首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >'Dry gets drier, wet gets wetter': A case study over the arid regions of central Asia
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'Dry gets drier, wet gets wetter': A case study over the arid regions of central Asia

机译:“干得变干燥,湿得湿润”:以中亚干旱地区为例

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The dry gets drier, wet gets wetter (DGDWGW) paradigm well describes the pattern of precipitation changes over the oceans. However, it has also been usually considered as a simplified pattern of regional changes in wet/dry under global warming, although GCMs mostly do not agree this pattern over land. To examine the validity of this paradigm over land and evaluate how usage of drought indices estimated from different hydrological variables affects detection of regional wet/dry trends, we take the arid regions of central Asia as a case study area and estimate the drying and wetting trends during the period of 1950-2015 based on multiple drought indices. These indices include the standardized precipitation index (SPI), the standardized precipitation evapotranspiration index (SPEI), the Palmer drought severity index (PDSI) and self-calibrating PDSI (sc_PDSI) with both the Thornthwaite (th) and Penman-Monteith (pm) equations in PDSI calculation (namely, PDSI_th, PDSI_pm, sc_PDSI_th and sc_PDSI_pm). The results show that there is an overall agreement among the indices in terms of inter-annual variation, especially for the PDSIs. All drought indices except SPI show a drying trend over the five states of central Asia (CAS5: including Kazakhstan, Kyrgyzstan, Tajikistan, Turkmenistan and Uzbekistan). The four PDSIs and SPEI reveal a wetting tendency over the northwestern China (NW; including Xinjiang Uygur Autonomous Region and Hexi Corridor). The contrasting trends between CAS5 and NW can also be revealed in soil moisture (SM) variations. The nonlinear wet and dry variations are dominated by the 3-7 years oscillations for the indices. Relationships between the six indices and climate variables show the major drought drivers have regional features: with mean temperature (TMP), precipitation total (PRE) and potential evapotranspiration (PET) for CAS5, and PRE and PET for NW. Finally, our analyses indicate that the dry and wet variations are strongly correlated with the El Nin
机译:干燥变干燥,湿湿式(DGDWGW)范式良好描述了海洋降水变化的模式。然而,它通常被认为是全球变暖下的湿/干燥的区域变化的简化模式,尽管GCMS主要不同意土地上的这种模式。检查该范例对土地的有效性,评估不同水文变量估计的干旱指标如何影响区域潮湿/干燥趋势的检测,我们将中亚的干旱地区作为案例研究区,估计干燥和润湿趋势在1950 - 2015年期间,基于多次干旱指数。这些指数包括标准化降水指数(SPI),标准化降水蒸发散热指数(SPEI),帕尔默干旱严重程度指数(PDSI)以及桑特瓦特(TH)和Penman-Monteith(PM)的自我校准PDSI(SC_PDSI) PDSI计算中的方程(即,pdsi_th,pdsi_pm,sc_pdsi_th和sc_pdsi_pm)。结果表明,在年度年间变异方面存在整体协议,特别是对于PDSIS。除SPI之外的所有干旱指标都显示出中亚五个州的干燥趋势(Cas5:包括哈萨克斯坦,吉尔吉斯斯坦,塔吉克斯坦,土库曼斯坦和乌兹别克斯坦)。四个PDSIS和Spei揭示了中国西北部(NW;包括新疆UYGUR自治区和河西走廊)的润湿倾向。 CAS5和NW之间的对比趋势也可以在土壤水分(SM)变化中露出。非线性潮湿和干燥变化由3-7年振荡的指数主导。六个指数与气候变量之间的关系显示,主要的干旱司机具有区域特征:具有平均温度(TMP),Cas5的沉淀总(Pre)和潜在的蒸散(PET),并为NW进行预先和PET。最后,我们的分析表明,干燥和湿变化与EL nin强烈相关

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