Potential dust emissions from the southern Kalahari's dunelands

被引:24
作者
Bhattachan, Abinash [1 ]
D'Odorico, Paolo [1 ]
Okin, Gregory S. [2 ]
Dintwe, Kebonyethata [2 ]
机构
[1] Univ Virginia, Dept Environm Sci, Charlottesville, VA 22904 USA
[2] Univ Calif Los Angeles, Dept Geog, Los Angeles, CA 90095 USA
基金
美国国家科学基金会;
关键词
WIND EROSION; DESERT DUST; VEGETATION COVER; SOUTHWESTERN KALAHARI; LAND DEGRADATION; CLIMATE; BIOGEOCHEMISTRY; DESERTIFICATION; VARIABILITY; VELOCITIES;
D O I
10.1002/jgrf.20043
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Southern Hemisphere shows relatively low levels of atmospheric dust concentrations. Dust concentrations could, however, increase as a result of losses of vegetation cover in the southern Kalahari. There is some evidence of an ongoing remobilization of stabilized dunefields in the southern Kalahari where dune crests with sparse vegetation cover are reactivated during dry and windy periods, a phenomenon that is predicted to intensify with increased land degradation, overgrazing, and droughts. Despite the potentially important climatic and biogeochemical implications of dust emissions from the Kalahari, it is still unclear whether the predicted remobilization of the Kalahari dunes could be associated with increased dust emissions from this region. The dependence of sediment fluxes and dust emissions on vegetation cover in the Kalahari dunelands remains poorly understood, which prevents a quantitative assessment of possible changes in aeolian activity in this region under different land use and land cover scenarios. In this study, we report the results of an aeolian sediment sampling campaign over a variety of land covers in the southern Kalahari. We use these results to quantify the potential rate of dust emissions and its dependence on vegetation cover and to make an estimate of dust fluxes from a portion of the southern Kalahari. The results show that the loss of vegetation could lead to substantial increases in dust emission and nutrient loss.
引用
收藏
页码:307 / 314
页数:8
相关论文
共 73 条
  • [1] Mineral aerosol production by wind erosion: aerosol particle sizes and binding energies
    Alfaro, SC
    Gaudichet, A
    Gomes, L
    Maille, M
    [J]. GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (07) : 991 - 994
  • [2] [Anonymous], 2006, DESERT DUST GLOBAL S
  • [3] Sand dune mobility under climate change in the Kalahari and Australian deserts
    Ashkenazy, Y.
    Yizhaq, H.
    Tsoar, Haim
    [J]. CLIMATIC CHANGE, 2012, 112 (3-4) : 901 - 923
  • [4] Bagnold R.A., 1941, PHYS BLOWN SAND DESE, P265, DOI DOI 10.1177/030913339401800105
  • [5] The ASTER spectral library version 2.0
    Baldridge, A. M.
    Hook, S. J.
    Grove, C. I.
    Rivera, G.
    [J]. REMOTE SENSING OF ENVIRONMENT, 2009, 113 (04) : 711 - 715
  • [6] The Southern Kalahari: a potential new dust source in the Southern Hemisphere?
    Bhattachan, Abinash
    D'Odorico, Paolo
    Baddock, Matthew C.
    Zobeck, Ted M.
    Okin, Gregory S.
    Cassar, Nicolas
    [J]. ENVIRONMENTAL RESEARCH LETTERS, 2012, 7 (02):
  • [7] Bullard JE, 1997, EARTH SURF PROC LAND, V22, P165, DOI 10.1002/(SICI)1096-9837(199702)22:2<165::AID-ESP687>3.0.CO
  • [8] 2-9
  • [9] Sub-basin scale dust source geomorphology detected using MODIS
    Bullard, Joanna
    Baddock, Matthew
    McTainsh, Grant
    Leys, John
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2008, 35 (15)
  • [10] Factors affecting the nature and rate of dust production from natural dune sands
    Bullard, Joanna E.
    McTainsh, Grant H.
    Pudmenzky, Christa
    [J]. SEDIMENTOLOGY, 2007, 54 (01) : 169 - 182