Department of Geography, Environment and Geomatics

Slides:



Advertisements
Similar presentations
Convection, Global Winds, and Jet Stream
Advertisements

Drift of solar constants for the Earth (1), Venus (2) and Marc (3) due to increasing of Sun’s luminosity. Within an interval formed by carves 4 and 5 the.
The Last Glacial Maximum (LGM)
Climate models in (palaeo-) climatic research How can we use climate models as tools for hypothesis testing in (palaeo-) climatic research and how can.
The Holocene PCC Question 1) What does the Holocene ‘look like’ compared with glacial climate?
Composite of Sea Level – for last 600 k years. Note that SL was not always extremely low during glacial periods. From Rabineau et al, EPSL, 2006.
Factors That Affect Climate (Temp and Precipitation) Latitude, Elevation, Global Winds, Proximity to Water, Ocean Currents.
Lecture 30: Historical Climate Part V, ; Ch. 17, p
The Continuum of Hydroclimate Variability in Western North American during the Last Millennium AULT ET AL
Global Signatures of the “Little Ice Age” and “Medieval Climate Anomaly” and Plausible Dynamical Origins Michael E. Mann Penn State University with contributions.
Past and future impacts on the landscape and drainage of the Yorkshire Dales (Part 3) Dr Aidan Foley CLIMATE CHANGE.
Comparative analysis of climatic variability characteristics of the Svalbard archipelago and the North European region based on meteorological stations.
Slides for GGR 314, Global Warming Chapter 7: Heat and Water Stress, Terrestrial Species Extinctions Course taught by Danny Harvey Department of Geography.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Observed Oceans & Sea Level (from IPCC WG-I, Chapter 5) Observed Changes in Oceanic Climate and Sea Level Primary.
Ocean Currents What Are Currents? Current: a large stream of moving water that flows through the oceans. Currents carry water over very long distances.
Meeting of the CCl/OPACE2 Task Team on National Climate Monitoring Products How might NCMPs contribute in future IPCC reports ? Fatima Driouech TT on national.
Lecture 31: Historical Climate: Volcanoes and Sunspots
Validation of NARCCAP climate products for forest resource applications in the southeast United States. Willis Shem 1, Thomas Mote 2, Marshall Shepherd.
Reconstructing Climate History through Ice Core Proxies Natasha Paterson Econ 331 April 7 th, 2010.
What do glacial moraine chronologies really tell us about climate? Martin P. Kirkbride Geography School of the Environment School of the Environment University.
Lecture 32: Instrumental Observations Ch. 17. How has surface air temperature changed since 1800s? How have glaciers and sea level change in the past.
INTRODUCTION DATA SELECTED RESULTS HYDROLOGIC CYCLE FUTURE WORK REFERENCES Land Ice Ocean x1°, x3° Land T85,T42,T31 Atmosphere T85,T42,T x 2.8 Sea.
Orbital Forcing on Climate Finish Climates of Geologic Time Introduction to Orbital Factors Axial Tilt Axial Precession Changes in Earth’s eccentric orbit.
Evolution of Earth’s Greenhouse Effect Jeffrey T. Kiehl National Center for Atmospheric Research.
Comparing the Recession of Glaciers in the Torngat Mountains with Cirque Glaciers of the Canadian Rockies George Hill GE354 9 December 2015.
The Younger Dryas and Rapid Climate Change Bruno Tremblay McGill University
Impacts of Climate Change on Physical Systems Lesson Plan 4 – Day 2 PPT
CLIMATE GRAPHS. Temp In °C Precipitation In mm OTTAWA LABELS! CITY AT TOP TEMPERATURE ON LEFT IN °C PRECIPITATION ON RIGHT MONTHS ACROSS THE BOTTOM.
ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE, Borki Molo, Poland, 7-10 February 2007 Extreme Climatic and atmospheric.
Climate and Change How and why has climate changed in the past? Learning Objectives: To understand that climate has changed in the past through.
E R Thomas, E W Wolff and R Mulvaney
Lecture 20: Orbital Variations in Ice Sheets (Milankovitch Cycles)
Paleoclimate Models (Chapter 12).
Climates of Geologic Time
Oliver Elison Timm ATM 306 Fall 2016
climate notes page 3 Sun's Energy & Climate Change
Studies on Human-Environmental Dynamics in the Western HKH-region
Reconstructing Past Climates
Asian Monsoons and Climate
High-dimensional analysis of lymphoid CD4+ T cells identified distinct TFH cell subsets in HIV+ patients and HCs. High-dimensional analysis of lymphoid.
Holocene and Anthropocene
The Last Glacial Maximum (LGM)
Global Climate Change: Past and Future
The feasibility of Measuring Abyssal Ocean Temperature with Thermometers Embedded in the Trans-Ocean Communication Cables David Murphy, Bruce Howe, Roger.
Components of the yield trend.
by Joshua A.E. Fredrickson
Can I color yellow?. Can I color yellow?
How will precipitation change under global warming?
Fig. 1 Culturomic analyses study millions of books at once.
Prescribed forcings. Prescribed forcings. (Top) Volcanic forcing is indicated as global visible optical depth. (Middle) Solar forcing is obtained by scaling.
by A. Dutton, A. E. Carlson, A. J. Long, G. A. Milne, P. U. Clark, R
Slides for GGR 314, Global Warming Chapter 4: Climate Models and Projected Climatic Change Course taught by Danny Harvey Department of Geography University.
Evolution of the global surface temperature of the last 22 ka: the reconstructions of M13 (1) (blue) after 11.3 ka and by Shakun et al. Evolution of the.
Examples of AEGIS autonomous target selection.
Relative abundances of Propionibacterium species in different skin areas determined by 16S rRNA gene sequence analysis of 10 individuals. Relative abundances.
How Earth’s temperature is reflected on smaller geographic scales Gordon J. Aubrecht, II SOS-AAPT, Saturday 9 March 2013.
Fig. 1 Solar cycle and experimental setup.
Fig. 5 Time evolution results of the MIROC climate model simulation with freshwater hosing. Time evolution results of the MIROC climate model simulation.
Fig. 4 Latest Pleistocene climate proxies and moraine record from western Canada. Latest Pleistocene climate proxies and moraine record from western Canada.
Two REMS-like iterations demonstrating common patterns of rapid brightness changes of skin patterning. Two REMS-like iterations demonstrating common patterns.
Fig. 4 Energy balance analysis in STD systems.
by Andreas Keiling, Scott Thaller, John Wygant, and John Dombeck
Holocene climate change - facts and mysteries
Examples of AEGIS autonomous target selection.
Integrated mRNA and microRNA expression and DNA methylation clusters.
Relative impacts of mitigation, temperature, and precipitation on 21st-century megadrought risk in the American Southwest by Toby R. Ault, Justin S. Mankin,
Left upper lobe complete atelectasis 2 days after implantation of four endobronchial valves into the left upper lobe in a patient with emphysema. a) Chest.
Fig. 5 Simulation of the mechanical properties of the 3DGraphene foam in a wide temperature range down to the cryogenic region. Simulation of the mechanical.
Fig. 3 Global and basin-averaged sampling error compared with reconstructed temperature change. Global and basin-averaged sampling error compared with.
Fig. 2 Analysis of 1PCTCO2 experiments (JJA seasonal means).
Presentation transcript:

Department of Geography, Environment and Geomatics Holocene Climates K Gajewski Department of Geography, Environment and Geomatics University of Ottawa August 2016

Classical division of Holocene Climates in Europe

BP 2000 4000 6000 8000 10000 12000 14000 16000 From Hulme & Barrow. 1997. Climates of the British Isles. Routledge.

Global Temperature Curve This is the Holocene equivalent of the global temperature curve and the “Hockey Stick”

Average Global Temperatures for last 2ka (left) and 10ka (right) Estimated using different methods (top & bottom) Marcotte et al. 2013. Science

Average Global Temperatures Zonal means Marcotte et al. 2013. Science

Marcotte et al. 2013. Science

North American Mean temperature curve Milankovitch scale variability Millennial-scale regimes Comparison to European curve

Holocene Viau et al. 2006. J Geophysical Research 111, D09102,

Gajewski. 2008 Prog Phys Geogr 32:

Holocene climate sequence compared to full glacial

Millennial-scale climate variability: Europe Ruddiman book

Millennial-scale climate variability: off California Ruddiman book

Holocene Climates: Milankovitch scale

From Ruddiman text

Holocene Climates: Millennial scale

Glaciers

6k hydroclimate

6k compared to today Wanner et al. 2008. Quat Sci Rev 27:1791

Model output compared to Data

COHMAP. 1988. Science

COHMAP. 1988. Science

COHMAP. 1988. Science

Holocene regional time series

H. Wanner et al. / Quaternary Science Reviews 27 (2008) 1791–1828.

6 major cold periods in Holocene H. Wanner et al. / Quaternary Science Reviews 30 (2011) 3109-3123

6 major cold periods in Holocene Blue: cold Red: warm Grey: average Green: wet Brown: dry H. Wanner et al. / Quaternary Science Reviews 30 (2011) 3109-3123

Holocene climates causes

H. Wanner et al. / Quaternary Science Reviews 30 (2011) 3109-3123

Solar Activity, last 6000 years Wanner et al 2008

Solar Activity, last 3ka (upper); last 9ka (lower) Vieira et al. 2011. Astronomy & Astrophysics A6