A'/> Wavelet-based variability of Yellow River discharge at 500-, 100-, and 50-year timescales
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Wavelet-based variability of Yellow River discharge at 500-, 100-, and 50-year timescales

机译:基于小波的黄河排放的可变性,500-,100-和50年的时间尺度

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Abstract Water scarcity in the Yellow River, China, has become increasingly severe over the past half century. In this paper, wavelet transform analysis was used to detect the variability of natural, observed, and reconstructed streamflow in the Yellow River at 500-, 100-, and 50-year timescales. The periodicity of the streamflow series and the co-varying relationships between streamflow and atmospheric circulation indices/sunspot number were assessed by means of continuous wavelet transform (CWT) and wavelet transform coherence (WTC) analyses. The CWT results showed intermittent oscillations in streamflow with increasing periodicities of 1–6years at all timescales. Significant multidecadal and century-scale periodicities were identified in the 500-year streamflow series. The WTC results showed intermittent interannual covariance of streamflow with atmospheric circulation indices and sunspots. At the 50-year timescale, there were significant decadal oscillations between streamflow and the Arctic Oscillation (AO) and the Pacific Decadal Oscillation (PDO), and bidecadal oscillations with the PDO. At the 100-year timescale, there were significant decadal oscillations between streamflow and Ni?o 3.4, the AO, and sunspots. At the 500-year timescale, streamflow in the middle reaches of the Yellow River showed prominent covariance with the AO with an approximately 32-year periodicity, and with sunspots with an approximately 80-year periodicity. Atmospheric circulation indices modulate streamflow by affecting temperature and precipitation. Sunspots impact streamflow variability by influencing atmospheric circulation, resulting in abunda
机译:<![cdata [ 抽象 中国黄河的水资源稀缺在过去半个世纪日益严重。本文采用小波变换分析检测黄河500 - ,100-和50年时间尺度的自然,观察和重建流流的变化。通过连续小波变换(CWT)和小波变换相干(WTC)分析评估流流量系列的周期性和流流程和大气循环指数/太阳块数之间的共同关系。 CWT结果在流出中显示出间歇振荡,周期性为1-6 在所有时间尺度的周期性。在500年的流流量系列中确定了显着的多程度和世纪尺度周期。 WTC结果表明,具有大气循环指标和太阳黑子的流流的间歇性平衡。在50年的时间尺度,流流程和北极振荡(AO)与太平洋二等振荡(PDO)之间存在显着的Decadal振荡,以及PDO的Bidecadal振荡。在100年的时间尺度上,Streamflow和Ni之间存在显着的Decadal振荡,o 3.4,Ao和Sunspots之间。在500年的时间段,黄河中游的流出突出了与AO的突出协方态,大约为32年的周期,并且太阳黑子,周期大约为80年。大气循环指数通过影响温度和降水来调节流流。太阳黑子通过影响大气循环冲击流式变异性,导致Abunda

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