Climate Effects Network: Linking Causes and Impacts of Climate Change for Societal Benefit and Decision Support U.S. Department of the Interior U.S. Geological Survey Image from Google Earth The engine of the Earth’s climate system is it’s heat budget Climate Change: Natural vs. Anthropogenic Source: IPCC, Climate Change 2001: The Scientific Basis Past 100 Years: Alaska ¾ ¾ ¾ ¾ ¾ ¾ Average U.S. temperature increased 1°F over 100 years Alaska has warmed 4°F 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 Response of plants and animals Increased fire, drought, floods The The Climate Climate Effects Effects Dilemma Dilemma Point data indicate major change is underway where baseline regional data is sparse or nonexistent. Where and when these changes will disrupt ecosystem function or human activity is uncertain. What adaptation or mitigation strategies will be most effective are also uncertain. To understand the changes, measuring the effects on whole systems over time is necessary. Answers are needed now in some areas, and very soon in many. The The logistical logistical issue issue PROBLEM: It is not possible to assess the complex changes, interactions, and feedbacks caused by climate change at every specific location where DOI or USDA-FS resource managers need us to be. THE NECESSARY ASSUMPTION: Within broad ecoregions, the dominant processes controlling ecosystem responses to climate change are similar; however, ecosystem condition is highly variable. How Do We Do this? Multi-component –Multi scale Observations and Research Results For Decision Support The TheVision Vision––AANational NationalClimate ClimateEffects EffectsNetwork NetworkThat That Allows AllowsSystematic SystematicApplication Applicationof ofResearch ResearchResults Results A truly integrated National climate effect monitoring network capable of detecting and analyzing change at a range of temporal and spatial scales A scientific team focused on early detection and scientific analysis in support of adaptation or mitigation strategies An information dissemination and decision support system for cost effective, scientifically rigorous management and policy decisions The capacity for the next generation to protect and sustain our National trust resources through early detection of change Delaware River Basin Example Built on US Forest Service, USGS, and Park Service infrastructure and programs Multi-tier Monitoring Design Scale-appropriate monitoring linked through common indicators • Tier One –Intensive Areas Increasing temporal resolution ¾ Relatively small number of specific sites representing important processes • Tier Two – Condition Sample ¾ Gradient studies: representative of specified condition classes • Tier Three – Extensive Inventories and Surveys ¾ Representative regional statistical sample • Tier Four – Remote Sensing and Mapping ¾ Wall-to-wall coverage; stratification Increasing spatial resolution Steps Involved In Network Implementation • Determine specific climate effects and responses issues • Determine the types of data needed at each Tier of the framework • Assess what data is already being collected by existing programs (the “Foundation” Programs). • Complete a gap analysis relative to each issue • Request volunteer or funded enhancements of existing programs to fill the gaps • Fund new observation/research/decision support tool development to fill the gaps • Systematically ensure research is linked to applications for decision support Tier 1: Monitoring Intensification at 3 Watersheds in the Delaware River Basin French Creek Intensive Plots Tier 2:Regional Validation Plots Independent validation of estimates to test scaling methods. River C Some of the Intensive Forestry Measurements Added to Forest Inventory Plots Litterfall collector Foliar sampling Soil temperature logger Dendrometer band Scaling strategy FIA P2/P3 plot network CEMRI carbon plot network nested within Tier 3 – USFS FIA and FHM Plots measured with a 5year panel system to characterize forests of the Delaware River Basin. Added 3 soil samples at 3 depths to each forested plot, + stream survey. Remote Sensing: Building new tools through an integrated ground-truthing network AVIRIS Airborne Visible/InfraRed Imaging Spectrometer The resulting 224 band layer image is known as an “image cube”. When the data from each band is plotted on a graph, it yields a spectrum. Hallet, USFS Regional relation of deposition chemistry to soil and stream chemistry Annual Nitrogen deposition Soil Calcium Stream acid neutralizing capacity (ANC) Leveled N-dep model matches current soil Ca and stream pH map for Del basin. Possible Collaborative Observation and Research (CORE) Ecoregions Yukon River Basin Grasslands and North Slope Pacific Northwest Rainforest Southwest Mountains and Desert Northeast Temperate Forest Gulf Coast/ Florida Wetlands Tropical Forest Permafrost Temperature Romanovsky, 1999 1978 2002 (courtesy of B. Riordan) Globally and locally significant rapid change The Yukon Basin holds large stores of carbon Boreal Forest Ecosystems • 25 - 30% of Global Soil Pool • 30% Global Vegetation Pool Thermo-Karst Topography where permafrost is thawing METHANE FLUX Thermo-karst wetlands emitted 13 times more CH4 to the atmosphere than the permafrost plateau sites on an annual basis. mmol CH4 m-2 hr-1 1.0 0.8 Thermokarst wetlands Thermokarst edges Permafrost plateau 0.6 0.4 0.2 0.0 -0.2 3/20 4/9 4/29 5/19 6/8 6/28 7/18 8/7 8/27 9/16 CO2 CH4 CO2 CO2 CH4 CH4 PERMAFROST Wickland, 2006 Boreal Forest Changes with Changing Moisture and Temperature Summer (May:Aug) temperature vs. white spruce growth (Bonanza Creek LTER - Univ. of Alaska Experimental Forest) 1.2 1.0 0.8 0.6 0.4 1912 volcanic ash 2004 record hot 0.2 1993 & 95 spruce budworm defoliation KILL ZONE 0.0 9.0 10.0 11.0 12.0 13.0 14.0 15.0 16.0 17.0 previous May:Aug T (deg C) 18.0 19.0 20.0 21.0 MODIS Satellite, 10 August, 2005 Brooks Range Seward Peninsula Fairbanks Alaska Range Anchorage The Yukon River Basin: A rapidly changing landscape Will thawing permafrost greatly accelerate CO2 flux? • Landscape is Heterogeneous, Controlled by Soil Drainage • Permafrost Landscape Highly “Elastic” in C exchange C Loss Drier,warmer 60 Permafrost to Fire -- Landscapes 30 % of NPP Cooler, wetter Wetter,warmer Well drained V. Poorly Drained 0 0 100 C Loss to Decomposition % of NPP Harden et al, GCB Dec. 2000 How will changes in regional climate affect the hydrology of the Yukon River, and how will these changes affect water distribution, river flow, nutrient export to the coastal ocean, and salmon recruitment? How much of the C released from permafrost will emit to the atmosphere? …or discharge to rivers and the ocean? Linkage Linkage of of aa Climate Climate Effects Effects and and Responses Responses Network Network to to Land Land Management Management Issues Issues Leverage existing and new data and projects to examine long term association between climatechange effects and responses across spatial and temporal time scales (the CORE network) se on sp Predictive Capability Ch an ge Re Cl im ate tem Predict thresholds and approaching tipping points DSTs s Sy Provide responsive “focus” studies to address local needs Develop Decision Support Tools with local adjustment Management Response Monitoring Data, Research Results & Models Science and Management Questions • • • • • How will increases in temperature affect the hydrology of the Yukon River Basin and how will these changes affect water distribution and river flow? Will carbon flux “feedbacks” to warming resulting from changes in the land cover, soil active layer, and basin hydrologic regime potentially enhance global climate warming? What are the effects of climate change on the abundance, quality, distribution and access to subsistence resources? How will these changes affect the distribution, species, and quality of forest resources ? What strategies are needed to adapt to the likely effects of climate change and associated permafrost thawing on natural resources, human infrastructure, and local culture? Yukon Foundation Programs • • • • • • • Bonanza Creek/Caribou-Poker Flats LTER Tier 1 UAF/UAA Research and Modeling (eg. Scott Rupp) FWS/NPS monitoring programs Tier 1 Wolf Creek, Yukon Territories Tier 1 New USGS Research Watersheds- Hess Creek Soil carbon studies, Gradient Karst sites Tier 2 USGS- Yukon River monitoring program Tier 2 Yukon Foundation Programs • UAF/USEPA/Tribal Socio-economic studies Tier 3, • USGS District COOP/Basic Data Programs (Research and stream gaging) Tier 1, 2, 3 • Alaska Science Center mapping Tier 4 • Lake disappearance study- Tier 4 • EROS coverage development- Tier 4 • NASA, NOAA, EPA • USFS Forest Inventory & Analysis Prog (FIA)? Tier3 FOREST SERVICE INVENTORY SAMPLE PLAN? (12-15 years) Lower Yukon 5 yrs Upper Yukon – Porcupine 2 yrs n plots n plots 598 301 180 plots/yr 118 261 190 plots/yr Tanana River 5 yrs n plots 1010 89 220 plots/yr Ac/plot 23,600 94,400 Draft, Van Hees, 2005 Add Active Layer C, soil thickness, Roofed plots Tier 1: Research Installations USGS and UAF Research on the effects of wetter/dryer/warmer conditions on C flux Manipulated water table in wetlands Tier 2: Active-Layer Monitoring Stations Wind Speed and Direction Each AL Station Monitors the Following Climate Parameters: Air Temperature Terrestrial Snow Depth Shortwave Radiation • soil temperatures (5-120 cm) • soil moisture • active-layer depth & duration • snow depth & duration • albedo Permafrost Temperatures 5-120 cm Solar Panel Atmospheric • air temperature • wind speed & direction • cloudiness Soil Moisture @ 15cm Datalogger And Power sample rate = 30 sec 253 Tier 4: Remote Sensing positive 2004 Difference Between Predicted and Observed Temporally-Integrated NDVI (Coniferous Forests in YRB) anomalies 113 -112 negative anomalies Fires after 1997 outlined in black -283 Hydrologic Data Collection- USGS/Canada Fixed Station Network Intensive Sampling Yukon R. at Eagle Porcupine R. Yukon R. near Stevens Village June & Aug-Sept., 2002 Tanana R. Yukon R. at Pilot Station LTER NOAA-IPY USGS Pilot Station K k ku u oy r ve i R on Yuk Stevens Village ine p u rc er o P Riv June & Aug-Sept., 2003 Fort Yukon R iv e Tan ana Riv e r Eagle r Major Drainage Basins Upper Yukon R. & Headwaters Porcupine R. Tanana R. East Central Yukon R. Koyukuk R. & West, Lower Yukon R. Whitehorse Research Watersheds (Tier 1) and Fixed river stations (Tier 2) Ecosystem Modeling GEMS (General Ensemble Biogeochemical Modeling System) Requires modeling staff, data management, computing infrastructure National Benchmark Databases Land Cover: USGS Land Cover Trends Soil: STATSGO Climate: CRTUS2.0 (1900 – 2000) N Deposition: National Atmospheric Deposition Program Crop Information: USDA Agricultural Census Data FIA: Forest biomass, NPP, Age Distribution Data Assimilation GEMS Thousands of Sampling Blocks Carbon dynamics simulated at 60 m x 60 m spatial resolution within 20 km x 20 km or 10-km by 10-km sampling blocks Decision Support Systems CommunityViz USGS Integrated Regional Assessment of Climate Effects on Vegetation, Soil, and Water in Forested Landscapes Forest Soil FIA, FHM, NPS, Research, Remote sensing FIA/FHM- USGS Soil surveys, Research Air Climate Research, NADP Water NAWQA, WRD State/Fed QW Surveys, Research What do you see as top climate change issues in Alaskan Forests? What decision-making capabilities do your need? What improvements in understanding and predicting would you like to see from a network? How can we do this together? September 2007. Anaktuvuk River Fire North Slope tundra of Alaska Man-made or not, Large changes are underway The need for credible data The world’s most famous justification for monitoring data. Second-most famous monitoring justification? USGS Polar Bear Report 7 September 2007 Whether human-caused or not, scientists can continue to provide data on climate change and global warming, but all of us must decide how we are going to respond. Thank You Questions? Decision Support Scenarios: • Adaptation: The combination of ground and remote sensing data allows resource managers to focus adaptation strategies for managing trust resources into specific parts of the landscape. • Adaptation: Fire management teams use ecosystem performance maps to guide fire warnings and preparations, and to track invasive species. • Adaptation: Pipeline designers use combined network to plan cost-effective and least-disruptive pathways for new infrastructure through the rapidly changing northern landscape. Examples Examples of of Climate Climate Change Change Effects Effects Physical Effects: Measurable change in meteorological factors • Temperature, precipitation, seasonality, storm frequency and cloud cover Altered freshwater supply and flow patterns Increased drought, fire, flooding Physical changes to the land form (e.g. permafrost) Biological Effects: Loss or migration of keystone species Corresponding biotic responses Heightened risk of invasives, vector born diseases Feedback Loops: Changes in vegetation affect regional climate Carbon cycling Altered biogeochemical interactions The The GOAL GOAL –– A A National National Climate Climate Effects Effects Network Network That That Allows Allows Systematic Systematic Application Application of of Research Research Results Results A truly integrated National climate effect monitoring network capable of detecting and analyzing change at a range of temporal and spatial scales A scientific team focused on early detection and scientific analysis in support of adaptation or mitigation strategies An information dissemination and decision support system for cost effective, scientifically rigorous management and policy decisions The capacity for the next generation to protect and sustain our National trust resources through early detection of change Tier 2 – Condition Sample: Design for Soil CO2 Flux Delaware River Basin Delaware Water Gap Intensive Site Select new sample sites by forest type and moisture class Establish 12 sample locations on lines between subplots FIA plot design