Getting from here to there: protecting and promoting ecosystem services during the conversion of forests to fields in New England Alexandra Contosta1,

Slides:



Advertisements
Similar presentations
Climate Smart Agriculture East Africa Regional Knowledge Sharing Meeting Thomas Cole June 11, 2012, Addis Ababa, Ethiopia.
Advertisements

Agriculture and Greenhouse Gases Jill Heemstra, University of Nebraska - Lincoln Building Environmental Leaders in Animal Agriculture (BELAA)
AGRICULTURE AND AGRI-FOOD CANADA PRESENTATION TO : The Standing Senate Committee on Agriculture and Forestry February 24, Regina.
Carbon Offsets – Agriculture & Forestry Neil Sampson June 25, 2004.
 The Importance of Soil Ag and Tech ! Ms. Lacross.
Opportunities to Increase Carbon Sequestration Through Forestry Richard A. Birdsey USDA Forest Service Global Change Research Program Senate Agriculture.
Sensing Winter Soil Respiration Dynamics in Near-Real Time Alexandra Contosta 1, Elizabeth Burakowski 1,2, Ruth Varner 1, and Serita Frey 3 1 University.
Changing Land Use: Supplementary Material to Lesson 5 of the “East Africa Climate Change Curriculum Unit” Available at
Lesson Overview Lesson OverviewClimate Lesson Overview 4.1 Climate.
SILVOPASTURE IN SOUTHEAST Presented by: Joshua Idassi, Ph.D. Extension Forester Tennessee State University Cooperative Extension Program.
Renewable and Nonrenewable Resources
Pollution Delhi, India “Red Fort” covered by smog 2009.
Changes and Feedbacks of Land-use and Land-cover under Global Change Mingjie Shi Physical Climatology Course, 387H The University of Texas at Austin, Austin,
Rainforests around the world Rainforests layers Tallest trees of the rainforest, over 20 ft, with the most sunlight Primary layer, home to many animals.
December 6, 2013 USDA Climate Change Program Office.
Nelius Foley, Matteo Sottocornola, Paul Leahy, Valerie Rondeau, Ger Kiely Hydrology, Micrometeorology and Climate Change University College Cork, IrelandEnvironmental.
Investment in Sustainable Natural Resource Management (focus: Agriculture) increases in agricultural productivity have come in part at the expense of deterioration.
Carbon Sequestration in Farm and Forest Ecosystems Sarah Hines April 2009
CLIMATE CHANGE – THE FUTURE OF FARMING AND FORESTRY IN THE COTSWOLDS Richard Lloyd Board Member.
Lindsay Hutley (CDU) Jeremy Russell-Smith (NTG)
24 Global Ecology. Global Biogeochemical Cycles Atmospheric CO 2 affects pH of the oceans by diffusing in and forming carbonic acid.
Unit 9 Lesson 2 Human Impact on Land Copyright © Houghton Mifflin Harcourt Publishing Company.
Climate Change and Energy Impacts on Water and Food Scarcity Mark W. Rosegrant Director Environment and Production Technology Division High-level Panel.
Economic Impacts of GHG and Nutrient Reduction Policies in New Zealand Adam Daigneault Landcare Research Motu Climate Economics Research Workshop Wellington.
CO 2 - Net Ecosystem Exchange and the Global Carbon Exchange Question Soil respiration chamber at College Woods near Durham New Hampshire. (Complex Systems.
Investigating the Carbon Cycle in Terrestrial Ecosystems (ICCTE) Scott Ollinger * -PI, Jana Albrecktova †, Bobby Braswell *, Rita Freuder *, Mary Martin.
Carbon and water cycling along the western Sierra gradient Anne Kelly SSCZO annual meeting August 21, 2012.
Module #1 A Snapshot of Silvopasture Pine Silvopasture in the Southeast.
Ecological Succession Ecosystems are constantly changing in response to natural and human disturbances.
Modeling CO 2 emissions in Prairie Pothole Region using DNDC model and remotely sensed data Zhengpeng Li 1, Shuguang Liu 2, Robert Gleason 3, Zhengxi Tan.
Seasonal Emissions of N 2 O, NO, CO and CO 2 in Brazilian Savannas Subjected to Prescribed Fires Alexandre Pinto, Mercedes Bustamante, Laura Viana, Universidade.
Mechanical weathering, such as ice wedging, increases surface area by breaking larger rocks into smaller rocks. Draw conclusions about how mechanical weathering.
© British Nutrition Foundation 2011 The environment and sustainability.
THE EFFECTS OF DEFORESTATION JOIN THE REVOLUTION AND STOP POLLUTION Deforestation is the permanent removal of standing trees. 70% of the Puruvian Amazon.
Citations Aguiar, M.I., Maia, S.M.F., Xavier, F.A. da S., de Sá Mendonça, E., Filho, J.A.A., de Oliveira, T.S., Sediment, nutrient and water losses.
Climate & Biomes. Weather Short term day to day changes in temperature, air pressure, humidity, precipitation, cloud cover, & wind speed Result of uneven.
Citations Aguiar, M.I., Maia, S.M.F., Xavier, F.A. da S., de Sá Mendonça, E., Filho, J.A.A., de Oliveira, T.S., Sediment, nutrient and water losses.
HUMAN IMPACT on the BIOSPHERE Chapter 6-2 Renewable and Non-renewable Resources.
The Greenhouse Effect The sun emits solar radiation which the Earth absorbs (UV rays). The Earth emits its own energy (heat waves called infrared rays)
Taylor Conte1, Elizabeth Burakowski2
CARBON, WATER, LAND USE & CLIMATE
Carly Cipolla ATOC 4800 Final Project
Forests, Parks and Landscapes
Model Summary Fred Lauer
Chapter 1 The Importance of Soil.
Effects of genotypic diversity on forage stand productivity
CLIMATE AND AGRICULTURE: AGRO-CLIMATOLOGY WATER BUDGET AND CROP CALENDAR MADE BY-S hounack Mandal M.Sc Geography, SEM-1 ADAMAS UNIVERSITY TO:- Dr. Anu.
Tradeoffs Between Soil Carbon Sequestration and Greenhouse Gas Emissions in Grazed Pastures of Northeastern US Organic Dairy Farms Alexandra Contosta1,
Impacts of Climate Change on Agriculture
Temperate Grassland Kailey Oakes.
Global Atmospheric Changes
Earth Data Science Lindsay Barbieri.
Anthropogenic Causes: Land Use & Land Cover
Figure 1. Spatial distribution of pinyon-juniper and ponderosa pine forests is shown for the southwestern United States. Red dots indicate location of.
Ecosystem Services Examples:
Zeima Kassahun and Heidi Renninger Results and Discussion
regenerate RENEWABLE ________________ RESOURCES
Environmental modeling application domains
Determining the Influence of Winter on Ecosystem
Climate and Change.
Climate and Terrestrial Biodiversity
Rangeland Soil Carbon: State of Knowledge
Deforestation.
Climate and Terrestrial Biodiversity
Investigating land-climate interactions across land cover types
Unit 4 Primary Resource Activities
What is the difference between climate and weather
Studying Past Climates
Trees and Climate Action
Valuing the city’s trees- An evaluation of CAVAT and i-Tree Forest Assessments Using Public Perception of Ecosystem services Hazel Mooney
Presentation transcript:

Getting from here to there: protecting and promoting ecosystem services during the conversion of forests to fields in New England Alexandra Contosta1, Richard Smith2, Heidi Asbjornsen2, Joseph Orefice3, Nathan Siegert4 1Institute for the Study of Earth, Oceans and Space, University of New Hampshire, 2Department of Natural Resources and the Environment, University of New Hampshire, 3 Yale School of Forestry and Environmental Studies, Yale University, 4USDA Forest Service, Northeastern Area State and Private Forestry Objective 2: Quantify changes in supporting, regulating, and provisioning ecosystem services New England farmers are clearing their forests to expand their agricultural land base. Conversion to silvopasture may reduce, maintain, or increase water regulating services Conversion to silvopasture may mitigate losses in climate regulating services Silvopasture is the deliberate integration and livestock, forages, and trees, and may offer an alternative. Figure 5. Surface unsaturated and subsurface saturated hydraulic conductivity (Kh and Ksat) in forest, converted silvopasture, and converted open pasture (Stewart et al., in prep). Soil hydrology in silvopasture could be more similar to that of the forest or the converted open pasture depending on site and land use history. We aim to determine: 1) how forest-to-agriculture conversion affects ecosystem services; and 2) if conversion to silvopasture can minimize these impacts. Figure 7. Fluxes were measured weekly using a static chamber technique. Figure 1. Beef cattle grazing in silvopasture Figure 4. Precipitation, vapor pressure deficit, and sapflow within forest and silvopasture plots at the UNH ODRF. Yellow shaded area shows a period of historic drought in 2016 (Coble et al., in prep). The silvopasture was not as susceptible to drought, which might be related to higher soil moisture. Objective 1: Establish forest-to-field conversion plots at two sites in New England Figure 6. Total seasonal fluxes of CO2 and N2O in reference forest, converted silvopasture, converted open pasture, and reference pasture (Contosta et al., in prep). Fluxes from silvopasture soils of both greenhouse gases tended to fall between those of forests and open pastures. UNH ODRF North Branch Farm North Branch Farm UNH Organic Dairy Research Farm Figure 2 Location of plots at the UNH Organic Dairy Research Farm, Lee, NH, and North Branch Farm, Saranac, NY. Plots were established in 2015 at UNH and in 2012 at North Branch Farm. Silvopasture may minimize changes in microclimate that result from land use conversion. Figure 8. Soil temperature in converted silvopasture (thinned) more similar to reference forest than converted pasture (clear cut) and open pasture. Data collected continuously from weather stations (left). Year 1 Year 2 Year 3 Wood Provisioning may be enhanced with silvopasture Figure 9. Growth trends pre- and post-conversion show enhanced productivity in the silvopasture stand as compared to the intact forest, likely due to release from competition. Future Directions. Ongoing research will determine how forest-to-agriculture conversion affects supporting ecosystem services such as soil nutrient cycling as well as regulating services such as soil carbon sequestration. Figure 3. Second growth forest at the ODRF was either cleared for open pasture (top panels) or thinned for silvopasture (bottom panels). Cleared and thinned areas were seeded with perennial grasses. Figure 10. Soil cores will be used to understand changes in soil quality.