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A large set of potential past, present and future hydro-meteorological time series for the UK

机译:英国的一大套潜在的过去,现在和未来的水力气象时间序列

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Hydro-meteorological extremes such as drought and heavy precipitation can have large impacts on society and the economy. With potentially increasing risks associated with such events due to climate change, properly assessing the associated impacts and uncertainties is critical for adequate adaptation. However, the application of risk-based approaches often requires large sets of extreme events, which are not commonly available. Here, we present such a large set of hydro-meteorological time series for recent past and future conditions for the United Kingdom based on weather@home 2, a modelling framework consisting of a global climate model (GCM) driven by observed or projected sea surface temperature (SST) and sea ice which is down-scaled to 25 km over the European domain by a regional climate model (RCM). Sets of 100 time series are generated for each of (i) a historical baseline (1900-2006), (ii) five near-future scenarios (2020-2049) and (iii) five far-future scenarios (2070-2099). The five scenarios in each future time slice all follow the Representative Concentration Pathway 8.5 (RCP8.5) and sample the range of sea surface temperature and sea ice changes from CMIP5 (Coupled Model Intercomparison Project Phase 5) models. Validation of the historical baseline highlights good performance for temperature and potential evaporation, but substantial seasonal biases in mean precipitation, which are corrected using a linear approach. For extremes in low precipitation over a long accumulation period ( 3 months) and shorter-duration high precipitation (1-30 days), the time series generally represents past statistics well. Future projections show small precipitation increases in winter but large decreases in summer on average, leading to an overall drying, consistently with the most recent UK Climate Projections (UKCP09) but larger in magnitude than the latter. Both drought and high-precipitation events are projected to increase in frequency and intensity in most region
机译:水管气象极端,如干旱和重度降水可能对社会和经济产生很大影响。由于气候变化,潜在增加与此类事件相关的风险,适当地评估相关的影响和不确定性对于适当的适应至关重要。然而,基于风险的方法的应用通常需要大量的极端事件,这是通常不可用的。在这里,我们在@ HOVE 2的天气@ HOVE 2中展示了近期过去和未来条件的大量水力气象时间序列,这是由观察到或投影海面驱动的全球气候模型(GCM)组成的建模框架通过区域气候模型(RCM),温度(SST)和海冰在欧洲领域下降到25公里。为(i)历史基线(1900-2006)中的每一个,(ii)五个近期情景(2020-2049)和(iii)五个远期情景(2070-2099),为(ii)的历史基线(i)的每一个组成了100个时间序列。每个未来时间切片中的五种情景都遵循代表浓度通路8.5(RCP8.5)并采样海面温度和海冰范围从CMIP5(耦合型号互通项目5)模型。验证历史基线凸显了良好的温度和潜能蒸发性能,而是使用线性方法校正的平均沉淀的大量季节偏差。对于在较长的累积期(& 3个月)和较短持续时间(1-30天)的低水平中,时间序列通常代表过去的统计数据。未来的预测显示冬季的较小降水量,但平均夏季较大,导致整体干燥,与最近的英国气候投影(UKCP09)一致,但幅度大于后者。在大多数区域的频率和强度上投射出来都会增加干旱和高降水事件

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