Consequences of Climate Change for Rangelands: Unexpected Consequences of More Extreme Rainfall Patterns Alan K. Knapp Colorado State University Jana Heisler-White.

Slides:



Advertisements
Similar presentations
Climate Change: Science and Modeling John Paul Gonzales Project GUTS Teacher PD 6 January 2011.
Advertisements

Biomes What Is A Biome? If an organism is the simplest level of ecosystems, what level would a biome be? Make a flow chart. Biomes 1.
Terrestrial Environments Around the World
Effects of variable rainfall and increased nitrogen deposition on nitrous oxide production in a semi-arid grassland ecosystem A forethought of global change.
The Climate and the Human Activities The Climate and the Human Activities Natural Variations of the Water Cycle Natural Variations of the Water Cycle Water.
Scaling Laws, Scale Invariance, and Climate Prediction
Water Dynamics: The Experimental Perspective Alan K. Knapp Graduate Degree Program in Ecology, Colorado State University.
Plant Ecology - Chapter 17 Climate & Physiognomy.
Soil-mediated effects of a CO 2 gradient on grassland productivity: Interactions with resources and species change. Philip A. Fay USDA-ARS Grassland, Soil,
Climate Change Impacts in the United States Third National Climate Assessment [Name] [Date] Climate Trends.
Dave Sauchyn, Ph.D., P.Geo. C-CIARN Prairies Prairie Adaptation Research Collaborative Senate Committee on Agriculture and Forestry Ottawa, December, 2002.
Chapter 5 By: Genevie Lopez.
By Michelle Sampson , Victoria Gray , Michaella White, Liz Bellmickley
World Geography Unit 2: World Climate Patterns Ocean Currents and Other Factors That Affect Climate.
Consequences of Global climate Change. Impact of Global Warming Sea level rising Altered precipitation pattern Change in soil moisture content Increase.
Changing Vegetation in the Savanna: Supplementary Material to Lesson 4 of the “East Africa Climate Change Curriculum Unit” Available at
May 2007 vegetation Kevin E Trenberth NCAR Kevin E Trenberth NCAR Weather and climate in the 21 st Century: What do we know? What don’t we know?
Chapter 7 Climate and Terrestrial Biodiversity
Climate Change and its impact on Forests in Europe and North America Andrew J. R. Gillespie, Ph. D. United States Environmental Protection Agency.
Changes in the incidence of climate extremes and their links to climate change Neville Nicholls Monash University.
Impacts of Climate Change. Changes in polar and glacial ice Satellite measurements shown a trend in overall shrinking of Earth’s ice sheets Impacts: Rising.
Chapter 7 – Climate and Biodiversity
Biomes of the World.
Climate Change Impacts & Resource Management Stephen T. Gray Water Resources Data System WY State Climate Office University of Wyoming.
Climate.
Water, Climate, and Vegetation. Earth’s Water Water covers about 70% of the Earth’s surface, most of it is saltwater. Some areas never have enough water.
Climate Change. Have you noticed any change in our summer weather? Our winter weather? The arrival of spring? Have you noticed any change in our summer.
This postcard shows a warm coastal climate.
December 2002 Section 2 Past Changes in Climate. Global surface temperatures are rising Relative to average temperature.
Abstract Increasing global temperatures are projected to alter the intensity of the hydrological cycle (1). For example, precipitation patterns are predicted.
Carbon Dioxide (CO 2 ) Recent CO 2 Changes IPCC Reports.
Do Now 4/20 HW change: 34.9 ONLY OBJECTIVE: Identify and describe the characteristics of major terrestrial and aquatic biomes TASK: Copy definition into.
The Biosphere: An Introduction to Biomes. Earths Biomes Ecology Organization Population Community Ecosystem -scientific study of the interactions between.
Chapter 4: Kinds of Ecosystems Section 4.2: Grasslands, Chaparral, Deserts, and Tundra.
Gary McManus Associate State Climatologist Oklahoma Climatological Survey Global Climate Change and the Implications for Oklahoma.
Modern Climate Change Darryn Waugh OES Summer Course, July 2015.
Backward Forward Home Exit III. How will global warming affect our environment? 1. What kinds of climatic change will global warming bring about? According.
Unit 1: The World Physical Geography.
Warm Up: Biomes K-W-L:Desert.
Global Climate Change. 150 Authors 1,000 Contributing Authors 5 Years Work 130 Countries 1,000 Expert Reviewers The IPCC WGI Report.
Weather and Climate Determine Biomes
Chapter 11- Tropical climates Tropical climates are somewhat variable In terms of moisture In terms of temp on a day-night cycle Tropical climates are.
Do Now At your table, share some good things that have happened this week. You do not need to write this down. Make sure you have turned everything in.
Moisture Controls on Trace Gas Fluxes From Semiarid Soils Dean A. Martens and Jean E. T. McLain SWRC – Tucson and Water Conservation Laboratory – Phoenix.
Climate: The average, year-after-year conditions of temperature, precipitation, winds and clouds in an area.
Physical Effects of Climate Change. Effects of Climate Change in the Atmosphere  Heat Waves  Drought  Wildfires  Storms  Floods
In 1788 settlers brought 2 bulls and 5 cows to Australia Problem: Each cow deposited dung pats a day.
Climate and Terrestrial Biodiversity Chapter What Factors Influence Climate?  Concept 7-1 An area's climate is determined mostly by solar radiation,
Northeast Regional Climate Information Projected Climate Changes for the Northeast More frequent and intense extreme precipitation events, 100-year storm.
The Biosphere By: Ali Ball, Alex Wampler, Holly Rhoden, & Ada Tolliver.
Indianpipe –Monotropa uniflora. Tetraphis pellucida.
Chapter 18 section 2 Climate Regions What factors are used to classify climates? What are the six main climate regions? rainforest, savanna, desert, steppe,
Indicators and Effects of Climate Change
Long-term climate change & Short-term climate variability.
Biomes of the World.
Biomes of the World.
Climate change and meteorological drivers of widespread flooding in the UK EA/Defra/NRW Research and Development (R&D) project board meeting, London, March.
Section 2: Terrestrial Biomes
Climate Change slides for Exam Two
Regional analyses of aboveground net primary production (ANPP):
Defining Biomes Chapter 4.4.
Where did your dinner come from?
Climate Change and the Midwest: Issues and Impacts
Section 2: Terrestrial Biomes
Biomes of the World.
Ecologists classify the major ecosystems of the world into biomes.
Biomes of the World.
What is a biome? A BIOME is the largest geographic biotic unit, a major community of plants and animals with similar life forms and environmental conditions.
Why do different organisms live in different places?
The Geographies of Climate Change
Presentation transcript:

Consequences of Climate Change for Rangelands: Unexpected Consequences of More Extreme Rainfall Patterns Alan K. Knapp Colorado State University Jana Heisler-White University of Wyoming Melinda D. Smith Melinda D. Smith Yale University John M. Blair John M. Blair Kansas State University

Why should we care about climate change? – The Grassland Ecologist’s Perspective We may be witnessing one of the most profound climatic changes in the Earth's history. Predictions for the 21st century show warming of the troposphere especially in the Arctic, an increase in precipitation extremes, a decrease in snow and ice cover, and an increase in sea level. The danger facing society today is that anthropogenic global warming may be too fast to allow humans, and other species, to adapt to its detrimental impacts.

T. Riley and J.A. Klein Grasslands, rangelands, steppe, tundra, savanna and shrub- grasslands cover ~ 40% of the Earth’s land surface

Ecosystem Services Grasslands Provide: Forage for domestic livestock Forage for domestic livestock Habitat for native ungulates Habitat for native ungulates Habitat for grassland plants/animals Habitat for grassland plants/animals Migratory birds – breeding/forage Migratory birds – breeding/forage Soil erosion control Soil erosion control Carbon sequestration Carbon sequestration

Sala et al Grasslands (most) are water limited systems… Rainfall vs. Production across the Central US Setting the stage…

The world is getting warmer…. (thermometer evidence)

Dave Theobald Plant evidence…

Dave Theobald

Overpeck et al History provides few analogs for the type of climate change forecast…we are in uncharted waters… Little Ice Age: ’s - bitter winters, famine in Europe Younger Dryas – 1300 yr cold period (11,000 BP), then rapid warming IPCC predictions

Rainfall regimes CO 2 effects Temperature effects Soil moisture Plant water relations Water, temperature (and CO 2 ) are linked in grasslands and most ecosystems…

Global Climate Model (GCM) predictions for changes in mean annual rainfall changes are inconsistent with each other in magnitude and sign…But more extreme weather as the atmosphere warms is consistently predicted.

Dust Bowl of 1930’s in US Drought in Senegal More intense hurricanes and floods Are grasslands vulnerable to this aspect of climate change? Focus on “subtle” increases in “extreme” events – or shifts in rainfall patterns…not the obvious…but the pervasive… Proportion of total rainfall in the US from large (>5 cm) rainfall events Proportion (%) of rainfall in “extreme events”

Proportion of total rainfall in the US from large (>5 cm) rainfall events Proportion (%) of rainfall in “extreme events” Abundant evidence that rainfall regimes are changing Oklahoma

 12 rainfall manipulation plots  Collect, store, and reapply natural rainfall on intact grassland plots The Rainfall Manipulation Plot (RaMP) Experiment Address the impact of changes in size and timing of growing season rainfall To what extent will altered rainfall patterns affect ecological processes in grasslands?

Experimental manipulation: 50% longer inter-rainfall periods, larger individual rain events No change in total precipitation quantity Fewer events Greater storm size Increased dry periods

Ambient ppt timing: “typical” seasonal pattern Altered ppt timing: repeated deficits more extreme wetting and drying cycles Key driver of responses: Soil moisture dynamics Average soil water content in top 30 cm: - reduced by 12% Variability in soil moisture: - increased by 27%

All rainfall treatments

What about the Shortgrass steppe – & semi-arid and arid grasslands? Like all grasslands, a system of “extremes”

Frequent small events (10 day intervals, 15 mm events) Infrequent big events (30 day intervals, 47 mm events) All received “average” MAP amounts Shortgrass steppe

(9 events) - Heisler et al Semi-arid grassland Extreme rainfall events Long dry intervals Increases ANPP

Ojima and Lackett 2002 Tall-grass Mid-grass Short-grass Precipitation gradient Regional perspective

Semi-arid grassland Extreme rainfall events Long dry intervals Increases ANPP? With the same experimental design, how will these different grasslands respond? Mesic grassland Extreme rainfall events Long dry intervals Reduces ANPP?

SGS Experimental alteration of rainfall patterns across the Great Plains of North America Frequent, small events Fewer, infrequent large events VS. A = 12 events B = 6 events C = 4 events Total = 191 mm A = 12 events B = 6 events C = 4 events Total = 450 mm KNZ Semi-arid Mesic Jana Heisler

Mesic Grassland A shift from 12 to 4 events results in a 15% decrease in productivity. More “extreme” rainfall regime Shift to more extreme (large) rainfall events  reduced productivity

Semi-arid Grassland A shift from 12 to 4 events resulted in a 30% increase in productivity. More “extreme” rainfall regime Shift to more extreme (large) rainfall events  increased productivity

Sevilleta LTER – Central New Mexico Monsoon rainfall addition experiment: 20 mm events vs. four 5 mm events

Seasonally averaged soil water content, plant water status, photosynthesis, and production were highest in plots receiving a small number of large events Collins, Thomey, Johnson, Brown, Natvig, Friggens 20 mm events 5 mm events 20 mm events 5 mm events

Why do dry vs. mesic grasslands respond differently? Two aspects of more extreme rainfall regimes: 1. Larger rain events 2. Longer dry periods between events When soils are usually moist, longer dry periods are most important… When soil are already dry, larger rain events cause the greater response…

Wet relative to ambient Dry relative to ambient

Sala et al Responses to climate change depends on location even in the same grassland biome – this make generalizations a challenge… Prediction based on wet grassland responses Prediction based on dry grassland responses The future?

Goldewijk and Battjes (1997) Reid & Miller (1989) Vitousek (1994) NOA A Ecological Systems Climate Change is but one facet of “Global Change” Grazing J.A. Klein

…we are changing Earth more rapidly than we are understanding it. -Vitousek et al We have moved beyond questions such as “Is climate change happening?” There is little uncertainty about this. The uncertainty is with the consequences of climate change…

Key Points: Research indicates that subtle climate change can have surprising consequences. 1. Even “subtle” changes toward more extreme rainfall patterns can alter production and the sensitivity of the grasslands to changes in rainfall amounts 2. Grasslands can respond in opposing ways to the same form of climate change