2024
The IPCC's reductive Common Era temperature history
ESPER, Jan, Jason E. SMERDON, Kevin J. ANCHUKAITIS, Kathryn ALLEN, Edward R. COOK et. al.Základní údaje
Originální název
The IPCC's reductive Common Era temperature history
Autoři
ESPER, Jan, Jason E. SMERDON, Kevin J. ANCHUKAITIS, Kathryn ALLEN, Edward R. COOK, Rosanne ARRIGO, Sebastien GUILLET, Fredrik C. LJUNGQVIST, Frederick REINIG, Lea SCHNEIDER, Michael SIGL, Markus STOFFEL, Mirek TRNKA, Rob WILSON a Ulf BÜNTGEN (276 Německo, domácí)
Vydání
Communications Earth and Environment, London, Nature Publishing Group, 2024, 2662-4435
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10511 Environmental sciences
Stát vydavatele
Velká Británie a Severní Irsko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 7.900 v roce 2022
Organizační jednotka
Přírodovědecká fakulta
UT WoS
001209714400003
Klíčová slova anglicky
NORTHERN-HEMISPHERE TEMPERATURES; LAST MILLENNIUM; LARGE-SCALE; TREE-RINGS; SURFACE-TEMPERATURE; SUMMER TEMPERATURES; CLIMATE; RECONSTRUCTION; RESOLUTION; VARIABILITY
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 9. 5. 2024 08:41, Mgr. Marie Šípková, DiS.
Anotace
V originále
Common Era temperature variability has been a prominent component in Intergovernmental Panel on Climate Change reports over the last several decades and was twice featured in their Summary for Policymakers. A single reconstruction of mean Northern Hemisphere temperature variability was first highlighted in the 2001 Summary for Policymakers, despite other estimates that existed at the time. Subsequent reports assessed many large-scale temperature reconstructions, but the entirety of Common Era temperature history in the most recent Sixth Assessment Report of the Intergovernmental Panel on Climate Change was restricted to a single estimate of mean annual global temperatures. We argue that this focus on a single reconstruction is an insufficient summary of our understanding of temperature variability over the Common Era. We provide a complementary perspective by offering an alternative assessment of the state of our understanding in high-resolution paleoclimatology for the Common Era and call for future reports to present a more accurate and comprehensive assessment of our knowledge about this important period of human and climate history.