Variability of annual CO sub(2) exchange from Dutch grasslands
An intercomparison is made of the Net Ecosystem Exchange of CO sub(2), NEE, for eight Dutch grassland sites: four natural grasslands, two production grasslands and two meteorological stations within a rotational grassland region. At all sites the NEE was determined during at least 10 months per site...
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description | An intercomparison is made of the Net Ecosystem Exchange of CO sub(2), NEE, for eight Dutch grassland sites: four natural grasslands, two production grasslands and two meteorological stations within a rotational grassland region. At all sites the NEE was determined during at least 10 months per site, using the eddy-covariance (EC) technique, but in different years. The NEE does not include any import or export other than CO sub(2). The photosynthesis-light response analysis technique is used along with the respiration-temperature response technique to partition NEE into Gross Primary Production (GPP) and Ecosystem Respiration (R sub(e)) and to obtain the eco-physiological characteristics of the sites at the field scale. Annual sums of NEE, GPP and R sub(e) are then estimated using the fitted response curves with observed radiation and air temperature from a meteorological site in the centre of The Netherlands as drivers. These calculations are carried out for four years (2002-2005). Land use and management histories are not considered. The estimated annual R sub(e) for all individual sites is more or less constant per site and the average for all sites amounts to 1390 plus or minus 30 gC m super(− 2) a super(− 1). The narrow uncertainty band ( plus or minus 2%) reflects the small differences in the mean annual air temperature. The mean annual GPP was estimated to be 1325 g C m super(− 2) a super(− 1), and displays a much higher standard deviation, of plus or minus 110 gC m super(− 2) a super(− 1) (8%), which reflects the relatively large variation in annual solar radiation. The mean annual NEE amounts to -65 plus or minus 85 gC m super(− 2) a super(− 1). From two sites, four-year records of CO sub(2) flux were available and analyzed (2002-2005). Using the weather record of 2005 with optimizations from the other years, the standard deviation of annual GPP was estimated to be 171-206 gC m super(− 2) a super(− 1) (8-14%), of annual R sub(e) 227-247 gC m super(− 2) a super(− 1) (14-16%) and of annual NEE 176-276 gC m super(− 2) a super(− 1). The inter-site standard deviation was higher for GPP and R sub(e), 534 gC m super(− 2) a super(− 1) (37.3%) and 486 gC m super(− 2) a super(− 1) (34.8%), respectively. However, the inter-site standard deviation of NEE was similar to the interannual one, amounting to 207 gC m super(− 2) a super(− 1). Large differences occur due to soil type. The grasslands on organic (peat) soils show a mean net release of CO sub(2) of 220 |
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At all sites the NEE was determined during at least 10 months per site, using the eddy-covariance (EC) technique, but in different years. The NEE does not include any import or export other than CO sub(2). The photosynthesis-light response analysis technique is used along with the respiration-temperature response technique to partition NEE into Gross Primary Production (GPP) and Ecosystem Respiration (R sub(e)) and to obtain the eco-physiological characteristics of the sites at the field scale. Annual sums of NEE, GPP and R sub(e) are then estimated using the fitted response curves with observed radiation and air temperature from a meteorological site in the centre of The Netherlands as drivers. These calculations are carried out for four years (2002-2005). Land use and management histories are not considered. The estimated annual R sub(e) for all individual sites is more or less constant per site and the average for all sites amounts to 1390 plus or minus 30 gC m super(− 2) a super(− 1). The narrow uncertainty band ( plus or minus 2%) reflects the small differences in the mean annual air temperature. The mean annual GPP was estimated to be 1325 g C m super(− 2) a super(− 1), and displays a much higher standard deviation, of plus or minus 110 gC m super(− 2) a super(− 1) (8%), which reflects the relatively large variation in annual solar radiation. The mean annual NEE amounts to -65 plus or minus 85 gC m super(− 2) a super(− 1). From two sites, four-year records of CO sub(2) flux were available and analyzed (2002-2005). Using the weather record of 2005 with optimizations from the other years, the standard deviation of annual GPP was estimated to be 171-206 gC m super(− 2) a super(− 1) (8-14%), of annual R sub(e) 227-247 gC m super(− 2) a super(− 1) (14-16%) and of annual NEE 176-276 gC m super(− 2) a super(− 1). The inter-site standard deviation was higher for GPP and R sub(e), 534 gC m super(− 2) a super(− 1) (37.3%) and 486 gC m super(− 2) a super(− 1) (34.8%), respectively. However, the inter-site standard deviation of NEE was similar to the interannual one, amounting to 207 gC m super(− 2) a super(− 1). Large differences occur due to soil type. The grasslands on organic (peat) soils show a mean net release of CO sub(2) of 220 plus or minus 90 g C m super(− 2) a super(− 1) while the grasslands on mineral (clay and sand) soils show a mean net uptake of CO sub(2) of 90 plus or minus 90 g C m super(− 2) a super(− 1). If a weighing with the fraction of grassland on organic (20%) and mineral soils (80%) is applied, an average NEE of 28 plus or minus 90 g C m super(− 2) a super(− 1) is found. The results from the analysis illustrate the need for regionally specific and spatially explicit CO sub(2) emission estimates from grassland.</description><identifier>ISSN: 1726-4170</identifier><identifier>EISSN: 1726-4189</identifier><language>eng</language><ispartof>Biogeosciences, 2007-10, Vol.4 (5), p.803-816</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,781,785</link.rule.ids></links><search><creatorcontrib>J Jacobs, CM</creatorcontrib><creatorcontrib>G Jacobs, AF</creatorcontrib><creatorcontrib>Bosveld, F C</creatorcontrib><creatorcontrib>Hendriks, D</creatorcontrib><creatorcontrib>Hensen, A</creatorcontrib><creatorcontrib>Kroon, P S</creatorcontrib><creatorcontrib>Moors, E J</creatorcontrib><creatorcontrib>Nol, L</creatorcontrib><creatorcontrib>Schrier-Uijl, A</creatorcontrib><creatorcontrib>Veenendaal, E M</creatorcontrib><title>Variability of annual CO sub(2) exchange from Dutch grasslands</title><title>Biogeosciences</title><description>An intercomparison is made of the Net Ecosystem Exchange of CO sub(2), NEE, for eight Dutch grassland sites: four natural grasslands, two production grasslands and two meteorological stations within a rotational grassland region. At all sites the NEE was determined during at least 10 months per site, using the eddy-covariance (EC) technique, but in different years. The NEE does not include any import or export other than CO sub(2). The photosynthesis-light response analysis technique is used along with the respiration-temperature response technique to partition NEE into Gross Primary Production (GPP) and Ecosystem Respiration (R sub(e)) and to obtain the eco-physiological characteristics of the sites at the field scale. Annual sums of NEE, GPP and R sub(e) are then estimated using the fitted response curves with observed radiation and air temperature from a meteorological site in the centre of The Netherlands as drivers. These calculations are carried out for four years (2002-2005). Land use and management histories are not considered. The estimated annual R sub(e) for all individual sites is more or less constant per site and the average for all sites amounts to 1390 plus or minus 30 gC m super(− 2) a super(− 1). The narrow uncertainty band ( plus or minus 2%) reflects the small differences in the mean annual air temperature. The mean annual GPP was estimated to be 1325 g C m super(− 2) a super(− 1), and displays a much higher standard deviation, of plus or minus 110 gC m super(− 2) a super(− 1) (8%), which reflects the relatively large variation in annual solar radiation. The mean annual NEE amounts to -65 plus or minus 85 gC m super(− 2) a super(− 1). From two sites, four-year records of CO sub(2) flux were available and analyzed (2002-2005). Using the weather record of 2005 with optimizations from the other years, the standard deviation of annual GPP was estimated to be 171-206 gC m super(− 2) a super(− 1) (8-14%), of annual R sub(e) 227-247 gC m super(− 2) a super(− 1) (14-16%) and of annual NEE 176-276 gC m super(− 2) a super(− 1). The inter-site standard deviation was higher for GPP and R sub(e), 534 gC m super(− 2) a super(− 1) (37.3%) and 486 gC m super(− 2) a super(− 1) (34.8%), respectively. However, the inter-site standard deviation of NEE was similar to the interannual one, amounting to 207 gC m super(− 2) a super(− 1). Large differences occur due to soil type. The grasslands on organic (peat) soils show a mean net release of CO sub(2) of 220 plus or minus 90 g C m super(− 2) a super(− 1) while the grasslands on mineral (clay and sand) soils show a mean net uptake of CO sub(2) of 90 plus or minus 90 g C m super(− 2) a super(− 1). If a weighing with the fraction of grassland on organic (20%) and mineral soils (80%) is applied, an average NEE of 28 plus or minus 90 g C m super(− 2) a super(− 1) is found. The results from the analysis illustrate the need for regionally specific and spatially explicit CO sub(2) emission estimates from grassland.</description><issn>1726-4170</issn><issn>1726-4189</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNpjYuA0NDcy0zUxtLBkgbPNDTgYuIqLswwMjC0MLEw5GezCEosyE5MyczJLKhXy0xQS8_JKE3MUnP0VikuTNIw0FVIrkjMS89JTFdKK8nMVXEpLkjMU0osSi4tzEvNSinkYWNMSc4pTeaE0N4Oam2uIs4duQVF-YWlqcUl8bmZxcmoOUHFqfmlxvJGBgbmJhZGJMdEKAcazO-k</recordid><startdate>20071008</startdate><enddate>20071008</enddate><creator>J Jacobs, CM</creator><creator>G Jacobs, AF</creator><creator>Bosveld, F C</creator><creator>Hendriks, D</creator><creator>Hensen, A</creator><creator>Kroon, P S</creator><creator>Moors, E J</creator><creator>Nol, L</creator><creator>Schrier-Uijl, A</creator><creator>Veenendaal, E M</creator><scope>7SN</scope><scope>C1K</scope></search><sort><creationdate>20071008</creationdate><title>Variability of annual CO sub(2) exchange from Dutch grasslands</title><author>J Jacobs, CM ; G Jacobs, AF ; Bosveld, F C ; Hendriks, D ; Hensen, A ; Kroon, P S ; Moors, E J ; Nol, L ; Schrier-Uijl, A ; Veenendaal, E M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-proquest_miscellaneous_200748243</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>J Jacobs, CM</creatorcontrib><creatorcontrib>G Jacobs, AF</creatorcontrib><creatorcontrib>Bosveld, F C</creatorcontrib><creatorcontrib>Hendriks, D</creatorcontrib><creatorcontrib>Hensen, A</creatorcontrib><creatorcontrib>Kroon, P S</creatorcontrib><creatorcontrib>Moors, E J</creatorcontrib><creatorcontrib>Nol, L</creatorcontrib><creatorcontrib>Schrier-Uijl, A</creatorcontrib><creatorcontrib>Veenendaal, E M</creatorcontrib><collection>Ecology Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Biogeosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>J Jacobs, CM</au><au>G Jacobs, AF</au><au>Bosveld, F C</au><au>Hendriks, D</au><au>Hensen, A</au><au>Kroon, P S</au><au>Moors, E J</au><au>Nol, L</au><au>Schrier-Uijl, A</au><au>Veenendaal, E M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Variability of annual CO sub(2) exchange from Dutch grasslands</atitle><jtitle>Biogeosciences</jtitle><date>2007-10-08</date><risdate>2007</risdate><volume>4</volume><issue>5</issue><spage>803</spage><epage>816</epage><pages>803-816</pages><issn>1726-4170</issn><eissn>1726-4189</eissn><abstract>An intercomparison is made of the Net Ecosystem Exchange of CO sub(2), NEE, for eight Dutch grassland sites: four natural grasslands, two production grasslands and two meteorological stations within a rotational grassland region. At all sites the NEE was determined during at least 10 months per site, using the eddy-covariance (EC) technique, but in different years. The NEE does not include any import or export other than CO sub(2). The photosynthesis-light response analysis technique is used along with the respiration-temperature response technique to partition NEE into Gross Primary Production (GPP) and Ecosystem Respiration (R sub(e)) and to obtain the eco-physiological characteristics of the sites at the field scale. Annual sums of NEE, GPP and R sub(e) are then estimated using the fitted response curves with observed radiation and air temperature from a meteorological site in the centre of The Netherlands as drivers. These calculations are carried out for four years (2002-2005). Land use and management histories are not considered. The estimated annual R sub(e) for all individual sites is more or less constant per site and the average for all sites amounts to 1390 plus or minus 30 gC m super(− 2) a super(− 1). The narrow uncertainty band ( plus or minus 2%) reflects the small differences in the mean annual air temperature. The mean annual GPP was estimated to be 1325 g C m super(− 2) a super(− 1), and displays a much higher standard deviation, of plus or minus 110 gC m super(− 2) a super(− 1) (8%), which reflects the relatively large variation in annual solar radiation. The mean annual NEE amounts to -65 plus or minus 85 gC m super(− 2) a super(− 1). From two sites, four-year records of CO sub(2) flux were available and analyzed (2002-2005). Using the weather record of 2005 with optimizations from the other years, the standard deviation of annual GPP was estimated to be 171-206 gC m super(− 2) a super(− 1) (8-14%), of annual R sub(e) 227-247 gC m super(− 2) a super(− 1) (14-16%) and of annual NEE 176-276 gC m super(− 2) a super(− 1). The inter-site standard deviation was higher for GPP and R sub(e), 534 gC m super(− 2) a super(− 1) (37.3%) and 486 gC m super(− 2) a super(− 1) (34.8%), respectively. However, the inter-site standard deviation of NEE was similar to the interannual one, amounting to 207 gC m super(− 2) a super(− 1). Large differences occur due to soil type. The grasslands on organic (peat) soils show a mean net release of CO sub(2) of 220 plus or minus 90 g C m super(− 2) a super(− 1) while the grasslands on mineral (clay and sand) soils show a mean net uptake of CO sub(2) of 90 plus or minus 90 g C m super(− 2) a super(− 1). If a weighing with the fraction of grassland on organic (20%) and mineral soils (80%) is applied, an average NEE of 28 plus or minus 90 g C m super(− 2) a super(− 1) is found. The results from the analysis illustrate the need for regionally specific and spatially explicit CO sub(2) emission estimates from grassland.</abstract></addata></record> |
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title | Variability of annual CO sub(2) exchange from Dutch grasslands |
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