VOLCANO: EGU 2016. Recognizing and understanding the couplings between glacial cycles and the solid Earth

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EGU 2016. Recognizing and understanding the couplings between glacial cycles and the solid Earth
From: Luca Caricchi <Luca.Caricchi@xxxxxxxx>
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Dear colleagues,

Please consider submitting to this cross disciplinary session at EGU 2016. This session will be an occasion to discuss the links between surface dynamics, magmatism and volcanism.


CR6.2
Recognizing and understanding the couplings between glacial cycles and the solid Earth


SOLICITED SPEAKERS

Charles Langmuir (Harvard University), 

Tamsin Mather (University of Oxford) 

Jean-Arture Olive (Columbia University)


CONVENERS

Pietro Sternai (Department of Earth Sciences, University of Cambridge)

Luca Caricchi (Department of Earth Sciences, University of Geneva)

Sebastien Castelltort  (Department of Earth Sciences, University of Geneva)

Frédéric Herman (Institute of Earth Surface Dynamics, University of Lausanne)
Richard Katz (Department of Earth Sciences, University of Oxford)


ABSTRACT

Glacial cycles affect the processes through which water and rocks are redistributed across the Earth's surface, thereby linking the solid Earth and climate dynamics. The magma productivity is sensitive to pressure variations and therefore submarine and subaerial magmatic, volcanic and hydrothermal activity can be affected by glacial cycles and associated changes in continental ice load, sea level and surface denudation rates by erosion. In turn, emissions of solid aerosols and volatiles from the solid Earth modulate the climate system and therefore influence all processes involved with glacial-interglacial oscillations. Existing observational and modelling evidence about these linkages elicited controversy and further couplings amongst the cryosphere, atmosphere or geo-biosphere may still be unrecognized.
Exploration of these feedbacks is timely and promising in terms of societal and academic impact for it involves key factors related to climate change and tectonics, management of the territory and hazard assessments in fast-evolving and high-potential/risk environments such as glaciated, volcanic, tectonically active and hydrothermal terrains. Beyond this, recognizing and understanding the mutual forcing between climate, surface processes and the solid Earth dynamics, including the likely interactions with the human activity, is fundamental to apprehend the functioning of the Earth system as a whole and improve our living conditions within it.
With the aim of advancing the debate on the mass and energy fluxes across the Earth system, this session invites contributions pertaining to the recognition and understanding of the couplings between climate and the solid Earth dynamics through all kind of modelling and observations. Emphasis will be put on modern tools and interdisciplinary investigations, addressing the interactions between glacial processes, sea level change, sediment supply, landscape evolution and the volcanic, hydrothermal and tectonic activity on glacial/interglacial timescales. However, contributions about other linkages or more specific aspects of the Earth system evolution at all timescales relevant to glaciation are also welcome.





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