The oldest ice challenge: potential sites and new drilling technology Jérôme Chappellaz and the Ice&Lasers/Subglacior team Laboratoire de Glaciologie et.

Slides:



Advertisements
Similar presentations
Orbital-Scale Changes in Carbon Dioxide and Methane
Advertisements

CAVITY RING DOWN SPECTROSCOPY
C. VINCENT LGGE/CNRS DORIS DAYS 2-3 May 2000 Toulouse, France. DORIS campaigns at Dome Concordia, Antarctica in 1993 and C. Vincent 1, JJ. Valette.
Antarctic Ice Core Results to Date Amanda Solomon Geology 495 February 15, 2006.
GREENHOUSE GAS (CO 2, CH 4 ) AND CLIMATE EVOLUTION SINCE 650 KYRS DEDUCED FROM ANTARCTIC ICE CORES EPICA gas consortium J.-M. Barnola (1), U. Siegenthaler.
SEAT Traverse The Satellite Era Accumulation Traverse (SEAT) collected near-surface firn cores and Ultra High Frequency (UHF) Frequency Modulated.
Climate history near the divide between the Ross and Amundsen Seas by H. Conway, Ed Waddington, Tom Neumann, Ginny Catania, Erin Pettit, Felix Ng and Dave.
High variability of Greenland temperature over the past 4000 years estimated from trapped air in an ice core Takuro Kobashi National Institute of Polar.
1 Evaluation of radar measurements Hans-Peter Marshall, Boise State University and CRREL Snow Characterization Workshop, April 13-15, 2009.
Subglacial conditions of inland West Antarctica from US-ITASE deep radar reflection analysis WAIS Workshop September 30, 2005 Brian Welch, Bob Jacobel.
A Look into the Past Ice Cores By Felicia McDonald.
Dual Wavelength Isotope Ratio FS-CRDS Thinh Q. Bui California Institute of Technology ISMS 2014.
How do we know about the climate from thousands of years ago? PPT
- Past climate changes : general presentation and tools - Antarctic ice cores : from Byrd to Vostok - Byrd, old Dome C and Vostok - The last glacial-interglacial.
Circulation changes on Antarctic Peninsula from ice cores Liz Thomas 1, Gareth Marshall 1 Joe McConnell 2 & Paul Dennis 3 1.British Antarctic Survey 2.Desert.
The Role of Antarctica in Understanding the Earth’s Atmosphere and Climate Richard Brandt University of Washington and Paul Smith’s College Institut Polaire.
Glacial-Interglacial Variability Records of the Pleistocene Ice Ages
Fiber Optic Light Sources
Brian Siller, Ryan Matz, and Helen Waechter Recent Progress in Developing a Commercial Fiber-Loop Cavity Ring-Down System International Symposium on Molecular.
Fundamental of Fiber Optics. Optical Fiber Total Internal Reflection.
Dr. Ed Brook, Oregon State University US Ice Drilling Program
First high resolution analysis of the 5 3 band of nitrogen dioxide (NO 2 ) near 1.3 µm Didier Mondelain 1, Agnès Perrin 2, Samir Kassi 1 & Alain Campargue.
Greenhouse Gases and climate change. 2 Equilibrium: Energy/time in = Energy/time out Earth gains energy from the sun, by radiation Earth loses energy.
Proxy Records Ice Cores Dendrochronology Sediment records
Creating an Orbitally Tuned Chronology. Overview.
Evidence of Climate Change
Tree Rings
Climate Change and its Impact on Life. Making a distinction… Weather is….Climate is….
Antarctic Glaciology Julie Palais Program Manager NSF/Office of Polar Programs Antarctic Sciences Section.
Signals of climate change and the Southern Annular Mode in Antarctic stable isotope records David P. Schneider and Eric J. Steig Department of Earth and.
Infrared Spectroscopy using Quantum Cascade Lasers Peng Wang and Tom Tague Bruker Optics, Billerica, MA Laurent Diehl, Christian Pflügl and Federico.
Studying Paleoclimate to Reduce Climate Uncertainty
Absorption in bulk crystalline silicon and in the crystal surfaces Aleksandr Khalaidovski 1 Alexander Khalaidovski 1, Jessica Steinlechner 2, Roman Schnabel.
Energy in the Earth System. In the Earth system… Energy Flows Matter Cycles Life Webs Dr. Art’s Guide to the Planet Earth, Art Sussman, Ph.D.
A bipolar perspective on past climate change (and expectations for information from the Third Pole) Valérie Masson-Delmotte Laboratoire des Sciences du.
Absorption in bulk crystalline silicon and in the crystal surfaces Aleksandr Khalaidovski 1 Alexander Khalaidovski 1, Jessica Steinlechner 2, Roman Schnabel.
Inferred accumulation and thickness histories near the Ross/Amundsen divide, West Antarctica T. A. Neumann 1,2, H. Conway 2, S.F. Price 2, E. D. Waddington.
3.5 – Records of Past Climates Tree Rings, Fossils Coral Reefs, & Ice Cores.
Long-Term Changes in Global Sea Level Craig S. Fulthorpe University of Texas Institute for Geophysics John A. and Katherine G. Jackson School of Geosciences.
Class 19. Paleoceanography William Wilcock OCEAN/ESS 410.
Ice Cores, Stable Isotopes, and Paleoclimate
Extending the history of atmospheric CH 4 concentrations back to 650 kyr ago European Geosciences Union European Geosciences Union General Assembly 2005.
Reconstructing Climate History through Ice Core Proxies Natasha Paterson Econ 331 April 7 th, 2010.
Climate change and Antarctic glaciology Dr. Andrés Rivera Laboratorio de Glaciología y Cambio Climático Centro de Estudios Científicos (CECS), Valdivia.
Misure ottiche su atmosfere planetarie in laboratorio
Willie Soon. Introduction 1. The relationship between atmospheric CO2 and CH4 concentrations, temperature, and ice-sheet volume 2. Atmospheric CO2 radiative.
QualityTime-ESL1 Glaciology and Global Warming What is the connection? Marianne Raynaud Copyright 2015.
Marianne Raynaud Copyright 2005 QualityTime-ESL1 Glaciology and Global Warming What is the connection?
Antarctic ice cores : from Byrd to Vostok
I. Ventrillard-Courtillot, Th. Desbois, T. Foldes and D. Romanini
A new method for first-principles calibration
FREQUENCY-AGILE DIFFERENTIAL CAVITY RING-DOWN SPECTROSCOPY
Long-term temperature records in Antarctica: The view from ice cores David Schneider Department of Earth and Space Sciences University of Washington Seattle,
IceCube Dust Loggers Kurt Woschnagg, Ryan Bay Physics Department, UC Berkeley Instrumentation Session IceCube Collaboration Meeting Bartol, March 2004.
South Pole Glaciology with the IceCube telescope Kurt Woschnagg University of California, Berkeley for the IceCube Collaboration Open Science Conference,
Greenhouse Gas: Carbon Dioxide Thuan, Marko. Carbon Dioxide (CO 2 ) Colorless & odorless gas Ice Age (400 kyBCE) ppm Preindustrial (1700s)
Champaign, June 2015 Samir Kassi, Johannes Burkart Laboratoire Interdisciplinaire de Physique, Université Grenoble 1, UMR CNRS 5588, Grenoble F-38041,
Advanced LIGO UK 1 LIGO-G K OSEM Development UK Advanced LIGO project Stuart Aston University of Birmingham for the UK Advanced LIGO Team LSC.
Evidence of Climate Change page 18 We all have heard the term ‘global warming’ but is there any evidence that our climate is changing?
V.N. Litvinenko (SBU) C. Joshi, W. Mori (UCLA)
Five Special Days at Vostok and Concordia (Antarctica)
Snow Grain Size Workshop Grenoble, France, April 2013
T.F. Stocker, U. Siegenthaler, R. Spahni and the Bern and LGGE Teams
Stable Carbon Cycle–Climate Relationship During the Late Pleistocene
An accurate and complete empirical line list for water vapor
Reconstructed Temperature data from the Vostok Ice Core in Antarctica
Adapted from Ms. Pride Regents Biology SB1-03 or SB1-16
Lecture 21: Ice Core Records
National Institute for Environmental Studies, Tsukuba, Japan
Diode Laser Experiment
Presentation transcript:

The oldest ice challenge: potential sites and new drilling technology Jérôme Chappellaz and the Ice&Lasers/Subglacior team Laboratoire de Glaciologie et Géophysique de l’Environnement, Grenoble, France

Climate and CO 2 record covering the last 1.5 million years to evaluate climate sensitivity One shot with conventional ice core drilling operations : too risky and costly 40 kyr periodicity100 kyr periodicity The “Oldest Ice“ challenge Continental ice volume from δ18O stack of benthic foraminifera Lisiecki & Raymo, 2005

Where to find such old ice in Antarctica? Pattyn, 2010

IPICS Oldest Ice workshop, 6-7 October 2012, France

Best guess: 2500-m thickness max. Smooth bedrock Close to current domes or saddles Simple ice flow regime

Where to find such old ice in Antarctica? Current requirements : High-resolution 3D radar reconstructions 3D ice-flow modelling Shallow-intermediate drilling and snow radar for accumulation rate steadiness Rapid access drilling Van Liefferinge and Pattyn, 2013 Basal temperature

VANISH / EXPLORE 2011/2012 traverse L. Arnaud, O. Alemany, J. Chappellaz, E. Lefebvre, M. Lemeur, G. Teste (LGGE), M. Bes de Bec (IPG Strasboug), M. Schneebeli (SLF, Davos) A. Vende, D. Colin, A. Leluc (IPEV) M. Fily (LGGE métropole) Vostok Concordia Point Barnola

8 S2 DC S1B Example of isochrones between Concordia and S1B Lemeur et al., à soumettre Mean accumulation over the last 300 years: DC : 2.5 cm H 2 O/yr Point Barnola : 2.3 cm S2 : 2.1 cm S3 : 1.6 cm S4 : 1.6 cm S3 S4 Point Barnola

Bedrock: Texas radar

Run in a single field season down to bedrock Check statigraphic continuity within the ice sheet Real-time in-situ measurement of water isotopes (climate) and greenhouse gases (CH 4, maybe more) Innovative approach : in-situ probe with embedded OF-CEAS to qualify potential sites Design : O. Alemany

DFB diode laser PD signal PZ T LD translation Variable attenuator PD ref current ramp O.F. Advantages: Simple optical layout with few components Small cavity (~ 10 cc), small sample size Built-in frequency scale calibration (determined by cavity) High light transmission Switch between CEAS and CRDS modes for absorption calibration Optical self-locking and narrowing of the laser frequency to the very narrow cavity transmission peaks Optical Feedback Cavity Enhanced Absorption Spectroscopy (OF-CEAS) Morville et al., Patent 2005

Semi-continuous CH 4 profile from NEEM using OF-CEAS technology and CFA Chappellaz et al., 2013

How to handle the drilling chips ?

A 3500 hose pipe in one piece Certified to -40°C (to be tested up to -50°C) One winch for the hose One winch for the main cable (power, data) Winch and hose

50 mm external diameter!!! Laser Lens 1 PD ref Attenuator Cavity PD sig Wedge Lens 2 50 mm external diameter!!! OF-CEAS probe instrument R. Grilli, unpublished

OF-CEAS probe instrument housing Spectro housing First insulation Gas exit/vacuum Fluid channel x3 Second insulation

Conclusions The Oldest Ice challenge requires a lot of parallel tasks to reach success : snow radar, bedrock radar, modelling, rapid access drilling We hope that the Subglacior probe will be able to qualify sites and to provide the primary information (climate, GHG), notably in the vicinity of Concordia The LIA Vostok can frame the technological collaboration between the LGGE and Mining Institute, and future prospects south of Vostok

Thanks !