Holocene temperature evolution in the Northern Hemisphere high latitudes - Model-data comparisons

QUATERNARY SCIENCE REVIEWS

卷:173

Article

Zhang, Yurui^1,2  Renssen, Hans^2,3  Seppa, Heikki¹  Valdes, Paul J.⁴ 

[1] Univ Helsinki, Dept Geosci & Geog, POB 64, FI-00014 Helsinki, Finland

[2] Vrije Univ Amsterdam, Dept Earth Sci, Boelelaan 1085, NL-1081 HV Amsterdam, Netherlands

[3] Univ Coll Southeast Norway, Dept Nat Sci & Environm Hlth, N-3800 Bo I Telemark, Norway

[4] Univ Bristol, Sch Geog Sci, Bristol BS8 1SS, Avon, England

关键词: Holocene;    Paleoclimatology;    Paleoclimate modeling;    Fennoscandia;    N America;    Europe;    Greenland;    Russia;    Continental biotic proxies;    Ice cores;   

DOI  :  10.1016/j.quascirev.2017.07.018

来源: Elsevier

【 摘 要 】

Heterogeneous Holocene climate evolutions in the Northern Hemisphere high latitudes are primarily determined by orbital-scale insolation variations and melting ice sheets. Previous inter-model comparisons have revealed that multi-simulation consistencies vary spatially. We, therefore, compared multiple model results with proxy-based reconstructions in Fennoscandia, Greenland, north Canada, Alaska and Siberia. Our model-data comparisons reveal that data and models generally agree in Fennoscandia, Greenland and Canada, with the early-Holocene warming and subsequent gradual decrease to 0 ka BP (hereinafter referred as ka). In Fennoscandia, simulations and pollen data suggest a 2 degrees C warming by 8 ka, but this is less expressed in chironomid data. In Canada, a strong early-Holocene warming is suggested by both the simulations and pollen results. In Greenland, the magnitude of early-Holocene warming ranges from 6 degrees C in simulations to 8 degrees C in delta O-18-based temperatures. Simulated and reconstructed temperatures are mismatched in Alaska. Pollen data suggest strong early Holocene warming, while the simulations indicate constant Holocene cooling, and chironomid data show a stable trend. Meanwhile, a high frequency of Alaskan peatland initiation before 9 ka can reflect a either high temperature, high soil moisture or large seasonality. In high-latitude Siberia, although simulations and proxy data depict high Holocene temperatures, these signals are noisy owing to a large spread in the simulations and between pollen and chironomid results. On the whole, the Holocene climate evolutions in most regions (Fennoscandia, Greenland and Canada) are well established and understood, but important questions regarding the Holocene temperature trend and mechanisms remain for Alaska and Siberia. (C) 2017 Elsevier Ltd. All rights reserved.

【 授权许可】

Free