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Inter-hemispheric temperature variability over the past millennium

Inter-hemispheric temperature variability over the past millennium

http://www.wikidata.org/entity/Q56001264

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Sensitivity of proxies on non-linear interactions in the climate system.Early onset of industrial-era warming across the oceans and continents.Western Pacific hydroclimate linked to global climate variability over the past two millennia.Extensive wildfires, climate change, and an abrupt state change in subalpine ribbon forests, Colorado.Southern Annular Mode drives multicentury wildfire activity in southern South America.Colonization of the Americas, ‘Little Ice Age’ climate, and bomb-produced carbon: Their role in defining the Anthropocene Robust global ocean cooling trend for the pre-industrial Common Era Teleconnection stationarity, variability and trends of the Southern Annular Mode (SAM) during the last millennium Did interaction between human pressure and Little Ice Age drive biological turnover in New Zealand?Changes in Holocene climate and the intensity of Southern Hemisphere Westerly Winds based on a high-resolution palynological record from sub-Antarctic South Georgia A Reconstruction of Subtropical Western North Pacific SST Variability Back to 1578, Based on a Porites Coral Sr/Ca Record from the Northern Ryukyus, Japan Was the Little Ice Age more or less El Niño-like than the Medieval Climate Anomaly? Evidence from hydrological and temperature proxy data Pseudo-proxy tests of the analogue method to reconstruct spatially resolved global temperature during the Common Era Uplift rates from a new high-density GPS network in Palmer Land indicate significant late Holocene ice loss in the southwestern Weddell Sea Establishing the skill of climate field reconstruction techniques for precipitation with pseudoproxy experiments Tambora 1815 as a test case for high impact volcanic eruptions: Earth system effects Challenges and perspectives for large-scale temperature reconstructions of the past two millennia Comparing proxy and model estimates of hydroclimate variability and change over the Common Era Low atmospheric CO2 levels during the Little Ice Age due to cooling-induced terrestrial uptake Southern Hemisphere rainfall variability over the past 200 years What have we learnt from palaeoclimate simulations?A study of quasi-millennial extratropical winter cyclone activity over the Southern Hemisphere

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Inter-hemispheric temperature variability over the past millennium

http://www.wikidata.org/entity/Q56001264

description

im März 2014 veröffentlichter wissenschaftlicher Artikel

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wetenschappelijk artikel

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наукова стаття, опублікована в березні 2014

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name

Inter-hemispheric temperature variability over the past millennium

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Inter-hemispheric temperature variability over the past millennium

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type

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Inter-hemispheric temperature variability over the past millennium

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Inter-hemispheric temperature variability over the past millennium

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Inter-hemispheric temperature variability over the past millennium

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Inter-hemispheric temperature variability over the past millennium

@nl

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Nature Climate Change

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Inter-hemispheric temperature variability over the past millennium

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Andrew D. Moy

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Braddock K. Linsley

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Christoph C. Raible

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David Frank

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David J. Karoly

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Fidel González-Rouco

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Heinz Wanner

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Jens Zinke

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Joëlle Gergis

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Julie Elbert

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GLOBAL SURFACE TEMPERATURE CHANGE

Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia

Climate sensitivity constrained by temperature reconstructions over the past seven centuries

Global surface temperatures over the past two millennia

High-resolution palaeoclimatic records for the last millennium: interpretation, integration and comparison with General Circulation Model control-run temperatures

Continental-scale temperature variability during the past two millennia

Ensemble reconstruction constraints on the global carbon cycle sensitivity to climate.

High-frequency Holocene glacier fluctuations in New Zealand differ from the northern signature.

Onset of deglacial warming in West Antarctica driven by local orbital forcing.

Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation.

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362-367

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scholarly article

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10.1038/NCLIMATE2174

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5

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4

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Ricardo Villalba

Tas D van Ommen

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2014-03-30T00:00:00Z

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261404049

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1041547048

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