首页> 外文会议>IAHR World Congress >A FRAMEWORK FOR REGIONAL AND GLOBAL LONG-TERM AND MIDDLE-TERM ASSESSMENT OF FLOODS AND DROUGHTS UNDER AN APPROACH OF COMPUTATIONAL INTELLIGENCE LINKING EARTH OBSERVATION, GLOBAL CLIMATE AND HYDROLOGICAL MODELS
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A FRAMEWORK FOR REGIONAL AND GLOBAL LONG-TERM AND MIDDLE-TERM ASSESSMENT OF FLOODS AND DROUGHTS UNDER AN APPROACH OF COMPUTATIONAL INTELLIGENCE LINKING EARTH OBSERVATION, GLOBAL CLIMATE AND HYDROLOGICAL MODELS

机译:在连接地球观测,全球气候和水文模型的计算智能的方法下,区域和全球长期和中期评估洪水和干旱的框架

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Uncertainty in climate change prediction arises from three different sources: model uncertainty, scenario uncertainty, and internal variability (Yip et al., 2011). Model uncertainty arises because of an incomplete understanding of the physical processes and the limitations of implementation of the understanding. Scenario uncertainty arises because of incomplete information about future emissions. Internal variability is the natural unforced fluctuation of the climate system, it is aleatoric. A way to evaluate the total of these uncertainties is to calculate the spread of a multimodel ensemble (Boer, 2009), mostly by employing global models. However, global models have important drawbacks in their simulation of currently measured data as well as in the way this bias are incorporated into the future scenarios. Analysis of this type of uncertainty requires the use of large amount of data, and complex algorithms to determine trends and identify spatial patterns. Some work has been on the development of dynamic thresholds to identify extreme events in space and time. The trend in Europe is to explore adaptation that has the concept of "no regret solutions" and to look into adaptation capability of the different sectors of human development and its environment. For this, two key research areas are to be developed one by assessing the extreme situations using a bottomtop approach evolving the idea of actual changes attributed to unexpected climate (regional) and second on using global information (re-analysis data) and projecting models into the future with expected development of earth scenarios. In this paper we present the principles of a framework to address the long term and middle term prediction of floods and droughts working with ensembles of global hydrological models and using data driven models and evaluate the uncertainty of the results.
机译:气候变化预测的不确定性来自三种不同来源:模型不确定性,情景不确定性和内部变异性(YIP等,2011)。模型不确定性因对物理过程的不完全理解和实施理解的实施问题而不完整。由于有关未来排放的不完整信息,因此出现了场景不确定性。内部变异性是气候系统的天然良好的波动,它是炼层。一种评估这些不确定性的总体的方法是计算多模型集合(Boer,2009)的传播,主要是通过采用全球模型。然而,全球模型在他们对当前测量数据的模拟中具有重要的缺点,以及这种偏差纳入未来情景的方式。对这种类型的不确定性的分析需要使用大量数据和复杂的算法来确定趋势和识别空间模式。有些作品一直在开发动态阈值,以确定空间和时间的极端事件。欧洲的趋势是探索具有“无后悔解决方案”概念的适应,并展望人类发展不同部门及其环境的适应能力。为此,通过使用底部的方法来扩张归因于意外的气候(区域)的实际变化的思想以及使用全局信息(重新分析数据)和将模型投影进入的实际变化的思想来开发两个关键研究领域地球情景预期发展未来。在本文中,我们介绍了框架的原则,以解决与全球水文模型的集合和使用数据驱动模型的洪水和干旱的长期和中期预测,并评估结果的不确定性。

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