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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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Book ChapterDOI

A Preliminary Evaluation of Atmospheric Pollution as a Cause of the Global Temperature Fluctuation of the Past Century

TL;DR: In this paper, two globally extensive forms of atmospheric pollution (carbon dioxide and particulate loading) are each considered from the viewpoint of long-term changes in their world-average abundance, and the relevance of these to the observed fluctuation of planetary average temperatures in the past century.
Journal ArticleDOI

A 1200-year multiproxy record of tree growth and summer temperature at the northern pine forest limit of Europe

TL;DR: In this paper, the authors combined nine tree growth proxies from four sites, from the west coast of Norway to the Kola Peninsula of NW Russia, providing a well replicated (> 100 annual measurements per year) mean index of tree growth over the last 1200 years that represents the growth of much of the northern pine timberline forests of northern Fennoscandia.
Journal ArticleDOI

Cold conditions in Antarctica during the Little Ice Age — Implications for abrupt climate change mechanisms

TL;DR: In this article, the authors present new data from the Ross Sea, Antarctica, that indicates surface temperatures were ~ 2°C colder during the LIA, with colder sea surface temperatures in the Southern Ocean and/or increased sea-ice extent, stronger katabatic winds, and decreased snow accumulation.
Journal ArticleDOI

Global monsoon precipitation responses to large volcanic eruptions

TL;DR: Using a 1500-year volcanic sensitivity simulation by the Community Earth System Model version 1.0, it is discovered that the GM precipitation in one hemisphere is enhanced significantly by the remote volcanic forcing occurring in the other hemisphere.
Journal ArticleDOI

Spatio-temporal variability in volcanic sulphate deposition over the past 2 kyr in snow pits and firn cores from Amundsenisen, Antarctica

TL;DR: In this paper, a comprehensive pre-site survey has been carried out on Amund- senisen, Dronning Maud Land, East Antarctica, in the past decade.
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