Please use this identifier to cite or link to this item: https://cris.library.msu.ac.zw//handle/11408/5850
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dc.contributor.authorSonja Leitneren_US
dc.contributor.authorVictoria Carbonellen_US
dc.contributor.authorKlaus Butterbach-Bahlen_US
dc.contributor.authorMatti Barthelen_US
dc.contributor.authorRangarirayi Lucia Mhinduen_US
dc.contributor.authorPaul Mutuoen_US
dc.contributor.authorNina Buchmannen_US
dc.contributor.authorLutz Merbolden_US
dc.date.accessioned2023-09-22T10:46:43Z-
dc.date.available2023-09-22T10:46:43Z-
dc.date.issued2023-
dc.identifier.urihttps://cris.library.msu.ac.zw//handle/11408/5850-
dc.description.abstractThere is hot debate about whether grassland-based livestock production can be climate-smart or not. Greenhouse gas (GHG) emissions from livestock (primarily from enteric methane [CH4] and manure CH4 and nitrous oxide [N2O]) stand vis-à-vis vegetation CO2 uptake and soil carbon sequestration. In sub-Saharan Africa (SSA), livestock are a precious good that ensures the livelihoods of millions of people, which often belong to marginalized groups such as pastoralists. To protect their animals from predation and theft, livestock are secured in overnight enclosures (“bomas” in Kiswahili), which form the center of many pastoral settlements. However, in these enclosures manure accumulates for months or even years, making them a potential hotspot for GHG emissions. Here, we present the first year-long measurements of GHG emissions from active and inactive (abandoned) bomas from an African rangeland at the ILRI Kapiti Research Station in Kenya. We found that active bomas were continuous sources for CO2, CH4 and N2O emissions, with flux peaks of up to 1940 mg CO2-C m‑2 h‑1, 1600 μg N2O-N m‑2 h‑1 , and 6690 μg CH4-C m‑2 h‑1. Even after their abandonment, fluxes from bomas continued to be elevated compared to savanna soil background emissions for all GHGs. When calculated over a full year and put in context with manure deposition rates into the bomas (GHG emission factors), we found that 12.6 ± 5.3 % manure-C was emitted as CO2, 2.4 ± 0.4 % manure-N was emitted as N2O, and 0.5 ± 0.1 % manure-C was emitted as CH4. GHG emissions from active bomas were not affected by rainfall seasonality or temperature, presumably because the moisture content of the fresh manure was always high due to urine input, and because temperature did not vary much during the year. In abandoned bomas, GHG emissions were driven by rainfall events that triggered emission pulses, leading to higher emissions during the wet season. The high N2O and CH4 emissions we found have implications for global GHG inventories, which currently do not have a category for overnight livestock enclosures and therefore do not account for these emissions. Furthermore, hotspots for GHG emissions such as these livestock enclosures need to be included to assess the full GHG budget of pastoral livestock systems and to develop management interventions for low-emission livestock production in developing countries.en_US
dc.language.isoenen_US
dc.publisherEuropean GeoSciences Unionen_US
dc.subjectTraditional livestock enclosuresen_US
dc.subjectgreenhouse gasen_US
dc.subjecthotspotsen_US
dc.subjectAfrican savanna landscapeen_US
dc.subjectKenyaen_US
dc.titleTraditional livestock enclosures are greenhouse gas hotspots in the African savanna landscape: The case of a rangeland in Kenya: Vienna, Austria & Online, 23–28 April 2023en_US
dc.typeconference paperen_US
dc.relation.publicationEGU General Assembly 2023en_US
dc.identifier.doihttps://doi.org/10.5194/egusphere-egu23-14773-
dc.contributor.affiliationMazingira Center, International Livestock Research Institute (ILRI), Nairobi, Kenya (s.leitner@cgiar.org)en_US
dc.contributor.affiliationMazingira Center, International Livestock Research Institute (ILRI), Nairobi, Kenya;Department of Environmental System Sciences, Institute of Agricultural Sciences, ETH Zurich, Universitaetsstrasse 2, 8092 Zurich, Switzerland; Institute of Meteorology and Climate Research, Atmospheric Environmental Research (IMK-IFU), Karlsruhe Institute of Technology (KIT), Garmisch-Partenkirchen, Germanyen_US
dc.contributor.affiliationInstitute of Meteorology and Climate Research, Atmospheric Environmental Research (IMK-IFU), Karlsruhe Institute of Technology (KIT), Garmisch-Partenkirchen, Germanyen_US
dc.contributor.affiliationDepartment of Environmental System Sciences, Institute of Agricultural Sciences, ETH Zurich, Universitaetsstrasse 2, 8092 Zurich, Switzerlanden_US
dc.contributor.affiliationMazingira Center, International Livestock Research Institute (ILRI), Nairobi, Kenya; Department for Land and Water Resources Management, Midlands State University, P Bag 9055, Gweru, Zimbabween_US
dc.contributor.affiliationMazingira Center, International Livestock Research Institute (ILRI), Nairobi, Kenyaen_US
dc.contributor.affiliationDepartment of Environmental System Sciences, Institute of Agricultural Sciences, ETH Zurich, Universitaetsstrasse 2, 8092 Zurich, Switzerlanden_US
dc.contributor.affiliationIntegrative Agroecology Group, Agroecology and Environment Division, Agroscope, Reckenholzstrasse 191, 8046 Zurich, Switzerlanden_US
item.openairetypeconference paper-
item.openairecristypehttp://purl.org/coar/resource_type/c_5794-
item.fulltextWith Fulltext-
item.cerifentitytypePublications-
item.grantfulltextopen-
item.languageiso639-1en-
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