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

被引:40
|
作者
Ichoku, Charles [1 ]
Ellison, Luke T. [1 ,2 ]
Willmot, K. Elena [3 ]
Matsui, Toshihisa [1 ,4 ]
Dezfuli, Amin K. [1 ,5 ]
Gatebe, Charles K. [1 ,5 ]
Wang, Jun [6 ,7 ,8 ]
Wilcox, Eric M. [9 ]
Lee, Jejung [10 ]
Adegoke, Jimmy [10 ]
Okonkwo, Churchill [11 ]
Bolten, John [1 ]
Policelli, Frederick S. [1 ]
Habib, Shahid [1 ]
机构
[1] NASA, Goddard Space Flight Ctr, Div Earth Sci, Greenbelt, MD 20771 USA
[2] Sci Syst & Applicat Inc, Lanham, MD USA
[3] Vanderbilt Univ, Nashville, TN 37235 USA
[4] Univ Maryland, ESSIC, College Pk, MD 20742 USA
[5] USRA, Columbia, MD USA
[6] Univ Nebraska, Dept Earth & Atmospher Sci, Lincoln, NE USA
[7] Univ Iowa, Ctr Global & Reg Environm Res, Iowa City, IA 52242 USA
[8] Univ Iowa, Dept Chem & Biochem Engn, Iowa City, IA 52242 USA
[9] Desert Res Inst, Reno, NV USA
[10] Univ Missouri, Kansas City, MO 64110 USA
[11] Howard Univ, Beltsville Ctr Climate Syst Observat, Washington, DC 20059 USA
来源
ENVIRONMENTAL RESEARCH LETTERS | 2016年 / 11卷 / 09期
关键词
sub-Saharan Africa; biomass burning; water cycle; land cover change; precipitation; fire; WESTERN EQUATORIAL AFRICA; FIRE DETECTION; CLIMATE-CHANGE; RAINFALL VARIABILITY; TROPICAL OCEANS; SAHEL RAINFALL; SOIL-MOISTURE; LAKE CHAD; PART I; SURFACE;
D O I
10.1088/1748-9326/11/9/095005
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The 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 degrees-10 degrees 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.
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页数:13
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