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  • 1
    Publication Date: 2017-09-09
    Description: Spatial covariance in the simulated temperature evolution over the past millennium has been reported to exceed that of multi-proxy-based reconstructions. Here, we use tree ring-based temperature reconstructions and state-of-the-art climate model simulations to assess temporal changes in Northern Hemisphere inter-continental temperature covariance during the last 1000 years. Tree ring-only approaches reveal stronger agreement with model simulations compared to multi-proxy networks. Although simulated temperatures exhibit a substantial spread among individual models, inter-continental temperature coherency is mainly driven by the cooling of large volcanic eruptions in 1257, 1452, 1600, and 1815 CE. The coherence of these synchronizing events appears to be elevated in several climate simulations relative to their own unforced covariance baselines and in comparison to the proxy reconstructions. This suggests that some models likely overestimate the amplitude of abrupt summer cooling in response to volcanic eruptions, particularly at larger spatial scales.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 2
    Publication Date: 2016-04-15
    Description: Accurate modelling and prediction of the local to continental-scale hydroclimate response to global warming is essential given the strong impact of hydroclimate on ecosystem functioning, crop yields, water resources, and economic security. However, uncertainty in hydroclimate projections remains large, in part due to the short length of instrumental measurements available with which to assess climate models. Here we present a spatial reconstruction of hydroclimate variability over the past twelve centuries across the Northern Hemisphere derived from a network of 196 at least millennium-long proxy records. We use this reconstruction to place recent hydrological changes and future precipitation scenarios in a long-term context of spatially resolved and temporally persistent hydroclimate patterns. We find a larger percentage of land area with relatively wetter conditions in the ninth to eleventh and the twentieth centuries, whereas drier conditions are more widespread between the twelfth and nineteenth centuries. Our reconstruction reveals that prominent seesaw patterns of alternating moisture regimes observed in instrumental data across the Mediterranean, western USA, and China have operated consistently over the past twelve centuries. Using an updated compilation of 128 temperature proxy records, we assess the relationship between the reconstructed centennial-scale Northern Hemisphere hydroclimate and temperature variability. Even though dry and wet conditions occurred over extensive areas under both warm and cold climate regimes, a statistically significant co-variability of hydroclimate and temperature is evident for particular regions. We compare the reconstructed hydroclimate anomalies with coupled atmosphere-ocean general circulation model simulations and find reasonable agreement during pre-industrial times. However, the intensification of the twentieth-century-mean hydroclimate anomalies in the simulations, as compared to previous centuries, is not supported by our new multi-proxy reconstruction. This finding suggests that much work remains before we can model hydroclimate variability accurately, and highlights the importance of using palaeoclimate data to place recent and predicted hydroclimate changes in a millennium-long context.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Ljungqvist, Fredrik Charpentier -- Krusic, Paul J -- Sundqvist, Hanna S -- Zorita, Eduardo -- Brattstrom, Gudrun -- Frank, David -- England -- Nature. 2016 Apr 7;532(7597):94-8. doi: 10.1038/nature17418.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of History, Stockholm University, SE-10691 Stockholm, Sweden. ; Centre for Medieval Studies, Stockholm University, SE-10691 Stockholm, Sweden. ; Bolin Centre for Climate Research, Stockholm University, SE-10691 Stockholm, Sweden. ; Navarino Environmental Observatory, GR-24001 Messinia, Greece. ; Department of Physical Geography, Stockholm University, SE-10691 Stockholm, Sweden. ; Helmholtz-Zentrum Geesthacht, Institute for Coastal Research, DE-21502 Geesthacht, Germany. ; Department of Mathematics, Stockholm University, SE-10691 Stockholm, Sweden. ; Swiss Federal Research Institute WSL, CH-8903 Birmensdorf, Switzerland.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/27078569" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; China ; *Climate ; Climate Change/*statistics & numerical data ; Ecosystem ; Geographic Mapping ; Geologic Sediments/chemistry ; History, 15th Century ; History, 16th Century ; History, 17th Century ; History, 18th Century ; History, 19th Century ; History, 20th Century ; History, 21st Century ; History, Medieval ; Hydrology ; Ice/analysis ; Mediterranean Region ; Models, Theoretical ; *Rain ; Soil/chemistry ; Spatio-Temporal Analysis ; Temperature ; Trees/anatomy & histology/growth & development ; Uncertainty ; United States
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2017-05-05
    Description: Volcanic eruptions have global climate impacts, but their effect on the hydrologic cycle is poorly understood. We use a modified version of superposed epoch analysis, an eruption year list collated from multiple datasets, and seasonal paleoclimate reconstructions (soil moisture, precipitation, geopotential heights, and temperature) to investigate volcanic forcing of spring and summer hydroclimate over Europe and the Mediterranean over the last millennium. In the western Mediterranean, wet conditions occur in the eruption year and the following 3 years. Conversely, northwestern Europe and the British Isles experience dry conditions in response to volcanic eruptions, with the largest moisture deficits in post-eruption years 2 and 3. The precipitation response occurs primarily in late spring and early summer (April-July), a pattern that strongly resembles the negative phase of the East Atlantic Pattern. Modulated by this mode of climate variability, eruptions force significant, widespread, and heterogeneous hydroclimate responses across Europe and the Mediterranean.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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