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Volcanic Forcing of Climate over the Past 1500 Years: An Improved Ice-Core-Based Index for Climate Models

TLDR
This paper extracted volcanic sulfate signals from each ice core record by applying a high-pass loess filter to the time series and examining peaks that exceed twice the 31-year running median absolute deviation.
Abstract
[1] Understanding natural causes of climate change is vital to evaluate the relative impacts of human pollution and land surface modification on climate. We have investigated one of the most important natural causes of climate change, volcanic eruptions, by using 54 ice core records from both the Arctic and Antarctica. Our recently collected suite of ice core data, more than double the number of cores ever used before, reduces errors inherent in reconstructions based on a single or small number of cores, which enables us to obtain much higher accuracy in both detection of events and quantification of the radiative effects. We extracted volcanic deposition signals from each ice core record by applying a high-pass loess filter to the time series and examining peaks that exceed twice the 31-year running median absolute deviation. We then studied the spatial pattern of volcanic sulfate deposition on Greenland and Antarctica and combined this knowledge with a new understanding of stratospheric transport of volcanic aerosols to produce a forcing data set as a function of month, latitude, and altitude for the past 1500 years. We estimated the uncertainties associated with the choice of volcanic signal extraction criteria, ice core sulfate deposition to stratospheric loading calibration factor, and the season for the eruptions without a recorded month. We forced an energy balance climate model with this new volcanic forcing data set, together with solar and anthropogenic forcing, to simulate the large-scale temperature response. The results agree well with instrumental observations for the past 150 years and with proxy records for the entire period. Through better characterization of the natural causes of climate change, this new data set will lead to improved prediction of anthropogenic impacts on climate. The new data set of stratospheric sulfate injections from volcanic eruptions for the past 1500 years, as a function of latitude, altitude, and month, is available for download in a format suitable for forcing general circulation models of the climate system.

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Dissertation

Weathering a medieval climate : gauging the impact of natural hazards on northern European society through archaeology and history, AD 1000-1550

TL;DR: In this paper, the authors investigate the occurrence of meteorological hazards in northern Europe and their impact on society during the medieval period (AD 1000-1550) and evaluate the duality of understanding in which disasters could be the result of spiritual or superstitious causes but could be mitigated through established and wellunderstood practical solutions.

Climate in Medieval time

TL;DR: In this article, the authors reviewed the evidence and concluded that although the High Medieval (1100 to 1200 A.D.) was warmer than subsequent centuries, it was not warmer than the late 20th century, and the warmest Medieval temperatures were not synchronous around the globe.

The Interactive Stratospheric Aerosol Model Intercomparison Project (ISA-MIP)

TL;DR: Timmreck et al. as discussed by the authors presented four co-ordinated inter-model experiments designed to investigate key processes which influence the formation and temporal development of stratospheric aerosol in different time periods of the observational record.

European and Mediterranean hydroclimate response to tropical volcanic forcing over the past millennium

TL;DR: This article used 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.
References
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Posted ContentDOI

The ENSO teleconnections to the Indian summer monsoon climate through the Last Millennium as simulated by the PMIP3

TL;DR: In this paper, the authors study the mean summer climate and its variability in India during the last Millennium (LM; CE 850-1849) with emphasis on the Medieval Warm Period (MWP) and Little Ice Age (LIA), after validation of the simulated current day climate and trends.
Dissertation

Effects of volcanic eruption source parameters on radiative forcing and sulfate deposition

TL;DR: In this paper, the role of individual and combined eruption source parameters were comprehensively investigated using interactive stratospheric aerosol models, perturbed parameter ensembles and statistical emulation, and the results revealed complex combined effects of the eruption parameters and illustrate the importance of explicitly simulating aerosol microphysical processes to determine aerosol mass, size and lifetime.

The influence of volcanic eruptions on growth of central European lowland trees in NE-Germany during the last Millennium

TL;DR: In this article, the effect of large volcanic eruptions on the growth rate of trees was investigated based on an unexplored comprehensive database with 1128 samples of long tree-ring width (TRW) chronologies of Quercus robur L. and Pinus sylvestris L, correlating with forest net primary production (NPP) originating from three different sites in eastern Germany (Greifswald, Eberswalde and Saxony).
Dissertation

Méthodes probabilistes d'extraction de signaux cachés appliquées à des problèmes de sciences de l'atmosphère

TL;DR: In this article, the authors discuss the problem of detecting and estimating the existence of signaux caches in the field of geophysics, and present a set of techniques to detect and estimate the presence of such caches.
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