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The droughts of 1997 and 2005 in Amazonia: floodplain hydrology and its potential ecological and human impacts

机译:1997年和2005年亚马逊河流域的干旱:洪泛区水文学及其潜在的生态和人类影响

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It is well known that most of the severe droughts in Amazonia, such as that of 1997, are El Nio-related. However, in 2005, the Amazon was affected by a severe drought that was not El Nio-related, as most of the rainfall anomalies that have happened in southwestern Amazonia are driven by sea surface temperature anomalies in the tropical North Atlantic. Earlier studies have analyzed both droughts in terms of their meteorological causes and impacts in terra firme (non-flooded) forests. This study compares the hydrological effects of both droughts on the Amazonian floodplain and discusses their potential ecological and human impacts based on an extensive literature review. The results revealed that the effects of the 2005 drought were exacerbated because rainfall was lower and evaporation rates were higher at the peak of the dry season compared to the 1997 drought. This induced a more acute depletion of water levels in floodplain lakes and was most likely associated with higher fish mortality rates. Based on the fact that the stem growth of many floodplain species is related to the length of the non-flooded period, it is hypothesized that the 1997 drought had more positive effects on floodplain forest growth than the 2005 drought. The fishing community of Silves in central Amazonia considered both droughts to have been equally severe. However, the 2005 drought was widely broadcasted by the press; therefore, the governmental mitigation efforts were more comprehensive. It is suggested that the availability of new communication technology and greater public awareness regarding environmental issues, combined with the new legal framework for assessing the severity of calamities in Brazil, are among the primary factors that explain the difference in societal response between the two droughts.
机译:众所周知,亚马逊河地区的大多数严重干旱(例如1997年)都与厄尔尼诺现象有关。但是,在2005年,亚马逊遭受了与厄尔尼诺现象无关的严重干旱,因为西南亚马逊地区发生的大部分降雨异常是由热带北大西洋海表温度异常驱动的。较早的研究从干旱的气象原因和对坚硬(非淹没)森林的影响方面分析了干旱。这项研究比较了两种干旱对亚马逊河漫滩的水文影响,并在广泛的文献综述的基础上讨论了其对生态和人类的潜在影响。结果表明,与1997年干旱相比,2005年干旱的影响更为严重,因为在旱季高峰期降雨较少,蒸发速率较高。这导致洪泛区湖泊中的水位急剧减少,最有可能与较高的鱼类死亡率相关。基于许多泛滥平原物种的茎生长与非淹没期的长短有关的事实,假设1997年干旱对泛滥森林的生长比2005年干旱具有更积极的影响。亚马孙地区中部的西尔维斯(Silves)捕鱼社区认为这两种干旱同样严重。但是,2005年的干旱被媒体广泛广播。因此,政府的缓解措施更加全面。建议采用新的通信技术和提高公众对环境问题的认识,再加上评估巴西灾难严重性的新法律框架,是解释两次干旱之间社会反应差异的主要因素。

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