Atul Jain University of Illinois, Urbana, IL 61801, USA

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Brian O Neill, NCAR 2010 LCLUC Spring Science Team Meeting Bethesda, MD April 20-22, 2010 Land-Use Change and Associated Changes in Biogeochemical and Biophysical Processes in Monsoon Asian Region (MAR) Atul Jain University of Illinois, Urbana, IL 61801, USA Email: jain1@uiuc.edu Team Members Ramakrishna Nemani, NASA Ames David Skole, Michigan State University

Land Cover Change in MAR 1765 2005 Less primary land, more secondary land, more cropland and pastureland Land use alters : Atmospheric CO 2, N cycle, albedo, runoff, soil water holding capacity, dust Biome Types Tropical Evergreen Tropical Deciduous Temperate Evergreen Temperate Deciduous Boreal Forest Savanna Grassland Shrubland Tundra Desert Polar Desert Cropland Pastureland Sec. Tropical Evergreen Sec. Tropical Deciduous Sec. Temperate Evergreen Sec. Temperate Deciduous Sec. Boreal Forest Jain and Yang (2005, GBC); Jain et al. (2009, GBC); Yang et al. (2009, GBC); Yang et al. (2010, Biogeoscience)

Terrestrial Ecosystems, Land Use Changes and Carbon Socio-Economic Model (PET) Dynamics ISAM Model The Terrestrial Observation and Prediction System (TOPS) population GDP Satellite Measurements

Satellite Measurements

Landset Satellite Data 1990 & 2000 2000 Area change (%) from 1990 Courtesy: David Skole (MSU)

Forest Area Change Based on MODIS Data (2000-2005) Courtesy: Matt Hansen (South Dakota State University )

Land Use and Land Cover of India Year 2000 Sensor: IRS 1D -WiFS Resolution: 180 m Year 2007-2008 Sensor: IRS P6 AWiFS Resolution: 56 m Courtesy: P. S. Roy (IRS )

Year 2007-2008 Sensor: IRS P6 AWiFS Year 2000 Sensor: IRS 1D -WiFS

Biophysical Products - LAI Application of AVHRR and MODIS Data Resolution: 8 km Correspond to the region covering parts of Rajasthan and Madhya Pradesh, where there has been significant changes in LAI. Percent change in mean peak annual LAI between decade 1 (1981-1990) and decade 2 (1995-2006) Courtesy: R. Nemani & S. Ganguly (NASA Ames )

LAI Derived from Landsat Global Land Survey 2005 (GLS2005) Two scenes (path-147,row-44 & path-146,row-44) correspond to the region shown in previous Slide. (courtesy: USGS Landsat Global Visualization Viewer)

LAI Derived from the GLS2005 Scenes are performed using Landset Ecosystem Disturbance Adaptive Processes System (LEDAPS) for radiometric calibration Landsat ID Path: 146 Row: 44 Acquisition Date: 6 th Oct, 2005 Landsat ID Path: 147 Row: 44 Acquisition Date: 1 st Nov, 2006

Impact of LCLUC on Biogeochemistry: Carbon and Nitrogen Dynamics & Emissions

LUC, Terrestrial Ecosystems and Environmental Factors CO 2 Climate Land Use Change Terrestrial Ecosystems N Fertilizer, Deposition Biomass Burning Atmospheric Chemistry

Questions? What are the relative contributions of LCLUCs for cropland, pastureland and wood harvest Secondary forests N deposition and fertilizer agriculture management Fire on Biogeochemistry (ecosystems and carbon and nitrogen dynamics) Biophysical Processes (LH, SH, Albedo) in and South and South East Asia (SSEA)? What are their synergistic effects?

Land Use Changes due to Different Activities (10 9 m 2 ) Crop Land Pasture Land Wood Harvest/Forest Fires Total Sources: Hurtt et al. (2006), Ramanlutty and Foley (1999), FAO (2008), MODIS Satellite

Secondary Forest Area from Cropland, Pastureland, and Wood Harvest Activities (10 9 m 2 ) Yang et. al. (2010, Biogeosciences)

ISAM Land-Surface Model Carbon and Nitrogen Cycling Jain and Yang (2005, GBC) Jain et al. (2005, GRL) Jain et al. (2006, JGR) Jain et al. (2009, GBC) Yang et al (2009, GBC) Yang et al.(2010, Biogeoscience) Calculate fluxes of carbon, nitrogen, energy, water, and the dynamical processes that alter these fluxes 18 Biome types 0.5 x 0.5 degree resolution 30 minutes temporal scale Season-to-interannual variability (penology)

ISAM Land-Surface Model ENERGY HYDROLOGY

Land Surface Heterogeneity in the ISAM Sub-grid land cover and plant functional types Vegetated: Primary & Secondary Forests, other biomes Agriculture: Crop, Pasture Glacier Lakes Mountains Urban 0.5 deg Longitude (~50 km) 0.5 deg Latitude (~50 km) ISAM represents a model grid cell as a mix of different land cover types.

Use of FLUXNET and Other Ground- Based Data in the ISAM Land Surface Model Development The Indian Institute of Remote Sensing (IIRS) has undertaken a National Carbon Project (NCP) to establish 6 carbon flux measurement towers using eddy covariance techniques: (1) Haldwani (mixed forest plantation) (2) Pauri (oak forest) (3) Barkot (sal forest) in Uttarakhand (4) Betul (teak forest) in Madhya Pradesh (5) Dandeli (tea plantation) and

Model Evaluation Using Satellite Data ANNUAL GPP Averaged for 2000-2006 MODIS vs. ISAM

1990s Net Terrestrial C Flux due to LUCs (gc/m 2 ) SSEA forests were releasing more C than absorbing Yang et. al. (2010, Biogeosciences)

Estimated Net Exchange of C (gc/m 2 /yr) for the 1990s in Secondary Forests Carbon stocks in forests are increasing in recent years due to reforestation and afforestation In some regions accumulation of carbon is reduced where nitrogen is a limiting nutrient or enhanced if the additional N is deposited in the forest regrowing regions Positive values represent net C release to the atmosphere and negative values represent net C storage in terrestrial biosphere Yang et. al. (2010, Biogeosciences)

The Impact of N Deposition and Fertilizer CO 2 & N Deposition Effect C Plant uptake, N2O emissions and Leaching N Fertilizer Application

Nitrogen Deposition - Fossil Fuel Burning 1900 2000 Galloway et al. (2004)

1990s N Deposition Effect on Carbon Uptake (gc/m 2 ) Without LUCs With LUCs N deposition leads to additional terrestrial carbon sink Yang et. al. (2010, Biogeosciences)

1990s N Deposition Effect on N2O Emissions and Leaching N2O Emissions (Kg N/ha) Leaching (gc/m2) Yang et. al. (2010, Biogeosciences)

Linking Socio-Economic and Biophysical Systems PET (Population-Economic-Technology) is a socio-economic dynamic system the principle economic activities related to agriculture and raising livestock, forest sector, management practices such as fertilizer use. Terrestrial ecosystem component of Integrated Science Assessment Model (ISAM) the biophysical potential of land for production, across and within regions

PET-ISAM Modeling Framework PET Population Households Terrestrial Ecosystems ISAM Supply of Land LGP at Grid Level Labor, Land, Capital Food and other goods LU Emissions CO2 and Climate Producers Energy Emissions Ocean Sea ice, Atmosphere

Length of Growing Period - Year 2000

ISAM/PET Agriculture Land Area Based on IPCC A2 Scenario (in 2050) Courtesy: Brian O Neill (NCAR)

ISAM/PET Primary Forest Area Based on IPCC A2 Scenario (in 2050) Courtesy: Brian O Neill (NCAR)

ISAM/PET Secondary Forest Area Based on IPCC A2 Scenario (2050) Courtesy: Brian O Neill (NCAR)

Thank you..

1990s Average Yearly Nitrogen Fertilizer Application (tons) International Fertilizer Industry Association (2005)

Nitrogen Fertilizer Effect on 1990s N2O Emissions and Leaching N2O Emissions (Kg N/ha) Leaching (gn/m2) Yang et. al. (2010, Biogeosciences)

1990s Contribution of LCLUC to N2O Emissions (KgN/ha/yr)

Impact of Land Cover and Land Use Changes on Biophysical Processes: Energy and Hydrology Fluxes Experiments Performed for the Period 1979-2004

Land Use Change Effect Latent Heat (W/m 2 ) 0.4 0.2 0.0-0.2-0.4-0.6 Ground Leaf Total Latent Heat Abs. Radiation (W/m 2 ) 0.04 0.00-0.04-0.08-0.12 CO2 Absorbed Radiation 1990-1 1991-1 1992-1 1993-1 1994-1 1995-1 1996-1 1997-1 1998-1 1999-1 2000-1 2001-1 2002-1 2003-1 2004-12

Land Use Change Effect Latent Heat (W/m 2 ) 0.4 0.2 0.0-0.2-0.4-0.6 Ground Leaf Total Linear (Total) Latent Heat Abs. Radiation (W/m 2 ) 0.04 0.00-0.04-0.08-0.12 CO2 Absorbed Radiation 1990-1 1991-1 1992-1 1993-1 1994-1 1995-1 1996-1 1997-1 1998-1 1999-1 2000-1 2001-1 2002-1 2003-1 2004-12

LH by Effect Latent Heat (W/m 2 ) Latent Heat (W/m2 ) 0.4 0.2 0.0-0.2-0.4-0.6 0.1 0.1 0.0-0.1-0.1-0.2-0.2-0.3 LUC Ground Leaf Total CO2 Latent Heat (W/m 2 ) 8.0 6.0 4.0 2.0 0.0-2.0-4.0-6.0-8.0 Climate 1990-1 1991-1 1992-1 1993-1 1994-1 1995-1 1996-1 1997-1 1998-1 1999-1 2000-1 2001-1 2002-1 2003-1 2004-12

LH by Effect Latent Heat (W/m 2 ) Latent Heat (W/m2 ) 0.4 0.2 0.0-0.2-0.4-0.6 0.1 0.1 0.0-0.1-0.1-0.2-0.2-0.3 LUC CO2 Ground Leaf Total Linear (Total) Latent Heat (W/m 2 ) 8.0 6.0 4.0 2.0 0.0-2.0-4.0-6.0-8.0 Climate 1990-1 1991-1 1992-1 1993-1 1994-1 1995-1 1996-1 1997-1 1998-1 1999-1 2000-1 2001-1 2002-1 2003-1 2004-12

Implementation of Broad Diversity of Crops in the ISAM

Population-Economy-Technology (PET) Model 9-Region CGE* Model, with Trade EU-27+ Transition Countries USA China Sub-Sah. Africa India Other Devel. Countries Latin America Other Indust. Countries Computable general equilibrium (CGE) model is an economic model that use actual economic data to estimate how an economy might react to changes in policy, technology or other external factors.

Area (Mill ha) 700 600 500 400 300 200 Pasture Forest Agriculture INDIA CHINA REST OF SSEA 100 0 1990 2050 1990 2050 1990 2050

LUC and Biophysical Drivers on Land Latent heat (forests > crops > bare ground) Albedo (bare ground > crops > forests) In tropics, LH effects dominate over albedo effects. Conversion of forests to crops in tropics increases albedo (cooling effect), but this is overwhelmed by large decrease in latent heat flux to atmosphere (warming effect), resulting in a net warming in tropics.

The Dynamics of Irrigation The dynamics of irrigation in tropics can alter the relative importance of these biophysical drivers. The LH flux over well-watered crops may be more than that from forests. Globally, crop irrigation comprises of 70% of all human water withdrawals. India leads the world in total irrigated land where irrigation withdrawals represent 80-90% of all water use. Pre-monsoon season NDVI anomalies have increased in the Indian subcontinent. Increases are strongly correlated with increases in irrigated area, not preceding rainfall

LUC and Biophysical Drivers on Land Surface roughness (forests > crops > bare ground) Stronger mixing due to greater surface roughness of forests (over crops or bare ground, increasing supply of moisture from surface and the microscale circulations

Effects of Energy, Hydrology, Irrigation and vegetation activity on Indian Summer Monsoon Variability Vegetation cover, surface roughness, and stomatal resistance all imparted to the development of convection and monsoon rainfall activities Vegetation and soil moisture introduce differential heating, which enhances frontal activity Stronger Asian summer monsoon associated with lower surface albedo (i.e., forests), greater soil moisture, less snow cover, and greater land-sea thermal contrast. Irrigation increases LH over land, which decreases sealand temperature contrast, which can thereby decrease summer monsoon. Indian monsoon was significantly weakened by increase in surface albedo (cropland) and by a reduction in surface roughness

LUC activities can be grouped into three main categories: agriculture (including crop growth and raising livestock) forestry (for the production of wood products such as timber or paper), and Production of biomass as an energy source (either commercial biomass or biomass fuels at the household level). A last category the management of land primarily as a carbon sink LCLUC in MAR Tropical Forests planetary savior promote avoided deforestation, reforestation, or afforestation Biofuel plantations to lower albedo and reduce atmospheric CO 2

Environmental Factors and Processes Environmental Factors (LUC, Climate etc.) Terrestrial Ecosystems Biogeochemistry Carbon and Nitrogen Fluxes Biophysics Energy and Water Fluxes Climate Change

LUC and C and N Dynamics Instantaneous C and N release after deforestation After abandonment C stored in secondary forest (SF) Stored C in SF could be enhanced due to CO2 fertilization or Wood Harvest or Wood Harvest C accumulation in SF could be constrained due to nutrient (e.g., N) limitation N Deposition can enhanced the C accumulation After LUC soil C and N are increased for a short while

Model Evaluation Using Ground-Based GPP Measurements LH

Revised PET Model Sectors

Data Challenge GTAP data used to calibrate PET model IPCC scenarios used as PET model input Land Use ISAM data from Satellite data Illustrative case, applies to data for cropland, forest, and pasture by region and AEZ. past future Year