'Ice volume' presentation slideshows

Reservoir volumes of water

498 views • 39 slides

d 18 O records Ice Volume

d 18 O records Ice Volume. Every 10-m change in sea level produces an ~0.1 ‰ change in d 18 O of benthic foraminifer The age of most prominent d 18 O minima Correspond with ages of most prominent reef recording sea level high stands Absolute sea levels estimates from reefs

501 views • 36 slides

2000 H 2 16 O

ice. 2000 H 2 16 O. 10 HD 16 O. 10 H 2 18 O. land. Latitude increasing. 1000 H 2 16 O. 3 HD 16 O. 3 H 2 18 O. 1000 H 2 16 O. 2000 H 2 16 O. 7 HD 16 O. 10 HD 16 O. 7 H 2 18 O. 10 H 2 18 O. ice. land. Latitude increasing. 500 H 2 16 O. 1000 H 2 16 O. 1 HD 16 O. 3 HD 16 O.

372 views • 31 slides

ABBE Level 3 Diploma in Domestic Green Deal Advice Annex D: Climate Change & Cutting Emissions

ABBE Level 3 Diploma in Domestic Green Deal Advice Annex D: Climate Change & Cutting Emissions. Presented by [Name]. Climate Change & Cutting Emissions. What is Climate Change?. Climate: is the average weather experienced over a long period of time Temperature Wind

433 views • 29 slides

What causes ice ages to occur about every ~100,000 years?

What causes ice ages to occur about every ~100,000 years? Evidence for ice ages over the last 2.5 Myr Changes in ice volume and sea level What causes ice ages? Astronomical control of solar radiation Milankovitch theory: insolation control of ice sheets

441 views • 29 slides

Cenozoic -The development of the Earth as we know it today

Cenozoic -The development of the Earth as we know it today. At only 66 million years long, the Cenozoic is only 1.4% of all geologic time. Age of Ocean Basins Is Well Constrained. The Circum-Pacific Orogenic Belt. Geological Provinces of the U.S. The North American Cordillera.

477 views • 22 slides

Coupling of the met.no ice model to MICOM

Coupling of the met.no ice model to MICOM. Jens Debernard Presented at LOM-meeting , 2 6 .-2 8 .1.200 5 , Miami. Coupling of the met.no ice model to MICOM and MIPOM. Jens Debernard Presented at LOM-meeting , 2 6 .-2 8 .1.200 5 , Miami. Overview. The sea ice model MI-IM

353 views • 21 slides

Sea ice modelling, forecasting, and validation activities at

Sea ice modelling, forecasting, and validation activities at Alfred Wegener Institute (AWI), Bremerhaven, Germany. Christian Haas. Modelling Thickness profiling SAR remote sensing. Operating stand-alone & coupled ice-ocean dynamic/thermodynamic models after Hibler & Lemke, Semtner

367 views • 20 slides

Ice-capped Summit

Ice-capped Summit.

234 views • 15 slides

Ice assimilation in Reanalysis UR025.4

Ice assimilation in Reanalysis UR025.4. Hao Zuo, Maria Valdivieso and Keith Haines ESSC, University of Reading. Summary of the Reanalysis.

336 views • 12 slides

Resolving Age Model Errors in U-series Dating of Stalagmites from Borneo

Resolving Age Model Errors in U-series Dating of Stalagmites from Borneo. Stacy Carolin Georgia Institute of Tech. April 28, 2011. Evidence for Abrupt Climate Change. Mapping Spectral Variability in Global Climate Project

258 views • 11 slides

THE NEED FOR DATA/MODEL INTEGRATION

THE NEED FOR DATA/MODEL INTEGRATION. Retrodiction/prediction is meaningless without meaningful error bars or probability distribution of model results Major challenge for climate change assessments

195 views • 11 slides

High Latitude Insolation and Climate Response

High Latitude Insolation and Climate Response. 23 April 2009 /// EAS 4803 Sean Miller. Introduction. Milankovitch: high latitude NH summer insolation drives glacial-interglacial cycles Changes in precession (19-23 kyr cycle), obliquity (41 kyrs), eccentricity (100 kyrs) are important

235 views • 11 slides

175 views • 9 slides

Objective This paper presents a statistical test of the orbital forcing of glacial terminations.

Objective This paper presents a statistical test of the orbital forcing of glacial terminations. Main Result Glacial periods terminated every two or third obliquity cycle at times of high obliquity. Obliquity pacing of the late Pleistocene glacial terminations P. Huybers, C. Wunsch.

209 views • 8 slides

????? ???

????? ???. Stage 7,11 ? insolation min Summer insolation min can lead termination MIS12.2 insolation?, largest ice volume of the past 600kyr 400kyr cycle, sea level variation max, insolation variation min.

260 views • 7 slides

Objective

Sea ice volume and age : Sensitivity to physical parameterizations and thickness resolution in the CICE sea ice model. Objective

162 views • 1 slides

Arctic and Antarctic sea ice variability during 1955-2001: A model study

219 views • 1 slides

ME Raymo & JX Mitrovica Nature 000 , 1 - 4 (2012) doi:10.1038/nature10891

84 views • 1 slides

RE Kopp et al. Nature 462 , 863-867 (2009) doi:10.1038/nature08686

Probability density plots of GSL and ice volume during the LIG. RE Kopp et al. Nature 462 , 863-867 (2009) doi:10.1038/nature08686.

154 views • 1 slides