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The role of hydrological model complexity and uncertainty in climate change impact assessment

机译:水文模型复杂性和不确定性在气候变化影响评估中的作用

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Little quantitative knowledge is as yet available about the role ofhydrological model complexity for climate change impact assessment. Thisstudy investigates and compares the varieties of different model response ofthree hydrological models (PROMET, Hydrotel, HSAMI), each representing adifferent model complexity in terms of process description, parameter spaceand spatial and temporal scale. The study is performed in the Ammerwatershed, a 709 km2 catchment in the Bavarian alpine forelands,Germany. All models are driven and validated by a 30-year time-series(1971–2000) of observation data. It is expressed by objective functions,that all models, HSAMI and Hydrotel due to calibration, perform almostequally well for runoff simulation over the validation period. Somesystematic deviances in the hydrographs and the spatial patterns ofhydrologic variables are however quite distinct and thus further discussed.Virtual future climate (2071–2100) is generated by the Canadian RegionalClimate Model (vers 3.7.1), driven by the Coupled Global Climate Model(vers. 2) based on an A2 emission scenario (IPCC 2007). The hydrologicalmodel performance is evaluated by flow indicators, such as flood frequency,annual 7-day and 30-day low flow and maximum seasonal flows. The modifiedclimatic boundary conditions cause dramatic deviances in hydrologic modelresponse. HSAMI shows tremendous overestimation of evapotranspiration, whileHydrotel and PROMET behave in comparable range. Still, their significantdifferences, like spatially explicit patterns of summerly water shortage orspring flood intensity, highlight the necessity to extend and quantify theuncertainty discussion in climate change impact analysis towards theremarkable effect of hydrological model complexity. It is obvious that forspecific application purposes, water resources managers need to be madeaware of this effect and have to take its implications into account fordecision making. The paper concludes with an outlook and a proposal forfuture research necessities.
机译:关于水文学模型复杂性在气候变化影响评估中的作用,尚缺乏定量知识。本研究调查并比较了三种水文模型(PROMET,Hydrotel,HSAMI)的不同模型响应的多样性,每种模型在过程描述,参数空间以及时空尺度方面代表着不同的模型复杂性。这项研究是在德国巴伐利亚前高地709 km 2 集水区Ammerwatershed上进行的。所有模型均由30年的观测数据时间序列(1971-2000年)驱动和验证。用目标函数表示,由于校准,所有模型(HSAMI和Hydrotel)在验证期内的径流模拟性能几乎相同。但是,水文图中某些系统性偏差和水文变量的空间模式非常不同,因此需要进一步讨论。 虚拟的未来气候(2071-2100)由加拿大区域气候模型(3.7.1版)生成,由基于A2排放情景的全球气候耦合模型(第2版)(IPCC 2007)。水文模型性能通过流量指标进行评估,例如洪水频率,每年7天和30天的低流量和最大季节性流量。修改后的气候边界条件导致水文模型响应剧烈变化。 HSAMI表现出对蒸散量的高估,而Hydrotel和PROMET的表现在可比范围内。尽管如此,它们的显着差异,如夏季缺水或春季洪水强度的空间明晰模式,凸显出有必要扩大和量化气候变化影响分析中的不确定性讨论,以达到水文模型复杂性的显着效果。显然,出于特定的应用目的,水资源管理者需要意识到这种影响,并必须将其影响考虑在内以做出决策。本文以展望前景和未来研究的必要性提出结论。

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