Biomass burning, land-cover change, and the hydrological cycle in Northern sub-Saharan Africa

dc.contributor.authorIchoku, Charles
dc.contributor.authorEllison, Luke
dc.contributor.authorWillmot, K. Elena
dc.contributor.authorMatsui, Toshihisa
dc.contributor.authorDezfuli, Amin
dc.contributor.authorGatebe, Charles K.
dc.contributor.authorWang, Jun
dc.contributor.authorWilcox, Eric M.
dc.contributor.authorLee, Jejung
dc.contributor.authorAdegoke, Jimmy
dc.contributor.authorOkonkwo, Churchill
dc.contributor.authorBolten, John
dc.contributor.authorPolicelli, Frederick S.
dc.contributor.authorHabib, Shahid
dc.date.accessioned2024-09-24T08:59:40Z
dc.date.available2024-09-24T08:59:40Z
dc.date.issued2016-09-14
dc.description.abstractThe Northern Sub-Saharan African (NSSA) region, which accounts for 20%–25% of the global carbon emissions from biomass burning, also suffers from frequent drought episodes and other disruptions to the hydrological cycle whose adverse societal impacts have been widely reported during the last several decades. This paper presents a conceptual framework of the NSSA regional climate system components that may be linked to biomass burning, as well as detailed analyses of a variety of satellite data for 2001–2014 in conjunction with relevant model-assimilated variables. Satellite fire detections in NSSA show that the vast majority (>75%) occurs in the savanna and woody savanna land-cover types. Starting in the 2006–2007 burning season through the end of the analyzed data in 2014, peak burning activity showed a net decrease of 2–7%/yr in different parts of NSSA, especially in the savanna regions. However, fire distribution shows appreciable coincidence with land-cover change. Although there is variable mutual exchange of different land cover types, during 2003–2013, cropland increased at an estimated rate of 0.28%/yr of the total NSSA land area, with most of it (0.18%/yr) coming from savanna. During the last decade, conversion to croplands increased in some areas classified as forests and wetlands, posing a threat to these vital and vulnerable ecosystems. Seasonal peak burning is anti-correlated with annual water-cycle indicators such as precipitation, soil moisture, vegetation greenness, and evapotranspiration, except in humid West Africa (5°–10° latitude), where this anti-correlation occurs exclusively in the dry season and burning virtually stops when monthly mean precipitation reaches 4 mm d⁻¹. These results provide observational evidence of changes in land-cover and hydrological variables that are consistent with feedbacks from biomass burning in NSSA, and encourage more synergistic modeling and observational studies that can elaborate this feedback mechanism.
dc.description.sponsorshipThis research was fully funded by NASA under its Research Opportunities in Space and Earth Sciences (ROSES)—2009 and 2013 Interdisciplinary Studies (IDS) Program (Dr Jack Kaye, Earth Science Research Director) through the Radiation Sciences Program managed by Dr Hal Maring. We also appreciate the efforts of providers of the large diversity of data products used for this study from various satellite sensors and global models.
dc.description.urihttps://iopscience.iop.org/article/10.1088/1748-9326/11/9/095005
dc.format.extent14 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m217tx-uvyd
dc.identifier.citationIchoku, Charles, Luke T. Ellison, K. Elena Willmot, Toshihisa Matsui, Amin K. Dezfuli, Charles K. Gatebe, Jun Wang, et al. “Biomass Burning, Land-Cover Change, and the Hydrological Cycle in Northern Sub-Saharan Africa.” Environmental Research Letters 11, no. 9 (September 2016): 095005. https://doi.org/10.1088/1748-9326/11/9/095005.
dc.identifier.urihttp://dx.doi.org/10.1088/1748-9326/11/9/095005
dc.identifier.urihttp://hdl.handle.net/11603/36352
dc.language.isoen_US
dc.publisherIOP
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC GESTAR II
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.titleBiomass burning, land-cover change, and the hydrological cycle in Northern sub-Saharan Africa
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0002-9998-2512

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