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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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Multi-fingerprint detection and attribution analysis of greenhouse gas, greenhouse gas-plus-aerosol and solar forced climate change

TL;DR: In this article, a multi-fingerprint analysis is applied to the detection and attribution of anthropogenic climate change, and the results are subject to uncertainties associated with the forcing history, which is poorly known for the solar and aerosol forcing, and inevitable model errors in the computation of the response to the forcing.
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A model-tested North Atlantic Oscillation reconstruction for the past millennium

TL;DR: A yearly NAO reconstruction for the past millennium is presented, based on an initial selection of 48 annually resolved proxy records distributed around the Atlantic Ocean and built through an ensemble of multivariate regressions, and suggests that positive phases were dominant during the thirteenth and fourteenth centuries.
Journal ArticleDOI

Thermal expansion of sea water associated with global warming

TL;DR: In this article, the relationship between greenhouse-gas forcing, global mean temperature change and sea-level rise due to thermal expansion of the oceans is investigated using upwelling-diffusion and pure diffusion models.
MonographDOI

The Weather and Climate: Emergent Laws and Multifractal Cascades

TL;DR: In this article, the authors provide an overview of the nonclassical, multifractal statistics of the atmospheric dynamics and provide a new perspective for modeling and understanding the atmosphere, by generalizing the classical turbulence laws, emergent higher-level laws of atmospheric dynamics are obtained and are empirically validated over time-scales of seconds to decades and length scales of millimetres to the size of the planet.
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