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Recognising bias in Common Era temperature reconstructions

Urheber*innen

Büntgen,  Ulf
External Organizations;

Arseneault,  Dominique
External Organizations;

Boucher,  Étienne
External Organizations;

Churakova (Sidorova),  Olga V.
External Organizations;

Gennaretti,  Fabio
External Organizations;

Crivellaro,  Alan
External Organizations;

Hughes,  Malcolm K.
External Organizations;

Kirdyanov,  Alexander V.
External Organizations;

Klippel,  Lara
External Organizations;

Krusic,  Paul J.
External Organizations;

Linderholm,  Hans W.
External Organizations;

Ljungqvist,  Fredrik C.
External Organizations;

/persons/resource/Josef.Ludescher

Ludescher,  Josef
Potsdam Institute for Climate Impact Research;

McCormick,  Michael
External Organizations;

Myglan,  Vladimir S.
External Organizations;

Nicolussi,  Kurt
External Organizations;

Piermattei,  Alma
External Organizations;

Oppenheimer,  Clive
External Organizations;

Reinig,  Frederick
External Organizations;

Sigl,  Michael
External Organizations;

Vaganov,  Eugene A.
External Organizations;

Esper,  Jan
External Organizations;

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Volltexte (frei zugänglich)

27339oa.pdf
(Verlagsversion), 3MB

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Zitation

Büntgen, U., Arseneault, D., Boucher, É., Churakova (Sidorova), O. V., Gennaretti, F., Crivellaro, A., Hughes, M. K., Kirdyanov, A. V., Klippel, L., Krusic, P. J., Linderholm, H. W., Ljungqvist, F. C., Ludescher, J., McCormick, M., Myglan, V. S., Nicolussi, K., Piermattei, A., Oppenheimer, C., Reinig, F., Sigl, M., Vaganov, E. A., Esper, J. (2022): Recognising bias in Common Era temperature reconstructions. - Dendrochronologia, 74, 125982.
https://doi.org/10.1016/j.dendro.2022.125982


Zitierlink: https://publications.pik-potsdam.de/pubman/item/item_27339
Zusammenfassung
A steep decline in the quality and quantity of available climate proxy records before medieval times challenges any comparison of reconstructed temperature and hydroclimate trends and extremes between the first and second half of the Common Era. Understanding of the physical causes, ecological responses and societal con- sequences of past climatic changes, however, demands highly-resolved, spatially-explicit, seasonally-defined and absolutely-dated archives over the entire period in question. Continuous efforts to improve existing proxy records and reconstruction methods and to develop new ones, as well as clear communication of all uncertainties (within and beyond academia) must be central tasks for the paleoclimate community.