The role of land cover in the climate of glacial Europe
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Published:2021-06-14
Issue:3
Volume:17
Page:1161-1180
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ISSN:1814-9332
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Container-title:Climate of the Past
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language:en
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Short-container-title:Clim. Past
Author:
Velasquez PatricioORCID, Kaplan Jed O.ORCID, Messmer MartinaORCID, Ludwig PatrickORCID, Raible Christoph C.
Abstract
Abstract. Earth system models show wide disagreement when simulating the climate of the continents at the Last Glacial Maximum (LGM). This disagreement may be related to a variety of factors, including model resolution and an incomplete representation of Earth system processes. To assess the importance of resolution and land–atmosphere feedbacks on the climate of Europe, we performed an iterative asynchronously coupled land–atmosphere modelling experiment that combined a global climate model, a regional climate model, and a dynamic vegetation model. The regional climate and land cover models were run at high (18 km) resolution over a domain covering the ice-free regions of Europe. Asynchronous coupling between the regional climate model and the vegetation model showed that the land–atmosphere coupling achieves quasi-equilibrium after four iterations. Modelled climate and land cover agree reasonably well with independent reconstructions based on pollen and other paleoenvironmental proxies. To assess the importance of land cover on the LGM climate of Europe, we performed a sensitivity simulation where we used LGM climate but present-day (PD) land cover. Using LGM climate and land cover leads to colder and drier summer conditions around the Alps and warmer and drier climate in southeastern Europe compared to LGM climate determined by PD land cover. This finding demonstrates that LGM land cover plays an important role in regulating the regional climate. Therefore, realistic glacial land cover estimates are needed to accurately simulate regional glacial climate states in areas with interplays between complex topography, large ice sheets, and diverse land cover, as observed in Europe.
Funder
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
Publisher
Copernicus GmbH
Subject
Paleontology,Stratigraphy,Global and Planetary Change
Reference113 articles.
1. Alsos, I. G., Sjögren, P., Brown, A. G., Gielly, L., Merkel, M. K. F.,
Paus, A., Lammers, Y., Edwards, M. E., Alm, T., Leng, M., Goslar, T.,
Langdon, C. T., Bakke, J., and van der Bilt, W. G. M.: Last Glacial
Maximum environmental conditions at Andøya, northern Norway;
evidence for a northern ice-edge ecological
“hotspot”, Quaternary Sci. Rev.,
239, 106364, https://doi.org/10.1016/j.quascirev.2020.106364, 2020. a 2. Álvarez-Solas, J., Montoya, M., Ritz, C., Ramstein, G., Charbit, S., Dumas, C., Nisancioglu, K., Dokken, T., and Ganopolski, A.: Heinrich event 1: an example of dynamical ice-sheet reaction to oceanic changes, Clim. Past, 7, 1297–1306, https://doi.org/10.5194/cp-7-1297-2011, 2011. a 3. Baena Preysler, J., Carrión Santafé, E., Torres Navas, C., and
Vaquero Rodríguez, M.: Mousterian inside the upper Paleolithic? The
last interval of El Esquilleu (Cantabria, Spain) sequence,
Quatern. Int., 508, 153–163, https://doi.org/10.1016/j.quaint.2018.11.015, 2019. a 4. Bartlein, P. J., Harrison, S. P., Brewer, S., Connor, S., Davis, B. A. S.,
Gajewski, K., Guiot, J., Harrison-Prentice, T. I., Henderson, A., Peyron, O.,
Prentice, I. C., Scholze, M., Seppä, H., Shuman, B., Sugita, S.,
Thompson, R. S., Viau, A. E., Williams, J., and Wu, H.: Pollen-based
continental climate reconstructions at 6 and 21 ka: a global synthesis,
Clim. Dynam., 37, 775–802, https://doi.org/10.1007/s00382-010-0904-1, 2011. a, b, c, d, e 5. Beghin, P., Charbit, S., Kageyama, M., Combourieu-Nebout, N., Hatté, C.,
Dumas, C., and Peterschmitt, J.-Y.: What drives LGM precipitation over the
western Mediterranean? A study focused on the Iberian Peninsula and
northern Morocco, Clim. Dynam., 46, 2611–2631,
https://doi.org/10.1007/s00382-015-2720-0, 2016. a, b, c, d
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