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Climate change, invasive species and forests Lee E. Frelich Director, The University of Minnesota Center for Hardwood Ecology Vice President, Eastern Native Tree Society Chair, Board of Directors, Great River Greening Dave Hansen Univ. of MN John Knuerr

Lee Frelich's "Climate Change & Forests" Presentation

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Within the next 50–100 years, the warming climate will have major effects on boreal and northern hardwood forests situated near the prairie–forest border of central North America. This biome boundary shifted to the northeastduring past episodes of global warming, and is expected to do so again. The climate of the future will likely lead to higher mortality among mature trees, due to the greater frequency of droughts, fires, forest-leveling windstorms, and outbreaks of native and exotic insect pests and diseases. In addition, increasing populations of native deer and European earthworm invasions will inhibit the establishment of tree seedlings. The expected net impact of these factors will be a “savannification” of the forest, due to loss of adult trees at a rate faster than that at whichthey can be replaced. This will cause a greater magnitude and more rapid northeastward shift of the prairie–forestborder, as compared with a shift solely attributable to the direct effects of temperature change.

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Page 1: Lee Frelich's  "Climate Change & Forests" Presentation

Climate change, invasive species and forests

Lee E. Frelich

Director, The University of Minnesota Center for Hardwood Ecology

Vice President, Eastern Native Tree Society

Chair, Board of Directors, Great River Greening

Dave HansenUniv. of MN

John Knuerr

Page 2: Lee Frelich's  "Climate Change & Forests" Presentation

Svante August Arrhenius(Nobel prize, Chemistry,1903)

Developed the hothouse theory forCO2 in 1896, and in 1905 predicted that raising CO2 content of the atmospherewould cause an increase in mean globaltemperature similar in magnitude tomodern predictions

Page 3: Lee Frelich's  "Climate Change & Forests" Presentation

Evidence that CO2 increase and climate change are caused by humans

1. Keeling curve corresponds to population and known emissions of CO2

2. Suess effect

3. Temperature profile of the atmosphere—warmer lower atmosphere and cooler stratosphere

4. Existing ‘Greenhouse effect’ of 56 degree F before human enhancementof heat trapping gases in the atmosphere

5. Models with human greenhouse gas enhancement match observed temperatures over the last 100 years, models with only naturalforcings on climate do not

Page 4: Lee Frelich's  "Climate Change & Forests" Presentation
Page 5: Lee Frelich's  "Climate Change & Forests" Presentation

Climate change occurs in the context of large year toyear variability—summer temperatures for 2009

Page 6: Lee Frelich's  "Climate Change & Forests" Presentation

Summer 2009—Example of regional temperature anomalies versus global mean in a warming climate. A cold summer in central and eastern North America, although 80% of the world had above average temperatures.

…and spatial variability

Page 7: Lee Frelich's  "Climate Change & Forests" Presentation
Page 8: Lee Frelich's  "Climate Change & Forests" Presentation

http://www.cgd.ucar.edu/ccr/ammann/millennium/CODES_MBH.html

Comparison of the original Mann ‘hockey stick’ reconstruction of temperature(red) with implementation of valid criticisms of the PC methodology (green).From Wahl and Amman 2006.

Tree ring analyses showing climate over the several hundred years

Page 9: Lee Frelich's  "Climate Change & Forests" Presentation

Osborne and Briffa 2006, instrumental record for northern hemisphere (red)and for records closest to proxy sites (green).

Tree ring analyses from 14 sites

Page 10: Lee Frelich's  "Climate Change & Forests" Presentation

Oerlemans, 2005 temperature reconstruction of global mean temperaturebased on 169 glaciers.

Page 11: Lee Frelich's  "Climate Change & Forests" Presentation

Borehole temperature data from Huang, Pollock and Shen, Nature, 2000

Temperature evidence from boreholes

Page 12: Lee Frelich's  "Climate Change & Forests" Presentation

From McCarthy, 2009, Science

Modeling of temperatureshowing how natural andhuman influences work together.

Page 13: Lee Frelich's  "Climate Change & Forests" Presentation

Natural versus human CO2 forcing on the climate

Page 14: Lee Frelich's  "Climate Change & Forests" Presentation
Page 15: Lee Frelich's  "Climate Change & Forests" Presentation

British Meteorological Office, December 2009

Page 16: Lee Frelich's  "Climate Change & Forests" Presentation

Migration maps for tree response to past climate change in 1000s years before present (M.B. Davis 1983)

Spruce White pine

Page 17: Lee Frelich's  "Climate Change & Forests" Presentation

Current and simulated future range of black spruce, from Lenihan and Neilson 1995.

300 mile shift is equal todistance moved in ~ 2000years in paleorecord

Page 18: Lee Frelich's  "Climate Change & Forests" Presentation

Forest cover of central North America (green)DeFries, R., M. Hansen, J.R.G. Townshend, A.C. Janetos, and T.R. Loveland (2000), 1 Kilometer Tree Cover Continuous Fields, 1.0, Department of Geography, University of Maryland, College Park, Maryland, 1992-1993.

It is possible that the pbf will move 500 km to the north and east, deforesting an area 2X the size of California

Page 19: Lee Frelich's  "Climate Change & Forests" Presentation

Native species have migrated in the past without going extinctwhat’s different now?

Rate of climate change—many species cannot migrate fast enoughFragmented environment—makes species to movement more difficultHabitat loss—less habitat now and can support fewer speciesInvasive species—can reproduce and move fast, they have opportunity

to displace native species during times of rapid change Exotic diseases and pests—can spread faster in a warmer climateDeer grazing—will increase in the north, can extirpate native plants

David Augustine

TNC

Page 20: Lee Frelich's  "Climate Change & Forests" Presentation

Minneapolis Star tribune

Before and after the 1999 blowdownin the Boundary Waters, northern MN

Page 21: Lee Frelich's  "Climate Change & Forests" Presentation

Wind plus fire = major forest transformationNick Fisichelli and Roy Rich, Cavity Lake Burn, Seagull Lake, July 2007.Photo: Dave Hansen, University of MN

Page 22: Lee Frelich's  "Climate Change & Forests" Presentation

Several forces are at work that may push MN foreststowards savanna:

If soils become drier for any reason sites can support fewer trees:

Warmer soilsHigher evaporation to precipitation ratioEuropean earthworms stripping the insulating duff layer

Page 23: Lee Frelich's  "Climate Change & Forests" Presentation

More drought = trees under stress and forest dieback

Photo: Dave Hansen

Page 24: Lee Frelich's  "Climate Change & Forests" Presentation

Native insects play a major role in forest changeBenign native insects can have outbreaks in a warmer climate.For example, mountain pine beetle in British Columbia—a native insect that caused massive tree mortality over 30 million acres of lodgepole pine forest, and could threaten jack pinein MN

Page 25: Lee Frelich's  "Climate Change & Forests" Presentation

Sylvania Wilderness maple and hemlock forest in 1988

Page 26: Lee Frelich's  "Climate Change & Forests" Presentation

Sylvania in 2006

Page 27: Lee Frelich's  "Climate Change & Forests" Presentation

Global warming orGlobal worming?

Earthworms are ecosystem engineers that can alter the structure of soil, and change the H2O, N and P cycles, Cdynamics and seedbed characteristics on a regional scale

Page 28: Lee Frelich's  "Climate Change & Forests" Presentation

Soil profile, no earthworms (left), with earthworms (right).The loss of the duff layer will affect summer soil temperature

Photos: Dave Hansen, University of MN

Page 29: Lee Frelich's  "Climate Change & Forests" Presentation

00.20.40.60.8

11.21.41.6

-5 0 5 10 15 20 25 30

Invasion timing (years)

Rin

g w

idth

inde

x

Worm freeworm invaded

Earthworm invasion in maple forest causes a decreasein tree ring width and loss of seedling density and herb specieson the forest floor

Page 30: Lee Frelich's  "Climate Change & Forests" Presentation

Recent literature shows that Earthworms also facilitate germination and establishment of European buckthorn and garlic mustard by changing the seed bed

Kathleen Knight

Photos: The Nature Conservancy

Page 31: Lee Frelich's  "Climate Change & Forests" Presentation

Exotic earthworms + deer =major transformation of theforest. Bare soil and lowernutrient status should favor hemlock over maple, but deer favor maple.

Both dominant species aredisfavored, combined withwarmer climate and sandysoils, probably meansSylvania will become oaksavanna in the future

Page 32: Lee Frelich's  "Climate Change & Forests" Presentation

Paul Jost

Summary of impacts on Lake Statestree species

Global warming and rate of migration:All species Sudden oak death: red oak, pin oakDeer: white cedar, yellow birch, white pine, oaksBalsam woolly adelgid: balsam firEmerald ash borer: green ash, black ash, white ashAsian long-horned beetle: red maple,sugar maple, aspenHemlock woolly adelgid: hemlockMountain pine beetle: jack pineNative insects: eastern larch, others Earthworms: sugar maple and others

Page 33: Lee Frelich's  "Climate Change & Forests" Presentation

Overall scheme for change at the prairie-forest border proposed by Frelich and Reich

Page 34: Lee Frelich's  "Climate Change & Forests" Presentation

We can expect a messy transitionHistory shows that development of a new ecosystem takes 100sto 1000 years to develop

Dave Hansen

Lee Frelich

Old

Transitional

New

Page 35: Lee Frelich's  "Climate Change & Forests" Presentation

Layne Kennedy

Lee Frelich and clones at work during Ham Lake Fire, Seagull Lake, May 6, 2007

Questions?