Looking Back in Time Through Marine Ecosystem Space: A Predators Perspective on Climate and Change in the Western Antarctic Peninsula William R. Fraser.

Slides:



Advertisements
Similar presentations
Individual-based Models Three Examples
Advertisements

Plant Sector Workshop March 21, MIT – Progress on the Science of Weather and Climate ExtremesMarch 29, 2012 Motivation –Billion-dollar Disasters.
Western Antarctic Peninsula Glacial History and its Importance to Understanding Contemporary Marine Ecosystem Structure and Function William R. Fraser.
1 Jean Pennycook penguinscience.com Introduction to Adelie Penguins.
Global Warming, Antarctica and Penguins Adelie Penguins Pictures Emperor Penguins Conservation Maps Movie Exit.
Global Warming Affects Polar Animals By Brandon Chalk J.T. Nelson Jacob Steinbach By Brandon Chalk J.T. Nelson Jacob Steinbach.
Space-Time Scales in Oceanography and the LTER Sampling Strategy Raymond C. Smith Palmer LTER Site Review 1994.
Bess Ward Department of Geosciences Princeton University.
US GLOBEC Before and After
Jean Pennycook Antarctic Penguins Cope with Climate Change.
Jean Pennycook Penguin Predation and Competition.
Climatology and Variability of Mesoscale Cyclones in the Western Antarctic Peninsula Region Dan Lubin Scripps Institution of Oceanography Rob Wittenmyer.
1 Climate change and the cryosphere. 2 Outline Background, climatology & variability Role of snow in the global climate system Contemporary observations.
The influence of extra-tropical, atmospheric zonal wave three on the regional variation of Antarctic sea ice Marilyn Raphael UCLA Department of Geography.
“Meso-Marine Ecosystems”: Management Units for the North Pacific? W. Sydeman 1, S. Batten 2, D. Hyrenbach 1, M. Henry 1, C. Rintoul 1, D. Welch 3, K. Morgan.
Sea Ice Presented by: Dorothy Gurgacz.
1.Sea Ice and Snow cover -Evidences As they melt mountain glaciers leave behind the an altered landscape with low albedo. a. shrinking glacial are around.
Global Warming Effects on Adelie Penguins
Outline Background, climatology & variability Role of snow in the global climate system Indicators of climate change Future projections & implications.
Comparative aspects of the biology of the Arctic and Antarctic marine ecosystems.
Ocean Response to Global Warming William Curry Woods Hole Oceanographic Institution Wallace Stegner Center March 3, 2006.
Penguins: The Odd Bird Out 5 th Grade. Penguins! Class – Aves Family –Spheniscidae – Penguins are the only animals in the Spheniscidae family Species.
Interannual and Regional Variability of Southern Ocean Snow on Sea Ice Thorsten Markus and Donald J. Cavalieri Goal: To investigate the regional and interannual.
Geographic Processes in Polar Lands Atmospheric Processes Biotic Processes Geomorphic Processes Hydrologic Processes © Karen Devine 2010.
Palmer LTER Palmer LTER Site Review Introduction to the Palmer LTER Ray Smith, UCSB Palmer LTER PI’s Ray Smith, UCSB Karen Baker, UCSD Bill Fraser, Montana.
December 2002 Section 2 Past Changes in Climate. Global surface temperatures are rising Relative to average temperature.
Antarctica. Strode’s College Antarctica AS Environmental Science The world’s largest wilderness ecosystem Antarctica is very large 98% is covered by ice.
The leopard seal as a barometer of climate warming Presentation by Tracey Rogers With support from: The tall poppy is a metaphor.
Introduction to Antarctica and the Antarctic, Why is it so cold? Jean Pennycook penguinscience.com.
Looking Back in Time Through Marine Ecosystem Space: Top Predator Perspectives on Climate and Change in the Western Antarctic Peninsula William R. Fraser.
Alaska Science Center International Polar Year Activities and the Alaska Science Center.
SNC2D Brennan Climate Change. Paleoclimate record Ice samples Sediment cores Pollen records Peat Bogs Fossil records Proxies –Use data that represents.
Leopards of the Sea. Species  Their species is the Hydrurga Leptonyx.  The Leopard Seals order is a Carnivora their suborder is the Pinnepedia.  The.
PALMER, ANTARCTICA Long Term Ecological Research PAL Summer Cruise LMG Jan, 2004.
Huw Griffiths Understanding global climate change through new breakthroughs in polar research
Polar Prediction The Scientific Challenges - Antarctica John Turner British Antarctic Survey Cambridge, UK.
ANALISIS OF OBSERVED GLOBAL AND REGIONAL CLIMATE CHANGE Konstantin Vinnikov Department Atmospheric and Oceanic Science College of Computer, Mathematical.
Module 4 Changes in Climate. Global Warming? Climate change –The pattern(s) of variation in climate (temperature, precipitation) over various periods.
Now You SEA Ice, Now You Don’t
Melting glaciers help fuel productivity hotspots around Antarctica
Components of the Global Climate Change Process IPCC AR4.
Introduction to Weddell Seals McMurdo Sound, Antarctica By Jean Pennycook.
Douglas G. Martinson Lamont-Doherty Earth Observatory Columbia University 12 years of Palmer LTER: Physical Oceanography, Spatiotemporal.
US-AMLR Datasets Pinniped research Mike Goebel. CCAMLR Ecosystem Monitoring Program “detect and record significant changes in critical components of the.
Lecture 32: Instrumental Observations Ch. 17. How has surface air temperature changed since 1800s? How have glaciers and sea level change in the past.
Western Antarctica & Antarctic Ice Shelves Eric Leibensperger EPS 131.
Welcome! The Topic For Today Is…. Your Topic Adelie Penguins Food Web Risk Status Climate Change Making Connections Bonus Question:
Typical Distributions of Water Characteristics in the Oceans.
Antarctic Marine Protected Areas: a strategy for robust, science-based conservation George M. Watters Southwest Fisheries Science Center Thanks to: A.
1 Melting glaciers help fuel productivity hotspots around Antarctica Kevin R. Arrigo Gert van Dijken Stanford University Melting glaciers help fuel productivity.
Southern Ocean GLOBEC Program Eileen E. Hofmann Third GLOBEC PRSW Boulder, February 2009.
Water Mass Distribution OEAS 604 Lecture Outline 1)Thermohaline Circulation 2)Spreading pathways in ocean basins 3)T-S diagrams 4)Mixing on T-S diagrams.
Interannual Time Scales: ENSO Decadal Time Scales: Basin Wide Variability (e.g. Pacific Decadal Oscillation, North Atlantic Oscillation) Longer Time Scales:
CE 401 Climate Change Science and Engineering evolution of climate change since the industrial revolution 9 February 2012
1 Assessing Vulnerability of Living Marine Resources in a Changing Climate Roger Griffis Climate Change Coordinator, NOAA Fisheries Service.
OEAS 604: Final Exam Tuesday, 8 December 8:30 – 11:30 pm Room 3200, Research Innovation Building I Exam is cumulative Questions similar to quizzes with.
Coastal Oceanography Outline Global coastal ocean Dynamics Western boundary current systems Eastern boundary current systems Polar ocean boundaries Semi-enclosed.
Recent decades of climate and cryospheric change on the Antarctic Peninsula David G. Vaughan British Antarctic Survey.
Antarctic Food Web. Krill in Antarctic Food Webs Phytoplankton.
The Large Ocean Basins Indian Ocean 2. Arctic Ocean 3. Pacific Ocean 4. Southern Ocean 5. Atlantic Ocean.
Biological structure of Fisheries Resources In Space And Time.
PALMER, ANTARCTICA Long Term Ecological Research Annual Meeting Big Trout Ranch, MT August, 2003.
Global Warming History & Geography
AT 25 DE MAYO / KING GEORGE ISLAND DISCUSSION and CONCLUSIONS
Climate induced shifts in the phytoplankton community biomass
The Process of Science Josh Kohut
Physical forcing of a Western Antarctic Peninsula ecosystem: observations from a coastal ocean observing network at Palmer Station. Travis Miles1, Oscar.
Hurricanes and Hatchlings Don’t Mix
A decadal analysis of phytoplankton community composition in the melting West Antarctic Peninsula Oscar Schofield1 Grace Saba1,
Shift in the Antarctic Peninsula Food Web in Response to Regional Warming Oscar Schofield1, Mark Moline2, Herve Claustre3, Thomas Frazer4, Maria Vernet5.
Presentation transcript:

Looking Back in Time Through Marine Ecosystem Space: A Predators Perspective on Climate and Change in the Western Antarctic Peninsula William R. Fraser Polar Oceans Research Group Sheridan, Montana

Outline PAL Space/Time Regional SettingPAL Space/Time Regional Setting Climate Change OverviewClimate Change Overview Geology and Adélie Penguin Population DistributionsGeology and Adélie Penguin Population Distributions Climate Change Effects and Ecosystem ResponseClimate Change Effects and Ecosystem Response Conclusions and Future DirectionsConclusions and Future Directions

The Western Antarctic Peninsula (WAP) The WAP is the only location in Antarctica where the Antarctic Circumpolar Current (ACC) is directly adjacent to the shelf break. The ACC is Antarcticas warmest water. Ross Sea gyre Weddell gyre D. Martinson

PAL Spatial Operational Area and Data Time Series WAP = 220,000 km 2 Anvers Isl Anvers Isl. Palmer Station LTER Grid = 120,000 km 2 LTER Research Top Predator Studies E. Erdman, SO-GLOBEC database

Sampling capitalizes on a nested grid approach by using research platforms that annually operate over large and small scales during the October-March period

Climate Change…surface air and ocean temperatures Meredith & King, 2005 Martinson et al., In Press Coldest Water in January Water Column D. Martinson ˚ C/year Significant at 0.05 ~5.4x global average British Antarctic Survey

Climate Change…sea and glacial ice 83% of glaciers are in retreat Major loss of perennial sea ice cover Duration of the sea ice season has decreased by 85 days during the last 25 years Cook et al Sea Ice Cover S. Stammerjohn Perennial Ice S. Stammerjohn

Breeding Distribution of Adélie Penguin Populations in the Western Antarctic Peninsula Region Photo by H. Geisz, PAL LTER Fraser & Trivelpiece 1996 Hypothesis: The breeding distribution of Adélie penguins is limited to regions where prey availability is predictable over ecological time scales (decades to centuries) Rationale? Adélie penguins are flightless and incapable of foraging at night, which greatly limits the range over which they can search for prey in summer when feeding chicks

Hypothesis Testing: Technological Advances Mapping the oceans floor Miniaturizing satellite-linked instruments to track Adélie penguins at sea

Hypothesis Testing: Geology and Bathymetry The Palmer Deep off Anvers Island ANVERS Is E. Domack

Hypothesis Testing: Bathymetry and Adélie Penguin Foraging Ecology Anvers Island E. Domack

Anvers Is Bathymetry and Adélie Penguin Foraging Ecology: Causal Factors and Larger Scales Primary Production Contour of regions of low pCO 2 (highlighted in red), based on WAP January cruises D. Karl, unpublished Adelaide Is

Anvers Is Bathymetry and Adélie Penguin Foraging Ecology: Causal Factors and Larger Scales Regions of Polynya Formation WINTER 2001 and 2002.

Anvers Is Bathymetry and Adélie Penguin Foraging Ecology: Causal Factors and Larger Scales Importance to Other Predators (Crabeater Seals)

Climate Change Effects and Ecosystem Response 0.107˚ C/year Significant at 0.05 ~5.4x global average Perennial Ice

One of the mechanisms by which climate change induces change in ecosystem structure is by disrupting the evolved life history strategies of component species. Rhodes & Odum 1996 New Paradigm…Climate Migration Key Physical Variables are Changing Along a North to South Gradient Sub-Antarctic Life History Groups are Replacing Antarctic Life History Groups WAP Ecosystem Structure is Changing in Fundamental and Possibly Unprecedented Ways

Key Implication: Ecological changes are due to region specific changes in sea ice as a temperature isotherm migrates north to south Sea ice data courtesy of E. Chapman How is Climate Migration Operating?

Net Average Effects?...Annual Winter Sea Ice no Longer Covers Approximately 50% of the WAP mmmmmm Adelaide Isl. Renaud Isl. Anvers Isl. Palmer Sta. WAP Ecosystem Structure is Changing in Fundamental and Possibly Unprecedented Ways Sub-Antarctic Life History Groups are Replacing Antarctic Life History Groups

North to South Changes in Primary Production (climatology, ) Relative to Penguin Populations M. Vernet

ADELAIDE IS ANVERS IS Statistically significant north to south differences in recruitment frequency and population size structure North to South Changes in Antarctic Krill (Euphausia superba) Populations Atkinson et al A two-fold decrease/decade in krill density

North to South Changes in Antarctic silverfish (Pleuragramma antarctica) Populations ANVERS IS ADELAIDE IS

North to South Changes in Populations of the Lanternfish (Electrona antarctica) ADELAIDE IS Silverfish ANVERS IS Lanternfish

North to South Changes in Stable Isotope Signatures (krill dominated diets at Palmer vs silverfish dominated diets at Avian Is PALMER STA AVIAN IS

North to South Penguin population changes Habitat optimum hypothesis: Too much ice is as detrimental to Adélie penguins as too little ice. Fraser & Trivelpiece 1996, AGU ANVERS IS ADELAIDE IS On Anvers Island chinstrap and gentoo penguins, two sub-Antarctic species, are replacing Adélie penguins

Conclusions and Future Directions Climate migration is having an impact on a range of ecosystem properties, from key physical variables to food web structureClimate migration is having an impact on a range of ecosystem properties, from key physical variables to food web structure Trends indicate that the ice- dependent life history group that once populated the northern sectors of the WAP are being replaced by an ice- intolerant life history group over ecological time scales.Trends indicate that the ice- dependent life history group that once populated the northern sectors of the WAP are being replaced by an ice- intolerant life history group over ecological time scales. Glacially incised, cross shelf canyons are focal points of physical and biological processes affecting WAP ecosystemsGlacially incised, cross shelf canyons are focal points of physical and biological processes affecting WAP ecosystems Future directions…Future directions… Antarctic Circumpolar Current

Future Directions Looking back in time through marine ecosystem space… … by emphasizing changes in sampling strategies that will capture climate migration and provide a more mechanistic understanding of marine ecosystem response