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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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Journal ArticleDOI

Climate and environmental context of the Mongol invasion of Syria and defeat at ‘Ayn Jālūt (1258–1260 CE)

TL;DR: In this article, the authors revisited previous arguments in light of climate and environmental changes in the aftermath of one the largest volcanic forcings in the past 2500 years, the Samalas eruption ~1257 CE, and argued that colder and wetter climates in 1258 and 1259 CE, while complicating and slowing the campaign in certain areas in the Caucasus and Anatolia, also facilitated the assault on Syria between January and March 1260.
Journal ArticleDOI

Investigating dynamic mechanisms for synchronous variation of East Asian and Australian summer monsoons over the last millennium

TL;DR: In this paper, the authors investigated the past behavior of the East Asian summer monsoon (EASM) and the Australian summer cyclone (ASM), and their phase relationship during the last millennium, and their dynamic mechanisms.
Journal ArticleDOI

Variability and predictability of decadal mean temperature and precipitation over China in the CCSM4 last millennium simulation

TL;DR: In this paper, the authors examined the modes of variability arising from the slow-decadal and intradecadal components of decadal mean temperature and precipitation over China, in a 1000-year (850-1850 AD) experiment using the CCSM4 model.
Journal ArticleDOI

Multi-centennial reconstruction of drought events in South-Western Iran using tree rings of Mediterranean cypress (Cupressus sempervirens L.)

TL;DR: In this article, the authors developed a regional ring-width chronology from Cupressus sempervirens L.E. in the Zagros Mountains, western Iran and reconstructed precipitation variability for the semi-arid region during the period 1560-2015C.E., showing that precipitation and minimum temperatures are positively correlated with radial growth, whereas maximum temperatures reveal negative impacts.
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