Tropical Peatlands and Global Carbon Budget Daniel Murdiyarso Center for International Forestry Research (CIFOR) I Nyoman Suryadiputra Wetland International – Indonesia Program (WI-IP) Regional Carbon Budgets Workshop: From.
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Tropical Peatlands and Global Carbon Budget Daniel Murdiyarso Center for International Forestry Research (CIFOR) I Nyoman Suryadiputra Wetland International – Indonesia Program (WI-IP) Regional Carbon Budgets Workshop: From Methodologies to Quantification Beijing, 15-18 November 2004 Outline Basic terminology and approaches Global significance of petlands Degrading peatlands Role of fires Methodologies and quantification Static vs dynamic Towards modeling/predictive capabilities Identified gaps Trends Conclusions 2 Basic terminology Carbon stock (mass/area) Carbon pool (mass) Carbon flux Carbon emissions (mass/area/time) C-budget: distribution of C in the compartments and flux rate between them (units??) Residual: how large? 3 Tropical peatlands Globally the area of tropical peat is ca. 40 Mha 50% in Indonesia Formed over a period of 10,000 years Depth ranges 1-12 m Store 5,800 t C/ha (> 10 x tropical forests) 4 Decreasing area (Mha) 1990 2002 35-40 25-30 Sumatra 7.2 6.5 Kalimantan 8.4 ? Indonesia 20 17 Southeast Asia 5 Peatlands and C-budgets Annual GHGs released due to peatland drainage or degradation 2-20 tC/ha (Maltby and Immirzy, 1993) Carbon stored in tropical peatlands 1700-2880 t C/ha (GACGC, 2000) Forest fires in Indonesia during 1997 and 1998 involved 2.12 Mha of peatlands (Tacconi, 2002) The estimated C-loss from peatland fires in 1997 ranged 0.81-2.57 Gt (Page et al., 2002). 6 Disturbance regimes and terrestrial C-budget CO2 Plant respiration GPP Soil and litter respiration Shortterm carbon uptake NPP 60 Gt/yr Mediumterm carbon storage NEP 10 Gt/yr Disturbance Long-term carbon storage NBP 1-2 Gt/yr 7 Source: IGBP Terrestrial Carbon Working Group (1998) Fire & Haze from Sumatra and Kalimantan Sep 11, 1997 8 Can hotspots tell anything? Source: Murdiyarso et al. (2002) 9 Estimated C-loss 7 Mt 10 But fire scars may not tell everything 1989 1997 11 Mega rice project – Central Kalimantan 12 LUC is both affecting and affected by climate change 1980 1982 1984 1986 1988 1990 1992 1994 1996 1998 2000 2002 El-Nino events Fire event 1982 1987 1991 1997 Area burnt (Mha) C-loss (Gt) 3.6 0.1 0.5 11.6 (2.1) Note: Global CO2 growth = 1.5 ppmv/yr (IPCC, 1995) 0.45 0.01 0.06 1.45 (0.47) 13 From methodologies to quantification? C- loss from peatland degradation (field data) Area of change – remote sensing Bulk density – lab analysis C-content – lab analysis Depth of peat layer – auger bor Emissions from volatile biomass burning Future development Leaching of dissolved elements (organic carbon) Towards modeling exercises 14 Estimating C-loss from peatlands n C-loss = (A x B x C x D) i=1 Bulk density (gcm-3) Decomposition level i C - organic (%) Range Mean Range Mean Fibric 0.10 – 0.12 0.10 - 53 Hemic 0.13 – 0.29 0.17 39 – 52 48 Sapric 0.25 – 0.37 0.28 29 – 54 45 Peaty soils* 0.22 – 0.69 0.34 29 – 40 35 *) Occupy relatively thin layer of less than 50 cm 15 0o Estimated C-loss 3.5 Gt 0o 16 Change of stocks Land-use trajectory and fallow periods High secondary forests Low secondary forests Primary forests Shrubs Bare Imperata Crop-based systems | | 5 10 Medium cycle Tree-based systems | 20 Long cycle 30 | Logged-over forests | 40 Years (Protected areas) Short cycle 17 C-stocks in changing land-use 250 3 200 150 2 100 50 1 0 18 CENTURY: Forest - Cassava - Imperata C Stock 60 SOMT NPP 400 40 200 20 0 410 SOMT (Mg C ha-1) NPP (Mg C ha-1 y -1) Carbon stock (Mg C ha-1) 600 0 420 430 Years 440 450 19 CENTURY: Forest - Rice/Bush fallow Carbon Stock (Mg C/ha) 600 60 400 40 200 20 0 410 SOMT (Mg C/ha) NPP (Mg C/ha/y) C Stock SOMT NPP 0 420 430 Years 440 450 20 Emissions from biomass burning - 1997 Emission (Mt) CO2 85-316 CO 7-52 NOx 0.2-1.5 Particulate matter Source: Levine (1998) 4-16 21 Burning and nutrient losses Nutrient losses due to volatilisation during the burning of residual biomass are generally higher than the losses by leaching (Bruijnzeel, 1998) This is not only for N, which comprise of more than 90 percent of the biomass but often also for mineral nutrients Reduction of burning in land clearing practices will reduce atmospheric losses Burning also increases leaching losses compared to non-burning practices (Malmer et al., 1994) 22 Trends – peatland development Needs of agricultural land expansions Growing oil-palm and pulpwood industries People in-migration into the area Unclear tenure systems (conflicts remain) 23 Trends – fire will be used Fire is the cheapest method for land clearing Fire can add ash that temporarily improve soil conditions Pests and weeds control The economic value of the biomass ‘waste’ is so low Smallholders’ wood pricing discourages producers 24 Economic values of peatlands goods* No Product Annual Quantity 1 Construction timber 2,850 m3 100,000 0.10 2 Fuel woods 4,400 m3 119,000 0.12 3 Mixed timber 375 m3 67 4 Wooden roofing 52,000 bundles 46,000 5 Bamboo 15,000 pieces 517 6 Rattan 164,273 pieces 7,300 7 Resin 223 kg 17 0 8 Medicinal plant 10,345 items 1,750 0 9 Deer 9,700 0.01 10 Pig 11 Singing birds 12 Fish Economic value ($) ** 168 Relative contribution 0 0.05 0 0.01 71 625 0 345 137 0 2,850,000 kg Total *) Based on survey conducted in East Kalimantan from 100 respondents. **) Converted using an exchange rate of US$ 1 = Rp 8,500 Source: Wetlands International, 2004 671,260 0.70 956,373 25 Fresh impetus …… 23 Jul 2004 – Indonesian Parliament approved the Law on the Kyoto Protocol ratification 23 Sep 2004 – Germany geared towards the inclusion of avoiding deforestation (in addition to A/R) in the CDM in the 2nd commitment period 23 Oct 2004 – Duma voted in favor of Russia’s accession to the Kyoto Protocol ASEAN Agreement on Fires and Haze Transboundary Pollution ASEAN Peatlands Management Initiative (APMI) 26 Future research questions What are our fundamental understanding of peatland ecosystems vulnerability to climate change? How can the understandings be disseminated to influence public policy-making? Are there scientifically sound adaptive management options for the ecosystems to mitigate climate change? How accessible the markets are? Multilateral: e.g GEF/GCF to pay extra for carbon removed in biodiversity/watershed conservation projects Bilateral: ODA, DNS Unilateral: national and local markets 27 Conclusions Peatland is an important terrestrial C-stocks under increasing human pressure Peat forest clearing followed by drainage makes the landscape more susceptible to fires Decreasing peatlands area is associated with decreasing depth and carbon content C and nutrients are mainly released into the atmosphere during fire in addition to DOC and nutrient leaching and drainage Modeling C-budgets on tropical peatlands requires the incorporation of human dimensions 28 Acknowledgements We gratefully acknowledge the support of the Canadian International Development Agency (CIDA) 29