Abstract
Paleoclimate information has played an instrumental role in showing how fast climate can vary and how large these changes can be. It provided the first vivid demonstration of the relationships between atmospheric greenhouse gas concentrations and surface air temperatures, as well as striking representations of climate change impacts and possible feedbacks within the climate system, such as those associated with vegetation or ice sheet changes. Here, a short review of recent advances in paleoclimate studies is provided, with the objective of showing what this information on past climates and environments can bring to research on current and possible future climates. We advocate that (1) paleoclimatic and paleoenvironmental information can be leveraged for narratives about climate change, in particular at the local and regional levels, (2) paleoclimate data is essential for out-of-range tests of climate models, since future climates are also out of the range of recent climate information used for calibrating climate models, (3) paleoclimate data, in particular for the last millennia, is essential for taking multi-centennial and multi-millennial variability into account when describing trends related to anthropogenic forcings and attributing climate change signals, in particular for extreme and rare events, and (4) paleoclimates also provide extremely valuable information for initializing the slow components of climate models. In addition, we show how paleoclimate studies can be beneficial to put recent and future climate change into context and improve our knowledge on key processes. They can both benefit from and contribute to models and knowledge based on the study of recent and future climates.
| Originalsprache | Englisch |
|---|---|
| Aufsatznummer | 1511997 |
| Fachzeitschrift | Frontiers in Climate |
| Jahrgang | 6 |
| DOIs | |
| Publikationsstatus | Veröffentlicht - 11 Dez. 2024 |
Fördermittel
The author(s) declare that financial support was received for the research, authorship, and/or publication of this article. MK and PB acknowledge the support from the CLIMERI-France research infrastructure as well Agence Nationale de la Recherche - France 2030 as part of the PEPR TRACCS programme under grant number ANR-22-EXTR-0001. CMC acknowledges the financial support from FAPESP (grants 2018/15123-4 and 2019/24349-9) and CNPq (grant 312458/2020-7). JZ and BLO-B acknowledge the support by the National Center for Atmospheric Research (NCAR), which is a major facility sponsored by the National Science Foundation (NSF) under Cooperative Agreement No.1852977. The CESM project was supported primarily by the National Science Foundation (NSF). Computing and data storage resources, including the Cheyenne supercomputer (doi: 10.5065/D6RX99HX), were provided by the Computational and Information Systems Laboratory (CISL) at NCAR. The Past Global Changes (PAGES) project receives support primarily from the Swiss Academy of Sciences and the Chinese Academy of Sciences. KR acknowledges funding through the Deutsche Forschungsgemeinschaft (STACY, grant no. 395588486) and the federal Ministry of Education and Research of Germany (PalMod III, grant nos 01LP2311C, 01LP2310A). Louise Sime is supported by the funding from NERC: The Sensitivity of the West Antarctic Ice Sheet to +2C: SWAIS2C. NE/X009386/1; and Assessing ocean-forced, marine-terminating glacier change in Greenland during climatic warm periods and its impact on marine productivity: KANG-GLAC NE/V006509/1. AR acknowledges funding from the European Research Council (ERC) under the European Union\u2019s Horizon 2020 research and innovation programme (grant agreement n. 802414).
UN SDGs
Dieser Output leistet einen Beitrag zu folgendem(n) Ziel(en) für nachhaltige Entwicklung
-
SDG 13 – Maßnahmen zum Klimaschutz
ÖFOS 2012
- 105204 Klimatologie
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