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Paleoclimate studies and natural-resource management in the Murray-Darling Basin I: past, present and future climates

机译:墨累达令盆地的古气候研究和自然资源管理:过去,现在和未来的气候

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This paper provides an incisive review of paleoclimate science and its relevance to natural-resource management within the Murray-Darling Basin (MDB). The drought of 1997-2010 focussed scientific, public and media attention on intrinsic climate variability and the confounding effect of human activity, especially in terms of water-resource management. Many policy and research reviews make statements about future planning with little consideration of climate change and without useful actionable knowledge. In order to understand future climate changes, modellers need, and demand, better paleoclimate data to constrain their model projections. Here, we present an insight into a number of existing long-term paleoclimate studies relevant to the MDB. Past records of climate, in response to orbital forcing (glacial-interglacial cycles) are found within, and immediately outside, the MDB. High-resolution temperature records, spanning the last 10~5 years, exist from floodplains and cave speleothems, as well as evidence from lakes and their associated lunettes. More recently, historical climate records show major changes in relation to El Ni?o-Southern Oscillation cycles and decadal shifts in rainfall regimes. A considerable body of research currently exists on the past climates of southeastern Australia but, this has not been collated and validated over large spatial scales. It is clear that a number of knowledge gaps still exist, and there is a pressing need for the establishment of new paleoclimatic research within the MDB catchment and within adjacent, sensitive catchments if past climate science is to fulfil its potential to provide policy-relevant information to natural-resource management into the future.
机译:本文对古气候科学及其与默里-达令盆地(MDB)内自然资源管理的相关性进行了深入研究。 1997-2010年的干旱将科学,公众和媒体的注意力集中在固有的气候变异性和人类活动的混杂影响上,特别是在水资源管理方面。许多政策和研究评论都在未考虑气候变化且没有有用的可行知识的情况下发表了有关未来计划的声明。为了了解未来的气候变化,建模者的需求和需求,需要更好的古气候数据来约束他们的模型预测。在这里,我们提供了对与MDB相关的许多现有长期古气候研究的见识。在MDB内部和外部都发现了过去对气候的响应,这是对轨道强迫(冰川-冰川间循环)的响应。洪泛区和洞穴洞穴斑块存在近10到5年的高分辨率温度记录,湖泊和相关的月球状突起也有记录。最近,历史气候记录显示出与厄尔尼诺-南方涛动周期和降雨制度的年代际变化有关的重大变化。目前,对澳大利亚东南部的过去气候存在大量研究,但尚未在较大的空间尺度上进行整理和验证。显然,仍然存在许多知识差距,如果过去的气候科学要发挥其提供与政策相关的信息的潜力,那么迫切需要在多边开发银行流域以及邻近的敏感流域内建立新的古气候研究。到未来的自然资源管理。

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