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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Increasing rainfall, decreasing winds, and historical changes in Santa Catarina dunefields, southern Brazil
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Increasing rainfall, decreasing winds, and historical changes in Santa Catarina dunefields, southern Brazil

机译:巴西南部圣卡塔琳娜州邓内菲尔德的降雨量不断增加,风势有所减少,历史发生了变化

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摘要

Morphological and vegetation changes on the Mo?ambique barrier dunefield system are examined for the period 1938-2002 from aerial photography, and a variety of factors are investigated as possible driving factors. Human factors include a decrease in grazing pressure and tree felling from the early 1960s onwards after 200years of these activities, and fires. In the 1960s tree planting also took place. During the period 1963 to 1970 there was a marked decline in drift potential (DP - potential sand transport), and then a period of very low DPs (1970-1974). This period falls within the time interval when vegetation cover significantly increased by ~70% along the Mo?ambique barrier (from 1956 to 1978). During the 1960s to present, the rainfall increased. Analyses of other transgressive dunefields in Santa Catarina and Rio Grande do Sul states show similar trends so it is likely that climatic factors such as increasing rainfall and decreasing DPs are responsible for driving dunefield changes and vegetation colonization of the barriers.
机译:通过航拍,研究了1938年至2002年这段时期内Moambique障碍物Dunnefield系统的形态和植被变化,并研究了多种可能的驱动因素。人为因素包括放牧压力的降低和经过200年此类活动后从1960年代初开始砍伐树木和火灾。在1960年代,还进行了植树活动。在1963年至1970年期间,漂流潜力(DP-潜在的沙子运输)显着下降,然后是DPs极低的时期(1970-1974年)。这个时期是在一个时间间隔内,当时沿莫桑比克屏障(从1956年到1978年)植被覆盖率显着增加了约70%。在1960年代至今,降雨量增加了。对圣卡塔琳娜州和南里奥格兰德州其他海侵沙丘的分析也显示出类似的趋势,因此,诸如降雨增加和DP减少等气候因素可能导致了沙丘的变化和屏障的植被定植。

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