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Modified water regime and salinity as a consequence of climate change: prospects for wetlands of Southern Australia

机译:气候变化导致水质和盐分改变:南澳大利亚湿地的前景

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The natural Australian landscape sustains a mosaic of wetlands that range from permanently wet to temporary. This diversity of wetland types and habitats provides for diverse biotic communities, many of which are specific to individual wetlands. This paper explores the prospects for southern Australian wetlands under modified water regime and salinity induced by climatic changes. Extended droughts predicted as a consequence of climate change (lower rainfall and higher temperatures) combined with human-induced changes to the natural hydrological regime will lead to reductions in the amount of water available for environmental and anthropogenic uses. Reduced runoff and river flows may cause the loss of some temporary wetland types that will no longer hold water long enough to support hydric communities. Species distributions will shift and species extinctions may result particularly across fragmented or vulnerable landscapes. Accumulation of salts in wetlands shift species-rich freshwater communities to species-poor salt tolerant communities. Wetlands will differ in ecological response to these changes as the salinity and drying history of each wetland will determine its resilience: in the short term some freshwater communities may recover but they are unlikely to survive and reproduce under long term increased salinity and altered hydrology. In the long term such salinized wetlands with altered hydrology will need to be colonized by salt tolerant species adapted for the new hydrological conditions if they are to persist as functional wetlands. As the landscape becomes more developed, to accommodate the need for water in a warmer drying climate, increasing human intervention will result in a net loss of wetlands and wetland diversity.
机译:澳大利亚的自然景观维持着从永久性湿润到临时性湿地的镶嵌。湿地类型和栖息地的多样性提供了多种生物群落,其中许多生物群落特定于单个湿地。本文探讨了在由气候变化引起的水状态和盐度改变的情况下,澳大利亚南部湿地的前景。气候变化(较低的降雨和较高的温度)以及人为引起的自然水文状况变化的结果,预计干旱将加剧,这将导致可用于环境和人为使用的水量减少。径流和河流流量的减少可能会导致一些临时湿地类型的丧失,这些湿地类型将不再拥有足够长的水来支持水生生物群落。物种分布将发生变化,特别是在零散或脆弱的景观中可能造成物种灭绝。湿地中盐的积累使物种丰富的淡水群落向物种缺乏盐的群落转变。湿地对这些变化的生态响应将有所不同,因为每个湿地的盐度和干燥历史将决定其复原力:短期内一些淡水群落可能会恢复,但在盐度增加和水文状况改变的情况下,它们不太可能生存和繁殖。从长远来看,如果这些盐渍化湿地要继续作为功能性湿地而存在,则需要适应新水文条件的耐盐物种定殖。随着景观的发展,为了适应温暖干燥气候中对水的需求,越来越多的人为干预将导致湿地和湿地多样性的净损失。

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