Global temperature change potential of nitrogen use in agriculture: A 50-year assessment
Nitrogen (N) use in agriculture substantially alters global N cycle with the short- and long-term effects on global warming and climate change. It increases emission of nitrous oxide, which contributes 6.2%, while carbon dioxide and methane contribute 76% and 16%, respectively of the global warming....
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| Veröffentlicht in: | Scientific reports 2017-03, Vol.7 (1), p.44928, Article 44928 |
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| description | Nitrogen (N) use in agriculture substantially alters global N cycle with the short- and long-term effects on global warming and climate change. It increases emission of nitrous oxide, which contributes 6.2%, while carbon dioxide and methane contribute 76% and 16%, respectively of the global warming. However, N causes cooling due to emission of NO
x
, which alters concentrations of tropospheric ozone and methane. NO
x
and NH
3
also form aerosols with considerable cooling effects. We studied global temperature change potential (GTP) of N use in agriculture. The GTP due to N
2
O was 396.67 and 1168.32 Tg CO
2
e on a 20-year (GTP
20
) and 439.94 and 1295.78 Tg CO
2
e on 100-year scale (GTP
100
) during years 1961 and 2010, respectively. Cooling effects due to N use were 92.14 and 271.39 Tg CO
2
e (GTP
20
) and 15.21 and 44.80 Tg CO
2
e (GTP
100
) during 1961 and 2010, respectively. Net GTP
20
was 369.44 and 1088.15 Tg CO
2
e and net GTP
100
was 429.17 and 1264.06 Tg CO
2
e during 1961 and 2010, respectively. Thus net GTP
20
is lower by 6.9% and GTP
100
by 2.4% compared to the GTP considering N
2
O emission alone. The study shows that both warming and cooling effects should be considered to estimate the GTP of N use. |
| doi_str_mv | 10.1038/srep44928 |
| format | Article |
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x
, which alters concentrations of tropospheric ozone and methane. NO
x
and NH
3
also form aerosols with considerable cooling effects. We studied global temperature change potential (GTP) of N use in agriculture. The GTP due to N
2
O was 396.67 and 1168.32 Tg CO
2
e on a 20-year (GTP
20
) and 439.94 and 1295.78 Tg CO
2
e on 100-year scale (GTP
100
) during years 1961 and 2010, respectively. Cooling effects due to N use were 92.14 and 271.39 Tg CO
2
e (GTP
20
) and 15.21 and 44.80 Tg CO
2
e (GTP
100
) during 1961 and 2010, respectively. Net GTP
20
was 369.44 and 1088.15 Tg CO
2
e and net GTP
100
was 429.17 and 1264.06 Tg CO
2
e during 1961 and 2010, respectively. Thus net GTP
20
is lower by 6.9% and GTP
100
by 2.4% compared to the GTP considering N
2
O emission alone. The study shows that both warming and cooling effects should be considered to estimate the GTP of N use.</description><identifier>ISSN: 2045-2322</identifier><identifier>EISSN: 2045-2322</identifier><identifier>DOI: 10.1038/srep44928</identifier><identifier>PMID: 28322322</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>119/118 ; 704/106 ; 704/106/47 ; Agriculture ; Carbon dioxide ; Climate change ; Climate effects ; Cooling ; Emissions ; Global temperatures ; Global warming ; Guanosine triphosphate ; Humanities and Social Sciences ; Long-term effects ; Methane ; multidisciplinary ; Nitrogen ; Nitrous oxide ; Ozone ; Science ; Temperature effects</subject><ispartof>Scientific reports, 2017-03, Vol.7 (1), p.44928, Article 44928</ispartof><rights>The Author(s) 2017</rights><rights>Copyright Nature Publishing Group Mar 2017</rights><rights>Copyright © 2017, The Author(s) 2017 The Author(s)</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c504t-ec5bfda0c90efd98e1d259a24f1c78f6cc2cfc2ecaac7ae59565f68db8681813</citedby><cites>FETCH-LOGICAL-c504t-ec5bfda0c90efd98e1d259a24f1c78f6cc2cfc2ecaac7ae59565f68db8681813</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC5359602/pdf/$$EPDF$$P50$$Gpubmedcentral$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC5359602/$$EHTML$$P50$$Gpubmedcentral$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,864,885,27923,27924,41119,42188,51575,53790,53792</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/28322322$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Fagodiya, R. K.</creatorcontrib><creatorcontrib>Pathak, H.</creatorcontrib><creatorcontrib>Kumar, A.</creatorcontrib><creatorcontrib>Bhatia, A.</creatorcontrib><creatorcontrib>Jain, N.</creatorcontrib><title>Global temperature change potential of nitrogen use in agriculture: A 50-year assessment</title><title>Scientific reports</title><addtitle>Sci Rep</addtitle><addtitle>Sci Rep</addtitle><description>Nitrogen (N) use in agriculture substantially alters global N cycle with the short- and long-term effects on global warming and climate change. It increases emission of nitrous oxide, which contributes 6.2%, while carbon dioxide and methane contribute 76% and 16%, respectively of the global warming. However, N causes cooling due to emission of NO
x
, which alters concentrations of tropospheric ozone and methane. NO
x
and NH
3
also form aerosols with considerable cooling effects. We studied global temperature change potential (GTP) of N use in agriculture. The GTP due to N
2
O was 396.67 and 1168.32 Tg CO
2
e on a 20-year (GTP
20
) and 439.94 and 1295.78 Tg CO
2
e on 100-year scale (GTP
100
) during years 1961 and 2010, respectively. Cooling effects due to N use were 92.14 and 271.39 Tg CO
2
e (GTP
20
) and 15.21 and 44.80 Tg CO
2
e (GTP
100
) during 1961 and 2010, respectively. Net GTP
20
was 369.44 and 1088.15 Tg CO
2
e and net GTP
100
was 429.17 and 1264.06 Tg CO
2
e during 1961 and 2010, respectively. Thus net GTP
20
is lower by 6.9% and GTP
100
by 2.4% compared to the GTP considering N
2
O emission alone. The study shows that both warming and cooling effects should be considered to estimate the GTP of N use.</description><subject>119/118</subject><subject>704/106</subject><subject>704/106/47</subject><subject>Agriculture</subject><subject>Carbon dioxide</subject><subject>Climate change</subject><subject>Climate effects</subject><subject>Cooling</subject><subject>Emissions</subject><subject>Global temperatures</subject><subject>Global warming</subject><subject>Guanosine triphosphate</subject><subject>Humanities and Social Sciences</subject><subject>Long-term effects</subject><subject>Methane</subject><subject>multidisciplinary</subject><subject>Nitrogen</subject><subject>Nitrous oxide</subject><subject>Ozone</subject><subject>Science</subject><subject>Temperature effects</subject><issn>2045-2322</issn><issn>2045-2322</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNplkVFLwzAUhYMobsw9-Ack4JNCNUmbLvFBGEOnMPBlD76FLL3ZOrqmJq2wf2_G5pgYAgm5X865nIvQNSUPlKTiMXhoskwycYb6jGQ8YSlj5yf3HhqGsCZxcSYzKi9Rj4n4HncffU4rt9AVbmHTgNdt5wGbla6XgBvXQt2WsegsrsvWuyXUuAuAyxrrpS9NV-34JzzGnCRb0B7rECCETfx3hS6srgIMD-cAzV9f5pO3ZPYxfZ-MZ4nhJGsTMHxhC02MJGALKYAWjEvNMkvNSNjcGGasYWC0NiMNXPKc21wUC5ELKmg6QM972aZbbKAw0dnrSjW-3Gi_VU6X6m-lLldq6b4VT7nMCYsCtwcB7746CK1au87XsWVFJUlTwVMqInW3p4x3ISZujw6UqN0Y1HEMkb05belI_oYegfs9EGIpJu1PLP-p_QCHiZPF</recordid><startdate>20170321</startdate><enddate>20170321</enddate><creator>Fagodiya, R. 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K. ; Pathak, H. ; Kumar, A. ; Bhatia, A. ; Jain, N.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c504t-ec5bfda0c90efd98e1d259a24f1c78f6cc2cfc2ecaac7ae59565f68db8681813</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>119/118</topic><topic>704/106</topic><topic>704/106/47</topic><topic>Agriculture</topic><topic>Carbon dioxide</topic><topic>Climate change</topic><topic>Climate effects</topic><topic>Cooling</topic><topic>Emissions</topic><topic>Global temperatures</topic><topic>Global warming</topic><topic>Guanosine triphosphate</topic><topic>Humanities and Social Sciences</topic><topic>Long-term effects</topic><topic>Methane</topic><topic>multidisciplinary</topic><topic>Nitrogen</topic><topic>Nitrous oxide</topic><topic>Ozone</topic><topic>Science</topic><topic>Temperature effects</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fagodiya, R. K.</creatorcontrib><creatorcontrib>Pathak, H.</creatorcontrib><creatorcontrib>Kumar, A.</creatorcontrib><creatorcontrib>Bhatia, A.</creatorcontrib><creatorcontrib>Jain, N.</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Health & Medical Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Biology Database (Alumni Edition)</collection><collection>Medical Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Hospital Premium Collection</collection><collection>Hospital Premium Collection (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Health Research Premium Collection</collection><collection>Health Research Premium Collection (Alumni)</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Health & Medical Complete (Alumni)</collection><collection>ProQuest Biological Science Collection</collection><collection>Health & Medical Collection (Alumni Edition)</collection><collection>Medical Database</collection><collection>Science Database</collection><collection>Biological Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>PubMed Central (Full Participant titles)</collection><jtitle>Scientific reports</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fagodiya, R. K.</au><au>Pathak, H.</au><au>Kumar, A.</au><au>Bhatia, A.</au><au>Jain, N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Global temperature change potential of nitrogen use in agriculture: A 50-year assessment</atitle><jtitle>Scientific reports</jtitle><stitle>Sci Rep</stitle><addtitle>Sci Rep</addtitle><date>2017-03-21</date><risdate>2017</risdate><volume>7</volume><issue>1</issue><spage>44928</spage><pages>44928-</pages><artnum>44928</artnum><issn>2045-2322</issn><eissn>2045-2322</eissn><abstract>Nitrogen (N) use in agriculture substantially alters global N cycle with the short- and long-term effects on global warming and climate change. It increases emission of nitrous oxide, which contributes 6.2%, while carbon dioxide and methane contribute 76% and 16%, respectively of the global warming. However, N causes cooling due to emission of NO
x
, which alters concentrations of tropospheric ozone and methane. NO
x
and NH
3
also form aerosols with considerable cooling effects. We studied global temperature change potential (GTP) of N use in agriculture. The GTP due to N
2
O was 396.67 and 1168.32 Tg CO
2
e on a 20-year (GTP
20
) and 439.94 and 1295.78 Tg CO
2
e on 100-year scale (GTP
100
) during years 1961 and 2010, respectively. Cooling effects due to N use were 92.14 and 271.39 Tg CO
2
e (GTP
20
) and 15.21 and 44.80 Tg CO
2
e (GTP
100
) during 1961 and 2010, respectively. Net GTP
20
was 369.44 and 1088.15 Tg CO
2
e and net GTP
100
was 429.17 and 1264.06 Tg CO
2
e during 1961 and 2010, respectively. Thus net GTP
20
is lower by 6.9% and GTP
100
by 2.4% compared to the GTP considering N
2
O emission alone. The study shows that both warming and cooling effects should be considered to estimate the GTP of N use.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><pmid>28322322</pmid><doi>10.1038/srep44928</doi><oa>free_for_read</oa></addata></record> |
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| subjects | 119/118 704/106 704/106/47 Agriculture Carbon dioxide Climate change Climate effects Cooling Emissions Global temperatures Global warming Guanosine triphosphate Humanities and Social Sciences Long-term effects Methane multidisciplinary Nitrogen Nitrous oxide Ozone Science Temperature effects |
| title | Global temperature change potential of nitrogen use in agriculture: A 50-year assessment |
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