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The Reality and Challenge of Climate Change

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Title: The Reality and Challenge of Climate Change


1
The Reality and Challengeof Climate Change
  • Climate change and variability are continuous
    and inevitable
  • Past range of variability is greater than the
    range observed in the instrumental record
  • Climate change has major effects on all natural
    and human systems

2
The National LevelClimate Change Science
Program (CCSP)
  • CCSP Strategic Goals
  • Climate variability and change
  • Carbon cycle
  • Ecosystems
  • Water cycle
  • Land use, land cover change
  • USGS is providing the groundtruth for
  • Long-term monitoring
  • Process level research
  • Geological record of climate change cycles
  • Distinguishing natural from anthropogenic
  • Ecological and physical impacts

3
Our Niches (where we have both depth and
breadth)
  • Other agencies increasingly look to USGS to be
    the unbiased source of good science
  • We look at things at all scalesand can connect
    them
  • We can integrate our monitoring, and can do
    targeted priority integration, pulling different
    sources of info together from different
    fields/different scales
  • We can extend our understanding of a process to
    larger or more local scales
  • We have fertile ground for collaboration with
    other disciplines

4
What do we need to do to be a significant
contributor/participant?
  • Play to our strengths
  • Monitoring
  • Process research
  • Many processes we study have relevance to climate
    change e.g. volcanos are a major perturbation
  • Climate history research
  • Simulating future change
  • Scenario-building / Consequences
  • Dynamics
  • Climate change leads to consequences

5
Overriding ThemesIntegration Translation
Data Standards
  • Can look into the past paleoclimate,
    paleoecology
  • Can look underground
  • Can look at carbon kinetics and processes by
    which landscapes evolve (at multiple timescales)
  • Carbon sequestration
  • Hydrates

6
Future PathsThe Brass Rings
  • Data Integration
  • Many disparate datasets
  • Decision Support
  • Scenarios
  • Our framework
  • Consequences
  • Climate history to inform scenarios
  • Possible ranges of climate variability, change
    and earth system response
  • Probabilities for various scenarios/risk
    statements

7
Project Foci
  • Sea level rise impacts and consequences
  • Biogeochemistry in soils whats where and where
    is it going
  • Carbonate systems, ancient and modern (e.g.
    corals)
  • Highlatitude change and consequences
  • Dryland systems
  • Connections to water, weathering, sediment cycle
  • Methane systems

8
(No Transcript)
9
Climate - past, present and future
10
What do we know with a high degree of confidence?
11
Past 20,000 Years
Vikings to Greenland
Vikings Leave
warmer
  • Small changes in temperature can lead to
    significant local human impacts
  • Big temperature changes have occurred rapidly
    that could have significant global human impacts

YD
10C (18F) increase in several decades at end of
Younger Dryas interval (YD)
Temperature in Central Greenland (C)
colder
Alley, 2000
Thousands of years before present
12
Past 100 Years Alaska
  • Average U.S. temperature increased 1F over 100
    years
  • Alaska has warmed 4F since 1950
  • Higher latitudes more sensitive to climate
    change
  • Changes in the ice cover of the
  • globe are of great interest to
  • American policymakers because of the magnitude of
    change of
  • Permafrost degradation
  • Melting of sea ice
  • Rates of coastal erosion

13
Past 100 Years Lower 48
  • Average U.S. temperature increased 1F (0.6C).
  • Warming was greatest at higher latitudes.
  • Precipitation has increased

20th Century Trends in Temperature
14
Increased Melting of Greenland Ice Sheet
Contributing to Sea-level Rise
Red shows seasonal surface melt extent for two
extreme years. Surface melt increased 16
between 1992 and 2002.
K. Steffen
15
As the Earth Warms, Sea-Level Rises
Two factors increased meltwater and thermal
expansion
Since the last glacial maximum (? 20,000 b.p.)
  • sea level has risen 120 m (400 ft)
  • past 100 years - 1.0 - 2.0mm/yr

Low lying coastal areas are proneto more
frequent inundation. As sea level rises,
flooding, erosion,and salt water intrusion will
accelerate.
16
Future Science Challenges
  • Rates of change
  • Linkages among carbon, climate and terrestrial
    ecosystems
  • Climate and water resources (availability, floods
    and drought)
  • Thresholds and feedbacks poorly understood.

17
Response to Climate Change
Projected Permafrost Degradation by 2100
18
As Climate Warms The Hydrologic Cycle Intensifies
20th century
21st century
(Milly, Dunne and Vecchia, Nature, 2005)
19
Linking Global to Regional Models
Source http//www-lsce.cea.fr/pmip2/ Kaplan et
al. (2003).
20
USGS Role in Global Change Science
  • Managers and Policymakers need
  • Predictions and forecasts of
  • impacts from future climate change
  • USGS provides
  • The physical and biological
  • research and observation
  • information that make the
  • forecasts possible, and make
  • existing forecasts more
  • comprehensive and accurate.

21
Climate Change Science is Relevant to all DOI
Bureaus
Major drivers
Direct effects
Coastal erosion and wetland loss
Changes in rainfall
Permafrost decline and sea ice retreat
Accelerated sea level rise
Higher evaporation rates Longer growing seasons
Changes in seasonal events Changes in timing and
volume of runoff Declining summer soil
moisture Loss of glaciers
Higher temperatures
More intense storms
Atmospheric C enrichment
Changes to landscape
Societal Impacts
Declines in surface water availability Offshore
facilities more vulnerable Loss of coastal storm
surge buffers More intense, more frequent
fires Emerging diseases
Shifts or loss of native plants and
animals Effects on natural area tourism Loss of
fresh water lens in coastal areas Inundation of
small islands
22
The National LevelClimate Change Science
Program (CCSP)
  • CCSP agencies are preparing 21 synthesis and
    assessment reports aimed at assessing climate
    change and its impacts
  • DOI is contributing to 13 of the 21 studies and
    has the primary lead on
  • Climate Change in the Arctic
  • Abrupt Changes in Global Climate
  • Ecosystem Thresholds
  • USGS has been involved in global change science
    for over two decades

23
USGS Global Change Programs Widely Distributed
Science
Science Disciplines
National Programs
Green Programs- formally tied to CCSP (26.4
Million in FY07)
24
USGS Global Change Research The World
Perspective
Global Change Science at USGS A World
Perspective ATMOSPHERIC COMPOSITION 1. Global
Dust Virginia Garrison CLIMATE VARIABILITY 2.
Atlas of Glaciers of the World Ritchie
Williams 3. Climate Change, Land Use, and
Environmental Sensitivity Phase 2 (CLUES2) Bob
Thompson 4. Cryospheric Studies (borehole
paleothermometry) Gary Clow 5. WAIS Divide
Drilling Program National Ice Core Laboratory
(cooperative with NSF) Joan Fitzpatrick 6.
Eolian History of North America Daniel Muhs 7.
Global Warming Analysis (PRISM 3D) Harry
Dowsett ECOSYSTEMS 8. Resilience of Corals to
Climate Change and Their Use in Designing Marine
Reserves - Charles Birkeland 9. Functional
Linkages Between Climate, Anthropogenic Factors
and the Epipelagic Community of the North Pacific
Ocean - Jennifer Nielsen
25
USGS Global Change Research The U.S.
Perspective
26
Global Change Science Visualization Tool
27
USGS Global Change Research The U.S.
Perspective
  • CLIMATE VARIABILITY
  • 1. Abrupt Climate Change Thomas Cronin
  • 2. Effects of climatic variability and land use
    on American Drylands Richard Reynolds
  • 3. Eolian History of North America Daniel Muhs
  • 4. Exploring Future Flora, Environments, and
    Climates Through Simulations (EFFECTS) Sarah
    Shafer
  • 5. Gulf of Mexico Climate and Environmental
    History Richard Poore
  • 6. Holocene Climate of the Pacific Coasts - John
    Barron
  • 7. Landscape Response to Quaternary Climate
    Change Milan Pavich
  • 8. Paleohydrologic History of the Mojave Desert
    Region Marith Reheis
  • 9. Western Lake/Catchment Systems (LACS) Joe
    Rosenbaum, Bob Thompson
  • 10. Regional and Global Climate Models Steve
    Hostetler
  • CARBON CYCLE
  • 11. Carbon Cycling in the Gulf Coast of Maine
  • Thomas Huntington
  • 12. Vegetation and Hydrogeomorphic Relations
    Cliff Hupp
  • 13. Sediment-Water Chemistry in Large River
    Systems
  • Bob Stallard
  • 14. Carbon Sequestration and Biogeochemical
    Cycling in Temperate
  • Forests - Steven Perakis
  • ECOSYSTEMS
  • 17. Everglades Ecosystem History Lynn Wingard
  • 18. Northern Gulf of Mexico Restoration Project
    Debra Willard
  • 19. Effects of Climate Change on Population
    Trajectories, Tropic Interactions, and Ecosystems
    - Thomas Martin
  • 20. Forest Dieback and Carbon Relations of
    Coastal Forests of the Southeast Under Changing
    Climate - Thomas Doyle
  • 21. Interactions of Climate Change and Other
    Environmental Factors with Invasive Plant
    Infestation in the Arid West - Jonathan Friedman
  • 22. Predicting the Persistence of Coastal
    Wetlands to Global Change Effects - Glenn
    Guntenspergen
  • 23. Response of Western Mountain Ecosystems to
    Climatic Variability and Change - Nathan
    Stephenson
  • 24. Sensitivity of Pacific Island Tropical
    Montane Cloud Forests to Climate Change David
    Foote
  • 25. Spatial and Temporal Effects of Climate
    Change on Great Lakes Wetlands - Douglas Wilcox
  • HUMAN CONTRIBUTIONS
  • 26. Navajo Nation Studies Margaret Hiza
    Redsteer
  • LAND USE
  • 27. Landcover Applications, Landscape Dynamics,
    and Global Change Larry Tieszen
  • 28. Land Cover Trends Tom Loveland, William
    Acevedo
  • 29. National Satellite Land Remote Sensing Data
    Archive (NSLRSDA) Tom Holm
  • 20. Forest Dieback and Carbon Relations of
    Coastal Forests of the Southeast Under Changing
    Climate - Thomas Doyle
  • WATER CYCLE
  • 30. Benchmark Glaciers Ed Josbergerand, Bill
    Bidlake, Rod March

28
USGS Global Change Research -- Alaska
CLIMATE VARIABILITY 1. Cryospheric Studies
(permafrost monitoring) Gary Clow 2. Ecosystem
and Climate History of Alaska Thomas Ager 3.
Eolian History of North America Daniel Muhs 4.
Paleoclimate record from deep core at Fort Yukon,
Alaska Thomas Ager CARBON CYCLE 5. Fate of
Carbon in Alaskan Landscapes Jennifer Harden 6.
Characterization of Biotic and Biogeochemical
Interactions at Environmental Interfaces Rob
Striegl, Kim Wickland ECOSYSTEMS 7. Polar Bear
Survival in a Vanishing Sea Ice Environment -
Steve Amstrup LAND USE 8. Landcover Applications,
Landscape Dynamics, and Global Change Larry
Tieszen 9. Land Cover Trends Tom Loveland,
William Acevedo 10. National Satellite Land
Remote Sensing Data Archive (NSLRSDA) Tom
Holm WATER CYCLE 11. Benchmark Glaciers Ed
Josbergerand, Bill Bidlake, Rod March 12. Trends
in Streamflow Characteristics in Alaska Glenn
Hodgkins
29
The Global LevelDOI Role in Global Earth
Observation System of Systems (GEOSS)
  • Partner with global community
  • Develop robust global on the ground monitoring
    networks
  • Integrate terrestrial observations with satellite
    observations
  • Support broad open dataand information sharing
    goals

30
CEOS Committee on Earth Observation Satellites
  • DOI chairs CEOS in 2007
  • 30 Nations and 20 participating organizations
  • Both satellite and on the ground data are
    required to better monitor, characterize, and
    predict changes in the Earth system.

31
The Way Forward

32
Backup Slides
  • Chesapeake LIDAR baseline and 2100 projection
  • Carbon Cycle
  • Emissions
  • Permafrost
  • Wildfires
  • Streamflow
  • Ecosystem Response
  • Land Resources

33
Global Change Sea Level Rise Blackwater
National Wildlife Refuge Area, 2002
Open water Intertidal marsh
High marsh
34
Global Change Sea Level Rise IPCC projection,
average case scenario, 2100 (6.2 mm/yr rise)
Open water Intertidal marsh
High marsh
35
The Natural Carbon Cycleand Anthropogenic Carbon
Dioxide
36
Increased Methane Emissions With Permafrost Thaw
  • Collapse wetlands can form when permafrost
    melts.
  • These wetlands release 15 to 30 times more
    methane to the atmosphere per year than
    permafrost soils.
  • Methane is a powerful greenhouse gas. Emissions
    from widespread collapse wetland formation could
    have strong positive feedbacks on climate
    warming.

37
Dissolved Organic Carbon (DOC) from the Yukon
River Contributes Nutrients to the Arctic Ocean
Food Web
DOC
  • The amount of DOC carried from the
    Yukon River to the Bering Sea during
    summer has decreased in recent years.
  • The decreased amount is thought to be emitted to
    the atmosphere as greenhouse gases.
  • This may have important consequences to climate
    warming and to the Arctic Ocean food web.

Striegl et al., 2005 2007
38
Carbon Cycle Research and Impacts
Projected Permafrost Degradation by 2100
39
Carbon, Climate and Wildfires
  • Extremely dry conditions and resultant high fuel
    levels lead to numerous wildfires
  • that cause
  • Carbon emissions to atmosphere
  • Permafrost degradation
  • Mercury release
  • Increased GHG

Brooks Range
Seward Peninsula
Fairbanks
Alaska Range
Anchorage
MODIS Image Summer, 2004
40
Global Change and Streamflow
USGS used 12 climate models to simulate 21st
Century global warming and related streamflow
changes
  • Results
  • Orange and red areas represent decreasing
    streamflow
  • Blue areas represent increasing streamflow
  • change in runoff by 2050 under greenhouse
    scenarios, 10 to 30 decreases in runoff in
    western US.

Milly, Dunne, and Vecchia, 2005, Global pattern
of trends in streamflow and water availability in
a changing climate Nature, p. 347-350.
41
Ecosystems Research and Responses
Source http//www-lsce.cea.fr/pmip Kaplan et al.
(2003).
42
Tools for Assessing Land Resources (Senegal)
Current and seasonal vegetation production
(MODIS NDVI)
Images of land surface (Landsat)
Land Use
Land Productivity (MODIS)
43
The Energy-Climate Feedback Loop
Hydrocarbon Energy Production and Use
Global Warming Sea-Level Rise Loss of
Biodiversity Ecosystem Health Water
Availability
Impacts on Hydropower Production Impacts on
Oil and Gas Production and Transportation
Infrastructure Energy transport Provides for New
Exploration Frontiers (Arctic Ocean) Enhanced
Transport
Climate Change
44
The Way Forward
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