Climate impact from peat utilisation in Sweden
The climate impact from the useof peat for energy production in Sweden hasbeen evaluated in terms of contribution toatmospheric radiative forcing. This wasdone by attempting to answer the question`What will be the climate impact if onewould use 1 m^sup 2^ of mire for peatextraction during 20 years?&...
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description | The climate impact from the useof peat for energy production in Sweden hasbeen evaluated in terms of contribution toatmospheric radiative forcing. This wasdone by attempting to answer the question`What will be the climate impact if onewould use 1 m^sup 2^ of mire for peatextraction during 20 years?'. Two differentmethods of after-treatment were studied:afforestation and restoration of wetland.The climate impact from a peatland -wetland scenario and a peatland -forestation - bioenergy scenario wascompared to the climate impact from coal,natural gas and forest residues.Sensitivity analyses were performed toevaluate which parameters that areimportant to take into consideration inorder to minimize the climate impact frompeat utilisation. In a `multiple generationscenario' we investigate the climate impactif 1 Mega Joule (MJ) of energy is produced every yearfor 300 years from peat compared to otherenergy sources.The main conclusions from the study are:*The accumulated radiative forcing from the peatland - forestation - bioenergy scenario over a long time perspective (300 years) is estimated to be 1.35 mJ/m^sup 2^/m^sup 2^ extraction area assuming a medium-high forest growth rate and medium original methane emissions from the virgin mire. This is below the corresponding values for coal 3.13 mJ/ m^sup 2^/ m^sup 2^ extraction area and natural gas, 1.71 mJ/ m^sup 2^/ m^sup 2^ extraction area, but higher than the value for forest residues, 0.42 mJ/ m^sup 2^/ m^sup 2^ extraction area. A `best-best-case' scenario, i.e. with high forest growth rate combined with high `avoided' methane (CH^sub 4^) emissions, will generate accumulated radiative forcing comparable to using forest residues for energy production. A `worst-worst-case' scenario, with low growth rate and low `avoided' CH^sub 4^ emissions, will generate radiative forcing somewhere in between natural gas and coal.*The accumulated radiative forcing from the peatland - wetland scenario over a 300-year perspective is estimated to be 0.73 -1.80 mJ/ m^sup 2^/ m^sup 2^ extraction area depending on the assumed carbon (C) uptake rates for the wetland and assuming a medium-high methane emissions from a restored wetland. The corresponding values for coal is 1.88 mJ/ m^sup 2^/ m^sup 2^ extraction area, for natural gas 1.06 mJ/ m^sup 2^/ m^sup 2^ extraction area and for forest residues 0.10 mJ/ m^sup 2^/ m^sup 2^ extraction area. A `best-best-case' scenario (i.e. with high carbon dioxide CO^sub 2^-uptake combined with high |
doi_str_mv | 10.1023/B:MITI.0000009894.59772.af |
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This wasdone by attempting to answer the question`What will be the climate impact if onewould use 1 m^sup 2^ of mire for peatextraction during 20 years?'. Two differentmethods of after-treatment were studied:afforestation and restoration of wetland.The climate impact from a peatland -wetland scenario and a peatland -forestation - bioenergy scenario wascompared to the climate impact from coal,natural gas and forest residues.Sensitivity analyses were performed toevaluate which parameters that areimportant to take into consideration inorder to minimize the climate impact frompeat utilisation. In a `multiple generationscenario' we investigate the climate impactif 1 Mega Joule (MJ) of energy is produced every yearfor 300 years from peat compared to otherenergy sources.The main conclusions from the study are:*The accumulated radiative forcing from the peatland - forestation - bioenergy scenario over a long time perspective (300 years) is estimated to be 1.35 mJ/m^sup 2^/m^sup 2^ extraction area assuming a medium-high forest growth rate and medium original methane emissions from the virgin mire. This is below the corresponding values for coal 3.13 mJ/ m^sup 2^/ m^sup 2^ extraction area and natural gas, 1.71 mJ/ m^sup 2^/ m^sup 2^ extraction area, but higher than the value for forest residues, 0.42 mJ/ m^sup 2^/ m^sup 2^ extraction area. A `best-best-case' scenario, i.e. with high forest growth rate combined with high `avoided' methane (CH^sub 4^) emissions, will generate accumulated radiative forcing comparable to using forest residues for energy production. A `worst-worst-case' scenario, with low growth rate and low `avoided' CH^sub 4^ emissions, will generate radiative forcing somewhere in between natural gas and coal.*The accumulated radiative forcing from the peatland - wetland scenario over a 300-year perspective is estimated to be 0.73 -1.80 mJ/ m^sup 2^/ m^sup 2^ extraction area depending on the assumed carbon (C) uptake rates for the wetland and assuming a medium-high methane emissions from a restored wetland. The corresponding values for coal is 1.88 mJ/ m^sup 2^/ m^sup 2^ extraction area, for natural gas 1.06 mJ/ m^sup 2^/ m^sup 2^ extraction area and for forest residues 0.10 mJ/ m^sup 2^/ m^sup 2^ extraction area. A `best-best-case' scenario (i.e. with high carbon dioxide CO^sub 2^-uptake combined with high `avoided' CH^sub 4^ emissions and low methane emissions from the restored wetland) will generate accumulated radiative forcing that decreases and reaches zero after 240 years. A `worst-worst-case' (i.e. with low CO^sub 2^-uptake combined with low `avoided' CH^sub 4^ emissions and high methane emissions from the restored wetland) will generate radiative forcing higher than coal over the entire time period.*The accumulated radiative forcing in the `multiple generations' - scenarios over a 300-year perspective producing 1 MJ/year is estimated to be 0.089 mJ/ m^sup 2^ for the scenario `Peat forestation - bioenergy', 0.097 mJ/ m^sup 2^ for the scenario `Peat wetland with high CO^sub 2^-uptake' and 0.140 mJ/ m^sup 2^ for the scenario `Peat wetland with low CO^sub 2^-uptake'. Corresponding values for coal is 0.160 mJ/ m^sup 2^, for natural gas 0.083 mJ/ m^sup 2^ and for forest residues 0.015 mJ/ m^sup 2^. Using a longer time perspective than 300 years will result in lower accumulated radiative forcing from the scenario `Peat wetland with high CO^sub 2^-uptake'. This is due to the negative instantaneous forcing that occurs after 200 years for each added generation.*It is important to consider CH^sub 4^ emissions from the virgin mire when choosing mires for utilization. Low original methane emissions give significantly higher total climate impact than high original emissions do.*Afforestation on areas previously used for peat extraction should be performed in a way that gives a high forest growth rate, both for the extraction area and the surrounding area. A high forest growth rate gives lower climate impact than a low forest growth rate.*There are great uncertainties related to the data used for emissions and uptake of greenhouse gases in restored wetlands. The mechanisms affecting these emissions and uptake should be studied further.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 1381-2386</identifier><identifier>EISSN: 1573-1596</identifier><identifier>DOI: 10.1023/B:MITI.0000009894.59772.af</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Afforestation ; Carbon dioxide ; Coal ; Emissions ; Environmental restoration ; Forest residues ; Gases ; Greenhouse gases ; Growth rate ; Methane ; Natural gas ; Peat ; Peatlands ; Sensitivity analysis ; Wetlands</subject><ispartof>Mitigation and adaptation strategies for global change, 2004, Vol.9 (1), p.37-76</ispartof><rights>Kluwer Academic Publishers 2004</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c348f-59a595dc73b015e04dd8bfaf5ff7f7149450dee5720fd3d2eaafc508e9a771553</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,4024,27923,27924,27925</link.rule.ids></links><search><creatorcontrib>Zetterberg, L.</creatorcontrib><creatorcontrib>Uppenberg, S.</creatorcontrib><creatorcontrib>Åhman, M.</creatorcontrib><title>Climate impact from peat utilisation in Sweden</title><title>Mitigation and adaptation strategies for global change</title><description>The climate impact from the useof peat for energy production in Sweden hasbeen evaluated in terms of contribution toatmospheric radiative forcing. This wasdone by attempting to answer the question`What will be the climate impact if onewould use 1 m^sup 2^ of mire for peatextraction during 20 years?'. Two differentmethods of after-treatment were studied:afforestation and restoration of wetland.The climate impact from a peatland -wetland scenario and a peatland -forestation - bioenergy scenario wascompared to the climate impact from coal,natural gas and forest residues.Sensitivity analyses were performed toevaluate which parameters that areimportant to take into consideration inorder to minimize the climate impact frompeat utilisation. In a `multiple generationscenario' we investigate the climate impactif 1 Mega Joule (MJ) of energy is produced every yearfor 300 years from peat compared to otherenergy sources.The main conclusions from the study are:*The accumulated radiative forcing from the peatland - forestation - bioenergy scenario over a long time perspective (300 years) is estimated to be 1.35 mJ/m^sup 2^/m^sup 2^ extraction area assuming a medium-high forest growth rate and medium original methane emissions from the virgin mire. This is below the corresponding values for coal 3.13 mJ/ m^sup 2^/ m^sup 2^ extraction area and natural gas, 1.71 mJ/ m^sup 2^/ m^sup 2^ extraction area, but higher than the value for forest residues, 0.42 mJ/ m^sup 2^/ m^sup 2^ extraction area. A `best-best-case' scenario, i.e. with high forest growth rate combined with high `avoided' methane (CH^sub 4^) emissions, will generate accumulated radiative forcing comparable to using forest residues for energy production. A `worst-worst-case' scenario, with low growth rate and low `avoided' CH^sub 4^ emissions, will generate radiative forcing somewhere in between natural gas and coal.*The accumulated radiative forcing from the peatland - wetland scenario over a 300-year perspective is estimated to be 0.73 -1.80 mJ/ m^sup 2^/ m^sup 2^ extraction area depending on the assumed carbon (C) uptake rates for the wetland and assuming a medium-high methane emissions from a restored wetland. The corresponding values for coal is 1.88 mJ/ m^sup 2^/ m^sup 2^ extraction area, for natural gas 1.06 mJ/ m^sup 2^/ m^sup 2^ extraction area and for forest residues 0.10 mJ/ m^sup 2^/ m^sup 2^ extraction area. A `best-best-case' scenario (i.e. with high carbon dioxide CO^sub 2^-uptake combined with high `avoided' CH^sub 4^ emissions and low methane emissions from the restored wetland) will generate accumulated radiative forcing that decreases and reaches zero after 240 years. A `worst-worst-case' (i.e. with low CO^sub 2^-uptake combined with low `avoided' CH^sub 4^ emissions and high methane emissions from the restored wetland) will generate radiative forcing higher than coal over the entire time period.*The accumulated radiative forcing in the `multiple generations' - scenarios over a 300-year perspective producing 1 MJ/year is estimated to be 0.089 mJ/ m^sup 2^ for the scenario `Peat forestation - bioenergy', 0.097 mJ/ m^sup 2^ for the scenario `Peat wetland with high CO^sub 2^-uptake' and 0.140 mJ/ m^sup 2^ for the scenario `Peat wetland with low CO^sub 2^-uptake'. Corresponding values for coal is 0.160 mJ/ m^sup 2^, for natural gas 0.083 mJ/ m^sup 2^ and for forest residues 0.015 mJ/ m^sup 2^. Using a longer time perspective than 300 years will result in lower accumulated radiative forcing from the scenario `Peat wetland with high CO^sub 2^-uptake'. This is due to the negative instantaneous forcing that occurs after 200 years for each added generation.*It is important to consider CH^sub 4^ emissions from the virgin mire when choosing mires for utilization. Low original methane emissions give significantly higher total climate impact than high original emissions do.*Afforestation on areas previously used for peat extraction should be performed in a way that gives a high forest growth rate, both for the extraction area and the surrounding area. A high forest growth rate gives lower climate impact than a low forest growth rate.*There are great uncertainties related to the data used for emissions and uptake of greenhouse gases in restored wetlands. The mechanisms affecting these emissions and uptake should be studied further.[PUBLICATION ABSTRACT]</description><subject>Afforestation</subject><subject>Carbon dioxide</subject><subject>Coal</subject><subject>Emissions</subject><subject>Environmental restoration</subject><subject>Forest residues</subject><subject>Gases</subject><subject>Greenhouse gases</subject><subject>Growth rate</subject><subject>Methane</subject><subject>Natural gas</subject><subject>Peat</subject><subject>Peatlands</subject><subject>Sensitivity analysis</subject><subject>Wetlands</subject><issn>1381-2386</issn><issn>1573-1596</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqFkEtLAzEUhYMoWKv_YejC3Yy5eUyS7mzxUai4sK5DOkkgZV5OZhD_vTOtILjxbs5dfBw4H0ILwBlgQu9Wy5fNbpPh4ympWMaVECQz_gzNgAuaAlf5-fhTCSmhMr9EVzEeRpoChxnK1mWoTO-SULWm6BPfNVXSOtMnQx_KEE0fmjoJdfL26ayrr9GFN2V0Nz85R--PD7v1c7p9fdqs77dpQZn0KVeGK24LQfcYuMPMWrn3xnPvhRfAFOPYOscFwd5SS5wxvuBYOmWEAM7pHN2eetuu-Rhc7HUVYuHK0tSuGaKGHAQQlf8PslwqrMgILv6Ah2bo6nGEFizHhICY2pYnqOiaGDvndduNerovDVhPwvVKT8L1r3B9FK6Np99mT3Pv</recordid><startdate>2004</startdate><enddate>2004</enddate><creator>Zetterberg, L.</creator><creator>Uppenberg, S.</creator><creator>Åhman, M.</creator><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7UA</scope><scope>7WY</scope><scope>7WZ</scope><scope>7XB</scope><scope>87Z</scope><scope>88I</scope><scope>8FK</scope><scope>8FL</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BEZIV</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FRNLG</scope><scope>F~G</scope><scope>GNUQQ</scope><scope>H97</scope><scope>HCIFZ</scope><scope>K60</scope><scope>K6~</scope><scope>L.-</scope><scope>L.G</scope><scope>M0C</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQBIZ</scope><scope>PQBZA</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>7TG</scope><scope>7TV</scope><scope>7U6</scope><scope>KL.</scope></search><sort><creationdate>2004</creationdate><title>Climate impact from peat utilisation in Sweden</title><author>Zetterberg, L. ; Uppenberg, S. ; Åhman, M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c348f-59a595dc73b015e04dd8bfaf5ff7f7149450dee5720fd3d2eaafc508e9a771553</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Afforestation</topic><topic>Carbon dioxide</topic><topic>Coal</topic><topic>Emissions</topic><topic>Environmental restoration</topic><topic>Forest residues</topic><topic>Gases</topic><topic>Greenhouse gases</topic><topic>Growth rate</topic><topic>Methane</topic><topic>Natural gas</topic><topic>Peat</topic><topic>Peatlands</topic><topic>Sensitivity analysis</topic><topic>Wetlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zetterberg, L.</creatorcontrib><creatorcontrib>Uppenberg, S.</creatorcontrib><creatorcontrib>Åhman, M.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ABI/INFORM Collection</collection><collection>ABI/INFORM Global (PDF only)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>ABI/INFORM Global (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ABI/INFORM Collection (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Business Premium Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Business Premium Collection (Alumni)</collection><collection>ABI/INFORM Global (Corporate)</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Business Collection (Alumni Edition)</collection><collection>ProQuest Business Collection</collection><collection>ABI/INFORM Professional Advanced</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ABI/INFORM Global</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>One Business (ProQuest)</collection><collection>ProQuest One Business (Alumni)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Pollution Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Mitigation and adaptation strategies for global change</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zetterberg, L.</au><au>Uppenberg, S.</au><au>Åhman, M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Climate impact from peat utilisation in Sweden</atitle><jtitle>Mitigation and adaptation strategies for global change</jtitle><date>2004</date><risdate>2004</risdate><volume>9</volume><issue>1</issue><spage>37</spage><epage>76</epage><pages>37-76</pages><issn>1381-2386</issn><eissn>1573-1596</eissn><abstract>The climate impact from the useof peat for energy production in Sweden hasbeen evaluated in terms of contribution toatmospheric radiative forcing. This wasdone by attempting to answer the question`What will be the climate impact if onewould use 1 m^sup 2^ of mire for peatextraction during 20 years?'. Two differentmethods of after-treatment were studied:afforestation and restoration of wetland.The climate impact from a peatland -wetland scenario and a peatland -forestation - bioenergy scenario wascompared to the climate impact from coal,natural gas and forest residues.Sensitivity analyses were performed toevaluate which parameters that areimportant to take into consideration inorder to minimize the climate impact frompeat utilisation. In a `multiple generationscenario' we investigate the climate impactif 1 Mega Joule (MJ) of energy is produced every yearfor 300 years from peat compared to otherenergy sources.The main conclusions from the study are:*The accumulated radiative forcing from the peatland - forestation - bioenergy scenario over a long time perspective (300 years) is estimated to be 1.35 mJ/m^sup 2^/m^sup 2^ extraction area assuming a medium-high forest growth rate and medium original methane emissions from the virgin mire. This is below the corresponding values for coal 3.13 mJ/ m^sup 2^/ m^sup 2^ extraction area and natural gas, 1.71 mJ/ m^sup 2^/ m^sup 2^ extraction area, but higher than the value for forest residues, 0.42 mJ/ m^sup 2^/ m^sup 2^ extraction area. A `best-best-case' scenario, i.e. with high forest growth rate combined with high `avoided' methane (CH^sub 4^) emissions, will generate accumulated radiative forcing comparable to using forest residues for energy production. A `worst-worst-case' scenario, with low growth rate and low `avoided' CH^sub 4^ emissions, will generate radiative forcing somewhere in between natural gas and coal.*The accumulated radiative forcing from the peatland - wetland scenario over a 300-year perspective is estimated to be 0.73 -1.80 mJ/ m^sup 2^/ m^sup 2^ extraction area depending on the assumed carbon (C) uptake rates for the wetland and assuming a medium-high methane emissions from a restored wetland. The corresponding values for coal is 1.88 mJ/ m^sup 2^/ m^sup 2^ extraction area, for natural gas 1.06 mJ/ m^sup 2^/ m^sup 2^ extraction area and for forest residues 0.10 mJ/ m^sup 2^/ m^sup 2^ extraction area. A `best-best-case' scenario (i.e. with high carbon dioxide CO^sub 2^-uptake combined with high `avoided' CH^sub 4^ emissions and low methane emissions from the restored wetland) will generate accumulated radiative forcing that decreases and reaches zero after 240 years. A `worst-worst-case' (i.e. with low CO^sub 2^-uptake combined with low `avoided' CH^sub 4^ emissions and high methane emissions from the restored wetland) will generate radiative forcing higher than coal over the entire time period.*The accumulated radiative forcing in the `multiple generations' - scenarios over a 300-year perspective producing 1 MJ/year is estimated to be 0.089 mJ/ m^sup 2^ for the scenario `Peat forestation - bioenergy', 0.097 mJ/ m^sup 2^ for the scenario `Peat wetland with high CO^sub 2^-uptake' and 0.140 mJ/ m^sup 2^ for the scenario `Peat wetland with low CO^sub 2^-uptake'. Corresponding values for coal is 0.160 mJ/ m^sup 2^, for natural gas 0.083 mJ/ m^sup 2^ and for forest residues 0.015 mJ/ m^sup 2^. Using a longer time perspective than 300 years will result in lower accumulated radiative forcing from the scenario `Peat wetland with high CO^sub 2^-uptake'. This is due to the negative instantaneous forcing that occurs after 200 years for each added generation.*It is important to consider CH^sub 4^ emissions from the virgin mire when choosing mires for utilization. Low original methane emissions give significantly higher total climate impact than high original emissions do.*Afforestation on areas previously used for peat extraction should be performed in a way that gives a high forest growth rate, both for the extraction area and the surrounding area. A high forest growth rate gives lower climate impact than a low forest growth rate.*There are great uncertainties related to the data used for emissions and uptake of greenhouse gases in restored wetlands. The mechanisms affecting these emissions and uptake should be studied further.[PUBLICATION ABSTRACT]</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1023/B:MITI.0000009894.59772.af</doi><tpages>40</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Afforestation Carbon dioxide Coal Emissions Environmental restoration Forest residues Gases Greenhouse gases Growth rate Methane Natural gas Peat Peatlands Sensitivity analysis Wetlands |
title | Climate impact from peat utilisation in Sweden |
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