIL; Petr DOBROVOLNÝ; R. GLASER; Juerg LUTERBACHER; SI. SENEVIRATNE; E. ZORITA; MJ. ALCOFORADO; M. BARRIENDOS; U. BIEBER; KH. BURMEISTER; C. CAMENISCH; A. CONTINO; U. GRUNEWALD; J. HERGET; I. HIMMELSBACH; T. LABBÉ; Danuta LIMANÓWKA; L. LITZENBURGER; Andrea KISS; Oldřich KOTYZA; O. NORDLI; K. PRIBYL; D. RETSO; D. RIEMANN; Christian ROHR; W. SIEGFRIED; JL. SPRING; J. SODERBERG; S. WAGNER a JP. WERNER. \textit{Tree-rings and people - different views on the 1540 Megadrought. Reply to Buntgen et al. 2015}. DORDRECHT: SPRINGER, 2015, 8 s. ISSN~0165-0009. Dostupné z: https://doi.org/10.1007/s10584-015-1429-8.

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