Hydrogen sulphide eruptions in the Atlantic Ocean off southern Africa: implications of a new view based on SeaWiFS satellite imagery

被引:91
作者
Weeks, SJ [1 ]
Currie, B
Bakun, A
Peard, KR
机构
[1] Univ Cape Town, Dept Oceanog, Ocean Space CC, ZA-7701 Rondebosch, South Africa
[2] Natl Marine Res & Informat Ctr, Minist Fisheries, Swakopmund, Namibia
[3] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Ctr Sustainable Fisheries, Coral Gables, FL 33124 USA
[4] Minist Fisheries, Marine Res Stn, Luderitz, Namibia
关键词
SeaWiFS; satellite identification; Benguela; hydrogen sulphide; methane; eruption; hypoxia; monitoring; southern Africa; Namibia; 10 degrees E-17 degrees E; 17 degrees S-29 degrees S;
D O I
10.1016/j.dsr.2003.10.004
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Conventional wisdom has held that eruptions of toxic hydrogen sulphide that occur from time to time in the ocean off southwestern Africa were rather isolated near-coastal features, limited both in extent and in ecosystem-scale consequences. Now, however, it has become possible to identify sulphide outbreaks by satellite remote sensing. This new capability appears to lead to a complete revision of the conventional view, with some eruption episodes being observed to affect areas of ocean surface exceeding 20,000 km(2). The occurrences are also seen to be more frequent and longer lasting than previously supposed. Example sequences of Sea-viewing Wide Field of View (SeaWiFS) images are presented to indicate general classes of eruption types that are observed and to support discussion of potential eruption mechanisms. Certain methodological problems in interpreting effects on local productivity are outlined. Spatial configurations of eruptions indicate that simple upward advection in the upwelling process may not be a sufficient explanation for the range of eruption characteristics experienced. Eruptions seem often to be coincident with One of two contrasting types of atmospheric weather situation: either (1) increased intensity of wind driven coastal upwelling, or (2) indications of passage of a low pressure weather cell (e.g. interruption of coastal upwelling, sudden warming of the sea surface, rainfall in the hinterland). Such a pattern may imply that related lowering of hydrostatic pressure at depth may tend to trigger incipient eruptions. It also suggests an episodic mechanism driven by the buoyancy introduced by the effervescence of gases trapped by hydrostatic pressure within the sea-floor sediments. Connotations of these phenomena to the local ecology and to that of the entire Benguela Current regional ecosystem would appear to be major. Their relevance to the valuable but extremely variable fishery resource populations of the region, which have undergone drastic declines in recent decades, is likely to be high. (C) 2003 Elsevier Ltd. All rights reserved.
引用
收藏
页码:153 / 172
页数:20
相关论文
共 30 条